B E H A V I O U R OF S A N D U N D E R S I M U L T A N E O U S I N C R E A S E IN STRESS RATIO A N D R O T A T I O N OF PRINCIPAL STRESSES by DHARMAPRIYA WIJEWICKREME B . Sc. (Eng) Hons., University of Peradeniya, Sri Lanka M . A . Sc., University of British Columbia, Canada A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF T H E REQUIREMENTS FOR T H E D E G R E E OF DOCTOR OF PHILOSOPHY in T H E FACULTY OF GRADUATE STUDIES DEPARTMENT OF CIVIL ENGINEERING We accept this thesis as conforming to the required standard T H E UNIVERSITY OF BRITISH COLUMBIA August, 1990 © D H A R M A P R I Y A W I J E W I C K R E M E , 1990 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. 1 further copying of this department or agree that permission for extensive thesis for scholarly purposes may be granted by his or her representatives. It is by the head of my understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of C'VtL £f*SG) //^/E~££i /A/i The University of British Columbia Vancouver, Canada Date DE-6 (2/88) /5" /rt(C<L(S 7 /<??Q. Abstract Drained behaviour of sands under simultaneous increase in stress ratio and principal stress rotation is investigated. The hollow cylinder torsional (HCT) device which permits independent control of four stress parameters: mean normal stress a'^, stress ratio R, intermediate principal stress parameter b and the inclination a CT of a[ to the vertical, is adopted as the testing device. In order to conduct complex stress path testing in the H C T device, a new automatic stress path control system is developed. The stress non-uniformities due to the curvature of the H C T specimen is assessed using an incremental elastic representation of sand behaviour, in order to delineate the domain of stress space that could reliably be explored using the H C T device. It is shown that previous assessments of stress non-uniformities assuming linear elastic soil grossly overestimate the stress non-uniformities in a H C T sand specimen. A much larger domain of stress space with acceptable levels of non-uniformities is apparent from the results of incremental elastic analysis. New domain of stress space for reliable exploration using the H C T device is delineated and the testing program is developed so that all stress paths lie within these acceptable limits. Tests are carried out on pluviated sand under saturated drained conditions. The deformations under increasing R and a a is shown to be path independent, if the final stress state is within the approximate bounds of R < 2 and ov < 45°, regardless of the b or relative density D , levels. r With increasing stress ratio R and/or principal stress rotation a. , the deformations gradually become path depena dent. Once loaded to a stress state within the domain R < 2 and a < 45°, the strain a response under subsequent principal stress rotation is shown to be independent of ii the previous loading history. It is demonstrated that the strain response under any general increasing R - a path in the domain of R < 2 and a a < 45° can be predicted using the results of a limited number of tests characterizing that domain. It is shown that these concepts can be extended to loading paths which involve simultaneous increase of three stress parameters. Strain increment direction a& is shown to be approximately coincident with and c totally governed by the stress increment direction direction when the stress increment is more inclined towards the vertical deposition direction. When the stress increment direction is inclined closer to the bedding plane, the strain increment direction depends in addition, on other parameters such as R, a a and D etc. T Under any stress path involving principal stress rotation, the deformations decrease with increasing density and therefore the principal stress rotation is more crucial in loose sands. Deformations increase with the level of stress ratio R. Level of b parameter does not affect deformations under principal stress rotation, if the rotations are small. However, with increasing a deformations due to principal stress a rotation tend to increase with decreasing b value. in Table of Contents Abstract ii List of Tables ix List of Figures xv List of Symbols xvi Acknowledgement xviii 1 Introduction 1 2 Review of Sand Behaviour Under General Stress Path Loading 5 2.1 Introduction 5 2.2 Anisotropic Nature of Sand 7 2.2.1 Inherent Anisotropy 8 2.2.1.1 Particle Fabric 8 2.2.1.2 Stress Strain Behaviour 9 2.2.2 2.3 2.4 Induced Anisotropy 12 Deformations due to Continuous Rotation of Principal Stresses . . . . 14 2.3.1 General Stress Strain Behaviour 14 2.3.2 Effects of Intermediate Principal Stress 21 2.3.3 Effect of Mean Normal Stress and Relative Density 2.3.4 Direction of Strain Increment Summary . ....... 24 27 31 iv Stress Non-uniformities in the Hollow Cylinder Torsional Device 33 3.1 Introduction 33 3.2 Definitions of Average Stresses, Strains and Non-uniformity Parameters 35 3.3 3.4 3.5 3.2.1 Average Stresses 35 3.2.2 Average Strains 37 3.2.3 Degree of Stress Non-uniformity 38 Finite Element Program and Mesh 39 3.3.1 Finite Element Program 39 3.3.2 Mesh Used 41 Stress Non-uniformities Under General Stress States in Non-linear Soil 51 3.4.1 55 Stress Non-uniformities in Loose Sand H C T Specimens . . . . 3.4.1.1 Comparison with Linear Elastic Material 55 3.4.1.2 Influence of Stress Ratio 64 3.4.1.3 Influence of Mean Normal Stress 68 3.4.2 Influence of Relative Density on Stress Non-Uniformities 3.4.3 Additional Remarks on Stress Non-uniformities ... 68 71 Estimation of Average Stresses 74 U B C Hollow Cylinder Torsional Device and Experimental Aspects 79 4.1 The U B C Hollow Cylinder Torsional Apparatus (UBC-HCT) . . . . . 79 4.1.1 General Description 79 4.1.2 Instrumentation of the H C T Device 82 4.1.2.1 Measurement of Deformations 84 4.1.2.2 Measurement of Surface Tractions 86 4.2 Stress Path Control and Data Acquisition 87 4.2.1 Basic Components of the Control System 87 4.2.2 Data Acquisition (Input to the Computer) 89 4.2.3 Control of Surface Tractions (Output from the Computer) v . . 91 4.2.4 4.3 5 Stress Path Control (Software) 93 Specimen preparation 96 4.3.1 General Considerations 96 4.3.2 Preparation Procedure 98 4.3.3 Repeatability of Test Results 103 4.3.4 Experimental Program 103 4.3.4.1 Material Tested 103 4.3.4.2 Testing Program 107 Results and Discussion 114 5.1 Introduction 114 5.2 Hydrostatic Loading 115 5.3 Deformation Under Increase in a Single Stress Parameter 118 5.3.1 5.3.2 Shear Loading of Loose Sand with Fixed Principal Stress Directions (R Paths) 118 5.3.1.1 Stress Strain Behaviour 118 5.3.1.2 Direction of Strain Increments and Strain Paths . . . 121 Principal Stress Rotations on Loose Sand at Constant R, b and <r' (a Paths) 121 m 5.3.3 5.3.4 5.4 5.3.2.1 Effect of R Level 121 5.3.2.2 Effect of b Parameter 126 5.3.2.3 Effect of Mean Normal Effective Stress 129 Response to a Loading at Higher Relative Densities 133 5.3.3.1 Stress Strain Behaviour 133 5.3.3.2 Direction of Strain Increments 133 Stress Path Dependence of Deformations 136 Deformation Under Simultaneous Increase in Stress Ratio and Principal Stress Rotation . 138 vi 5.4.1 Behaviour of Loose Sand under Linear R - a Paths 138 5.4.1.1 Stress Strain Behaviour 139 5.4.1.2 Direction of Strain Increment 139 5.4.1.3 Stress Path and Stress History Dependence of Deformations (R - a Paths versus a Paths) 5.4.2 Effect of b Parameter during R - a Loading of Loose Sand 142 . . 5.4.2.1 Stress Strain Behaviour 148 5.4.2.2 Direction of Strain Increment . 150 5.4.2.3 Stress Path and Stress History Dependence of Deformations 5.4.3 150 Effect of a-' during R - a Loading of Loose Sand m Stress Strain Behaviour 154 5.4.3.2 Direction of Strain Increment 156 5.4.3.3 Stress Path and Stress History Dependence of Defor156 Response to R - a Loading at Higher Relative Densities . . . . 160 5.4.4.1 Stress Strain Behaviour 160 5.4.4.2 Direction of Strain Increment 160 5.4.4.3 Stress Path and Stress History Dependence of Deformations 5.4.5 5.5 154 5.4.3.1 mations 5.4.4 148 163 Deformations under Multi-Linear R - a Loading 166 5.4.5.1 Stress Strain Behaviour 166 5.4.5.2 Direction of Strain Increment 168 Deformation Under Simultaneous Increase in Three Stress Parameters 168 5.5.1 Stress Strain Behaviour 170 5.5.2 Direction of Strain Increment 170 vii 5.6 5.7 Prediction of Deformations Under Simultaneous Increase in Stress Ratio and Principal Stress Rotation 173 5.6.1 Introduction 173 5.6.2 Prediction Method 175 Prediction of Deformations Under Simultaneous Increase of a' ^ R and m a 182 a 6 Summary and Conclusions 194 Bibliography 198 Appendices 204 A Cross Anisotropic Elastic Material Behaviour 204 B Membrane Penetration Corrections 208 C Deformation Characteristics of Test Series E , C , M , K , I and O 212 vm List of Tables 3.1 Hyperbolic Soil Parameters used in the Analysis 41 3.2 Comparison of average stresses 78 C.l Index - Deformation Characteristics of Test Series E , C, M , K , I and 0 213 ix List of Figures 2.1 Expression of stress at a point 6 2.2 Inherent anisotropy of pluviated Ottawa sand - after Sayao (1989) . . 2.3 Induced anisotropy on initially isotropic sand - after Arthur et al. (1981) 13 2.4 State boundary surface of sand - after Symes et al. (1984) 17 2.5 Drained principal stress rotation tests - after Symes et al. (1988) . . . 19 2.6 Strain development due to cyclic principal stress rotation - after Sayao (1989) 2.7 22 Effect of stress ratio on strain development due to principal stress rotation - after Sayao (1989) 2.8 23 Effect of a' on strain development due to principal stress rotation m after Sayao (1989) 2.9 10 25 Effect of D on strain development due to principal stress rotation T after Sayao (1989) 26 2.10 Definition of stress and strain increment directions 28 2.11 Strain increment directions during cyclic principal stress rotation - after Sayao (1989) 30 3.1 Loading and stress conditions in H C T specimens 36 3.2 The definition of parameters for the hyperbolic model - after Duncan et al. (1980) 40 3.3 Cross section of the F E mesh used 42 3.4 One sector of the F E mesh with end beam elements 43 x 3.5 Distribution of r g across the wall under pure torque - Linear elastic 2 material 3.6 47 Distribution of o> and ag across the wall under different external and internal pressures - Linear elastic material 48 3.7 One sector of the concise F E mesh with end beam elements 50 3.8 Comparison of stress distributions across the specimen wall from the full F E mesh versus concise F E mesh - Linear elastic material 3.9 52 Comparison of stress distributions across the specimen wall from the full F E mesh versus concise F E mesh - Incremental elastic material . . 53 3.10 Dependence of (3 on the stress path 54 3.11 Stress paths used in the F E analysis 56 R 3.12 Distribution of stress ratio across the wall of the specimen with material behaviour: <r' = 300 kPa; R = 2.0; D = 30% m . 57 r 3.13 Distribution of stress ratio across the wall of the specimen with material behaviour: tr' = 300 kPa; R = 3.0; D = 30% m 58 T 3.14 Variation of f3 vs R with material behaviour: a' = 300 kPa: D = 30% 60 R m T 3.15 Contours of /3 at R = 2, a' = 300 kPa, D = 30% 62 3.16 Contours of /3 at R = 3, a' = 300 kPa, D = 30% 63 R m R r m T 3.17 Effect of stress ratio on the non-uniformities: a' — 300 kPa: D — 30% 65 m 3.18 Variation of 0 r with R: a' = 300 kPa: D = 30% R m 66 r 3.19 Variation of /3R vs R with material behaviour: a' = 300 kPa: D = 30% 67 m r 3.20 Effect of a' on the value of f3 , D = 30 % 69 3.21 Effect of D on variation of /3 with R 70 3.22 Variation of j3 with the mobilized friction ratio 72 3.23 Variation of f3 vs D for different stress states 73 3.24 Stress strain relations under different initial modulus 75 m R T r H R R T XI 3.25 Comparison of average stress ratios from incremental vs linear elastic analysis D = 30%, a' = 300 kPa 77 4.1 Schematic of the U B C - H C T device - after Sayao (1989) 80 4.2 Details of the U B C - H C T device - after Sayao (1989) 81 4.3 Polished end platen with radial ribs - after Sayao (1989) 83 4.4 Rotational displacement measuring system - after Sayao (1989) . . . . 85 4.5 Schematic layout of the stress path control system 88 4.6 Data acquisition process 90 4.7 Comparison between manually controlled versus automated stress path T m testing 92 4.8 Flow chart for the program used in stress path testing 94 4.9 Performance of the stress path control system 97 4.10 Sample preparation by water pluviation - after Sayao (1989) 99 4.11 Levelling the upper surface of the sample - after Sayao (1989) . . . . 101 4.12 Repeatability of H C T test results in a hydrostatic stress path . . . . 104 4.13 Repeatability of H C T test results in a stress path with simultaneous increase of stress ratio and principal stress rotation 105 4.14 Particle size distribution of medium Ottawa sand 106 4.15 Terminology used in identifying a stress path in R-a^ stress space . . 108 4.16 Notation used in identifying a stress path in R-a 109 a stress space . . . . 4.17 H C T testing program - (contd. next page) Ill 4.18 H C T testing program (contd. from previous page) 112 5.1 Stress-Strain response under hydrostatic loading of medium loose Ottawa sand 116 5.2 Strain path in hydrostatic loading of medium loose Ottawa sand . . . 117 5.3 Effect of relative density on strain paths in hydrostatic loading . . . . 119 xii 5.4 Effect of on the stress strain behaviour in R paths 120 5.5 Strain increment directions in an R path with ov = 45° 122 5.6 Strain paths in directional shear loading 123 5.7 Effect of R level on deformation due to principal stress rotation 5.8 Effect of R level on the direction of strain increment 127 5.9 Effect of b parameter on deformation due to principal stress rotation . 128 . . . 5.10 Effect of b parameter on the direction of strain increment 125 130 5.11 Effect of <r' on deformation due to principal stress rotation 131 5.12 Effect of a-' on the direction of strain increment 132 m m 5.13 Effect of D on deformations due to principal stress rotation 134 5.14 Effect of D on the direction of strain increment 135 5.15 Stress path dependence of deformations from R and a tests 137 5.16 Stress strain behaviour under linear R - a loading 140 5.17 Direction of strain increment under linear R - a. loading 141 r r 5.18 Stress path dependence of deformations under principal stress rotation - Test Series A 143 5.19 Stress path dependence of deformations at higher stress ratios . . . . 145 5.20 Direction of strain increments under linear R - a loading leading to higher stress ratios 147 5.21 Effect of b parameter on the behaviour under linear R - a loading . . 149 5.22 Effect of b parameter on the direction of strain increment in linear R a loading 151 5.23 Effect of b parameter on stress path dependence of deformations - Test Series E : 152 5.24 Effect of b parameter on stress path dependence of deformations - Test Series C 153 5.25 Effect of aln on the behaviour under linear R - a loading xiii 155 5.26 Effect of a' on the direction of strain increment in linear R - a loading 157 m 5.27 Effect of a' on stress path dependence of deformations - Test Series M 158 m 5.28 Effect of <r' on stress path dependence of deformations - Test Series K 159 m 5.29 Effect of D on the behaviour under linear R - a loading T 161 5.30 Effect of D on the direction of strain increment in linear R - a loading 162 r 5.31 Effect of D on stress path dependence of deformations - Test Series I T 164 5.32 Effect of D on stress path dependence of deformations - Test Series 0 165 T 5.33 Stress path independence observed in a tri-Hnear R - a loading path . 167 5.34 Strain increment directions under a tri-linear R - a loading path . . . 169 5.35 Deformation under simultaneous increase in three stress parameters cr^, R and a 171 ff 5.36 Strain increment directions under a a' - R - a path m 172 5.37 Constant R principal stress rotation loading to characterize material behaviour 174 5.38 Deformations under shear loading with = 0° for medium loose Ot- tawa sand - Series A 177 5.39 Strains from a paths with R = constant for medium loose Ottawa sand - Series A 178 5.40 Curve fitting technique illustrated for test Series A 180 5.41 Predicted and observed stress strain behaviour - Series A 181 5.42 Predicted and observed stress strain behaviour - Series E 183 5.43 Predicted and observed stress strain behaviour - Series C 184 5.44 Predicted and observed stress strain behaviour - Series M 185 5.45 Predicted and observed stress strain behaviour - Series K 186 5.46 Predicted and observed stress strain behaviour - Series I 187 5.47 Predicted and observed stress strain behaviour - Series 0 188 xiv 5.48 Predicted and observed stress strain Behaviour - tri-linear stress path OABC 189 5.49 Characterization of material behaviour under - R - a loading using a test series A , M and K 191 5.50 Predicted and observed stress strain behaviour - a' - R - a path (path m AB) 193 A. l Cross anisotropic elastic material 205 B. l Membrane penetration correction curve - after Vaid and Negussey (1984)209 C. l Deformations under shear loading with a — 0° - Test Series E . . . . 214 C.2 Deformations under a paths with R = constant - Test Series E . . . . 215 C.3 Deformations under shear loading with a = 0° - Test Series C . . . . 216 C.4 Deformations under a paths with R — constant - Test Series C . . . . 217 C.5 Deformations under shear loading with a = 0° - Test Series M . . . . 218 C.6 Deformations under a paths with R — constant - Test Series M 219 a ff a C.7 Deformations under shear loading with a ff . . . = 0° - Test Series K . . . . 220 C.8 Deformations under a paths with R = constant - Test Series K . . . . 221 C.9 Deformations under shear loading with a — 0° - Test Series I . . . . 222 a C.10 Deformations under a paths with R = constant - Test Series I . . . . 223 C . l l Deformations under shear loading with = 0° - Test Series 0 . . . . 224 C.12 Deformations under a paths with R — constant - Test Series 0 . . . . 225 xv List of Symbols <J - Normal stress r - Shear stress A - Prefix indicating an increment cr\ - Major effective principal stress cr' - Intermediate effective principal stress 2 a' - Minor effective principal stress R - Effective principal stress ratio ( = a[j'a' ) 3 a' m 3 - Effective mean normal stress ( = £i+£2±£i) c' —a' b - Intermediate principal stress parameter ( = J _J) a a a - Direction of <J\ with respect to the deposition direction Acr - Direction of Aa[ with respect to the deposition direction e Normal strain 7 Shear strain Major principal strain Intermediate principal strain £3 Minor principal strain Volumetric strain ( = a -f ei + es) l/max Maximum shear strain ( = £1 — £3) Volumetric and maximum shear strains under hydrostatic loading [R — 1 ; b and ov undefined). { V}RI £ {lmax}n - Volumetric and maximum shear strains due to changes in R only, with a a xvi — 0°. (fc and a' held constant). m i f}a> {7mai} £ Q - Volumetric and maximum shear strains due to changes in a a& c a only, with R, b and cr'^ held constant. - Direction of A e with respect to the deposition direction a Th - Torque about the vertical axis F z Pi,P - Vertical Force - Internal and external confining pressures e Ri,R e - Internal and external specimen radii H - Specimen height D - Relative density r J3R - Stress non-uniformity coefficient R path - Stress path with variation of R only, with fixed values of er^, b, and a . a a path - Stress path with variation of a only, with a fixed values of a' , fc, and R. m R — a path - Stress path with simultaneous variation of R and a , c with fixed values of a'^ and b. u' — R — a path m - Stress path with simultaneous variation of a'^, R and a^, with a fixed value of b. xvn Acknowledgement I wish to express my sincere gratitude to my supervisor Professor Y . P . Vaid for his guidance, valuable suggestions and the encouragement throughout this research. Special thanks are due to members of my examining/supervisory committee, Professors P . M . Byrne, W.D.L. Finn, Y . P . Vaid, R . G . Campanella, D.L. Anderson, S.M. Calisal and P.V. Lade and Dr. M . K . W . Lee for their helpful criticism and suggestions. Assessment of stress non-uniformities would not have been possible without the 3-D finite element program 3DSLB developed by my colleague Francisco Salgado, and his valuable assistance during program execution. Assistance and advice given by Dr. D. Negussey during my graduate studies at U.B.C. is deeply appreciated. I would also like to thank my colleagues Alberto, Mustapha, Ralph, Carlos, Sasi and Hendra for their helpful discussions. Sincere thanks are extended to Mr. S. Jackson and Mr. R. Nussbaumer of the electronic workshop for their co-operation in the development of the stress path control system, and Mr. A. Brookes and H . Schrempp of the mechanical workshop for their skills in making several improvements to the H C T apparatus. The Izaak Walton Killam Graduate Fellowship (1986-1987) and the University of B.C. Graduate Fellowship (1988-1989) awards, which provided the financial support during my doctoral program, are gratefully acknowledged. Finally, I would like to extend very special thanks to my wife Nilmini for her continuous encouragement and support throughout this research. xvin Chapter 1 Introduction Field loading of soils is frequently associated with rotation of principal stresses. Since most sedimentary deposits are inherently anisotropic, rotation of principal stresses alone would produce volumetric and shear deformations in a soil mass. The ability to characterize behaviour under such loading conditions is essential for satisfactory geotechnical design of structures. The influence of anisotropy has largely been neglected in the modelling of soil behaviour, primarily because of its complexity and general unavailability of data under generalized stress path loading. In order to study the anisotropic behaviour and the effects of principal stress rotation, the laboratory testing devices should have the ability to exercise control on both the directions and magnitudes of principal stresses. As a result of research work over two decades, two testing devices have emerged that could impose continuous rotation of principal stresses on a soil specimen: viz. the directional shear cell (DSC) (Arthur et al., 1977) and the hollow cylinder torsional (HCT) device (Hight et al., 1983). The DSC in its present state of development can operate only under plane strain conditions and at low confining pressures. On the other hand, in the H C T device independent control of three principal stresses and rotation of principal stresses in one plane can be exercised. Frequently, an alternate set of equivalent stress parameters: effective mean normal stress a' — (c{-f <r' + cr )/3 m 2 3 shear stress q = {a' — a' ) (or stress ratio R — a[ / a' ), intermediate principal stress x 2 3 parameter b '= (a' — a' ) / (<x^ — a' ), and the inclination of major principal stress to 2 z 3 the vertical (angle a of <r\ with deposition direction) are used to interpret H C T test a 1 y Chapter 1. 2 Introduction results. Since these parameters describe completely the stress states involving two dimensional principal stress rotation, the H C T device has the versatility of simulating many practical stress path loadings that actually occur in the field. In early research under generalized stress path loading, the interest focused mainly on the strength behaviour of sand. Stress ratios mobilized under general working conditions typical of deformation problems in geotechnical engineering are at a much lower level than at the failure state. Comprehensive knowledge of the effects of principal stress rotations at such moderate stress ratios is very limited. The only contributions to this area of research have come from the laboratory studies on sands using the H C T device (Symes et al., 1984, 1988; Sayao, 1989). Real field loading generally involves increase in several stress parameters .simultaneously. Laboratory investigations have, however been restricted to stress paths in which only one stress parameter is increased at a given time (Sayao, 1989; Hight et al., 1983; Symes et al., 1988). No attempts have been made to carry out stress path tests where simultaneous increase of more than one stress parameter occurs in a controlled manner. It is widely recognized that sand behaviour is stress path dependent. Yet, not enough is known about the stress path dependent strain response, particularly under principal stress rotations. It has also been suggested that the initial deposition anisotropy governs sand behaviour if the associated strains on loading are moderate, regardless of the stress path. These conclusions have been arrived at from the results of only a limited number of tests. Lack of knowledge and understanding regarding sand behaviour under generalized stresses led to the evolution of the main theme of this research. As such, a comprehensive investigation on the drained behaviour of sand under simultaneous increase in stress ratio and principal stress rotation is carried out using the H C T device. The results are compared with those from stress paths in which only one stress parameter Chapter 1. Introduction 3 is permitted to increase. Possible path independent domain of the stress space is identified based on these comparisons. Hence a procedure for predicting stress strain response under simultaneous increase of stress ratio and principal stress rotation is proposed using the observed behaviour from stress paths, wherein the principal stress rotations occurred at constant levels of stress ratio. A systematic testing program was designed in order to achieve the above objectives. All tests were carried out using reconstituted specimens of saturated sand under drained conditions. Sand behaviour is examined predominantly at medium loose relative density D of 30% in which principal stress rotation effects are expected to be T most pronounced. Stress ratio levels were mainly restricted to those below 2.0. Tests were carried out to delineate the effects of mean normal stress cr' and intermedim ate principal stress parameter b under otherwise identical stress paths. Behaviour of denser sand with D = 50% and 70% was also investigated. For all stress paths the dir rectional changes in principal stress increment in response to applied stress increment and stress directions is also investigated, in order to understand possible changes in inherent anisotropy during loading. The accomplishment of these objectives required complex stress path tests, which may involve simultaneous increase in all four surface tractions in the H C T device. The manual control of these tractions together is a difficult, if not impossible task. This necessitated the development of a new automatic stress path testing facility with a feed back control system. Another important consideration in the use of the H C T device is the level of stress non-uniformities across the wall of the specimen that arise due to the curvature of the specimen. A proper assessment of these non-uniformities is essential in evaluating the quality of data from H C T tests. It is necessary to identify the domain of stress space which may result in unacceptable stress non-uniformities and hence constitute the "no-go" regions. Previously, stress non-uniformities in H C T specimens have been Chapter 1. Introduction 4 assessed, mostly with the assumption that the soil behaviour is linear elastic. Stress non-uniformities determined from linear elastic assumptions lead to overestimation of actual stress non-uniformities if the soil is non-linear. No systematic analysis of stress non-uniformities in H C T specimens has been made which recognizes nonlinear soil behaviour. Hence a reevaluation of stress non-uniformities in the H C T specimens using a nonlinear elastic representation of soil behaviour was undertaken, as a prerequisite to the experimental investigation. Chapter 2 Review of Sand Behaviour Under General Stress Path Loading 2.1 Introduction Even though experimental evidence suggests anisotropic behaviour, sand is traditionally characterized based on the assumption of isotropy. This is primarily (i) to preserve simplicity in modelling and (ii) need for complex testing devices for characterizing behaviour of anisotropic material. In general, the state of stress at a point in a sand deposit can be expressed in terms of six parameters: three principal stresses a' ,cr cr x 2y 3 and their inclinations to a set of orthogonal coordinate axes (Fig. 2.1). A n equivalent set of parameters, mean effective stress a' m = [a[ -+- a + c )/3; effective stress ratio R = <y\l<r' \ intermediate 2 principal stress parameter b = (a' of <r\,cr 2 a n 3 2 3 — ^' )/{c[ 3 — &' ) are commonly used instead 3 d <T3. One of the reference coordinate directions is normally taken as the vertical deposition direction. Controlled changes in the magnitudes of stresses and their inclinations to the reference directions are extremely important in the study of anisotropic material behaviour. In most soil testing devices such as conventional triaxial, true triaxial and plain strain, principal stresses are fixed in direction and at most, only an interchange of principal directions (called jump rotations) can be imposed. No device has yet been developed which allows principal stress rotation in three dimensions. The only devices that allow controlled rotation of principal stresses in one plane are the directional 5 Figure 2.1: Expression of stress at a point Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 7 shear cell (DSC) (Arthur et al., 1977) and the hollow cylinder torsional (HCT) device (Hight et a l , 1983; Vaid et al. 1990). The H C T device has the added advantage of being the only apparatus that allows independent control of the magnitudes of all stress parameters a' , R, b, and a m CT (inclination of a[ with vertical deposition direction). In this chapter conceptual and experimental evidence in support of anisotropic nature of sand is first presented. The measured deformation response of sands is then critically reviewed, with emphasis placed on drained behaviour. Only pre-failure behaviour is considered which is central to the solution of deformation as opposed to stability problems in sands. The interpretation of hollow cylinder data close to failure could be questionable due to potentially excessive stress non-uniformities across the wall of the specimen (see Chapter 3). The new directions in research that would enhance the current understanding of the behaviour of sand as an anisotropic material are identified and a research program is proposed to accomplish these objectives. 