6th International Conference on Gas Hydrates


You don't seem to have a PDF reader installed, try download the pdf

Item Metadata


5804.pdf [ 396.16kB ]
JSON: 1.0040970.json
JSON-LD: 1.0040970+ld.json
RDF/XML (Pretty): 1.0040970.xml
RDF/JSON: 1.0040970+rdf.json
Turtle: 1.0040970+rdf-turtle.txt
N-Triples: 1.0040970+rdf-ntriples.txt
Original Record: 1.0040970 +original-record.json
Full Text

Full Text

   A LABORATORY PROTOCOL FOR THE ANALYSIS OF NATURAL GAS HHYDRATES  Hailong Lu; John A Ripmeester The Steacie Institute for Molecular Sciences National Research Council of Canada 100 Sussex Drive Ottawa, Ontario, K1A OR6 CANADA   ABSTRACT For a number of years the NRC group has been working on a laboratory protocol for the analysis of gas hydrate that has been recovered from various natural sites. The expectation was that a comprehensive set of techniques would become available for the general use of hydrate researchers around the world.  With the current set of available techniques a good picture of natural gas hydrates can be obtained, although the emerging complexity of the hydrate-mineral system still demands additional work.  Here we present a suite of techniques that will take a researcher from preservation techniques to hydrate occurrence, gas/water/sediment ratios, gas and isotope analysis, P-T behaviour, structure, composition, degree of water conversion to hydrate, hydrate homogeneity and decomposition behaviour.   As more detailed studies become possible a variety of more subtle features are revealed, for instance the role of minor gas components in hydrate stability, decomposition behaviour and heterogeneity in structure and composition.   Keywords: Gas hydrates, NMR, Raman, diffraction, Calorimetry, stability, composition, decomposition                                                       Corresponding author: Phone: +1 613 993 2011 Fax +1 613 998 7833 E-mail: john.ripmeester@nrc-cnrc.gc.ca Proceedings of the 6th International Conference on Gas Hydrates (ICGH 2008), Vancouver, British Columbia, CANADA, July 6-10, 2008.  INTRODUCTION  One of the key elements in coming to terms with the various issues involving natural gas hydrate is to understand it as a mineral system. This means that, as for other minerals, a number of properties may be quite specific to the location where they are found. There are a number of features that distinguish hydrates from most other mineral systems.  For instance, hydrate becomes unstable once it is removed from its pressure-temperature stability zone where it is found in nature.  What is more, hydrates, as clathrates, are non-stiochiometric, and since all known naturally occurring hydrates have at least two kinds of cavities which may or may not be completely filled, compositions and cage occupancies are variable [1, 2, 3].  Further, hydrates are labile, that is, their composition reflects not only the conditions during the initial formation process, but also this also changes if the nature of the fluids in contact with the hydrate change with time. This can lead to heterogeneity in composition and structure on a variety of scales [4, 5]. Sediment composition and particle (pore) sizes also play a key role in hydrate formation and accumulation, and in establishing the degree of water saturation and the level of conversion to hydrate [6].  HYDRATE RECOVERY Careful attention to hydrate recovery from natural sites is a first and essential part of the laboratory characterization of natural gas hydrates, and this starts in the field.  Unless pressure coring methods are used, decomposition of some hydrate is inevitable, although self preservation often helps the cause [7].  Since cores decompose from the outside in, the best hydrate samples will be found in the center of the core.  For characterization of the hydrate phase, it is sufficient to store recovered core sections in liquid nitrogen as rapidly as possible upon recovery for transfer to the laboratory [8].  If sediment structure is to be preserved as well, far more elaborate techniques are required as the cores should not be frozen. In-por e  hydr a t eH ydr a t e  s t or e d i n l i qui d ni t r oge nM a s s i ve  hydra t eO bs e rva t i onP X R D  S C X R DR a m a n 13C  N M RA m ountChe m i c a l  &Is ot opec om pos i t i on(G C, M S )G a s , w a t e rP -T  s t a bi l i t y  de t e rm i ne d i ns m a l l  vol um e  pre s s ure  c e l lConve nt i ona lH i gh pre s s ureCoupl e d w i t