2.2 Anisotropic Nature of Sand The discrete nature of particles and their spatial arrangement characterizes the mechanical behaviour of a sand mass. Casagrande and Carillo (1944) distinguished between two types of anisotropy in soils, viz. inherent and induced. Inherent anisotropy was defined as a physical characteristic inherent in the material before any deformations are imposed. On the other hand, the anisotropy due exclusively to the strain associated with the applied stress was called induced anisotropy. Although the above distinction gave a convenient means of classifying anisotropy, Saada (1981) correctly pointed out that any current state of a sand can be treated as an inherently anisotropic state for the next loading increment. Additional definitions such as initial anisotropy (Symes et al., 1984) have thus evolved, which takes into Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 8 account both the induced anisotropy due to past events and the inherent anisotropy. 2.2.1 2.2.1.1 Inherent Anisotropy Particle Fabric During the origin of a sand deposit, individual grains assume a position in the sand mass depending on the mode of deposition and the shape of grains. The term fabric has been used to describe the spatial arrangement of solid particles and the associated voids in a granular mass. Oda (1972) investigated the grain structure of sand by examining thin sections of both natural and reconstituted sand samples. The thin sections were obtained after infiltrating a resin binder into the voids of the sand specimen. The results indicated that during deposition under gravity, non spherical sand grains preferred to rest with their long axis oriented in a nearly horizontal direction. Oda also found that the majority of particle contact normals were oriented in a direction parallel to that of deposition. These observations revealed that the preferred alignment of non spherical particles as well as the preferred orientation of particle contacts, contributed towards creating an anisotropic fabric after deposition. Several investigations have shown that sand specimens comprised of even spherical grains, when deposited under gravity exhibit anisotropic behaviour (Haruyama, 1981; Oda, 1981; Shibuya and Hight, 1987). Since there is no longitudinal axis in the case of spheres, this anisotropic behaviour has been attributed solely to the preferred orientation of particle contact normals in the direction of deposition. The anisotropy in sand revealed by examining the grain structure has been further corroborated by laboratory stress-strain response observations. In the earliest laboratory experiments, Kjellman (1936) reported significant differences in the three principal strains during hydrostatic compression of cubical sand specimens. Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 9 The anisotropy in natural sand deposits has been reported by Ladd et al. (1977) using undisturbed triaxial samples of loose Niigata sand obtained by a freezing technique. They observed that under hydrostatic compression in the conventional triaxial cell, the radial strains induced were more than twice the vertical strains. Miura and Toki (1984) conducted drained triaxial compression and extension tests on undisturbed samples (obtained using a freezing technique) from two relatively homogeneous sand deposits. The results indicated that the vertical direction insitu was less compressible than the horizontal direction. Due to the difficulties in undisturbed sampling of sand, the anisotropic behaviour of sands has been studied mainly using laboratory reconstituted samples. Oda et al. (1978) have shown that the sand specimens prepared by laboratory pluviation (i.e. deposition under gravity) closely simulate the sedimentation process and the resulting fabric of water deposited sands insitu. They also demonstrated the anisotropic nature of pluviated Toyoura sand by testing tilted specimens in the plane strain device. Miura and Toki (1984) carried out triaxial tests on pluviated sand in a manner identical to their tests on undisturbed samples (see previous paragraph). Their results also showed very similar stress-strain characteristics between the undisturbed and the water pluviated sand. Reconstituted pluviated specimens thus enable a convenient means of studying the behaviour of water deposited insitu sands. 2.2.1.2 Stress Strain Behaviour Several investigations reflecting inherent anisotropy in pluviated sands can be found in literature. The observations showing loading direction dependent behaviour of pluviated Ottawa sand made by Sayao (1989) using the H C T device are reproduced in Fig. 2.2. Each sample was loaded with a fixed inclination ( a ) to the direction a of deposition while cr' and b were held constant. m out at several angles a a Such loading tests were carried of a[ to the deposition direction. A profound effect of Figure 2.2: Inherent anisotropy of pluviated Ottawa sand - after Sayao (1989) Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 11 initial anisotropic fabric of sand is apparent in both volumetric and shear strain responses (Fig. 2.2). The stiffest response is seen for loading in the vertical (a a = 0°) deposition direction. In general, the strain response becomes softer with increasing values of ov. But, at lower stress ratios, shear with a strain response than that obtained at a a a = 55° shows a stiffer = 45°. Sayao (1989) noted that similar observations ha.ve also been made by Miura (1985), who explained this observation using the concept of mobilized planes of Matsuoka (1974). It was suggested that the maximum deformability occurs when the mobilized planes (i.e. plane of maximum stress obliquity) and the bedding plane are coincident. At lower R values (i.e. lower mobilized friction angles), the mobilized plane is inclined to the major principal stress direction by approximately 4 5 . As such, when the inclination of the major principal o1 stress OLA is 45° to the vertical, the mobilized plane at lower R values would make an angle of 90° with the vertical. This indicates approximate coincidence of bedding and mobilized planes, and thus affirming the maximum deformability oberved at a v = 45°. Results in support of the general increase in deformability of sand with increasing a have also been reported by Symes et al. (1988) in H C T tests, Arthur and Menzies a (1972) in cubical triaxial tests on tilted samples and Arthur et al. (1981) in directional shear cell (DSC) tests. The mechanical behaviour of pluviated sands is generally considered to be cross anisotropic. This implies, that the behaviour should be symmetrical about the vertical axis. Miura (1985) reported H C T tests on two identical samples of pluviated sand. One sample was loaded with a fixed inclination of major principal stress a a measured clockwise to the direction of deposition and the other was loaded with the same magnitude of a,? but inclined in the anticlockwise sense to the vertical. He observed an identical strain response, indicating the symmetrical nature of pluviated sand about •"•mobilized plane is inclined to the major principal direction by an angle of (45° + <f>/2) Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 12 the direction of deposition. Wong and Arthur (1985) reported DSC tests on sand samples loaded, so that the plane o{a[-a' is coincident with the bedding plane. They 3 observed that the strain response was unaffected by the orientation of <r[ in the horizontal bedding plane. Although the tests were aimed at checking the performance of DSC, the results demonstrated that the pluviated sands are cross anisotropic and the behaviour is symmetrical about the vertical deposition axis. It should be noted that the foregoing laboratory observations on stress strain behaviour strongly corroborate the concepts of anisotropic particle fabric proposed by Oda (1972). 2.2.2 Induced Anisotropy Oda et al. (1985) observed that the spatial arrangement of solid particles and the associated voids in sand undergo progressive changes when subjected to shearing stresses. They found that the contact normals concentration tend to increase along the direction of <r[ while the elongated grains align in a direction perpendicular to the direction of <r[. They also noted that a new fabric of the sand continuously evolves in response to the applied stresses. Arthur et al. (1980, 1981) investigated such stress induced anisotropy of Leighton Buzzard sand using the DSC. Some of their results are reproduced in Fig. 2.3. The DSC specimens were presheared in the original plane of isotropy (i.e. the plane normal to the deposition direction) until R — 6 with <r' = 14 kPa and fixed directions of z principal stresses (N.B. Since DSC is a plane strain device the value of <T'2 could not be controlled). Then the specimens were unloaded back to the condition <T[ = a' = 14 3 kPa in the horizontal plane and were subsequently reloaded with different angles (a) to the direction of initial loading. They observed that the stiffness of sand progressively decreases with increasing angle a to the previous loading direction, which is a reflection of the induced anisotropy due to preshear in the plane which was initially isotropic. Chapter 2. Review of Sand Behaviour Under General Stress Path Loading Dry Leighton Buzzard Sand : D =95% Reloading Figure 2.3: Induced anisotropy on initially isotropic sand - after Arthur et al. (1981) 13 Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 14 Mould et al. (1982) also reported results in support of induced anisotropy in Leighton Buzzard sand, tested in the cubical triaxial device. This device can impose only jump rotations of 90°. The samples were initially sheared in the original plane of isotropy upto a stress ratio R of 4.5 with a' = a = 14 kPa and fixed principal stress 2 3 directions. They were then unloaded back to hydrostatic state before reloading in a direction perpendicular to the preshear direction. A marked reduction in the stiffness of sand was noted during reloading compared to that under virgin loading. When the specimen was again unloaded and reloaded in the original preshear direction, the strain response was much similar to that of the first reloading, although the loading directions had changed by 90°. Even though Mould et al. did not offer a detailed explanation for the observed behaviour, the results clearly demonstrated the profound changes that could occur in a granular fabric due to a simple loading process. 2.3 Deformations due to Continuous Rotation of Principal Stresses 2.3.1 General Stress Strain Behaviour Arthur et al. (1979, 1980) reported deformations under cyclic rotation of principal stresses with constant stress ratio R on dense sand using the directional shear device (DSC). They observed that the major principal strain accumulated continuously with cyclic rotation of principal stresses. Cyclic stress rotations in the DSC were achieved by maintaining boundary shear stresses constant. The normal stresses in the <r\ — <T'Z plane were controlled so as to achieve constant R conditions. Since the DSC is a plane strain device, the sand experiences fluctuations in the mean normal effective stress a' as well as the b parameter during shear. Therefore, the isolated influence m of the principal stress rotations on the sand behaviour cannot be investigated in the DSC. Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 15 The H C T apparatus is the only device which allows independent control of the stress parameters a^, b, R and a . Drained H C T tests where the magnitudes of the a principal stresses (and hence (T' ,b and R) were kept constant and only a„ was varied, m have been reported by Symes et al. (1982, 1988), Miura (1985), and Sayao (1989). Symes et al. (1982) reported a principal stress rotation test carried out on dense ( D = 88%) Ham river sand. A relatively high stress ratio [R — 3.5) was used with r b = 0.5 and a' — 200 kPa. They observed that at the initial stages of principal stress m rotation (a ff < 35°) contractive deformations developed, but at larger rotations the deformations became dilative and the specimen eventually failed (reached very large strains) at a„ m 65°. On the other hand, Miura (1985) reported results from similar tests on dense Toyoura sand (D T — 82%) carried out with R = 4, b = 0.5 and a' = m 98 kPa which contradict observations of Symes et al (1982). He observed an initial dilative behaviour for rotations upto a a % 120° followed by steady contraction. Both Ham river and Toyoura sands are similar, being uniform sands of mainly subangular quartz particles with D 50 of 0.18 and 0.3 mm respectively. The only difference between the two tests was in the values of R and a' . m This disparity alone cannot possibly explain the above contrasting results. It is important to point out that results described above have been obtained for principal stress rotations on very dense samples, at rather high R values. As will be shown in Chapter 3, the stress non-uniformities across the H C T specimen wall are likely to be much more severe in the case of dense samples, especially at higher stress ratios. Therefore confidence in these results become questionable. Moreover, Sayao (1989) pointed out that stress non-uniformity effects are likely to be more severe in Miura's H C T results, because of his smaller specimen dimensions and the higher R value (i? — 4) used. It is probable that the differences in stress non-uniformities could have led to the reported differences between the observed strain responses. Such results illustrate the importance of identifying the domain of stress space in a given Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 16 H C T device that leads to unacceptable stress non-uniformities, and classifying these as the 'no go' regions of stress space for the purpose of studying deformation response under general stress paths. The effect of principal stress rotations on the undrained response of sand have been examined by Symes et al. (1984). H C T tests were performed with constant total principal stresses while the direction of a was rotated on medium loose Ham 1 river sand. A progressive increase in pore water pressure was observed with increasing angle of principal stress rotation. Based on these undrained results Symes et al. (1984) proposed a unified framework to understand the effects of initial anisotropy and principal stress rotation on sand behaviour. This consisted of the concept of a state boundary surface originally proposed by Roscoe et al. (1958) but modified to include OL0 as an additional parameter. Symes et al. (1984) constructed a bounding surface (BS) in the 3-D space comprising q - a„ - a' , for each constant void ratio m and b conditions. (N.B. q = [a[ — <T' )/2) 3 The BS was divided into two main regions: (a) contractant region (b) dilatant region. The contractant region was further subdivided into post-peak and pre-peak zones (Fig. 2.4). If the sand state is on the pre-peak zone of the BS, it would be stable. On the other hand in the post-peak zone unstable response would occur under stress controlled conditions. This is usually followed by a tendency to dilate (i.e. drop in pore pressures). For an element of soil which exists on the BS, "loading" and "unloading" was distinguished by the direction of the effective stress increment vector in the q-a^-a^ space. If the stress increment vector is directed towards the outside of the BS, or in the limiting case where the stress increment is tangential to the BS, the path was considered as "loading". If the stress increment vector is directed towards the inside of the BS, the path was considered as "unloading". Symes et al. (1984) made qualitative predictions of pore pressure response under Chapter 2. Review of Sand Behaviour Under General Stress Path Loading (a) Contractant Region Ham River Sand b = 0.5 : D r = 44 % (b) Complete Surface Figure 2.4: State boundary surface of sand - after Symes et al. (1984) Chapter 2. Review of Sand JBeAaviour Under General Stress Path Loading 18 a given stress increment, based on the position of effective stress path (ESP) with respect to the BS. When the ESP was beneath the BS, pore pressure development was small. On the other hand, large pore pressures were observed when ESP was on the BS. Initially the validity of BS concept was shown limited only for undrained principal stress rotations up to 45° from the deposition direction. Shibuya and Hight (1987), using undrained H C T tests on Ham river sand demonstrated that the concept of BS is applicable to the complete domain of rotations —90° < OL„ < +90°, if the "shear strains are small" so that the induced anisotropy effects are negligible. However no guidelines were presented as to what constitutes "small strains". The BS approach for undrained response was further supported by the results from H C T tests on pluviated glass ballotini. In their recent work, Symes et al. (1988) using a limited number of tests, extended the concept of the BS to drained loading by taking into account the volume changes occurring during drained principal stress rotation. The void ratio changes in drained tests were incorporated into the BS by using an equivalent effective mean normal stress tr' ; defined as <r' me me = exp ( ° ^ ' ) , where e — void ratio at cr' = unity, e e 0 m = current void ratio and A = slope of the virgin hydrostatic consolidation line. Unlike clays, the value of A for sands is generally quite low, and not even constant with stress level (Chern, 1985). Therefore A value derived from laboratory tests will be susceptible to questionable interpretations. As such, the positioning of the BS will also be questionable due to the difficulties in evaluation of A. To highlight some of the observations under drained loading, typical results from Symes et al. (1988) on Ham river sand are reproduced in Fig. 2.5. In tests LR1 and LR3, specimens were initially sheared upto R — 1.55 and R = 2.6 respectively with a a = 0°. Then the principal stresses were rotated from a a = 0° to 45° at constant R, a' and b. Finally the value of R was increased until failure at constant m Chapter 2. Review of Sand Behaviour Under General Stress Path Loading Figure 2.5: Drained principal stress rotation tests - after Symes et al. (1988) Chapter 2. Review of Sand Behaviour Under General Stress Path Loading a' , b and a m CT 20 — 45°. In this last phase of the tests LR1 and LR3, the stress path was identical to that of L4 where R was increased from hydrostatic stress state to failure with a ff = 45°. All tests were carried out with constant b = 0.5 and a' = 300 kPa. m It was noted that both volumetric and shear strains in tests LR1 and LR3 matched closely the strains in L4 at common stress states F and G respectively. This indicates a stress path independent behaviour, although such stress path independence is not apparent in their earlier results (Hight et al., 1983). Furthermore, in shear loading with a CT = 45° subsequent to principal stress rotation, specimens LR1 and LR3 exhibited strain response very similar to those of specimen L4. It is to be noted that in these stress paths, neither R nor a experienced decrease during the course of the a test. Symes et al. (1988) suggested that these tests imply a total loading condition and the stress paths would He on the BS. They concluded that the initial anisotropy is the overriding factor in determining the behaviour of sand for stress paths involving "moderate amount of shear strain", but no limits on these strain levels were suggested. It is important to emphasize that the validity of the BS for drained loading has been tested using few tests carried out at limited R levels and the stress rotations a ff restricted to 45°. There is no experimental evidence to support the uniqueness of BS concept at larger principal stress rotations under drained conditions. Sayao and Vaid (1989) correctly pointed out that the effects of induced anisotropy and previous stress history effects are intrinsically neglected when the BS is considered unique in its position and/or shape. The observations on the BS have also been limited to constant a' and b values of 200 kPa and 0.5 respectively. Thus the concept of bounding surface m should be applied with caution, in spite of the attractiveness which comes as a result of its conceptual simplicity in describing principal stress rotation effects in sand. Sayao (1989) noted that very little is known about the effects of principal stress rotation on sand response at moderate levels of stress ratio. He carried out a comprehensive investigation on the behaviour of Ottawa sand under rotations of principal 21 Chapter 2. Review of Sand Behaviour Under General Stress Path Loading stresses using the H C T device. Volumetric and maximum shear strain response in two way (av = 0° —» ±60°) cyclic principal stress rotation on a loose sample by Sayao (1989) are reproduced in Fig. 2.6. Steady contractive deformations are observed regardless of whether the a 0 is increased or decreased on either side of the vertical direction. Larger volumetric strains develop for the increasing phases of a. than for a the decreasing phases. This is in accordance with the BS concepts of Symes et al. (1988). However it was observed that the hardening effects usually associated with one way rotation cycles are greatly reduced in the case of two way cyclic rotations, suggesting inapplicabihty of the BS concept under such conditions. Although some recovery of the maximum shear strains is observed during the decreasing a ff phase, the residual maximum shear strains increase with each cycle. Furthermore, the rate of strain per cycle decrease as the number of cycles increase. These drained cyclic rotation results from Sayao (1989) would imply a progressive pore pressure build up under cyclic undrained principal stress rotation. Effect of the level of stress ratio at which principal stress rotation is imposed, on the strain development is shown in Fig. 2.7 (Sayao, 1989). With increasing o^, both e and ^ ax increase with the level of R. Thus principal stress rotations occurring at v m higher stress ratios could lead to large undesirable deformations in a sand mass. 2.3.2 Effects of Intermediate Principal Stress Most of the investigations on the effects of a' on deformation response have been 2 carried out in terms of parameter b = (<r' — o-' )/(a[ — a' ), which defines the relative 2 3 3 magnitude of a' with respect to a\ and a' . This parameter was first introduced by 2 3 Habib (1953) in investigating strength characteristics of clays and sands in torsional triaxial tests. Bishop (1966) suggested that the influence of <r' on soil response can be 2 well portrayed in terms of b rather than a' itself. Sayao (1989) noted that although 2 large number of investigations are reported on the effect of b on strength parameters Chapter 2. Review of Sand Behaviour Under General Stress Path Loading D =20% : (J =300kPa : 22 b = 0.5 Figure 2.6: Strain development due to cyclic principal stress rotation - after Sayao (1989) Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 23 Figure 2.7: Effect of stress ratio on strain development due to principal stress rotation - after Sayao (1989) Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 24 (Bishop, 1966; Sutherland and Mesdary, 1969; Green, 1971; Lade and Duncan, 1973; Haruyama, 1981), there was very little work done on its effects on pre-failure stress strain behaviour. Sayao (1989) carried out a comprehensive investigation on the effects of b on deformations along several stress paths, including those with principal stress rotation. From shear tests (increasing R) with constant <r' 6, and a it was observed that the m: c softest response occurred at b = 0 and the stiffest at b = 0.3. It was noted that the plain strain problems (6 % 0.3) may have their deformations largely overpredicted when data from triaxial tests (b — 0) is used. From H C T tests with continuously changing b parameter under constant R, a a and cr' conditions, Sayao (1989) observed a progressive accumulation of strains in m medium loose sand. However, in the range of b~ 0 to 0.4 which corresponds to most loading conditions in the field, the sensitivity of strains to the changes in b was found to be relatively low. 2.3.3 Effect of Mean Normal Stress and Relative Density The increasing contractant behaviour under increasing confining pressure at constant relative density and decreasing relative density at constant confining pressure are a well recognized characteristic of granular materials (Lee and Seed, 1967; Vesic and Clough, 1979). Sayao (1989) observed that this observation is vahd even for stress paths involving principal stress rotation with fixed R, b, a' and D . Some of his results are reproduced m in Figs. 2.8 and 2.9 to illustrate these features. T Sands tend to become more isotropic with increasing relative density (El-Sohby and Andrawes, 1972). Therefore, principal stress rotations would induce lesser strains at higher relative densities. The results reproduced in Figs. 2.8 and 2.9 also show that the rotation of principal stresses in general induces progressively larger volume contractions regardless of the relative Chapter 2. Review of Sand Behaviour Under General Stress Path Loading Figure 2.8: Effect of a' on strain development due to principal stress rotation - after Sayao (1989) m 25 Figure 2.9: Effect of D on strain development due to principal stress rotation - after Sayao (1989) r Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 27 density (except at the highest D = 60%) and the mean normal stress. T As discussed in the foregoing sections, valuable research has been carried out on the isolated effect of each stress parameter on sand behaviour. Under general field loading situations however, simultaneous changes in all stress parameters R, a' , b and m a generally occur. Therefore, it would be of great importance to examine whether a the separate effects of each stress parameter on sand response could be combined to obtain behaviour under stress paths, where more than one stress parameter changes. Hight et al. (1983) and Symes et al. (1988) have reported only two H C T tests in which the stress ratio and the direction of principal stress a was varied simultaneously. No G attempts have been made to study comprehensively the behaviour of sand under simultaneous changes in the magnitude and directions of principal stresses. 2.3.4 Direction of Strain Increment Any stress path could be viewed as a combination of a series of discrete stress increments. Therefore the strain increment direction a& in relation to the directions of e the applied stress cv and the stress increment a , always provide a better insight on Acr the sand behaviour than that obtained from the examination of total strain response alone. In studies of material behaviour in the H C T device, the directions of stress and strain increments (a^ and a& ) are also expressed with reference to the same c vertical deposition axis to which direction a CT of cr is referred to (Fig. 2.10). 1 Symes et al. (1988) examined the relationships between a, a& and a^ , in drained c a principal stress rotation tests on medium loose Ham river sand. They observed that for stress paths which involved "loading" in terms of the bounding surface, the strain 2 increment direction a& was lying between the stress direction a „ and stress increment c direction c t i , . For loading paths at higher stress ratios, a^c was much closer to a a than a^o-. On the other hand, for unloading (in terms of the BS) stress paths, a^ c 2 loading and unloading is defined in section 2.3.1 Chapter 2. Review of Sand Behaviour Under General Stress Path Loading (a) Direction of Major Principal Stress Direction of I Deposition T flr (b) Direction of Major Principal Stress Increment (c) Direction of Major Principal Strain Increment a AT (A£ 2 l A7 (A*e,A7 z e / ) z e / ) 2 A7, if 2 2 Figure 2.10: Definition of stress and strain increment directions Chapter 2. Review of Sand Behaviour Under General Stress Path Loading was lying close to 29 irrespective of the magnitude of a and the level of stress ratio a R. They attributed the inequality of induced during "loading paths". and a^a to the more irrecoverable strains The agreement between a^ versus e during "unloading paths" was alternatively suggested to be due to the high recoverable strains associated with unloading. It has already been demonstrated that the sand is inherently anisotropic. It is therefore important to examine whether the coincidence of stress and strain increment directions could be directly viewed as a reflection of the recoverability of strains. If, for example, the material behaviour is isotropic elastic, the stress and strain increment directions would coincide. On the other hand, if it is cross anisotropic, even under ideal elastic conditions the coincidence of a^j and OAO- is not a necessity. It can be demonstrated that in a given cross anisotropic elastic material, the stress and strain increment directions will coincide only under a unique loading condition (Appendix A). It is therefore important that any correspondence between a^ c and should be interpreted only with due consideration given to material anisotropy. The interpretations based on ideas directly applicable to isotropic elasticity will be of little assistance to the understanding behaviour of a material which is known to be anisotropic. The examination of strain increment directions during deformation is still important, since it can be used as a qualitative indicator of the changes in anisotropy during stress path loading. Sayao (1989) examined the relation between a& and a^cr under c cyclic rotation of principal stresses at constant R, b and a' . m Typical results for a loose sand are reproduced in Fig. 2.11. The increasing phases of a a {a. from 0° to a ±60°), always resulted in larger differences between a& and a^a-- On the other hand c decreasing a towards zero from either side of its maximum amplitude resulted in a ^ a £ close to a^o-. As such, the strain increment directions clearly reflected the changes in anisotropy that took place during cyclic principal stress rotation. Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 30 Figure 2.11: Strain increment directions during cyclic principal stress rotation - after Sayao (1989) Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 2.4 31 Summary The foregoing literature review indicates that major advances have been made in the understanding of the separate effects of principal stress rotation and other stress parameters on the behaviour of cross anisotropic sands. The behaviour under general field loading conditions involve simultaneous changes in all six stress parameters a' , m R, b and the inclinations of the principal stress to the three cordinate axes fixed in the material. The H C T device enables an independent control of a' R,b, m) principal stress rotation a a and in one plane and hence a systematic study of material behaviour that includes principal stress rotation in one plane. The previous research using the H C T has concentrated on deformation due to changes in only one of these parameters at a given time. No comprehensive study has been made to investigate the behaviour of sands under simultaneous increase of these stress parameters in a controlled manner. It has been suggested that the initial anisotropy governs the behaviour under principal stress rotation, if the induced strains are small. These conclusions have been based on a limited number of tests which envelopes only a small domain of the stress space. Serious stress non-uniformities can develop in the H C T specimens of a given geometry under certain loading conditions. Thus it is imperative to delineate the domain of stress space available to the H C T device, for confident exploration of sand response under generalized stress path loading (see Chapter 3). Stress non-uniformities have been assessed mostly assuming sand to be linear elastic. Sands, however, are nonlinear in their stress strain response. In order to delineate the domain of stress space that could be reliably explored using the H C T , the non-uniformities assessed on the basis of non-linear soil behaviour are therefore essential. No such assessment has so far been made which uses stress ratio R as the index of stress non-uniformity. It is the purpose of this thesis to explore further some of the unanswered territories Chapter 2. Review of Sand Behaviour Under General Stress Path Loading 32 of stress strain behaviour of cross anisotropic sands. The University of B.C. H C T apparatus is used in accomplishing this task. A detailed assessment of the stress nonuniformities in the H C T specimen having the geometry used at U B C is carried out assuming an incremental elastic hyperbolic representation of sand behaviour. The domain of stress space that could reliably be explored without introducing serious stress non-uniformities is thus identified. The stress paths for the experimental testing program are chosen so that they would he within this domain. The testing program was designed particularly to study the effects of simultaneous increase in more than one stress parameter on sand response, and investigate possible interrelationships between this response and the response from tests in which only one stress parameter was varied. Chapter 3 Stress Non-uniformities in the Hollow Cylinder Torsional Device 3.1 Introduction The stress distribution within a hollow cylindrical torsional (HCT) specimen is nonuniform due to the curvature of the specimen wall as well as end restraint effects. The latter is common to most soil testing devices and could be minimized by selecting sufficiently long specimens together with end platens that reduce radial shear at the ends (Saada and Townsend, 1981; Hight et al., 1983; Vaid et al., 1990). On the other hand, stress non-uniformities due to the curvature of the specimen can occur even when the boundary stresses are uniformly applied. Investigations into the stress non-uniformities due to curvature of the wall in H C T specimens have been reported by Hight et al. (1983) and Sayao and Vaid (1988). Hight et al. examined stress non-uniformities across the wall of the specimen in terms of the distribution of individual stress components. Sayao and Vaid argued that the assessment of stress non-uniformities should be based on the variation of effective stress ratio R across the specimen wall, because the deformation behaviour of granular material is intimately linked to the level of R and not to individual stress components. Their analysis revealed that although the level of stress non-uniformities according to Hight et al.'s criterion were in the acceptable range, serious non-uniformities were in fact present in terms of the distribution of R. Based on these studies, Sayao and Vaid delineated the domain of stress space that could reliably be explored using the 33 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 34 hollow cyhnder device of a given geometry. The assessment of stress non-uniformities in the H C T apparatus have been mostly carried out assuming that sand behaviour is linear elastic. This was mainly due to the readily obtainable closed form solutions to describe the stress distributions in a linear elastic hollow cyhnder. In general, the assumption of linear elastic behaviour permits the presence of large stress gradients and hence high stress non-uniformities. Since the soil behaviour is non-linear (modulus degradation associated with increasing shear) the results emanating from a linear elastic analysis would generally overestimate stress non-uniformities. Although this would provide a conservative upper bound on the non-uniformities, it is important to point out that this conservatism is achieved at the expense of severely limiting the domain of the general stress space that could reliably be explored. A rational assessment of stress non-uniformities should be based on a material stress strain law which models the deformation modulus degradation characteristics of soils. Hight et al. (1983) did report a limited study on stress non-uniformities in H C T specimens assuming a strain hardening elasto-plastic material behaviour. Since the non-uniformities were assessed for individual stress components, their results did not reflect the non-uniformity of stress ratio R across the wall of the specimen, a measure most crucial in the case of granular material. So far there has not been any detailed examination of the stress non-uniformities in terms of R, which takes the non-linearity of the sand behaviour into account. In order to interpret data from a H C T test, relationships have to be established between average stresses and the surface tractions (see section 3.2). Like stress nonuniformity evaluation, the average stresses are commonly estimated with the assumption that the sand response is linear elastic. It is therefore important to investigate the validity of the linear elastic assumptions in the estimation of average stresses even if soil is assumed non-linear in assessing stress non-uniformities. No attempts have Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 35 been made to examine this important aspect, upon which the entire concept of stress path testing and interpretation of data in a H C T device is based. In this chapter the stress non-uniformities arising due exclusively to the curvature of the H C T specimen are examined using the finite element (FE) analysis. A n incremental elastic hyperbolic stress strain law is used to model sand behaviour. These results are then compared with the stress non-uniformities obtained if the soil was assumed linear elastic. The domain of stress space that could reliably be explored without introducing unacceptable stress non-uniformities is identified based on the results from the F E analysis. The effects of confining pressure and relative density of sand on stress non-uniformities are also examined. Finally, the average stresses obtained from linear elastic analysis are compared with those derived from F E analysis, in order to verify the validity of linear elastic assumption for the computation of average stresses. 3.2 Definitions of Average Stresses, Strains and Non-uniformity Parameters In order to follow a given stress path, four surface tractions applied to the H C T specimen need be varied in a prescribed manner. They are: vertical force F , torque z Th, external and internal pressures: P and Pi respectively (Fig. 3.1). At any given e point in the H C T specimen these tractions induce stresses cr a , cr and T as shown 2) T e ZS in Fig. 3.1. In response to these stresses four non-zero strain components e , e , e$ z r and e g develop. z 3.2.1 Average Stresses Interpretation of results from H C T tests is made by considering the entire specimen as a single element, deforming as a right circular cylinder. In order to compute Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device Figure 3.1: Loading and stress conditions in H C T specimens 36 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 37 surface tractions for following a given stress path or vice versa, average stresses are usually computed assuming a linear elastic isotropic material (Hight et al., 1983; Sayao, 1989). The expressions for cr , a r s and r z6 are obtained by averaging the stresses over the volume of the specimen. The vertical stress <r is assumed to be z distributed uniformly across the cross section, and thus obtained using equilibrium considerations only. The resulting expressions are: •K{RI - *r _ (P Rl - P Rf) ^ 2(P e t - P )RlRfhx{R /R ) e " (Rl - Ri) ' (3.1) Rj) i (Rl - n i R1Y 4?Ufi - Rf) 3 e where, R e Ri - External Radius of the H C T specimen - Internal Radius of the H C T specimen The radial stress a is usually the intermediate principal stress a in H C T tests. T 2 Using the Mohr's circle on cr , <xg and T e, the major a and minor <T principal stresses 2 z x 3 and the inclination a of the major principal stress ai to the vertical can be calculated a (Fig. 3.1). 3.2.2 Average Strains The average strain components in the specimen are calculated using the following expressions. Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device AH 38 (3.4) ~H AR - e ARj (3.5) R — Ri e ,AR 6 6 7 r f + e ARj\ = ~ ( /? , p _ 2A0 (fi - JZ?) " W{R\-R\) ) (-) 3 6 3 e ( ] where ff, AH - Height and change in height of the specimen AO - Angular displacement at the base of the specimen The change in the inner radius AR{ is obtained from the measured values of AH and volume change of the inner chamber. The external radius change AR can then e be computed from the measured values of AH, volume change of the sample and the derived value of AR{. 3.2.3 Degree of Stress Non-uniformity The degree of stress non-uniformity in the H C T specimen is assessed in terms of the variation of stress ratio across the wall (Sayao and Vaid, 1988) and is given by the non-uniformity coefficient, n PR where. {.Rrnax Rmiri) B /<3 \ -°> 6 Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 39 Rmax - Maximum stress ratio across the wall of the specimen Rmin - Minimum stress ratio across the wall of the specimen R 3.3 av - Average stress ratio across the wall of the specimen Finite Element Program and Mesh 3.3.1 Finite Element Program The three dimensional F E program 3DSLB developed at U B C by Salgado (1990) was employed for stress analysis in the H C T specimen. The program uses cubical isoparametric elements ("brick" elements) with 8 nodes per element. Each node can assume 6 degrees of freedom: viz. 3 displacements and 3 rotations. The program also has the ability to include beam elements in the F E mesh, thus making provision to accomodate the feature of soil structure interaction. Although the program has the capability of using complex stress strain models, an isotropic incremental elastic hyperbolic model as proposed by Duncan et al. (1980) was used. Soil modelling using such a constitutive law has been claimed to result in deformation predictions which agree favourably with measured deformations in the field ( N S F / N S E R C Workshop, 1980). Soil parameters used in hyperbolic modelling are given in Fig. 3.2 and the relevant equations signifying parameter usage are: (3.9) (3.10) B, (3.11) Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device f, Parameter K E B ks n fa, A<f> Rj k m { t B Name Asymptotic deviator stress Failure deviator stress Initial tangent modulus Tangent bulk modulus Modulus Number Modulus exponent Friction angle parameters Failure ratio Bulk modulus number Bulk modulus exponent Function Relate Ei to cr' 3 Relate (cr[ — <T )J to <r' Relate (<r[ - <r^) to (<rj - <r' \ Value of B /P at a' - P 3 3 uit t a z s 3 a Figure 3.2: The definition of parameters for the hyperbolic model - after Duncan et al. (1980) 40 Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 41 Table 3.1: Hyperbolic Soil Parameters used in the Analysis k E n k B m 0.5 0.5 0.5 300 500 900 0.25 0.25 0.25 A<j) Rf 0 4 9 0.9 0.7 0.6 % 30 75 100 500 900 1500 33 41 50 <f> = ^ - A ^ l o g ^ j (3.12) In the F E program two independent incremental elastic moduli, the tangent Young's modulus E and the tangent bulk modulus B define the stress strain ret t lationship. The values of E and B for a given sand depend upon the stress level as t t shown in the above equations. The parameters to compute these moduli are usually obtained from conventional triaxial tests. Since the aim of this study was to assess the stress non-uniformities in the H C T test for a general sand specimen, representative values of soil parameters were obtained as suggested by Byrne et al. (1987). These are listed in Table 3.1 for three relative density states. 3.3.2 Mesh Used The hollow cylinder specimen was simulated using an axisymmetric polygonal cross section with 12 sectors as shown in Fig. 3.3. The dimensions of the mesh was chosen to represent the University of B.C. H C T device. The U B C - H C T has the following dimensions: external diameter = 152 mm (6.0 in), internal diameter = 102 mm (4.0 in) and height = 305 mm (12.0 in). The effects of end platens were simulated by having a series of beam elements at the top and bottom ends of the F E mesh as shown in Fig. 3.4. The beam elements connect the nodes lying on a radial line from Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device i i Outline of the Actual Right Cylidrical Cross section Mesh Used in the Analysis Figure 3.3: Cross section of the F E mesh used 42 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device A Z Figure 3.4: One sector of the F E mesh with end beam elements 43 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device the central node which is at the central axis of the specimen (OA and OB in Fig. 3.4). Each end platen is simulated by 12 such radial lines in order to match the selected number of sectors. Each radial line has 6 nodes in addition to the central node, thus requiring 6 beam elements for interconnecting these nodes. Since the analytical study was aimed at investigating stress non-uniformities arising due only to the curvature of the specimen, it was necessary to specify boundary conditions so that the effect of specimen curvature alone contributed to the nonuniformities. This was achieved by satisfying the following end conditions in the F E analysis. 1. At the top and bottom end platens (simulated by beam elements) there is no restraint to the movement of the soil in the radial direction (no radial end restraint). 2. Both end platens act as rigid bodies against any mode of deformation which involves bending of the beam elements. Full friction should develop between the end platens and the soil to arrest any slip in the circumferential direction. ( i.e. soil elements in contact with end platen undergo an angular movement about the central axis O^OB, which is identical to the angular movement of the end platen itself). 3. Vertical (i.e. axial) displacement and rotation about the vertical axis of the top platen is held fixed, whereas the bottom platen is allowed to move any desired amount in these two modes of motion. The first requirement was achieved by having beam elements with very low cross sectional area so that the axial stiffness of the beams was neglegibly small ( value of E A = 1.8 x 1 0 - 1 1 N). This made the relative movements of the nodes in the radial direction of the mesh to be unaffected by the presence of these structural elements, thus satisfying the zero radial end restraint condition. 44 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device The second boundary condition was simulated by increasing the flexural rigidity of the beam elements (in all directions of bending) to a significantly high value (value of EI = 1.8 x 10 N m ) , and connecting each beam element to its end nodes with full 5 2 moment resisting capacity. Thus, due to the high flexural rigidity and the imposed end fixity conditions for the beam elements, the nodes lying on a radial fine at the beginning of loading remained radial during any stage of loading. This ensured a rigid end platen condition against torsional mode of loading. Since the soil and beam elements had common nodes at the top and bottom ends, the soil elements automatically experienced an angular displacement identical to that of the end platens, thus accomplishing the no circumferential slip condition at the ends. The third boundary condition requires the top end platen to be held fixed against the vertical (axial) movement and rotation about the vertical axis. The zero vertical displacement requirement at the top end platen was achieved by prescribing all the nodes lying on the horizontal cross section through OA (Fig. 3.4) to have zero displacement in the vertical direction. In arresting the rotational movement of the top platen, only node OA was held fixed against rotation about the vertical axis. Due to the rigid beam element assembly (as described in the previous paragraph), the other nodes lying on that cross section through OA were automatically held against rotation. On the other hand, all nodes at the bottom end platen were given the freedom to move both in the vertical and rotational modes. Finally, in order to keep the vertical axis OAOB aligned and vertical under any loading condition, the movement of the nodes OA and OB in the horizontal plane was not permitted. As described previously the hollow cylindrical specimen is loaded by applying four surface tractions. In order to load the specimen along a desired stress path, the surface tractions are back calculated from the average stresses obtained from linear elastic considerations ( i.e. equations 3.1 to 3.3). In simulating these tractions in 45 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device the F E analysis, the external vertical force and the torque about the vertical axis is applied at the bottom of the specimen at the central node OB (Fig. 3.4). On the other hand, the internal and external pressures on the specimen walls are distributed by applying equivalent nodal loads on the interior and exterior vertical faces of the mesh. The full cyhnder was modelled by six 2.0 in. (5.0 cm) high elements in the vertical direction (Fig. 3.4). In order to check the validity of the numerical analog in computing stresses in the hollow cylindrical specimen, two loading cases in classical linear elasticity were simulated, and the results compared with closed form solutions. The loading cases selected were: 1. hollow cylinder subjected to pure torque only 2. hollow cyhnder subjected to different internal and external pressures only Figures 3.5 and 3.6 illustrate comparisons between the F E and closed form solutions for the two loading cases considered. The close agreement between the two solutions gives credibility to the use of this polygonal mesh, and the stiffness parameters selected for the beams, for numerically simulating the actual hollow cylindrical specimen. Furthermore, the F E analysis results show that all elements located at a given radius have identical stress states, confirming the expected perfect symmetry of stresses about the vertical axis. The stress state is dependent only on the radial location (not dependent on 8) and independent of the vertical location of the elements. ( i.e. an element neighbouring an end platen has a stress state identical to that of an element located away from the ends, provided both are at the same radial location ). This confirmed that the selected parameters for the beam elements effectively simulated the zero radial end restraint condition, which was an important requirement to be met in this analysis. 46 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device T h (Torque) <CD> Applied Torque = 80 Nm Figure 3.5: Distribution of r material z6 across the wall under pure torque - Linear elastic 47 48 Chapter 3 Stress Non-uniformities in the Hollow Cyhnder Torsional Device 50 60 70 80 Radius mm Figure 3.6: Distribution of a and ere across the wall under different external and internal pressures - Linear elastic material T Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device The imposed zero end restraint condition implies that under a given loading condition, the stress distributions across the wall would be independent of the height of the specimen. Thus, stress non-uniformities due to the curvature of the specimen wall could possibly be assessed with a lesser number of elements in the longitudinal (vertical) direction of the F E mesh, resulting in very large savings in computational effort. It was therefore decided to investigate the feasibility of replacing the full cyhnder mesh with a concise F E mesh (Fig. 3.7) that contains only one element in the longitudinal direction. Other than the difference in the number of elements in the longitudinal direction, the concise F E mesh is identical to the full mesh in terms of the beam element assembly and the end boundary conditions. With concise and the full F E mesh idealizations, the H C T specimen was subjected to identical loading conditions as given below, and the resulting stress distribution across the wall compared for the two representations. 1. Hollow cyhnder specimen of linear elastic isotropic material under, • a pure torque of 80 Nm • external and internal pressures of 450 and 200 kPa respectively 2. Hollow cyhnder specimen of incremental elastic loose sand (D T = 30%) in a stress path loading in which the stress ratio R is increased from 1 to 2 with, • b = 0.0; a„ = 45° and a' = 300 kPa m • b = 0.5; = 0° and a' = 300 kPa m • b = 0.5; a , = 45° and a' m = 300 kPa The first two loading cases for the linear elastic material (item No. 1 above) are identical to those presented in Figs. 3.5 and 3.6. The stress path loadings simulated 49 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device ONLY ONE SECTOR IS SHOWN FOR THE PURPOSE OF CLARITY PROPERTIES OF BEAM ELEMENTS E = Youngs Modulus = 2 kN/m 2 2 -11 A = X-Sectional Area = 0.9 x 10 m I = 2nd Moment of Area = 0.9 x 10 rn 5 (all bending directions) Figure 3.7: One sector of the concise F E mesh with end beam elements 50 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device (item No. 2 above) were selected directly from the main stress non-uniformity investigation program described in section 3.4. In this manner the suitability of using the concise mesh was checked for both linear elastic and incremental elastic representations. Fig. 3.8 compares the stress distribution across cyhnder wall using the concise mesh with that from the full F E mesh for loading of the linear elastic material. Similar comparisons of the distribution of stress ratio R across the wall for loading of the incremental linear elastic material are presented in Fig. 3.9. Excellent agreement between the results show that the zero end restraint conditions are fully satisfied with the use of concise mesh. Thus, the concise mesh only was used in the assessment of stress non-uniformities due exclusively to the curvature of the specimen. 3.4 Stress Non-uniformities Under General Stress States in Non-linear Soil Stress non-uniformities in the H C T specimen were assessed predominantly for loose sand (D = 30%). Loose density was selected because the effects of principal stress T rotation have been found to be more profound in loose sands (Sayao, 1989). Theoretically an infinite number of stress paths can be followed in loading to a given stress state, denned by the parameters a' , R, b and a , Because of the m r non-linearity of the selected constitutive law, the stress non-uniformities at the target stress state will depend on the stress path executed to that stress state. This prompted some preliminary analyses to investigate the dependence of the degree of stress nonuniformity coefficient /3R on the stress path followed. Results of these analyses are presented in Fig. 3.10, which also shows different stress paths followed to identical target stress states. It may be observed that the stress non-uniformities do depend on the stress path followed to the target stress 51 Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 52 200 150 - CO CD © © 100 N • 50 - © Concise FE Mesh O Fu" ^ Mesh -1 1 1 1 1 1 1 1 1 1 1 1 1 r Hoop Stress 1000 © P Cu V) S 55 T •= 80 Nm n P w © ©• = 200 kPa =450 kPa 500 © © Radial Stress © 50 ~i i i i i 60 i i i i i 70 i i i i 80 Radius mm Figure 3.8: Comparison of stress distributions across the specimen wall from the full F E mesh versus concise F E mesh - Linear elastic material Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 2.5 a (a) b = 0.0 cc =45 f f © 2 1.5 2.5 i i - i 1 1 i i 1 1 1 1 r™ (b) b - 0.5 : cc 2- 1.5 - i 1 r 2.5 (c) b = 0.5 : cc 2 ./S) a . - « ° ® ° O Concise FE Mesh Full FE Mesh 1.5 Radius cm Figure 3.9: Comparison of stress distributions across the specimen wall from the full F E mesh versus concise F E mesh - Incremental elastic material 53 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device b = Constant : 0 = 45 : a. 3 0*' m = 300 kPa B R 2 A C O 45 A D 0 e g Stress Path r R b OA CA OB CB 0.0 0.077 0.078 0.066 0.091 0.5 0.133 0.145 0.070 0.090 1.0 0.060 0.052 0.032 0.029 Figure 3.10: Dependence of (3R on the stress path Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device state. (5R values along stress paths C A and C B are larger than those obtained along paths OA and OB respectively, for b values of 0.0 and 0.5. However for b = 1.0 the reverse is true. It is virtually impossible to assess (3R for every stress path to the target stress state. Based on the above limited path dependence study, only increasing R stress paths with all other stress parameters held constant (i.e. similar to C A and C B ) were selected for a detailed exploration of stress non-uniformities in the (R, b, cv) stress space. Figure 3.11a illustrates one such path in the generahzed stress space. Along all stress paths, for a given D the value of a' was held constant T while different combinations of b and a shows combinations of b and a ff CT m were used for each stress path. Fig. 3.11b selected for the analysis. The non-uniformity coefficients at different R values along R paths are computed and compared with those obtained assuming linear elastic isotropic material. The effect of mean normal stress on /3R is then assessed for loose sand at selected b, a„ combinations. Finally, the influence of increasing relative density on /3# is examined for a limited combinations of cr' , b and ov. m 3.4.1 Stress Non-uniformities in Loose Sand H C T Specimens 3.4.1.1 Comparison with Linear Elastic Material Figure 3.12 compares the distribution of stress ratio R across the wall of the H C T specimen for the incrementally linear and linear elastic analyses. The comparisons are made at three arbitrarily selected stress states: (a) a' = 300 kPa, R = 2.0, b — m 0.0, a , = 45°; (b) a' = 300 kPa, R = 2.0, b = 0.5, ac R = 2.0, b = 0.5, a — 45°. Similar comparisons made at a higher stress ratio R — m a = 0°; and (c) a' = 300 kPa, m 3 for otherwise identical a' , b and a , conditions are shown in Fig. 3.13. It may be m noted that for all stress states, linear elastic material shows large variations of stress 55 er 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device Typical stress path simulated in the FE analysis D (J = constant r = constant / (b) 1 m T • «o—* | 0.5 - 1 CL n r" 20 1 1—•—i 40 a . r 60 n r - 80 Deg Figure 3.11: Stress paths used in the F E analysis 57 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 2.5 0.177 (a) b = 0.0 cc 2 V A L U E O F / ? I S INDICATED R IN T H E BOX. 1.5 2.5 - i 0.218 CC 2 1 1 i I 1 r- (b) b = 0.5 0.086 1.5 I i 2.5 (c) b = 0.5 : CC 2--" 0.133 Incremental Elastic Hyperbolic 0.297 Linear Elastic 1.5 -T 1 1 1 - -1 1 1 r~ Radius cm Figure 3.12: Distribution of stress ratio across the wall of the specimen with material behaviour: a' = 300 kPa; R = 2.0; D = 30% m T Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device (b) b = 0.5 3.5- 2.5 —I 1 r~ 4 - (c) b = 0.5 3.5 a „ - 4 5 0.533 . : 3 Incremental Elastic Hyperbolic 2.5 H Linear Elastic -t - i 1 1 1 r- r- 6 7 Radius cm Figure 3.13: Distribution of stress ratio across the wall of the specimen with material behaviour: <rL = 300 kPa; R = 3.0; D = 30% T 58 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device ratio across the wall and thus higher (3R values when compared with those for the incremental elastic material. Figs. 3.12 and 3.13 also indicate that flp for a given 1 (b, a ) a condition increases with increase in R, for the linear elastic material. For the incremental elastic material on the other hand, (3R values show a much smaller increase, or even a decrease with increase in R for certain combinations of 6 and a . a The stress non-uniformity coefficients (3R were evaluated in a similar manner at R — 2 and 3 for several values of a , but for three selected values of b parameter a 0.0, 0.5, and 1.0. The results shown in Fig. 3.14 reveal that for a given stress state, /3R estimated from linear elastic assumption are always higher than those based on incremental elastic assumption. For an increase in R from 2 to 3 for a given a ff) /3R increases substantially in the case of linear elastic material. For the incremental elastic material on the other hand, (3R at R = 3 is less than that at R — 2, for most stress states. In the incremental elastic material, large gradients of R would not exist, as the stresses across the wall of the specimen gradually redistribute as a result of modulus degradation associated with increasing R. In contrast, for the linear elastic material, the elastic moduli remain unaltered with stress level, and therefore no redistribution of stresses can occur resulting in much sharper gradients of R. It may be argued that the soil is not accurately modelled by an incremental elastic hyperbolic stress strain law. Yet, it is a much superior approximation to the non-linear behaviour of real soils than the linear elastic assumption. The foregoing analyses show that the assessment of stress non-uniformities based on linear elasticity could lead to estimates of /3R which are larger than that actually present in a H C T sand specimen. The results presented in Figs. 3.12 - 3.14 were restricted to selected combinations of b and a . c 1 Figures 3.15 and 3.16 present the contours of (3R encompassing the Value of fin is indicated inside the boxes in the figures. 59 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 60 (a) b = 0.0 cc R = 2.0 0.5 R = 3.0 (c)b = 1.0 Linear Elastic Incremental Elastic Hyperbolic 0.5 - 60 (X a 80 Deg Figure 3.14: Variation of /3R VS R with material behaviour: a' 30% m = 300 kPa: D T Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device entire domain of b and a for two R values. a 61 The contours for the incremental elastic material are drawn using results of 0R evaluated at several (fc, ov) locations shown in Fig. 3.11b. The contours of /3R for linear elastic material are reproduced from Sayao (1989). It may be observed that for any stress state within the full domain of (6, a ) , the linear elastic material law always overestimates the magnitude of 0R, when a compared to that obtained using the incremental elastic material law. Based on the linear elastic analysis, Sayao (1989) suggested that a (3R value less than 0.2 could be considered as an acceptable limit to delineate the domain of stress space that could be reliably explored using the H C T device. Considering the much smaller non-uniformities arising in incremetal elastic material, a much larger domain of the general stress space is available for exploration, even if the acceptable limit of non-uniformity level is restricted to a smaller value of 0.1. This is illustrated by the shaded domains of /3R > 0.1 and /3R > 0.2 in Figs. 3.15 and 3.16. Although the magnitudes of (3R from linear elastic analysis are much larger than those obtained for the incremental elastic material, some similar trends in topographical features in (3R contours can be identified (Figs. 3.15 and 3.16). Excepting the vicinity of (b = 1.0, a a = 0°) at R — 3 (Fig. 3.16b), the approximate locations of peaks and valleys of J3R in (6, a ) space tend to be similar regardless of the material a behaviour or R level. It appears that a significant redistribution of stresses has occurred in the neighbourhood of (b — 1.0, a = 0°) at R = 3 in the incremental elastic a sand (Fig. 3.16b) giving rise to exceptionally low /3R values, compared to those at lower R — 2 for the same material. It has been pointed that stress non-uniformities across the wall of the H C T specimen are caused by the differential pressures across the wall (P — Pi) and the torque e T h applied to the specimen. In agreement with this, high {3R values would be ex- pected in the vicinity of the corners {b = 0.0 : a c = 90°) and (6 = 1.0 : a a = 0°) where the value of (P — Pi) is high and in the regions where Th is high (i.e. in the e Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 63 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device vicinity of 64 = 45°). On the other hand, /3R is low in the neighbourhood of the corners (b = 0.0 : a , = 0°) and (b = 1.0 : a ff = 90°), where (P - P ) as well T have e { h relatively low values. It is also interesting to note that for some combinations of b and ov, (3R is low even when both differential pressure across the wall as well as the torque are applied (e.g. in the vicinity of b = 0.5 and OL0 = 25°; b = 0.5 and o. = 70° etc. See Figs. a 3.15 and 3.16). It appears that the effects of (P — Pi) and e in inducing stress non-uniformities have acted in a compensating manner under these combinations of b and a , thus giving rise to lower /3R values. a 3.4.1.2 Influence of Stress Ratio In the previous section, stress non-uniformity coefficients were shown only for two selected levels of stress ratio R — 2 and R — 3. The variation 0R with gradual increase in stress ratio for three selected values of b is plotted in Fig. 3.17. (3R is shown as a function of a„ for several R levels at fixed D — 30% and a' = 300 kPa. T m These results show that J3R increases with increasing stress ratio R at lower levels of R. However, with increase in R level, the rate of increase in /3R with R decreases, causing either (3R to reach a maximum or even decrease after reaching a peak value for certain combinations of b and a . a This feature becomes clearer in a plot of (3R VS R for selected combinations of b and a^, as shown in Fig. 3.18. A gradually decreasing rate of change of 0R with respect to R can be explained by a gradual redistribution of stresses within the soil specimen as a result of modulus degradation in the non-linear elastic material. Such redistribution of stresses would not occur in a linear elastic material. This effect is further illustrated in Fig. 3.19 where /3R versus R for a linear elastic material is compared with that for the incremental elastic material, for the same stress conditions considered in Fig. 3.18. Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 65 Figure 3.17: Effect of stress ratio on the non-uniformities: a' = 300 kPa: D = 30% m r Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device Figure 3.18: Variation of (3R with R: <r'= 300 kPa: D = 30% n r 66 Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device Figure 3.19: Variation of (3R VS R with material behaviour: a' 30% m = 300 kPa Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 3.4.1.3 68 Influence of Mean Normal Stress Figure 3.20 presents the effects of the level of mean normal effective stress a' on /3R m at R — 2 and 3, for the same combinations of b and a 6 = 0.0, a„ = 45°; b = 0.5, a a = 0° and b = 0.5, a a considered in Fig. 3.19. (viz. ff = 45°). The results show that the influence of <r' on stress non-uniformities is very little in the a' range considered (i.e. m m from 100 kPa to 900 kPa). Therefore, it can be concluded that under moderate stress levels (that would usually be encountered under most field conditions) the effect of a' on J3R is small. m 3.4.2 Influence of Relative Density on Stress Non-Uniformities For a given sand the hyperbolic parameters change with increasing density (see Table 3.1). A n immediate consequence of increase in D is the increase in E , B r (a[ — <T ) U (see Equations 3.9 to 3.12). t t and A limited number of F E analyses were 3 u carried out to study the effect of relative density on (3R. Fig. 3.21 illustrates the effect of relative density D , on the variation of /3R with r R for one arbitrarily selected stress state a' = 300 kPa; b — 0.5 and m = 45°. It can be observed that excepting the region of low R, (3R increases with increasing density for a given R . This is because of the increasing stiffness E against deformation with t increasing density. Consequently the degree of stress redistribution would be less in sand of higher D , thus resulting in higher (3R. r It is important to note in Fig. 3.21 that initially /3R increases with increasing R regardless of D . With continuing increase in R, the rate of change of (3R with respect T to R decreases and (3R reaches a maximum after a certain value of stress ratio. The maximum of (3R occurs at a higher value of R for dense sands than for loose sand. It appears that the occurrence of the maximum of (3R depends more on the ratio of the mobilized stress ratio to the failure stress ratio than on the mobilized stress ratio itself. This is illustrated in Fig. 3.22 in which 0R is plotted against the mobilized Chapter 3. Stress Non-uniformities in the Hollow Cylinder Torsional Device 0.1 - (a) b = 0.0 : _ o • cr - o • • • 0.05 I - 1 R = 2.0 1 o r 1 i i R=3.0 r —T T (b) b = 0.5 : 0.1 • m cr 0.05 H t 1 ' " 1 i r r • i i i 0.15 • m 0.1 ' (c)b = 0.5: 0.05 i i r - 0 r 1 i > 1 i 500 Mean Normal stress 1000 (J kPa m / Figure 3.20: Effect of a' on the value of j3 , D = 30 % m R r 69 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device Figure 3.21: Effect of D on variation of /3R with R r 70 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 71 friction ratio F R . F R is denned as, FR = (3.13) where, Rmob - Stress ratio mobilized Rf - Stress ratio at failure The Fig. 3.22 shows that peak value of /3R occurs around a F R value of about 60% regardless of density state. Figure 3.23 shows a plot of (3R VS D for three selected stress states: (a) a' = 300 T kPa, b = 0.0, a a = 45°; (b) a' m m = 300 kPa, b = 0.5, a„ = 0°; and (c) cr' = 300 m kPa, b = 0.5, av = 45° at two levels of R = 2 and 3. (3R may be seen to increase with relative density at a faster rate at higher R value. It is also important to emphasize that for a given R the stress non-uniformities become increasingly large at higher relative densities, indicating a decrease in the size of the domain of stress space available for reliable exploration of generalized stress path behaviour. The foregoing analyses reveal that for a given stress state, loose sand specimens will have lesser degree of stress non-uniformities across the wall than dense specimens. Therefore, interpretations of H C T test data on very dense specimens at higher stress ratios should be carried out with caution. 3.4.3 Additional Remarks on Stress Non-uniformities The hyperbolic parameters to represent non-linear sand behaviour were selected based on suggestions by Byrne et al. (1987) for "average sands". Considerable variations in these parameters (especially k E> kg and 4>) can occur depending upon the minerolog- ical composition, grain shape and gradation of sand. For example, at a given density and confining stress, a carbonate sand could have lower modulus of deformation E{ Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device Figure 3.22: Variation of (3R with the mobilized friction ratio Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 0.3 tt (a) b = 0.0 = 0 45 0.2 R=3 cc R=2 0.1 0 0.3 ^ 1 ( «, - (b) b = 0.5 0 0.2 cc 0.1 H 0 0.3 ~i 1 1 1 r~ —\ r~ R=3 (c) b = 0.5 0.2 A R=2 cc 0.1 20 ' 40 ' 60 ' 80 ' 100 ' 120 Relative Density % Figure 3.23: Variation of (3R VS D for different stress states T Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 74 but friction angle still identical to that of an "average sand". It is important to assess stress non-uniformities that would arise in specimens of such "non-average" sand. It is clearly not practical to analyse stress non-uniformities for all possible combinations of soil parameters. Nevertheless, some appreciation of {3R changes with different hyperbolic parameters can be inferred from the results already presented. It has been established that the linear elastic material assumption yields higher (3R at a given stress state when compared to an incremental elastic material assumption. The stress strain behaviour of these two materials can be schematically illustrated by curves A and B in Fig. 3.24. It is clear from this figure that the sole contributing factor in reducing /3R in the incremental elastic material is the degrading modulus of deformation with increasing shear stress. The stress strain curve C in Fig. 3.24 depicts a material having a smaller initial modulus E{ but other hyperbolic parameters identical to curve B . The main difference between curves B and C is that the material represented by curve C will always have lower tangent modulus than that for curve B at a given value of shear stress (or R). Using the already established /3R differences in material representations by curves A and B, it can be inferred that the stress nonuniformities would be smaller in the material having lower initial modulus E{ (e.g. curve C). In other words a softer material will give rise to lesser non-uniformities than a stiffer material. 3.5 Estimation of Average Stresses In order to interpret test data or to conduct a stress path test in the H C T device, it is necessary to establish a one to one correspondence between the set of surface tractions P , Pi, F and Th and the induced average stress components a , tr , <rg and e z z P r g. The soil is usually assumed to be linear elastic, both for computation of average z stresses from the surface tractions or computation of target surface tractions in order to reach the target average stress state. It is important to assess whether this method Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device Figure 3.24: Stress strain relations under different initial modulus 75 Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 76 of computation is justified considering that the sand behaviour is in fact non-linear. Comparisons of stress components at identical surface tractions using linear elastic and incremental elastic hyperbolic material approximations, for three selected stress states are presented in Table 3.2. In spite of the differences in stress non-uniformities across the wall, the average values of stresses may be seen to agree remarkably well. This aspect is further examined in Fig. 3.25 by comparing the average stress ratios at several stress states. The results illustrate that the computed average R values based on hyperbolic incremental elastic behaviour closely agree with those obtained from linear elastic analysis. Thus for a given set of surface tractions, the computed average stresses bear little sensitivity to the material stress strain law, even though the stress distribution is dependent on the material constitutive law. The use of elastic assumption is thus justified for computing average stresses from the applied surface tractions and vice versa. Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device 77 (a) b = 0.0 • 1 4 - (b) b = 0.5 cc o ft cc V) Ui 2 CO 1 4 (c)b = 1.0 • • - • • • • • R = 2.0 20 R=3.0 60 40 a a 80 Deg Dashed Lines - Linear Elastic Points - Incremental Hyperbolic Elastic Figure 3.25: Comparison of average stress ratios from incremental vs linear elastic analysis D = 30%, a' = 300 kPa r m Chapter 3. Stress Non-uniformities in the Hollow Cyhnder Torsional Device Table 3.2: Comparison of average stresses <r' = 300 kPa : R = 2.0: D - 30% m Stress kPa <?e R T b = 0.0 a„ •= 45° L. Elas. Inc. Elas. L. Elas. 337.5 225.0 337.5 112.5 450.0 225.0 2.00 337.4 228.1 335.1 109.5 445.2 227.2 1.96 400.0 300.0 200.0 000.0 400.0 200.0 2.00 b = 0.5 : ov = 0° b = 0.5 a, = 45° Inc. Elas. L. Elas. Inc. Elas. 400.2 297.9 202.1 000.0 400.2 202.1 1.98 300.0 300.0 300.0 100.0 400.0 200.0 2.00 300.0 300.0 300.0 101.5 401.5 198.5 2.02 78 Chapter 4 U B C Hollow Cylinder Torsional Device and Experimental Aspects A detailed description of the U B C hollow cyhnder torsional (HCT) device has been given by Vaid et al. (1990). Therefore only important features of the apparatus and steps in specimen preparation will be briefly outlined. In order to carry out general stress path tests, a new, fully automated control system was developed. The design considerations, stress path control, and performance of the new system are presented in detail in this chapter. 4.1 The U B C Hollow Cylinder Torsional Apparatus (UBCHCT) 4.1.1 General Description The U B C - H C T apparatus is capable of subjecting a hollow cylindrical specimen of soil to an axial load, torque about the vertical axis, and different internal and external pressures. Independent control of these surface tractions enables the specimen to be loaded along a prescribed stress path in the four dimensional stress space (R,a-' , b, m a ). The domain of this stress space that could be explored by the apparatus without ff introducing serious stress non-uniformities has been discussed in the previous chapter. A schematic diagram of the U B C - H C T is given in Fig. 4.1. Important details are enlarged and presented in Fig. 4.2. The hollow cyhnder specimen is 15.2 cm 79 Ciapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects LVDT ( POSITIONING BOLT AH) TOP CROSS BEAM CHAMBER TOP TOP CAP TOP PLATEN PLEXIGLASS CELL LOADING FRAME SOIL SPECIMEN RIGID ROD BASE PLATEN BASE PEDESTAL EXTERNAL PRESSURE PORE PRESSURE PRESSURE TRANSDUCER INTERNAL PRESSURE LVDT ( •SUPPORTING TABLE Q ) 1 LINEAR-ROTARY BEARING TORQUE CABLES LOADING SHAFT TORQUE CELL CENTRAL PULLEY TORQUE PULLEY TORQUE PISTONS (TWO PAIRS) THRUST BEARING AXIAL LOAD PISTON AXIAL LOAD CELL 0 SCALE (cm) 20 Figure 4.1: Schematic of the U B C - H C T device - after Sayao (1989) 80 Chapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects ±± TOP CROSS BEAM (LOADING FRAME) EXTERNAL PRESSURE 2. BOLT jj • r* LOCATING PIN INTERNAL PRESSURE I—I 0 I I I SCALE (cm) I 5 Figure 4.2: Details of the U B C - H C T device - after Sayao (1989) Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 82 (6 in) external diameter, 10.2 cm (4 in) internal diameter, and 30.0 ± 0.2 cm long. Considerations involved in the selection of specimen dimensions are described in detail by Sayao (1989). The test specimen is laterally confined by internal and external water pressures acting on flexible rubber membranes, 0.3 mm thick. The transfer of torsional shear stresses to the specimen end requires that no slip occur between the end platens and the soil, in the circumferential direction. At the same time minimization of end restraint calls for no restraint to deformation in the radial direction. Both these requirements were achieved by using pohshed anodized aluminum end platens having twelve thin radial ribs (1 mm thick and 2.3 mm deep) machined as an integral part of the platens (Fig. 4.3). The radial ribs prevent the circumferential slip and pohshed anodized surface provide the low friction condition in the radial direction. Drainage of the specimen is achieved through six 12.5 mm porous discs set 60° apart, flush with each platen surface (Fig. 4.3). The specimen is fixed at the top. The vertical load is applied at the bottom by means of a double acting air piston. By varying the air pressure on one side of this piston against a fixed back pressure on the other side, a given vertical compressional or extensional load can be apphed. In a similar manner torque is applied at the bottom of the specimen by two pairs of identical single acting air pistons and a system of pulleys and cables. A dual thrust bearing isolates the rotary movement of the sample from being transmitted to the bottom vertical loading piston. 4.1.2 Instrumentation of the H C T Device A choice had to be made between external versus internal measurement of loads and displacements. Both external and internal instrumentation have their own merits and disadvantages. Previous experience at U B C has shown that external measurement of Chapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects A) P E R S P E C T I V E B) P L A N V I E W C) SIDE VIEW h 0 i 1 5 SCALE (cm) Figure 4.3: Polished end platen with radial ribs - after Sayao (1989) 83 Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 84 strains can give very reliable results, provided proper care is taken to eliminate bedding and tilting errors (Negussey, 1984). On the other hand, internal instrumentation gives rise to additional difficulties in terms of specimen preparation and testing procedures etc. Sayao (1989) made a detailed review of these two measuring techniques, and based on that analysis, an external instrumentation system was adopted for the U B C - H C T device. 4.1.2.1 Measurement of Deformations A minimum of four strain components are needed to describe the complete configuration of the H C T specimen at any given instant. This is achieved by monitoring the vertical and angular displacements of the specimen's base platen, volume change of the specimen, and the volume change of the inner chamber. The displacement measurements are made with the use of linear variable displacement transducers (LVDT) in order to track the vertical and circumferential movements. The L V D T mounted on the loading frame's top cross beam (Fig. 4.1) measures the height change of the specimen and thus the axial strain e . The rotation z of the base platen is converted into linear tangential displacement by using the system shown in Fig. 4.4. This L V D T reading is used to obtain the circumferential shear strain 7 g. Locations of the LVDT's are chosen so as to minimize the compliance 2 errors in the axial L V D T and the cross talk effects in the circumferential L V D T due to axial straining of the specimen. Both LVDT's can reliably detect movements in the order of 1 /xm. This results in a resolution of about 5 X 10~ % in both e and 7 g. 4 z z The volume changes of the inner chamber and the soil specimen are obtained by measuring the height of displaced water in graduated pipettes together with sensitive differential pressure transducers (DPT). Measured volume changes are corrected to account the effects of membrane penetration as proposed by Vaid and Negussey (1984a). Chapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects COUNTER WEJGHT Figure 4.4: Rotational displacement measuring system - after Sayao (1989) Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 86 The correction procedure and the magnitude of correction for the test sand are detailed in Appendix B. For all tests a back pressure of 200 kPa was used to ensure a fully saturated condition. Two pipettes of 5.4 mm inner diameter placed in parallel are used to measure the specimen volume change. When small volume changes occur, only one pipette of this dual system is employed in order to enhance the measurement resolution. The D P T can reliably detect volume changes in the order of 3 m m thus resulting in a 3 resolution of about 5 x 1 0 % in volumetric strain e after correcting for membrane _4 v penetration effects. The volume change of the inner chamber of the H C T apparatus is measured using a single pipette of 7.9 mm inner diameter. The D P T for the inner chamber could thus reliably detect volumetric variations in the order of 10 m m which equals 2 X 1 0 % 3 _4 of the total volume of the inner chamber. 4.1.2.2 Measurement of Surface Tractions The stress components at a given instant are calculated from the values of four surface tractions apphed on the H C T specimen. The four surface tractions consist of vertical load, axial torque, and internal and external chamber pressures. The pore water pressure and the chamber pressures are monitored using sensitive pressure transducers having a resolution in the order of 0.25 kPa. The vertical load is measured using a force transducer capable of detecting load changes in the order of 230 grams. The resulting resolution in the vertical stress cr is about 0.22 kPa. z Axial torque measurements are made with a torque transducer possessing a very low cross talk. This transducer can measure torques as low as 0.05 Nm corresponding to a resolution in measurement of shear stress r g in the order of 0.1 kPa. z Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 4.2 87 Stress Path Control and Data Acquisition In the U B C - H C T apparatus described by Sayao (1989), data acquisition was achieved through a multi-channel scanner and an A / D converter communicating with a personal computer. During a generalized stress path test, the control of the four surface tractions was achieved by manual adjustment of the compressed air pressure regulators. Simultaneous and independent control of these four surface tractions is essential when loading the specimen along complex stress paths. In order to follow a prescribed stress path, smooth changes of surface tractions are needed. These requirements render manual control of surface tractions a time consuming and extremely cumbersome task. In the case of drained tests, the surface tractions must be applied slow enough to avoid any localized undrained conditions occurring in the specimen. Moreover, subsequent to any applied load increment, sufficient time should be allowed for the specimen to achieve deformation equilibrium. Mejia et al. (1988) observed that creep deformations in sand become increasingly significant at higher stress ratios. As such, more time would be required for deformation equilibrium to be reached at higher R values. The recording of data and the application of the next load increment should be made only after such equilibrium state is reached. Again, manual control of surface tractions possess serious limitations in the achievement of these objectives. To meet the above requirements a program was undertaken to design a new integrated stress path control and data acquisition system. 4.2.1 Basic Components of the Control System A schematic layout of the stress path control system is shown in Fig. 4.5. The system consists of four motor set (stepper motor) precision regulators that control surface tractions. Nine transducers monitor various loads, pressures, and deformations (as -Op -LTH DATA ACQUISITION -~3~~}- SYSTEM -LTH -LTH -Ur - S - o • STEPPER MOTORS TRANSDUCERS Figure 4.5: Schematic layout of the stress path control system Chapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects 89 discussed in section 4.1.2). A n I B M personal computer connected to a data acquisition system anchors the input-output control. Basic features of the input-output control are described in the following sections. 4.2.2 Data Acquisition (Input to the Computer) All transducers were excited with a stable D.C power supply of 6.0 V . The LVDT's being high output devices, did not need any signal amplification. The remaining transducers were of bonded strain gage type with an output of about 3 m V / V . Signal outputs of these transducers were brought upto 2.0 V full scale using variable gain amplifiers. The feedback control system requires updated values of stress and strain in the specimen, in order to carry out its decision making process. It is therefore important that all transducer readings correspond to the same instant on the time scale. As such, simultaneous reading of transducers became a prime consideration in the development of the data acquisition system. In the system designed, the scanning is triggered simultaneously on all channels in response to a "start scan" pulse from the computer (Fig. 4.6). The signal from each transducer over a 50 ms period is integrated by an analog circuit and the average value is obtained. This average value is then digitized by the A / D converter and temporarily stored in a memory chip. The digital output from the A / D conversion yields a decimal number ranging from 1 to 40000 (~ 16 bits in binary) corresponding to an analog range of 0 to 4.0 V . This corresponds to resolution of the tranducer outputs to be in the order of 0.1 mV. At the end of conversion, the digital voltages are retrieved by the computer in a sequential manner. The system has a low noise level of not exceeding ± 0 . 1 mV thus making maximum use of the resolution available. With the low noise level and the high sensitivity of the transducers used it was possible to achieve a high precision in •8 START C H A N N E L S C A N PULSE FROM P C f CHANNEL INT CHANNEL INT ANALOG PC t = t ] — i — — | A/D |—| M~ SIGNALS o 0 o IN o 0 0 o o 0 0 o 0 0 0 o o 0 o SEQUENTIAL I RETRIEVAL O F C O N V E R T E D INFORMATION BY P C a. I t > t + 50 ms o A / D = A/D C O N V E R T E R o M CHANNEL INT —(A^D~|—[~M § I E N D O F A/D CONVERSION PULSE TO PC t = t + 50 ms o Figure 4.6: Data acquisition process = M E M O R Y CHIP INT = A N A L O G INTEGRATOR § • to n B a. •9 "a CD o to o Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 91 the acquired data. 4.2.3 Control of Surface Tractions (Output from the Computer) The surface tractions are controlled by four Fairchild motorset precision regulators powered by a 24 Volt D . C . supply. Regulators have the ability to impose pressures within a range from 0 to 700 kPa (zz 0 — 100 psi). In response to a logic sequence from the computer, a control chip outputs a series of square pulses to the stepper motors. These pulses change the regulated air supply accordingly. The logic sequence from the computer contains information pertaining to the direction of rotation, and the number of pulses needed to achieve each pressure change. A single pulse advances the motor regulator by one step. Approximately 12 to 13 pulses are needed to obtain a pressure change of 1 kPa, thus enabling the regulators to impose a pressure change as low as 0.1 kPa. Since the motors are operated according to a computer controlled feed back facility, any discrepancies occurring due to factors such as backlash of gear box, etc. are immediately corrected. Regulator motors can change pressures at a rate of approximately 3.0 kPa/s to 14 kPa/s. In applying a given stress increment in drained tests, the rate of change of pressures should be slow enough to ensure that no localized undrained conditions occur in the sample. Sayao (1989) carried out H C T tests with manual control of surface tractions, in which the pressure changes were imposed in a slow manner so as to ensure fully drained conditions. Fig. 4.7 compares the results of a stress path test from the new automated system with those from an identical test (but manually controlled) by Sayao (1989). To achieve a given stress increment in the automated test, the regulators were set at the slower rate of 3.8 kPa/s. Little difference between deformations in the two tests indicate that fully drained conditions were ensured using the automated system. The rate of pressure change selected was thus confirmed to be Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects D r =30% : fj 7 m = 300kPa : b = 0.5 • a 0 92 ii Deg Figure 4.7: Comparison between manually controlled versus automated stress path testing. Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 93 slow enough to avoid localized undrained conditions. As such, this rate was selected as the operating rate of regulators for all tests carried out in this research. 4.2.4 Stress Path Control (Software) The algorithm used for the closed loop controlled stress path testing is presented in Fig. 4.8. Microsoft Quickbasic Version 4.0 was used as the programming language for the main module. For scanning and sending pulses to the stepper motors, subroutines written i n assembler language were used. The program consists of seven major components: 1. Input of initial information : viz. specimen dimensions, reference readings for transducers, etc. 2. Skempton's B value check for saturation 3. Input of stress path to be followed 4. Control of surface tractions 5. Check for deformation equilibrium 6. Data storage 7. Application of next loading increment Once the initial information is fed into the computer, the specimen is loaded hydrostatically in an incremental manner. Monitoring pore pressure increments during undrained loading enable a check on saturation. If the specimen is saturated (a B value > 0.98 was considered as acceptable), the computer reads a file from the floppy disk containing the information on the desired stress path to be followed. This information contains the (cr' , R, b, a ) coordinates of the key turning points in the stress m a Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects Figure 4.8: Flow chart for the program used in stress path testing 94 Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 95 path. The program has the ability to take the specimen from one stress state to the other along a straight hne path. The number of increments needed to accomplish this is prescribed so that the computer could linearly interpolate and determine the intermediate stress states. By increasing the number of increments to reach the final stress state, the stress changes within a single increment will decrease. For all tests reported in this thesis, the maximum change in any stress component over a given increment did not exceed 3 kPa. Pressure control routine governs the incremental changes in the surface tractions to move the stress state along the prescribed stress path. To accomplish a small load increment, the target values of the four surface tractions (viz. external and internal pressures, torque, and vertical load) are calculated. The differences between the current and the target surface tractions are then computed and the number of pulses required to bridge the difference in each regulator is calculated. The pulses are then sent to the stepper motors simultaneously so that all regulators are activated together. Each surface traction is adjusted until the current tractions are within a given tolerance from the target values. The tolerance for the surface tractions were stipulated so that no stress component would deviate more than 0.5 kPa from its target value. After the increment of loading, deformation equilibrium is checked by monitoring the development of strains e , e , e and 7 . The specimen is considered to be in v z T 2t deformation equilibrium if the following criteria for strain rate is satisfied by all strain components: i.e. the change in an individual strain component within a minute, does not exceed 5% of the change in the same strain component within the immediately previous minute. If the specimen has not reached equilibrium, further monitoring is continued. Since the specimen dimensions are updated each time the transducers are read, the control decisions could be based on the most recent configuration of the specimen. Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 96 Once the specimen has reached deformation equilibrium, all data pertaining to the current stress state is stored on the floppy disk and the next loading increment is applied in a similar manner. The performance of the control system is demonstrated in Fig. 4.9 by a typical stress path test. In this test the specimen was loaded under simultaneously increasing stress ratio R and rotation a„ of a[ to vertical while a' and b were held constant (Fig. m 4.9a). This required the magnitudes of all four boundary tractions to be changed in a controlled manner. Figs. 4.9b and 4.9c present a comparison between the desired and the actually obtained values of all stress components. Close agreement between the desired and the actual data points shows the excellent capability of the automatic control system for carrying out generalized stress path tests. 4.3 Specimen preparation 4.3.1 General Considerations In the laboratory, a test specimen is assumed to represent an element of soil at a point in the soil mass. Therefore the method of specimen preparation must promote development of homogeneity within the test specimen. Pluviation is considered to simulate the deposition process and the resulting fabric found in natural sedimentary deposits and artificial deposits such as hydraulic fills (Oda et al., 1978; Miura and Toki, 1984). Laboratory studies on pluviated sands, should therefore give a close indication of the behaviour of these deposits. Furthermore, water pluviation followed by vibration has been found to be the most effective technique of reconstituting homogeneous saturated sand specimens with controlled density (Vaid and Negussey, 1984b). As such, water pluviation was selected as the technique of specimen reconstitution. Chapter 4. UBC HoUow Cyhnder Torsional Device and Experimental Aspects 98 Both the uniformity of the particle size distribution and density across the specimen is simulated by water pluviation if the sand is uniformly graded. Well graded sands tend to seggregate during pluviation, and for these sands an alternative deposition method suggested by Kuerbis and Vaid (1988) has to be used to ensure specimen homogeneity. In this study a uniform sand was used (as will be found in a later section) and therefore the question of seggregation did not arise. 4.3.2 Preparation Procedure The procedure adopted for the preparation of H C T test specimens and the assembly of the U B C - H C T device to carry out testing has been described in detail by Sayao (1989). Since the same procedure was employed in this study, only the important steps are presented herein. Initially a known dry weight (approximately 5 kg) of sand was boiled in several flasks and then left overnight under vacuum. All drainage lines were saturated with deaired water and all the porous stones were boiled and allowed to cool at room temperature. A reference height was established by placing an aluminum dummy specimen of known height between the bottom and top platens. A dial gage mounted on a movable stand was used to obtain a reference reading on the top platen. This reading was later used for determining the height of the sand sample at the end of preparation. An annular hollow cylindrical cavity for the placement of sand was formed using inner and outer split moulds with two matching rubber membranes (0.3 mm thick) stretched over them. The annular cavity was first filled with deaired water, followed by pluviation of sand through water. This process is illustrated in Fig. 4.10. During the pluviation process, the flasks containing the deaired sand were traversed over the annular area of the cavity to achieve an approximately level surface at all times. Except in the case of dense samples, no vibrations were imparted to the sample until Chapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects Figure 4.10: Sample preparation by water pluviation - after Sayao (1989) Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 100 the top platen was placed on the deposited sand after preparation. However, dense samples had to be partially vibrated during pluviation to avoid excessive descent of the top platen during final densification. Once the sand was deposited to a level shghtly in excess of the target height, the pluviation was terminated. Then the top surface of the specimen was levelled to the desired height by siphoning off excess sand using a low suction head as shown in Fig. 4.11. This siphoning method is a convenient means of levelling which minimizes disturbance to the particles underneath. The siphoned sand was oven dried and weighed in order to obtain the actual dry weight of sand in the specimen. The top end platen with saturated porous stones was then placed on the levelled surface. Disturbance of the top surface due to penetration of the platen ribs has negligible effects because of the large dimensions of the sample (Tatsuoka et al., 1983) and also because the loose pluviated sand cannnot become any looser (Vaid, 1983). The sample was then vibrated while monitoring the reference height dial gage, until the target density was reached. A low amplitude high frequency vibrator was used in this densification process and both top and bottom drainage lines were kept open to minimize the generation of any excess pore pressure. Vaid and Negussey (1988) have shown that densification with a small vertical confinement on the top cap promotes a uniform density distribution over the height of the specimen. They have also observed that by this densification technique the possibilty of bedding errors is automatically ehminated, since the top cap smoothly follows the movement of the top suface of the specimen during densification. After densification, deaired water was percolated (with a low gradient) upward through the specimen to remove any air bubbles entrappped between the rubber membranes and the top platen. Then the membranes were sealed to the top platen using O-rings and a vacuum of 20 kPa was immediately apphed to the drainage line at Chapter 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects 101 Figure 4.11: Levelling the upper surface of the sample - after Sayao (1989) Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 102 the bottom of the specimen. This vacuum provided the effective confinement to the specimen during dismantling of the split moulds. With the split moulds removed, the dimensions of the sample (i.e. height, outer and inner circumferences) are obtained. Height was obtained using the measurement on the reference dial gage. A measuring tape was used to determine the outer circumference. Inner cavity area was derived from the volume needed to raise the water level by 50 mm in the inner chamber. The inner and outer diameters of the sample was then computed after correcting for membrane thickness. The top loading cap was then clamped to the top platen followed by the assembly of the cell chamber . The top cross beam was then swung into position and bolted 1 to the reaction frame. The specimen was then raised upward by pressurizing vertical loading piston until the top cap is in contact with the cross beam. Using a bolt and a locating pin, the top cap was anchored to the cross beam, thus arresting both vertical and rotational movements of the specimen top. Internal and external chambers were then filled with deaired water. Special care was taken to ensure full saturation of the inner chamber. The central rod for monitoring vertical displacements was then mounted which also sealed the inner chamber. At the end of assembly, a hydrostatic confining stress of 30 kPa was apppbed undrained to bring the pore pressure to a value above zero. Then by increasing the hydrostatic confining pressure incrementally, the Skempton's B value was determined in several steps to check for saturation. Specimens were considered saturated if B value was greater than 0.98. The specimen was then hydrostatically consolidated to an effective stress of 50 kPa against a back pressure of 200 kPa. Stress path loading reported in this study was always initiated from this 50 kPa reference hydrostatic effective stress state. 1 Refer Figs. 4.1 and 4.2 for details Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 4.3.3 103 Repeatability of Test Results As discussed earlier, it is important to have a specimen preparation procedure which is capable of repheating specimens. Replication of specimens can be achieved only by following identical preparation techniques and test control routines. This aspect was evaluated by repeated testing of several identical samples loaded along identical stress paths. Results from repeated testing of several identical samples in hydrostatic compression are presented in Fig. 4.12. Excellent repeatability may be observed in both volumetric as well as axial strain responses. Results of two identical samples subjected to a stress path with simultaneous increase in stress ratio and principal stress rotation are shown in Fig. 4.13. Considering the small magnitudes of the induced strains, again good repeatability is observed in both volumetric and maximum shear strain response. 4.3.4 4.3.4.1 Experimental Program Material Tested Medium Ottawa sand ASTM-C-109 was used as the testing material in this program. This sand has been extensively used in laboratory research at U B C and elsewhere. Ottawa sand is a rounded quartz sand with a specific gravity of 2.67. The sand is uniformly graded (C = 1.9) and has an average particle size D u 50 of 0.4 mm. The particle size distribution is given in Fig. 4.14. Previous research at U B C has shown that in Ottawa sand the amount of particle crushing under moderate stresses is negligible and thus it could be recycled conveniently for testing purposes (Chern, 1985). Reference maximum and minimum void ratios for the sand are 0.82 and 0.50 respectively. Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects Hydrostatic Effective Stress kPa Figure 4.12: Repeatability of H C T test results in a hydrostatic stress path 104 Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 105 Figure 4.13: Repeatability of H C T test results in a stress path with simultaneous increase of stress ratio and principal stress rotation Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects Figure 4.14: Particle size distribution of medium Ottawa sand 106 Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 107 4.3.4.2 Testing Program A testing program was developed with the main objective of studying the behaviour of sand subjected to stress paths involving simultaneous increase in stress ratio R and rotation of principal stresses a . It was intended to compare the behaviour in stress a paths with simultaneous increase in R and a c with those in which these parameters varied individually. The comparisons of induced strains were aimed at investigating possible stress path independent behaviour that involves principal stress rotation. The stress paths were chosen so that the stress parameters a' , R, b and m were either increasing or remained constant at all times. Stress paths involving decrease of any of the stress parameters are not considered in this study. The testing program composed of three main types of stress paths. The terminology used to identify these stress paths is given below and illustrated in Fig. 4.15. R Path : Stress Path with increasing R while other stress parameters a' , b and a m CT are held constant. a Path : Stress Path with increasing a a while other stress parameters cr' , b and R m are held constant. R - a Path : Stress Path with increasing R and a a while other stress parameters a' and b are held constant. m In order to conveniently identify or make reference to a particular test, each test was given an identification number (Fig. 4.16). This number consist of five characters of which the first is a letter from the alphabet and the remaining four are a sequence of digits from 0 to 9. The first character identifies the series name (eg. all tests in Series A will begin with the character ' A ' ) . The next three characters in the identification number locates the path of the test in the R-a c stress space as illustrated in Fig. 4.16. The fifth character was needed for record purposes only. Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 108 Figure 4.15: Terminology used in identifying a stress path in R-ct stress space a Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 109 Dj. = constant: 0" m = constant: b = constant M001 OC at which rotation Is Imposed R level Identification Series Identification character f*4001 ) *2001 *045 *3002 *1001 90 Figure 4.16: Notation used in identifying a stress path in R-a stress space a Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects 110 The details of the testing program developed to meet the above objectives are given in Figs. 4.17 and 4.18. As mentioned in section 4.3.2, stress path loading of all specimens was initiated from an initial hydrostatic stress state of (r' = 50 kPa. m From this initial stress state, the specimens were hydrostatically consohdated to the prescribed value of cr' . Then R and ot were increased as necessary, while maintaining m c the values of er' and b parameter at constant values. All tests were stress controlled m and carried out under fully drained conditions against a back pressure of 200 kPa. Sand behaviour was examined predominantly at a relative density of 30%. Loose density state was selected because of its greater susceptibihty to deformations due to principal stress rotation. Test Series A (D = 30%, cr' = 300 kPa, and b = 0.5) T m forms the centre of the testing program (Fig. 4.17). All other test series were built around Series A so that the effects of various stress parameters and relative density on sand behaviour could be investigated in a systematic manner. For example, test Series E and C were complimentary to A , and were conducted to examine the effect of b parameter on behaviour in test Series A . Similarly test Series K and M were performed to investigate the effect of mean normal stress. The behaviour of medium and dense sand was investigated by conducting test Series I and O. In each test series, deformation response under principal stress rotation was studied at several constant R levels (as illustrated by the right hand side diagram of each series in Figs. 4.17 and 4.18). This was necessary in order to investigate region of possible stress path independent behaviour in R - a a space. Some specific tests were carried out in order to supplement and generalize the characteristic behaviour observed from the main testing program. The stress paths imposed in these tests are illustrated at the bottom of the Fig. 4.18. Test O A B C D was carried out in order to examine deformation behaviour under a multi-linear stress path in R - OLC space, and test A B was intended to investigate the deformation behaviour under simultaneous variation of three stress parameters cr' ,R, and a m a as opposed to Chapter 4. UBC HoUow Cyhnder Torsional Device and Experimental Aspects to d _ A4001 K A3002 ^ A1001 < § A2001 , 1 CO LU CC lil CO 30 46 60 a . Duo id CO d (X.Dag E3001 E2001 CO UJ cc 111 II o d 111 CO C3001 C2001 o CO UJ cc UJ CO II s K3001 II K2001 CO UJ cc UJ CO d II M3001 M2001 CO UJ cc UJ CO Figure 4.17: H C T testing program - (contd. next page) 111 er 4. UBC Hollow Cylinder Torsional Device and Experimental Aspects Figure 4.18: H C T testing program (contd. from previous page) Chapter 4. UBC Hollow Cyhnder Torsional Device and Experimental Aspects only two parameters R and a in other series. c Chapter 5 Results and Discussion 5.1 Introduction This chapter presents a detailed examination of the results obtained from the testing program outlined in Chapter 4. Initially, the stress strain behaviour of medium loose Ottawa sand, subjected to stress paths wherein only one stress parameter is varied at a time is presented. These constitute loading under: hydrostatic paths, R paths and a paths . In R paths the stress ratio is increased while other stress parameters 1 a' , b and a m a are held constant. In a paths the principal stresses a[ and cr' are 3 continuously rotated while a' , b and R are held constant. Effects of the levels of R, m b and a-' in a tests are systematically assessed. The behaviour under similar stress m paths is then examined for different material densities. Deformation characteristics under these stress paths are essential (i) to examine the inherent anisotropic nature of pluviated sand, and (ii) to form a data base for possible prediction of strain response under loadings involving simultaneous increase of several stress parameters, treated as superposition of events in which only one parameter increases. Then, a comprehensive investigation of sand behaviour under stress paths involving simultaneous increase of stress ratio and principal stress rotation (R - a tests) is presented. This is the main objective of this thesis. Initially, stress paths with hnear variation of R versus a are considered. The effects of the levels of a' , b and relative a m density D in R - a path loading are investigated separately in a systematic manner. r Possible stress path independence of deformations is initially assessed by comparing 1 terminology as defined in Chapter 4. 114 Chapter 5. Results and Discussion 115 deformations from linear R - a paths with those obtained from increase in R alone and OL0 alone, at common terminal stress states. Such path independence of strain response is also examined at intermediate stress states with the aid of a tests carried out at lower R levels. The influence of stress path history on the deformations along a common principal stress rotation path is also investigated. Behaviour under a multi-linear R - a path is examined in order to encompass general R - a paths. Finally, deformation response is studied under stress paths involving simultaneous increase in three stress parameters at a time. Only those stress paths involving increasing values of stress variables (total loading paths) are considered in this thesis. A l l stress path tests were initiated from the reference hydrostatic stress state of 50 kPa . The deformations are presented in 2 terms of volumetric (e %) and maximum shear strain (7 v moa: %) responses. In chapter 3, it was shown that the stress non-uniformities in the H C T specimen are much smaller than those estimated previously based on linear elasticity (Sayao, 1989). Therefore a much larger domain of stress space could be explored without introducing unacceptable non-uniformities than considered in previous investigations. The stress non-uniformity coefficient J3R rarely exceeded 0.1 in the region of stress space explored. 5.2 Fig. Hydrostatic Loading 5.1 presents typical stress-strain response under hydrostatic compression of medium loose Ottawa sand. The associated strain path is given in Fig. 5.2. Shear strains during hydrostatic loading arise as a consequence of the vertical strain smaller than the horizontal. This implies inherent anisotropy typical of water deposited sand (El-Sohby and Andrawes, 1972; Negussey, 1984). A linear strain path between horizontal and vertical strains suggests that the degree of anisotropy is preserved during 2 N.B. b and o. are undefined and R = 1 at a hydrostatic stress state a E 0.05 4 50 100 150 200 250 300 Hydrostatic Stress kPa Figure 5.1: Stress-Strain response under hydrostatic loading of medium loose Ottawa sand Chapter 5. Results and Discussion Figure 5.2: Strain path in hydrostatic loading of medium loose Ottawa sand 117 118 Chapter 5. Results and Discussion hydrostatic loading (El-Sohby and Andrawes, 1973). Strain paths under hydrostatic loading for three different relative densities are shown in Fig. 5.3. With increasing relative density, the degree of inherent anisotropy decrease. Similar observations have been made by El-Sohby and Andrawes (1972). For dense sand (D — 70%) the ratio of horizontal to the vertical strain approaches T unity, indicating close to isotropic behaviour. These results are in agreement with those reported by Negussey (1984) for hydrostatic loading of Ottawa sand using the conventional triaxial device. 5.3 Deformation Under Increase in a Single Stress Parameter 5.3.1 Shear Loading of Loose Sand with Fixed Principal Stress Directions (R Paths) 5.3.1.1 Stress Strain Behaviour Figure 5.4 presents results of three R tests on medium loose Ottawa sand at a. = 0, a 45 and 90 degrees. All samples were initially consolidated to a hydrostatic stress a' m — 300 kPa. Stress ratio R was then increased at constant a while values of a' and b c m were held constant at 300 kPa and 0.5 respectively (R paths A3002, A0451 and A0901 in Fig. 5.4). A marked dependence of deformations on the direction of loading may be noted. The shear stiffness is greatest when major principal stress cx' is coincident with x the direction of deposition [a. = 0°). With increasing a both volumetric and shear a a deformations increase, affirming the inherent anisotropic nature of the pluviated sand. These results support the findings on the anisotropy of pluviated sands by previous researchers. (Sayao, 1989; Symes et al., 1982; Arthur and Menzies, 1972; Yamada and Ishihara, 1979; Oda, 1972 and 1976). Chapter 5. Results and Discussion Figure 5.3: Effect of relative density on strain paths in hydrostatic loading Chapter 5. Results and Discussion D r = 30 % : $ ' = 300 k P a m , : b = 0.5 0.4 -| Stress Ratio R Figure 5.4: Effect of ct on the stress strain behaviour in R paths a Chapter 5. Results and Discussion 5.3.1.2 121 Direction of Strain Increments and Strain Paths For R tests with ov = 0° and 90° (i.e. tests A3002 and A0901) the principal stress and stress increment directions coincide with the axes of anisotropy. Hence the directions of principal stresses and strain increments coincide. Major principal strain increment directions and the stress increment direction for the R test A0451 (with a = 45° c = 45°) are presented in Fig. 5.5. It may be noted that the direction of strain increment is close to that of stress increment direction a^, with a shght bent towards the bedding plane (i.e. horizontal direction). The results are in agreement with those observed by Sayao (1989) and Symes et al. (1982 and 1988). Since-the strain increment directions a& throughout R paths A3002 and A0901 is c constant at 0° and 90° respectively, and in R path A0451 is also essentially constant (= 47°), the directions of cumulative principal strain vectors in these paths would also remain unchanged. Fig. 5.6 gives the cumulative principal strain paths for the R tests. Initially linear strain paths can be observed regardless of the direction of a . This indicate that under directional shear, the inherent anisotropy is preserved ff in the small stress ratio region R < 2. Similar observations of inherent anisotropy have been made by Negussey (1984) and Sayao (1989). 5.3.2 Principal Stress Rotations on Loose Sand at Constant R, b and a' (a Paths) m 5.3.2.1 Effect of R Level In these tests the rotation angle was varied continuously while values of R, b and a' were held constant. All tests were initiated with samples isotropically consolidated to 300 kPa, and then sheared under identical a. — 0°, b — 0.5 and a' — 300 kPa, c m until specified values of R = 1.35, 1.65, 2.0 and 2.5, prior to principal stress rotation er 5. Results and Discussion 90 2.0 R o 1.0 0 CD D <^5 o to ^5 to 50 H • o o ° o 45 a „ Deg 0 " JL D D 0 • o • D D D • 40 PI 30 « (Y - 4 5 Deg 20 S 10 0 1.2 1.4 1.6 1.8 Stress Ratio R Figure 5.5: Strain increment directions in an R path with ct„ = 45 Chapter 5. Results and Discussion Figure 5.6: Strain paths in directional shear loading Chapter 5. Results and Discussion 124 from 0° to 90° (Tests A1001, A2001, A3002 and A4001). The selection of R values particularly encompassed behaviour under principal stress rotation at moderate as well as low R. Behaviour at stress ratios as high as 2.5 can be confidently examined because stress non-uniformities across the specimen wall would still be acceptable (Chapter 3). Stress Strain Behaviour Volumetric and maximum shear response due to principal stress rotation in a paths on medium loose Ottawa sand are shown in Fig. 5.7. Principal stress rotation induces contractive deformation that increases with irrespective of the level of R. For a given a , the volumetric strain increases with the level of R. Similar comments CT apply to the development of 7 x • ma The rate of strain development due to principal stress rotation increases with increasing R for a given value of ct^, and for a given stress ratio, it is dependent on the current value of a„. The volumetric strain rate with respect to ct for a given R is a enhanced further as the major principal stress direction moves from vertical (a a — 0°) towards the bedding plane (ov = 90°). A similar trend may be noted for the rate of change of maximum shear strain with respect to a a until a a % 60°. However, for rotations involving ct greater than about 60°, there is a gradual drop in the rate of a maximum shear strain development. In Sayao's (1989) a tests, a a was limited to 60° and therefore no such drop in the rate of 7 x with respect to a. was reported. This ma indicates that the observations at lower a a a do not necessarily reflect the behaviour at larger values of principal stress rotation, and extrapolation of data from lower a a to larger a a should be carried out with caution. The nature of deformations in a tests have an important implication on the undrained behaviour of anisotropic sands. Contractive deformations under drained conditions suggest significant pore pressure increase under undrained conditions and hence possible liquefaction or large deformations. This concern become more crucial Chapter 5. Results and Discussion Figure 5.7: Effect of R level on deformation due to principal stress rotation 125 Chapter 5. Results and Discussion 126 as the stress ratio increases because of increased contractive deformations that would accompany a given amount of principal stress rotation, as shown in Fig. 5.7. Direction of Principal Strain Increment Figure 5.8 shows the direction of major principal strain increment ot&. in response c to a loading. Since stress parameters <r' , b, and R are fixed and only the direction of m CT\ changes, the direction of the imposed stress increment must lead the current direction of principal stress a by 45° (Ishihara and Towhata, 1982). This condition is a closely achieved by the stress path control as shown in Fig. 5.8. For lower stress ratios R < 2, at the beginning of the rotation ( a ^ a ss 45°) the strain increment direction «Ac is close to a^o-- As the rotation progress, strain increment direction deviates away from stress increment direction a ^ , , and moves closer to the direction of major principal stress OL„ for rotations up to 90°. The observed trend in strain increment direction a^ c is also dependent on the level of stress ratio R. At higher R values, there is a larger deviation between and a ^ , even at the beginning of rotation. rotation, become much closer to a a Also, with increasing principal stress at higher R, when compared to that under lower R. Similar results have also been experimentally observed by Sayao (1989) and Symes et al. (1988) on rotation tests carried out to limited ranges of a^. These observations will be examined again in a later section (section 5.4.1.2) in conjunction with the results under stress paths involving simultaneous increase in R and a^. 5.3.2.2 Effect of b Parameter Stress Strain Behaviour Deformations in a tests similar to those described in section 5.3.2.1 at R = 2 level, but now with b = 0.0 and b = 0.3 are shown in Fig. 5.9. Results for test A3002 with b — 0.5 in Fig. 5.7 are also included. There appears to be no significant influence of the intermediate principal stress parameter on the volumetric strain development Chapter 5. Results and Discussion Figure 5.8: Effect of R level on the direction of strain increment 127 Chapter 5. Results and Discussion 128 Figure 5.9: Effect of b parameter on deformation due to principal stress rotation Chapter 5. Results and Discussion 129 regardless of OL„ . However, significant differences may be observed between maximum shear strain ( 7 m a x ) induced for a given value of a . Sayao (1989), based on his a principal stress rotation tests which were carried up to a a = 60°, concluded that effect of b parameter on strain response under a paths is insignificant. The results in Fig. 5.9 however indicate that although this influence is less significant at smaller a , it does become accentuated at larger values of a. . a a Direction of Strain Increment Figure 5.10 shows the effect of b parameter on the relation between the directions of stress increment, strain increment and stress. The direction of the strain increment a^j seems to be unaffected by the magnitude of b parameter. Thus for any given a , , b parameter may be considered to have small effect on strain directions during rotation of principal stresses. 5.3.2.3 Effect of Mean Normal Effective Stress Stress Strain Behaviour Figure 5.11 presents results of a tests at R — 2 and cr' levels of 100 and 200 kPa, m but otherwise identical to those described in section 5.3.2.1. The response under a' m = 300 kPa (test A3002, Fig. 5.7) is also reproduced. Deformations due to principal stress rotations increase with increasing mean normal stress level. This is consistent with the generally observed behaviour of granular materials, which show increased contractive and deformable response under increasing confining stress levels. Direction of Strain Increment The direction of strain increments are presented in Fig. 5.12. Despite significant effects of a' on the magnitudes of volumetric and maximum shear strains, the strain m increment direction a.& is relatively unaffected by the level of <r' . c m Chapter 5. Results and Discussion Figure 5.10: Effect of b parameter on the direction of strain increment Chapter 5. Results and Discussion Chapter 5. Results and Discussion Figure 5.12: Effect of <r' on the direction of strain increment 132 133 Chapter 5. Results and Discussion 5.3.3 Response to a Loading at Higher Relative Densities Samples with D = 50% and 70% were subjected to a paths identical to that for r specimen A3002 at D = 30% in Fig. 5.7. Thus stress state of the samples was T a' — 300 kPa, b = 0.5 and a„ = 0° prior to principal stress rotation at R = 2. m 5.3.3.1 Stress Strain Behaviour Both volumetric and shear deformations shown in Fig. 5.13 decrease markedly with increasing relative density. This is due to the reducing degree of inherent anisotropy of sands (getting closer to becoming isotropic) under increasing packing density, as demonstrated in Fig. 5.2. As a result, principal stress rotations induce less deformations in dense sand. Regardless of density state, the volumetric strains are contractive and increase with increasing principal stress rotation. At higher density levels, however, the value of maximum shear strains (7 x) increases up until a value of a ma rotation of principal stresses beyond 70°, 7 m a x CT % 70°. With further starts to decrease indicating a stiffening of the distortional mode of deformation. 5.3.3.2 Direction of Strain Increments Possible cause behind the decrease in distortional strains at higher a is revealed by examining the directions of strain increments a^ denser sand, a& initially is close to a^ . c a c as shown in Fig. 5.14. For As rotation builds up, a& moves closer e to ctg-. However, with further increase in rotation this trend is changed once again, and a^ starts to come closer to ct^. Since ~f ax — £i m — £3 is a vector quantitj , r both magnitude and directional changes in incremental strains A e i and A e , govern 3 increase or decrease in ^m - Consequently, the observed decrease in 7 x at larger ax a a ma can be attributed to the changing trend in the direction of major principal strain Chapter 5. Results and Discussion Figure 5.13: Effect of D on deformations due to principal stress rotation T Figure 5.14: Effect of D on the direction of strain increment T Chapter 5. Results and Discussion 136 increment shown in Fig. 5.14. 5.3.4 Stress Path Dependence of Deformations In loading of medium loose sands along R and a paths under fixed <r' — 300 kPa m and b = 0.5 (sections 5.3.1 and 5.3.2), stress state (R, a) — (2, 45°) is common to R 3 paths A0451 and a path A3002, and the state (2, 90°) is common to R path A0901 and a path A3002 (Fig. 5.15). Likewise, stress states (1.65, 45°), (1.65, 90°), (1.35, 45°) and (1.35, 90°) can be identified as points of intersections of R paths A0451 and A0901 with a paths A2001 and A1001. It would be of interest to examine stress path dependence of deformation, by comparing deformations accumulated at these common stress states arrived through different stress paths. Figure 5.15 shows comparison of volumetric and maximum shear strains developed in R paths with those in a paths in medium loose sand. A close match for both volumetric strain e and maximum shear strain "f x may be noted at common stress v ma states (2, 45°), (1.65, 45°) and (1.35, 45°), indicating path independent stress strain behaviour. Note, that strains in a paths must include strains developed during R loading from the starting R = 1 state. At the common stress state (2, 90°), (1.65, 90°) on the other hand, the volumetric as well as maximum shear strains developed through a paths of test A3002 and A2001 respectively are significantly higher than those along R path A0901. This can be explained in terms of the effects of continuous principal stress rotation on deformations, w hich become much pronounced at higher r R and a a levels, as observed in Fig. 5.7. a paths A3002 and A2001 experiencing continuous principal stress rotation over the full range of 90° are more prone to development of strains, than path A0901, which involves no principal stress rotation at all. This leads to a wider difference between strains at the common stress points (2, 90°) and (1.65, 90°). Coordinates (R, a„) in the stress space. Chapter 5. Results and Discussion D (J =30% r b-= 0.5 Q Ft S - A2001 P A09C A3002 0.4 : m 0.5 2.0 = 300 kPa 7 A1001 I' U T 0.3 - 1.0 / / 90 46 ,x x 4 i 0.2 D° O S /: ,0' 0.1 X X X , ++ ++ + -H t V i + ++++' It X IH- + 0 -II- • A3002 x A2001 + A1001 « A0451 A A0901 Arrows Indicate common points for R paths 0.5 D O o ° xx x o x * x X XX' xx XXX XXX xxl x i. t v -Six xxx xxx ,+ ++ + + + 0 + L xx 1)0 + + + + + +++ + + ++ + + + ++ + + + T 20 40 60 t I 60 a Deg ff Figure 5.15: Stress path dependence of deformations from R and ct tests Chapter 5. Results and Discussion 138 The deformations at common stress state (1.35, 90°) show less significant path dependence when compared to those observed at higher R levels at a c = 90°. This can be expected, since the deformations due to principal stress rotations are small at lower levels of stress ratios. 5.4 Deformation Under Simultaneous Increase in Stress Ratio and Principal Stress Rotation Under constant levels of b and a' it is possible to impose simultaneous increase in R m and a. along any arbitrary path in the R - OL„ space. A comprehensive investigation a was made of deformation under hnear R - a paths. A limited study was also carried out under a multi-linear stress path in the R - a a space. Effects of levels of b and a' m during hnear R - a paths and of relative density under identical hnear R - a paths was also investigated. Possible path independence of deformations is initially assessed by comparing strains from a paths with those from R - a paths at common terminal stress states. Later, the investigations on possible path independent deformation response are extended to cover intermediate stress states in R - a domain. CT 5.4.1 Behaviour of Loose Sand under Linear R - a Paths Samples of medium loose Ottawa sand ( D = 30%) were loaded along several hnear r R - a paths under constant b = 0.5 and cr^ — 300 kPa (test Series A ) . Each sample was subjected to a stress path which had two phases. In the first phase R and ov were increased simultaneously in a hnear manner (i.e. R - a path). This phase ended when the stress ratio R reached a target value of 2.0. Tests in this series differed from each other by the fact that the slope of R - a path was different in each test. As such, the first phase of the tests A3301, A3451, A3601 and A3901 ended at a , = 30, Chapter 5. Results and Discussion 139 45, 60 and 90 degrees respectively (Fig. 5.16). At the end of the first phase (after reaching R — 2) all samples (except A3901) were subjected to continuous principal stress rotation upto ct^ = 90°, while the values of cr' , R and b were held constant at m 300 kPa, 2.0 and 0.5 respectively. This made the second phase of the tests to be of type a and coincident with the a path of test A3002. 5.4.1.1 Stress Strain Behaviour Figure 5.16 shows the effect of the slope of R - a path on deformation response of medium loose Ottawa sand. Contours of constant R values are also drawn on the same plot to highlight the effects of mobilized stress ratio. For a given value of ov, sand in which higher stress ratio is mobilized accumulates larger strains. Deformations at low mobilized R (< 1.5) may be seen to be dependent on R only and largely independent of principal stress rotation a of up to about 30°. a These observations are consistent with the deformation response observed from principal stress rotation tests with constant R, b and a' in Fig. 5.7, wherein the m effect of R on the deformations due to principal stress rotations were found to be more pronounced at higher R levels. 5.4.1.2 Direction of Strain Increment The direction of strain increment a ^ in linear R - a paths is given in Fig. 5.17. Unlike c a paths where direction of stress increment leads a by 45°, in R - a paths a& G initially assumes a value close to ct . With increasing rotation, a diverges more and more from a . c The direction of strain increment crement a A c r until a A ( 7 essentially coincide with that of stress in- approaches approximately 45°. This trend may be noted for all the R - a paths, even though in each stress path the values of R and a are a continuously changing in a different manner. For a^ > about 45°, strain increment a a Chapter 5. Results and Discussion D =30% : (J "=300kPa m : 7 b«=0.5 0.5 A3002 0.4 H R R «2.0 0.3 0.2 O O 0.1 H o A A A 1 v - x " - - R - 1.65 35 o * + A3301 o A3451 A A3601 X A3901 R = 2.0 O£ A A 0.5 s O + O A " V * - * - - R = 1.65 •<S A •X • XX R = 1.35 1 20 40 1 i 60 80 Figure 5.16: Stress strain behaviour under hnear R - a loading er 5. Results and Discussion Figure 5.17: Direction of strain increment under linear R - a loading Chapter 5. Results and Discussion 142 direction gradually deviates from stress increment direction and moves closer to the direction of stress. It is of interest to examine these results which contrast with the observations from continuous principal stress rotation tests with fixed R, in which the strain increment direction a& was markedly influenced by the level of stress ratio e (Fig. 5.8). It is also important to note that in a paths (where 0° < a. < 90°), the a applied principal stress increment was always in the region of 45° < a^ ff < 135°. These findings suggest that the direction of strain increment a& is almost totally dec termined by the direction C K A ^ , if the applied stress increment direction a.\ is inclined a between 0° and 45° (i.e. closer to the direction of deposition). On the other hand, more the direction of the applied stress increment is inclined closer to the bedding plane (i.e. > 45°), the direction of strain increment appears to be influenced not only by but also by the effects of other parameters such as R and a„. 5.4.1.3 Stress Path and Stress History Dependence of Deformations (R - a Paths versus a Paths) Linear R - a paths A3301, A3451, A3601 and A3901 intersect a path of test A3002 at a c = 30, 45, 60 and 90 degrees respectively at common stress points (Fig. 5.18). Strains developed during loading until common stress states (R, a^) = (2, 30°), (2, 45°), (2, 60°) and (2, 90°) along R - a and a paths are shown in Fig. 5.18. It may be noted that excepting in test A3901, both volumetric and maximum shear strains that develop along the two paths, match closely at the common stress states. This reflects a stress path independent deformation behaviour. In the case of test A3901, the strains developed at — 90° along R - a path are significantly less than those accumulated along a path in test A3002. In test A3002 principal stress rotations occur from a a = 0° to 90°, at R = 2 throughout rotation. In test A3901 however, principal stress rotations from 0° to 90° occur while R varies linearly with a from 1 to 2. As such, along path A3901 stress rotation 0° - 90° occur a Chapter 5. Results and Discussion D 143 =30% : (J =300kPa / r : b = 0.5 m 0.5 A A, A3002 0.4 AQ. 0.3 _4° CA_> 0.2 A D ^ 1 n . + O D 0.1 3°V DO' <>v A + DO xxx E 0.5 o A3002 + A3301 o A3451 A A3601 x A3901 A XX' A ^ > 0 4 0+ 0 A + • 3 AD DO ' ion' + o 20 0 D + o A ^ A + O A O A v 1 40 I 60 — r~ 80 a Deg a Figure 5.18: Stress path dependence of deformations under principal stress rotation - Test Series A 144 Chapter 5. Results and Discussion with R always < 2. Since strain development increases with R level at larger values of a , sand in test A3901 which has little exposure to high R values would develop c less strains compared to A3002 which has R = 2 throughout principal stress rotation of 0 to 90 degrees. The foregoing observations therefore suggest that the deformations under stress paths with increasing R and a a are essentially path independent upto a stress ratio of 2, if the rotations are moderate (about less than 60 degrees). Under larger principal stress rotation, the deformations gradually become path dependent. observations by Symes et al. (1988) from loadings where R and a a Limited was increased in a sequential manner indicate similar path independent behaviour for Ham river sand. The concept of a state boundary surface (BS) by Symes et al. (1984, 1988) and Shibuya and Hight (1987) imphes that for "loading" paths, the path independence of deformation should be observed for rotations up to a = 90°. Test results on Ottawa a sand in Fig. 5.18, however do not support this contention at larger values of a . a Once hnear R - a phases of tests A3301, A3451, A3601 have been terminated at R — 2, the tests follow an a path identical to that of test A3002 (Fig. 5.16). Deformation behaviour in these common a phases of tests A3301, A3451 and A3601 are also presented in Fig. 5.18. It may be noted that the stress strain characteristics of the a phases of tests A3301, A3451 and A3601 closely agree with that of test A3002. This suggest that not only deformations are path independent for loading until a given stress state, the history of previous stress path loading also has no influence on the deformations along a subsequent common stress path. Effect of Stress Ratio Deformations in linear R - a path A4451 terminating at R = 2.5 and a ff = 45° are compared with deformations in a path A4001 at R = 2.5 in Fig. 5.19 for medium loose Ottawa sand. The values of (r' , b and D for these two tests were 300 kPa, m T 0.5 and 30% respectively, identical to those for the tests described in the previous Chapter 5. Results and Discussion D -=30% : (J -300kPa / : b-= 0.5 m 0.5 A4001 0.4 H R 0.3 90 02 0.1 moo DO 0<> 00 oo $ O 0> 0 42 1.5 c§ E • A4001 o A4451 1 H 0.5 H oo rio 0« Jl 0 o * O O «> <f>0 oo oo< —r- 40 20 a Deg ff Figure 5.19: Stress path dependence of deformations at higher stress ratios Chapter 5. Results and Discussion 146 section. At the common stress state (R, a ) = (2.5, 45°), the strains accumulated c through test A4001 are significantly higher than those developed in test A4451. This difference cannot possibly be attributed to higher stress non-uniformities within the specimen at R = 2.5, since /3R is quite low even at this level of stress ratio. It appears that path independent deformation behaviour observed at lower mobihzed R levels will not extend to R levels larger than some threshold value. The results presented so far suggest that loading along stress paths which include principal stress rotations exhibits path independent behaviour, provided principal stress rotations and mobihzed stress ratios are held below certain threshold values. In order to establish these threshold bounds precisely, extensive stress path testing need to be done in R - a space. Nevertheless, based on the test results presented for a medium loose Ottawa sand, it can be concluded that path independent deformation response is found for stress states defined by <r' = 300 kPa; b = 0.5; 0° < a m a < 60° and R < 2. Strain and stress increment directions during test A4451 are given in Fig. 5.20. Approximate coincidence of stress and strain increment directions may still be observed for a& < 45°. With increasing rotation, the direction of strain increment a& a e moves closer and closer to the major principal stress direction a . These results are CT similar to the observations on strain increment directions given in Fig. 5.17 at lower levels of R. It is to be noted that the above observations have been made from a test series with values of intermediate principal stress parameter b and mean normal effective stress a' m fixed at 0.5 and 300 kPa respectively. Furthermore, the results were restricted only to medium loose Ottawa sand. Stress path independence at other values of b parameter, a' and relative density D is examined in the next sections. As noted earher, it is not m T practical to perform a large number of tests in order to establish precisely the domain of path independent strain response. Therefore, in the following sections possible Chapter 5. Results and Discussion 147 Figure 5.20: Direction of strain increments under linear R - a loading leading to higher stress ratios Chapter 5. Results and Discussion 148 path independence is investigated predominantly within the bounds of R < 2 and OL < 45°. These bounds were chosen mainly because most field situations are likely C to fall within these stress ranges under general loading conditions. 5.4.2 Effect of b Parameter during R - a Loading of Loose Sand In order to investigate possible path independent behaviour under different b parameters, two additional series of tests were performed at fixed b values of 0.3 (Series E) and 0.0 (Series C) respectively (Fig. 4.17). Except for the difference in b values, the tests in each series were conducted at identical fixed values of = 300 kPa, and D — 30%, the conditions identical to those imposed in Series A . Somewhat lesser T number of linear R - a paths were explored when compared to those in Series A . All R - a paths in Series E and C were such that once a stress ratio of 2.0 was reached, further loading was carried along the a path of tests E3001 and C3001 respectively. 5.4.2.1 Stress Strain Behaviour Deformation response under a selected R - a loading on medium loose Ottawa sand at three different levels of b, but identical a' m = 300 kPa (paths A3451, E3451 and C3451) is presented in Fig. 5.21. The b parameter does not appear to influence deformations in a significant manner for the selected R - a path in which maximum values R and a„ are limited to 2 and 45° respectively. These results regarding the influence of b on deformation are consistent with those observed under a paths within a similar domain of R and a , (Fig. 5.9), and also in previous findings of Sayao (1989). However, it is cautioned that the effect of b' level could be significant if principal stress rotations are relatively large. Chapter 5. Results and Discussion 149 Figure 5.21: Effect of b parameter on the behaviour under linear R - a loading Chapter 5. Results and Discussion 5.4.2.2 150 Direction of Strain Increment Directions of stress and strain increment for the same stress paths considered in the previous section are plotted in Fig. 5.22. There is no significant effect of b parameter on the direction of strain increment a^ . A near coincidence of stress and e strain increment directions occurs in the domain of 0° < a^ ff < 45°. When exceeds approximately 45°, the direction of strain increment tends to move gradually towards the direction of major principal stress a . These results support further the c observations in Figs. 5.17 and 5.20. that if a is closer to the direction of deposition, Ao- ~ Ac regardless of the current values of R and a . a a 5.4.2.3 Stress Path and Stress History Dependence of Deformations Figure 5.23 compares deformations along R - a stress paths (Series E) with those along a paths at common stress states for fixed b value of 0.3. The strains developed along linear R - a stress paths of tests E3301 and E3451 match closely the strains accumulated along a path of test E3001 at the common stress states (R, a ) = (2, a 30°) and (2, 45°). Thus path independence of deformations is also noted under a b value of 0.3. R - a loading along path E3901, however resulted in significantly lower deformations when compared with that along a path of test E3001 at the common stress state (R, ov) = (2, 90°). Therefore, hkewise the results in test Series A , for paths involving larger rotations of principal stresses (Fig. 5.18) the behaviour gradually changes from path independent to path dependent. Figure 5.24 which presents results similar to those in Fig. 5.23 but under b = 0.0 (Series C), also shows essentially identical deformations at common stress points regardless of the stress path. Thus, deformations are path independent in the domain R < 2.0 and 0° < a < 45°. c Figure 5.22: Effect of b parameter on the direction of strain increment in hnear R a loading Chapter 5. Results and Discussion D 152 =30% : (J =300kPa 7 : b = 0.3 m 0.6 E3001 2.0 R •// i/fy*^ > / 1.0 / 0 1 1 1 30 -tLo<° | ! 1 0.4- 90 46 • C O HO! 0 A A 0.2 A + W° « / 0 A A A ^ 4 E3001 E3301 E3451 o E3901 A 3 •+ E • ° « o + o + 0.5 9 + a / rj O + « 0 0° + + TP o 4 + + 41D A AA -1— 20 o O O aA A A ' ~~l— 40 ~1— 60 i 80 a Deg a Figure 5.23: Effect of b parameter on stress path dependence of deformations - Test Series E Chapter 5. Results and Discussion D 153 =30% r : ff 7 m = 300kPa : b = 0.0 0.6 (I C3001 + * + n 0.4 + CP 90 C o + 0.2 •tf n D D D 0 D n O V J D O 0 O 4 ^ * 4' * 0+0*0+0° 1.5 C3001 3* -t C3301 o C3451 1 •o +o 3 E B 0.5 0°+ ,D • D U T a O O 1 + + 0« o — I 20 40 60 80 Figure 5.24: Effect of b parameter on stress path dependence of deformations - Test Series C Chapter 5. Results and Discussion 154 Tests E3301 and E3451 (b — 0.3) after reaching R = 2 follow an a path identical to that of test E3001 (Fig. 5.23). The sand response along common legs of these a paths of tests E3301, E3451 and E3001 are nearly identical. This imphes that R - a path stress history has no influence on the subsequent deformation behaviour. A similar, essentially stress history independent behaviour may be noted from test results of Series C (6 = 0.0) illustrated in Fig. 5.24. 5.4.3 Effect of a' during R - a Loading of Loose Sand m Two series of tests with a' = 200 kPa (Series M) and a' — 100 kPa (Series K ) were m m carried out to examine the influence of a' . A constant value of b = 0.5 and a medium m loose condition (D = 30%) for the density was chosen for these two series so that T the results from Series A (which also had a b parameter equal to 0.5 and D ~ 30%) T could be conveniently supplemented. For both the series, only one R - a path moving from (R, a ) = (1.0, 0°) to (2.0, 45°) (tests M3451 and K3451, see Fig. 4.17) was a considered in order to investigate possible path independent strain response. 5.4.3.1 Stress Strain Behaviour The strain response under identical R - a paths, but different cr^ values (paths A3451, M3451 and K3451) is presented in Fig. 5.25. It may be noted that for a given R - a CT state, volumetric and shear strains induced in the sand increase with increas- ing mean normal stress cr^. This behaviour is consistent with observations made from a paths (Fig. 5.11), and also with the generally observed granular material behaviour reflecting increasing contractancy and shear deformability with increasing confinement. -Chapter 5. Results and Discussion 156 Chapter 5. Results and Discussion 5.4.3.2 Direction of Strain Increment The dependence of strain increment direction a& , on a' level during R - a paths is c m illustrated in Fig. 5.26. There seems no noticeable effect of mean normal stress state on a Ac- Coincidence of stress and strain increment directions observed for a < 45° Acr in the previous sections, still remain unaltered even under different values of cr' . Thus m the direction of strain increment a^c is coincident with and totally governed by the direction of stress increment, regardless of the values of R, b, cr'^ and a , provided ff a Aa < 45°. 5.4.3.3 Stress Path and Stress History Dependence of Deformations The comparison of strains induced through different stress paths for Series M (a' = 200 m kPa) is presented in Fig. 5.27. The deformations accumulated through stress path M3451 very nearly agree with those observed from stress path M3001, thus exhibiting a path independent strain response at a stress state of (R, a ) = (2.0, 45°). A n a identical behaviour pattern is revealed from the comparison of results of tests K3001 and K3451 (Fig. 5.28) at a' = 100 kPa. m These observations when considered along with the previous results from test Series A , E and C, it is possible to arrive at a very general conclusion with regard to path independent deformation behaviour of medium loose Ottawa sand. The conclusion is that, the deformation behaviour of medium loose Ottawa sand under increasing and R ("total loading") is path independent irresepective of the values of b parameter or a' , provided the final stress conditions are within the domain of m R < 2.0 and 0° < a , < 45°. Moreover, the stress strain behaviour under a paths subsequent to the R - a paths of tests M3451 and K3451 tend to closely follow the results from a paths of Figure 5.26: Effect of a'^ on the direction of strain increment in linear R - a loading Chapter 5. Results and Discussion D -30% 158 : fi 7 r 0.4 «200kPa : b - 0.5 m M3001 5b CP 0.3 H • 90 > 0.2 • ^o • o o o 0.1 0 0 ° ° 0 -*p ~i i ° 1 1 1 i 1 r <p#>, 0.8 • M3001 © M3451 on 0 OD 0.6 3 E 0.4 • . • 0-2 - i a o o o o t 0 -f 1 | D D O ° D DO o D i 20 1 1 1 40 i 60 i i 80 a Deg a Figure 5.27: Effect of er^ on stress path dependence of deformations - Test Series M Chapter 5. Results and Discussion D -=30% 159 : (T 0.3 H «100kPa 7 r : b = 0.5 m K3001 • • o °0 0.2 H 90 , D o° of* 0.1 A • • • • D O J] o • o [] o 0.6 u DO o 0 oo o —~~\ 1 1 1 1 1 1 r oo<j o D K3001 o K3451 o_ o Do 0.4 H OS CP 3 E •o 0.2 0« —I 20 1 1 1 40 1 60 i r— 80 a Deg a Figure 5.28: Effect of c' on stress path dependence of deformations - Test Series K m 160 Chapter 5. Results and Discussion tests M3001 and K3001 respectively, thus indicating no effect of stress path history (Figs. 5.27 and 5.28). These results corroborate the previous findings from test series A, E and C, that for increasing R - a paths, deformations at a given stress state is determined by the current (R, ov) value and not by the actual path taken to reach that stress state. 5.4.4 Response to R - a Loading at Higher Relative Densities In order to examine the influence of packing density on stress strain behaviour under hnear R - a paths, two tests were conducted with initial relative densities of 50% (test 13451) and 70% (test 03451) respectively. Both samples were initially isotropically consolidated to 300 kPa and then subjected to an R - a path (as shown in the key diagram of Fig. 5.29), with b and er' held constant at 0.5 and 300 kPa respectively. m This is identical to the stress path of test A3451 at D - 30% (Fig. 5.16). T 5.4.4.1 Stress Strain Behaviour A comparison of volumetric and maximum shear strains induced at the three different relative densities but under identical R - a loading is given in Fig. 5.29. A retardation in strain development with increasing relative density may be noted. This is in agreement with the previous observations on the sand behaviour reflecting decreasing strains with increasing density. 5.4.4.2 Direction of Strain Increment Directions of strain increment in relation to the directions of apphed stress increment and stresses, for the above tests are presented in Fig. 5.30. The direction of strain increment a^ is approximately coincident with the stress increment direction E Chapter 5. Results and Discussion Figure 5.29: Effect of D on the behaviour under hnear R - a loading r 161 Figure 5.30: Effect of D on the direction of strain increment in linear R - a loading T 163 Chapter 5. Results and Discussion for OL^U < 45°. This is in agreement with the previous findings (Figs. 5.17, 5.22 and 5.26) in that the direction of strain increment is governed entirely by the direction of stress increment, if the apphed stress increment is inclined less than 45° to the vertical. Figure 5.30 also shows that under identical R - a paths relative density D has no T appreciable effect on the directions of strain increment. It is much in contrast to the significant effects of relative density on a^ , observed under a paths where principal c stress rotations were imposed with constant R (see Fig. 5.14). This difference in strain increment direction presumably arises due to difference in the directions of the imposed stress increment under the two stress paths. path (Fig. 5.30) For the selected R - a was in the range of 0° — 70°, whereas in a paths between 45° — 90° (Fig. 5.14). These ranges of ranged are such that, for a paths, the apphed stress increment is more inchned towards the direction of bedding plane, but for R - a paths, the apphed stress increment is more inchned towards the direction of deposition, during the entire loading path. The previous finding that strain increment direction approximately coincides with stress increment direction (Figs. 5.17, 5.22, and 5.26) if a.& < 45°, now appears to be vahd regardless of the relative density a state of sand. 5.4.4.3 Stress Path and Stress History Dependence of Deformations Possible stress path dependence of deformations at different relative densities is examined in Figs. 5.31 and 5.32 (Test Series I and 0). Strains developed along R - a stress paths in both test series I and 0 are compared with strains along stress paths in which R and a CT vary individually. Approximately equal deformations at common stress state (i2, a ) = (2, 45°) r indicate path independence for both test Series I ( D = 50%, Fig. 5.31) and Series r Chapter 5. Results and Discussion D =50% 164 : (T r =300kPa 7 : b = 0.5 m 02. A ri O 2.0 13001 °r . O D n> 1 Do 1.0 90 > o o 0.1 p^O DoCP A n 0 0 ,•0' -i— 1 : 1 1 1 1 i r <P. J 0.4 A o 13001 o 13451 • o D D O D O O $ D o O D • 0.2 rh D i 0 -f- 20 1 r— 40 i 60 1 r— 80 Q^Deg Figure 5.31: Effect of D on stress path dependence of deformations - Test Series I T Chapter 5. Results and Discussion D =70% : (J 0.08 =300kPa / r : b = 0.5 m o* D ••-VD° 0.06 H .0 o O Q l D • v 0 0 ^ 0 ° ° • • > 0.04-^ 0.02 H o 4 -i 1 1 o O3001 o 03451 1 1 1 r 0 _ • 0.2 R 8 E O3001 2.0 0.1 4 1.0 ~i — i 20 1 1 40 90 45 1 1 60 i r - 80 Figure 5.32: Effect of D on stress path dependence of deformations - Test Series T Chapter 5. Results and Discussion 0 (D T — 70%, Fig. 5.32). 166 Behaviour of Ottawa sand under total loading paths can therefore be regarded as path independent regardless offc,cr' , and D provided m T R < 2.0 and 0° < a„ < 45°. Following linear R - a loading, deformations under common a paths in tests 13451 and 03451 (a,, from 45° to 90°) match closely with those in a tests 13001 and O3001 respectively. These results further support the insignificant effect of stress path history observed earlier in test Series A , E , C, M and K . 5.4.5 5.4.5.1 Deformations under Multi-Linear R - a Loading Stress Strain Behaviour Linear variation of R - a „ , selected so far is only one method of varying R and a in an increasing manner. This was mainly chosen because of its simplicity. A medium loose Ottawa sand sample was loaded under a tri-linear R - a stress path (OABCD) as shown in Fig. 5.33. Other stress parameters a' and b were held constant at 300 kPa m and 0.5 respectively, so that a direct comparison could be made between deformations under this stress path and those under a path A3002 at R — 2 at common stress state C. Figure 5.33 shows deformations under this tri-linear R - a stress path. The results strongly corroborate the proposed notion of path independent deformation response of Ottawa sand under stress paths involving increasing R and ov in the domain of R < 2.0 and 0° < a a < 45°. Beyond the stress point C (ov — 45°) the sample was loaded along the stress path CD identical to that for test A3002. Near identical strain response on further loading along C D with that of test A3002 suggests little effect of stress path history. Chapter 5. Results and Discussion D r =30 % : 167 0'm = : b = 0.5 300 kPa OJS A3002 c 2.0 D 0.4 O 7 / 03 1.0 0 o v A 1.5 • D O a a o o c ,Q 15 30 45 90 • .o o* o D O D ' • O O o 02 ,• n 0.1 - , o oo • • a ° 0 O o D o o o o o o o <» oo0 -»- T 1 20 1 1 —i 40 60 r 80 O D oo D n • Stress Path OABCD DO 0.8 o 3 A3002 -CO 0.6 . co E • 0.4 - D D O 05 o o o o o oo «' ^ „ 0 0 4*- ~r— 20 1 1 60 40 a 0 D e ~l— 80 9 Figure 5.33: Stress path independence observed in a tri-linear R - a loading path Chapter 5. Results and Discussion 5.4.5.2 168 Direction of Strain Increment The strain increment directions for the multi-linear R - a path are illustrated in Fig. 5.34. In order to achieve the tri-linear variation of R and ov the direction of stress increment varied in a discontinuous manner. During the stress path segment OA, stress and strain increment directions are nearly coincident as observed earlier under all previous hnear R - a stress paths (Figs. 5.17, 5.22, 5.26 and 5.30) for a&cr < 45°. Along segment A B the stress increment direction and hence he within 60° to 75° (i.e. equals a , -f- 45°, > 45°). According to the findings in the previous sections (Figs. 5.17, 5.22, 5.26 and 5.30) the strain increment direction a^ c along this constant R segment (a loading) should deviate from the stress increment direction towards the stress direction a . A sudden jump reflecting changes in a and a& are clearly apparent in Fig. 5.34 at A , where sudden changes in loading path c from R - a to a occurs. The very initiation of the third phase B C of the tri-linear stress path is associated with another jump in the directions of stress and strain increments resulting in the stress increment direction oriented very close to 45°. It is interesting to note that the direction of strain increment a& is once again almost coincident with stress c increment direction at this initiation point B of this linear R - a segment of the trilinear path. The results demonstrate that the near coincidence of stress and strain increment directions for < 45° is not only restricted to hnear R, - a paths, but also vahd under more complex loading involving swift changes in R vs a . CT 5.5 Deformation Under Simultaneous Increase in Three Stress Parameters The preceding investigations have focussed on stress paths involving simultaneous increases in R and only, and no change in cr' or b parameter was allowed during m Figure 5.34: Strain increment directions under a tri-linear R - a loading path Chapter 5. Results and Discussion 170 loading. It is of fundamental as well as practical interest to examine, whether the observed behaviour patterns from these results will also be vahd for loading along stress paths in which more than two stress parameters vary at a given time. This aspect was probed in a test which involved simultaneous increase in a^, R and a CT (path A B , Fig. 5.35; defined as a' - R - a path). A medium loose sample was initially m a isotropically consohdated to a hydrostatic stress of 100 kPa, and then subjected to a hnear variation of a' , R and a„ until (<r' , R, ov) = (300 kPa, 2.0, 45°). During m m the course of loading b was maintained at a fixed value of 0.5. In this manner the strains developed until the final stress state could be directly compared with those which develop along a path A3002, which also passes through the same stress state « , R, a ) = (300 kPa, 2.0, 45°). a 5.5.1 Stress Strain Behaviour Deformations along a' - R - a„ path A B are presented in Fig. 5.35. Strains induced m until the terminal state (cr' , R, a ) = (300 kPa, 2.0, 45°) along <r^ - R - a m CT a stress path may be seen to be in close agreement with those in a test A3002. This indicates that the stress path independent behaviour observed under R - a paths could be extended to those paths in which three stress parameters vary simultaneously. It may be pointed out that very elaborate investigations are needed before such stress path independent behaviour and the domain of its vahdity is generalized to all loading paths lying in the 3 dimensional c' - R - a. space, or even the 4 dimensional stress m space a' , R, a m 5.5.2 a a and b. Direction of Strain Increment The direction of strain increment along stress path A B is plotted in Fig. 5.36. It is interesting to note that even with simultaneous increase in three stress parameters, the characteristic that strain increment direction ~ OL&a for < 45° still Chapter 5. Results and Discussion D r =30% : b = 0.5 0.5 0.4 A it • • o • o o a 0.3 0.2 4 0.1 4 a^Deg v 0 0 1 0.6 A\ 3 0.4 1 1 1 1 1 a TEST A3002 = PATH ACDB © STRESS PATH AB A n 1 r 1 OD D • O 0 E • 0.2 • A 0 + .©•' 1 1 10 1 1 20 1 1 30 I I 40 1 50 Figure 5.35: Deformation under simultaneous increase in three stress parameters R and a a Figure 5.36: Strain increment directions under a cr' - R - a path m Chapter 5. Results and Discussion 173 remains valid. For a^o- > 45°, a gradual deviation of from OJAO- towards av is observed which is also consistent with the results from previous R - a paths. 5.6 Prediction of Deformations Under Simultaneous Increase in Stress Ratio and Principal Stress Rotation 5.6.1 Introduction Experimental investigations presented so far in this chapter have shown that the stress strain behaviour of sand under simultaneous increase of shear and principal stress rotation is path independent provided the final stress state is within the domain R < 2.0 and 0° < a ff < 45°. Therefore it should be possible to estimate the deformation at any given stress state within the above domain, by carrying out a single test which would pass through that particular state of stress. Although there are many options for selecting such a stress path, a simple choice would be to use a sequential stress path wherein each sequence consists of increase in only one stress variable (e.g. increase R to the desired amount with a , fixed at 0° followed by increase in the value of a„' at constant R) . 4 It is practically not possible to conduct a test each time deformations at a given (R, a ) stress state are needed. Since the stress path independence has already been a demonstrated, it would be of interest to investigate the posssibihty of characterizing material behaviour in the domain R < 2.0 and 0° < a a < 45° for fixed a' m and b conditions, using a finite number of tests traversing this stress domain. As discussed in the previous paragraph, a reasonable choice would be to perform tests wherein principal stress rotation occur under constant R (with constant a' and b values), at m different levels of R, as shown in Fig. 5.37. Using the observation that the material behaviour is path independent, strains 4 the values of a' and b parameter are held constant throughout the test. m Chapter 5. Results and Discussion D r = constant : (J 174 m = constant : b = constant R a B -o (R a f f ) a R. o Figure 5.37: Constant R principal stress rotation loading to characterize material behaviour. 175 Chapter 5. Results and Discussion accumulated at any given (R, ct ) stress state A (for a certain combination of b and a cr^J can be considered as the superposition of strains due to: • increase in R from hydrostatic stress state to the desired value with a CT = 0° and constant <r' and b (Path OB). m • increase in a with a' , R and b fixed at the desired value (Path BA). a m Using this concept, the volumetric strain e„ and maximum shear strain 7 x under ma R - a stress paths were predicted for the domain of R < 2 and 0° < a < 45°, using a test results from stress paths which involved increase in one stress parameter only at a time (Fig. 5.37). The details of the procedure developed for these predictions are presented in the next section. Deformation predictions were made for all series of tests (Series A through O) presented in the previous sections of this chapter. These predictions were then compared with the measured results. In order to characterize the behaviour for each test series, a minimum of two principal stress rotation tests at different R levels had to be performed with relevant constant a' , b and D conditions for that series. m T It is also important to point out that the comparison of the predicted and experimental results for the R - a paths would not only check the success of the superposition of strains but also affirm the validity of the stress path independence at all stress points along a given stress path. 5.6.2 Prediction Method The concept of prediction of strains begins with the basic assumption that the superposition of strains is valid . This assumption can be expressed in terms of the 5 following equations: All the strain components are considered with reference to hydrostatic stress state immediately prior to R - a loading. 5 Chapter 5. Results and Discussion 176 total (5.1) a 'maxJJl total ~T~ X^max (5.2) a where, Subscript R denotes strains due to changes in R only, with a — 0°. Subscript a denotes strains due to changes in a only, with R = constant. c c The prediction of strains at a given stress state requires that all strain components on the right hand side of the above equations be evaluated. In order to demonstrate the method of prediction more effectively, the procedure is apphed to the test series A (i.e. <r' = 300 kPa; b = 0.5; D = 30%). Test data is presented in parallel with m r the general explanation of the method. Values of {E }R n d { 7 x } H are established from the experimental results along a V ma the stress path where R is increased with a = 0°. It is important to note that these a strains are dependent only on the stress ratio, since all other stress parameters a' , b m and a are fixed. Results for series A , are given in Fig. 5.38. These results constitute a the R path with a, = 0° of test A3002. Values of { e „ } and { y } / a max a are however dependent on both R as well as a (see a Fig. 5.39). These strains for the example case of Series A are presented in Fig. 5.39. These results are identical to those in Fig. 5.7 except for the fact that the strains are now expressed with reference to the hydrostatic stress state of 300 kPa. Strains are plotted only for 0° < a < 45°, which is the domain of interest, and represent a a phases of tests A1001, A2001, A3002 in which principal stresses were rotated at fixed R values of 1.35, 1.65 and 2.0 respectively. Since the experimental results for {£u} and {frn.ax} a Q were developed only for finite values of J?, a method of interpolation was required to obtain these strains at intermediate values of R. Interpolation could Chapter 5. Results and Discussion Figure 5.38: Deformations under shear loading with a sand - Series A 177 ff = 0° for medium loose Ottawa Chapter 5. Results and Discussion 178 30% : (T =300kPa 7 : b - 0.5 m (a) R A3002 2.0 g5 0.1 1.65 A2001 1.35 A1001 0° ] R=2.0 1.0 90 0 0 <> 0 o 1.65 o<> 1.35 0« ,o<> oo o 0.5 (b) 0.4 H 0.3 3 R=2.0 0 o E 0.2 1.65 o<> .0° o<> 0.1 oo o o 0 0 . 6 oo .0 o o o oo oo oo 1.35 oo o o o oo o o O ° ~T~ —I— 10 20 ~i— 30 - 1 — 40 a Deg ff Figure 5.39: Strains from a paths with R = constant for medium loose Ottawa sand - Series A Chapter 5. Results and Discussion 179 be achieved in two ways. The first is to use a graphical method, and the second choice is to use a curve fitting technique. Since the graphical method proved to be cumbersome and time consuming, the second alternative of curve fitting was adopted. Use of power functions of the form given below could adequately approximate the { e „ } and { 7 a m a x } Q characteristics for any desired value of a and R. {e } v = k {R-l) *a > m a {7m«} 1 a = (5.3) n ir fc (#-l) V m 2 2 (5-4) where ki, m i , rix and fc , m-2, ri2 are constants obtained from curve fitting for 2 {e„} and { 7 Q m o x } Q respectively. (Units of a„ in the above equations are degrees and the resulting strain components are in percentage strains). Suitability of curve fit for the results of test series A is illustrated in Fig. 5.40. A satisfactory representation of both volumetric and maximum shear strain characteristics of a paths may be noted. It is emphasized that the curve fitting exercise was used only as a tool for continuous interpolation, and no physical significance is attached to the parameters derived for the mathematical expression for the curves. The predictions were made for deformation under R - a loading paths A3301, A3451, A3601 and A3901 (see Fig. 5.16) in the domain 0° < a < 45° and 1 < R < 2, a using equations 5.1 through 5.4. The predicted and experimentally observed results are compared in Fig. 5.41. It can be seen that the prediction of strains at any given stress state (R, a ) is succesfully achieved by superposition of the results obtained a from stress paths wherein only one stress parameter is allowed to increase at a time. It is also important to reiterate that the close match between the predicted and the measured behaviour confirms stress path independence of deformations in the domain of R < 2.0 and 0° < a„ < 45°. er 5. Results and Discussion D =30% : (J =300kPa f r : 1.25 0 10 b = 0.5 m 20 a 1.4S 30 40 Deg ff Figure 5.40: Curve fitting technique illustrated for test Series A Chapter 5. Results and Discussion D =30% r : (J =300kPa / : b = 0.5 m A3002 Figure 5.41: Predicted and observed stress strain behaviour - Series A Chapter 5. Results and Discussion 182 Deformation predictions similar to those for series A were also made for R - a paths in several other test series E , C, M , K , I, 0 and also for the tri-linear stress path. In order to characterize the behaviour in each series, at least two principal stress rotation tests (a tests) under different but fixed levels of R and the R test at a„ = 0° are needed at the specified a' , b and D conditions of that series. Test data m T for characterizing behaviour in the Series E , C, M , K , I and 0 (along with the fitted curves for interpolation) are given in Appendix C. Comparison between the predicted and experimentally observed strains for each test series E , C, M , K , I, O including the tri-hnear R - a path are presented in Figs. 5.42 through 5.48 respectively. Excellent agreement between predicted and measured results confirms that the stress strain behaviour for given <r^, b values, in the R - a space can be predicted successfully with the use of a limited number of principal stress rotation tests performed at different stress ratios. The underlying principles behind such predictions is the experimentally demonstrated path independent deformation behaviour in the domain of R < 2.0 and 0° < ov < 45°. 5.7 Prediction of Deformations Under Simultaneous Increase of o-' , R m and a a The stress-strain response under - R - a path A B (Fig. 5.35) was predicted by an approach similar to the one used in the prediction of strains under R - a loading in the previous section. Along this stress path, values of a' , R and a were simultaneously m a increased in a linear manner from an initial hydrostatic stress state a' = 100 kPa m until a' = 300 kPa; R — 2; and ct = 45° was achieved. A path independent strain m CT response would imply that the strains at any given a' , R, a m c state along path A B could be evaluated by following any loading path ending at that state. Since the data base characterizing the material behaviour consisted of hydrostatic paths and R and Chapter 5. Results and Discussion Figure 5.42: Predicted and observed stress strain behaviour - Series E Chapter 5. Results and Discussion D =30% : (J / = 300 kPa b = 0.0 3 E a Deg ff Figure 5.43: Predicted and observed stress strain behaviour - Series C Figure 5.44: Predicted and observed stress strain behaviour - Series M Chapter 5. Results and Discussion D =30% : J - 100 kPa 7 r : b = 0.5 m 0.15 K3001 2.0 R I • f 0.1 1.0 / 0 - s I 45 s s 1< J / 00 ] 90 Co /© 0.05 < 0 it K o j / ) s^— r ~i 1 l 0.4 1 r K3001 o 0.3 K3451 H Predicted 1.0 _ - - " " - ^ _ — " - / 8 XO© — — *~ 0.1 4 ! o-f " ^ ~i 10 20 r 30 40 Figure 5.45: Predicted and observed stress strain behaviour - Series K Figure 5.46: Predicted and observed stress strain behaviour - Series I Figure 5.47: Predicted and observed stress strain behaviour - Series 0 Chapter 5. Results and Discussion D r =30 % : 0 / m = 300 kPa : b = 0.5 0.2 ^ 0.6 D — 0.4 H Experimental Predicted Stress Path OABC A3002 8 E 02 n— 40 Figure 5.48: Predicted and observed stress strain Behaviour - tri-linear stress OABC Chapter 5. Results and Discussion 190 a paths carried out at several constant a' conditions (Series A , M and K ) as shown m in Fig. 5.49, the strains at a given a , R, a m stress state P was obtained by the c superposition of strains due to: • hydrostatic loading from initial to the desired value a' m (path OC). • increase in R from above hydrostatic stress state to the desired value with = 0° and constant a' and b (path CB). m • increase in a CT with a' , R and b held constant at the desired value (path BP). m This can be expressed mathematically, { v} i = £ tota {7max}tota( = { e * } ^ + {e } v {Tmai}^^ + R + {e„} {"Jmax} R (-) 5 a + {7max} 5 (5-6) a where, subscript cr' indicate strains under hydrostatic loading from initial to the m required a' m state. For the superposition to be apphed for the prediction of strain response under a' - R - a path A B , all strains were referenced to the initial 100 kPa m hydrostatic stress state of the path. {e }o./ and {7 ax} ' u m a CT r e obtained from hydrostatic compression test results. Values {C }R and {f ax}R V m are dependent on R as well as a' m level. R tests at a. = 0° from test series A , M and K gives the strain components { £ „ } and a R {f ax}R as functions of R, only for three distinct values of a' (= 300, 200 and 100 kPa). m m {e } v R and {irnax}R at any intermediate cr is obtained by interpolating between these known m R path results. Strain components {e„} and {"f } max a are dependent on all three stress parameters a' , R and a . Again, the a test results from series A , M and K provide the data m ff Chapter 5. Results and Discussion 191 Figure 5.49: Characterization of material behaviour under a' - R - a test series A , M and K m ff loading using Chapter 5. Results and Discussion 192 base to characteristize these strain components. Therefore, in this case the values of { v} e a n a d {l'max} at the given a' ^ R, a state is derived after interpolation between a m a all these three variables. The strain response under <r' - R - a path (path A B ) was predicted using a m graphical interpolation, and the comparison between predicted and measured strain responses is given in Fig. 5.50. Very good agreement between the predicted and observed results further corroborates the previously demonstrated stress path independent deformation behaviour of sand under general "total loading" paths involving principal stress rotation. Chapter 5. Results and Discussion 193 Chapter 6 Summary and Conclusions The main objective of this research was to study the drained behaviour of sand under simultaneous increase in stress ratio and principal stress rotation. Hollow cyhnder torsional (HCT) device was adopted in this study, due to its inherent advantage of being the only apparatus which is capable of independently controlling the four stress parameters: mean normal effective stress cr' , stress ratio R, intermediate principal m stress parameter b, and the direction of major principal stress a^. These four parameters adequately describe any stress state involving two dimensional principal stress rotation and have been found to influence the behaviour of inherently anisotropic materials. Manual control of surface tractions in the H C T device is extremely cumbersome, especially in the case of complex stress path tests. In view of this, an automatic stress path control system was developed as a part of the research program. During stress path loading, stress non-uniformities develop across the walls of the H C T specimen due to its curvature. Therefore a good understanding of the non- uniformities was essential before carrying out stress path testing in the H C T device. It was noted that the stress non-uniformities have been assessed mainly based on the assumptions of linear elastic material behaviour. A finite element simulation of the H C T specimen was performed to study the stress non-uniformities during general stress path tests. The sand behaviour was represented by an incremental elastic hyperbolic model in the analysis. It was revealed that for any given stress state, the hnear elastic assumptions overestimates the stress non-uniformity coefficient /3R in 194 Chapter 6. Summary and Conclusions 195 the H C T specimen. The results showed that (3R did not continuously increase with increasing R as in the case of hnear elastic material. Instead, /3R values reached a plateau or sometimes even suffered a drop after the peak with increasing stress ratio. The domain of stress space that could reliably be explored using the H C T device was found to be much larger than that previously suggested based on hnear elastic considerations. For a given stress state, (3R values increased with increasing density of the specimen. Therefore, the available domain of stress space for reliable exploration decreases for denser sand specimens. The experimental program was designed to systematically examine the sand response under simultaneous increase of stress ratio R and the direction of major principal stress a . Tests were also carried out where the stress parameters R and ct^ ff increased individually. Only the stress paths with increasing stress parameters ("loading paths") were considered in this study. No tests were carried out where any of the parameters cr , R, b and a m a experienced a decrease during loading. A l l tests were performed on saturated samples of pluviated sand under drained conditions. Emphasis was placed on examining the response of medium loose sand (D = 30%) under r hnear R - a loading paths. Additional investigations were also made on the sand behaviour under multi hnear R - a paths and loading with simultaneously increasing a' , R and a . m a Deformations from stress paths with individual variations of stress parameters were compared with those from simultaneously increasing R - a a at common stress states. The results showed that the strain response of the medium loose sand is path independent provided the final stress state is within the domain of approximately R < 2 and 0° < a a < 45°. At higher stress ratios and/or larger principal stress rotation angles the deformations were clearly path dependent. In such situations, sand which was subjected to principal stress rotation at a higher stress ratio was observed to develop the largest strains. Furthermore, sand initially loaded to a stress Chapter 6. Summary and Conclusions 196 state within the confines of R < 2 and 0° < ct < 45°, exhibited no signs of previous a stress history effects on the strain response under a subsequent common loading path. This observed stress path and stress history independent deformation behaviour of loose sand was found to be valid irrespective of the levels of intermediate principal stress parameter b or the mean normal effective stress a' . Similar tests performed m at higher densities corroborated these findings, thus extending the validity of the observations to the general sand behaviour. The major principal strain increment direction a increment direction a^ c Ac and the major principal stress were approximately coincident when a . < 45°. This was Ao found valid regardless of the magnitudes of stress parameters R, a , cr' and b or a m relative density D . However, for a - > 45°, strain increment direction a T Ao towards the major principal stress direction a r Ae moved with increasing R or principal stress rotation. In other words, the strain increment direction a^j was almost totally governed by and coincident with the stress increment direction a& , when ct& was CT inclined closer to the direction of deposition. When a was inclined closer to the direction of bedding plane, the strain increment direction was dependent not only on aAo- but also on other parameters such as ov, R and D etc. T The strain response under tri-linear R - a loading and simultaneous increase in three stress parameters also supported the notion of stress paths and stress history independent behaviour in the domain of R < 2 and 0° < ct < 45°. It was demona strated that the sand response under "loading paths" within the above domain could be predicted by the results of a limited number of stress path tests characterizing the strain response in that stress domain. 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Series, No. 118, Dept. of Civil Engineering, Univ. of British Columbia, Canada. [53] Vesic, A . S . and Clough, G . W . (1968). "Behaviour of Granular Materials Under High Stresses", Journal of the Soil Mech. and Found. Eng. Division, ASCE, Vol. 94, No. SMS, pp. 661-688. [54] Yamada, Y . and Ishihara, K . (1979). "Anisotropic Deformation Characteristics of Sand Under Three Dimensional Stress Conditions", Soils and Foundations, Vol. 19, No. 2, pp. 79-94. [55] Wong, R . K . S and Arthur, J . R . F . (1985). "Induced and Inherent Anisotropy in Sand", Geotechnique, Vol. 35, No. 4, PP- 471-4&1- Appendix A Cross Anisotropic Elastic Material Behaviour Cross anisotropic elastic material exhibits a rotational symmetry about one of the coordinate axes. Let Z be the axis of elastic symmetry and X — Y be the plane of isotropy as shown in Fig. A . l a . The incremental stress strain relation for a cross anisotropic elastic material (under 2-D principal stress rotation in X — Z plane) can be written as, > 1 Ae E V E u' E x Ae y Ae 1 z A-) xz 0 ^ v' E< 0 t/ 0 E V E 1 E 1 i/' E> E' 0 0 Aa Aa 1 y > < Aa 0 1 G' x J (A.l) z AT XZ where, E - Young's modulus in the plane X — Y E' - Young's modulus in the Z direction G' - Shear modulus in the plane X — Z v - Poisson's ratio in the plane A' — V" v' - Poisson's ratio in the plane X — Z This leads to, Ae x = \,Aa -^A<r -^Aa x y 204 z (A.2) Appendix A. Cross Anisotropic Elastic Material Behaviour Z (Axis of elastic symmetry) (Afx, A 7 zx/2) Figure A . l : Cross anisotropic elastic material Appendix A. Cross Anisotropic Elastic Material Behaviour Ae 2 v' - — Aa E' = x v' - —Aa E' v y + 1 —Aa E 1 206 z (A.3) (A.4) From equations A.2 and A.3, ( Ac (Ae - A e ) {Aa - Aa ) 2 x 2 ) E' E Defining Aa k, and •^ x x Z 2L = k, ~E' (A.5) and substituting in Eqn. A.5 yields, yx Act* E (Ae - Ae ) (Acr, - A<r ) 2 V E + x x ' x + E' ^ jL - 1 f + i ^ (A.6) Using Mohr circle for stress increments in Fig. A . l b , the direction of stress increment a^j with respect to Z direction can be written as, tan 2 a A 2Ar. C T — A<J2 - Ac (A.7) Similarly using Mohr circle for strain increments in Fig. A . l c , the direction of strain increment a ^ with respect to Z direction can be written as, e tan 2aA E = AT* A e - Ae* (A.8) 2 Coincidence of stress increment and strain increment directions implies, tan2aAo- = tan2aA . Therefore, from Eqns. A.7 and A.8, e A 7x2 AT 7 i XZ _ ^ f A e - Ae 1 \ Acr - ACT- J 2 z x (A.9) Appendix A. Cross Anisotropic Elastic Material Behaviour 207 Combining Eqns. A.4, A.6 and A.9 we get the condition for coincidence of stress increment and strain increment directions as, (A.10) For a given cross anisotropic linear elastic material the parameters E, E', G', v and v' are constants. Therefore, the condition expressed by Eqn. A.10 would be satisfied only under certain values of k zx and k , yx which is related to the applied loading conditions. This implies that the coincidence of stress and strain increment directions would not occur under any arbitrary loading condition, even if the material is cross anisotropic elastic. Conversely, the coincidence of stress and strain increments along an arbitrary loading path in an anisotropic material is not a sufficient condition to conclude that the material is elastic. Appendix B Membrane Penetration Corrections A minimum of four strain components are required to define the complete configuration of a hollow cylindrical specimen. In the U B C - H C T device, two strain components e and Ee are estimated indirectly from the measured volume changes of the specimen T and the internal confining chamber. (See section 3.2 for details). Both inside and outside vertical surfaces of the H C T specimen are covered by 0.3 mm thick rubber membranes. In testing granular materials, when drained stress paths of varying cell pressures are imposed, the measured volume changes are subject to error resulting from membrane penetration. Therefore it is important to correct the measured volume changes for membrane penetration effects before the values are employed in strain computations. The test results in this thesis have been presented after correcting for membrane penetration effects, using the method proposed by Vaid and Negussey (1984). Vaid and Negussey observed a linear variation between the unit membrane penetration e m and the logarithm of effective confining stress. Unit membrane penetration results for Ottawa sand ASTM-C-109 (with a 0.3 mm thick rubber membrane) are reproduced in Fig. B . l . The measured volume change of the sand specimen was corrected as follows. {AV } - {AV h + s M 208 t (B.l) {AV } M {AV } M e (B.2) Appendix B. Membrane Penetration Corrections 209 Effective Confining Pressure kPa Figure B . l : Membrane penetration correction curve - after Vaid and Negussey (1984) Appendix B. Membrane Penetration Corrections 210 where, AV§ {AVs} - Corrected volume change of the specimen - Measured total volume change of the specimen t {AVM} - Total membrane penetration volume change 4 {AV^}I - Volume change due to penetration of internal membrane {AVjf} - Volume change due to penetration of external membrane e For the current values of internal (or external) effective confining pressure and the imposed increments A P / (or AP '), the change in corresponding unit membrane e penetration {Ae } Tn values of {AVM} (or ( A e } ) i m were obtained from the curve in Fig. B . l . The 1 e and {A14f} were then obtained using the following equations. e { {AV } M I {AV } M e = {Ae } = {Ae } A m m Ai i e e (B.3) (B.4) where, Ai - Surface area of the internal membrane covering the specimen A - Surface area of the external membrane covering the specimen e In a similar manner the volume change of the internal chamber was corrected as given below. AVj = {AV^ + iAVM}, where, X N.B. the value of {Ae } is positive, for positive AP'. m (B.5) Appendix B. Membrane Penetration Corrections AVj {AVi} t - Corrected volume change of the internal chamber - Measured total volume change of the internal chamber 211 Appendix C Deformation Characteristics of Test Series E , C, M , K , I and O As discussed in Chapter 5 (Section 5.6), in order to predict deformations under R a paths, the characteristic behaviour is obtained by means of several a paths and an R path with a c = 0°. Such characterization was demonstrated for the test Series A (Figs. 5.37 and 5.39). Similar tests were carried out on several test series (Series E through 0) and the resulting deformation data are presented in this appendix. The data were utihzed to predict the strain response under R - a paths for these test series presented in Figs. 5.42 through 5.47. For each series the volumetric and maximum shear strain responses under following loading conditions are presented. • R loading with a = 0° a • a loading under different R levels (R = 1.65 and 2.0) Test results are presented in Figs. C . l through C.12. The contents of each figure are summarized in Table C . l . In prediction of response under R - a paths, the data from a paths were interpolated using a curve fitting technique as described in section 5.6.2. In order to examine the suitabihty of fit, the fitted curves are superimposed on the experimentally observed volumetric and maximum shear strain data. 212 Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and 0 213 Table C . l : Index - Deformation Characteristics of Test Series E , C, M , K , I and 0 Figure No. Series No. R path a paths E C M K I 0 C.l C.3 C.5 C.7 C.9 C.ll C.2 C.4 C.6 C.8 CIO C.12 All strain components are referenced to the hydrostatic stress state immediately before R loading. Appendix C. Deformation Characteristics of Test Series E, G, M, K, I and O D =30% r : (J =300kPa : b = 0.3 m 0.2-, Stress Ratio R Figure C . l : Deformations under shear loading with a„ = 0° - Test Series E 214 Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and 0 Figure C.2: Deformations under a paths with R — constant - Test Series Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and 0 Figure C.3: Deformations under shear loading with a = 0° - Test Series C a Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and O D 0 r 10 =30% : (J f m =300kPa 20 : 30 b = 0.0 40 a Deg ff Figure C.4: Deformations under a paths with R = constant - Test Series C 217 Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and O D =30% r : fT 7 = 200kPa : b = 0.5 m Stress Ratio R Figure C.5: Deformations under shear loading with a a — 0° - Test Series M Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and O D =30% : Q r =200kPa / : b = 0.5 m 0.15 1.54 (a) 0.1 { £ H v } % = 0-24E-03 * (R-1) 1.57 * (X e Curve Fit o Experimental Oo 0.05 H T (b) •y {'max 1 1.72 > % = 0-63E-03 * (R-1) * r 1.52 a. 0.3 H 3 Of Deg a Figure C.6: Deformations under a paths with R = constant - Test Series M 219 Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and O D 1 r =30% 1.2 : fT 1.4 m =100kPa : 1.6 b = 0.5 1.8 2 Stress Ratio R Figure C.7: Deformations under shear loading with a = 0° - Test Series K a Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and 0 D =30% : (J r =100kPa / : b = 0.5 m 0.1 (a) 0.08 v % = 0 - 5 6 E - * (R-1)* * 04 a" 7 H — 0.06 j£ {£ } o Curve Fit Experimental > 0.04 Oo 0.02 0 (b) r y {'max , 1.55 }a % = 2.29E-03 * (R-1) * 1.08 a 3 E Figure C.8: Deformations under a paths with R = constant - Test Series K Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and 0 D r = 50 % : (T m = 300 kPa : b = 0.5 0.15 -i 1 1.2 1.4 1.6 1.8 2 Stress Ratio R Figure C.9: Deformations under shear loading with a a = 0° - Test Series I Appendix C. Deformation Characteristics of Test Series E, C, M, K, I and O a Deg ff Figure C.10: Deformations under a paths with R — constant - Test Series I 223 Appendix G. Deformation Characteristics of Test Series E, C, M, K, I and O D =70% r : (T m =300kPa : b = 0.5 0.1 -T 1 1.2 1.4 1.6 1.8 2 Stress Ratio R Figure C . l l : Deformations under shear loading with cn — 0° - Test Series O a 224 Figure C.12: Deformations under a paths with R = constant - Test Series 0
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Behaviour of sand under simultaneous increase in stress ratio and rotation of principal stresses Wijewickreme, Dharmapriya 1990
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Title | Behaviour of sand under simultaneous increase in stress ratio and rotation of principal stresses |
Creator |
Wijewickreme, Dharmapriya |
Publisher | University of British Columbia |
Date Issued | 1990 |
Description | Drained behaviour of sands under simultaneous increase in stress ratio and principal stress rotation is investigated. The hollow cylinder torsional (HCT) device which permits independent control of four stress parameters: mean normal stress σ'[subscript]m, stress ratio R, intermediate principal stress parameter b and the inclination α[subscript]σ of σ'₁ to the vertical, is adopted as the testing device. In order to conduct complex stress path testing in the HCT device, a new automatic stress path control system is developed. The stress non-uniformities due to the curvature of the HCT specimen is assessed using an incremental elastic representation of sand behaviour, in order to delineate the domain of stress space that could reliably be explored using the HCT device. It is shown that previous assessments of stress non-uniformities assuming linear elastic soil grossly overestimate the stress non-uniformities in a HCT sand specimen. A much larger domain of stress space with acceptable levels of non-uniformities is apparent from the results of incremental elastic analysis. New domain of stress space for reliable exploration using the HCT device is delineated and the testing program is developed so that all stress paths lie within these acceptable limits. Tests are carried out on pluviated sand under saturated drained conditions. The deformations under increasing R and α[subscript]σ is shown to be path independent, if the final stress state is within the approximate bounds of R ≤ 2 and α[subscript]σ ≤ 45°, regardless of the b or relative density D[subscript]r, levels. With increasing stress ratio R and/or principal stress rotation α[subscript]σ, the deformations gradually become path dependent. Once loaded to a stress state within the domain R ≤ 2 and α[subscript]σ ≤ 45°, the strain response under subsequent principal stress rotation is shown to be independent of the previous loading history. It is demonstrated that the strain response under any general increasing R - α path in the domain of R ≤ 2 and α[subscript]σ ≤ 45° can be predicted using the results of a limited number of tests characterizing that domain. It is shown that these concepts can be extended to loading paths which involve simultaneous increase of three stress parameters. Strain increment direction α[subscript]Δε is shown to be approximately coincident with and totally governed by the stress increment direction α[subscript]Δσ when the stress increment direction α[subscript]Δσ is more inclined towards the vertical deposition direction. When the stress increment direction is inclined closer to the bedding plane, the strain increment direction depends in addition, on other parameters such as R, α[subscript]σ and R[subscript]r etc. Under any stress path involving principal stress rotation, the deformations decrease with increasing density and therefore the principal stress rotation is more crucial in loose sands. Deformations increase with the level of stress ratio R. Level of b parameter does not affect deformations under principal stress rotation, if the rotations are small. However, with increasing α[subscript]σ deformations due to principal stress rotation tend to increase with decreasing b value. |
Subject |
Sand Strains and stresses |
Genre |
Thesis/Dissertation |
Type |
Text |
Language | eng |
Date Available | 2011-02-17 |
Provider | Vancouver : University of British Columbia Library |
Rights | For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use. |
DOI | 10.14288/1.0050457 |
URI | http://hdl.handle.net/2429/31410 |
Degree |
Doctor of Philosophy - PhD |
Program |
Civil Engineering |
Affiliation |
Applied Science, Faculty of Civil Engineering, Department of |
Degree Grantor | University of British Columbia |
Campus |
UBCV |
Scholarly Level | Graduate |
Aggregated Source Repository | DSpace |
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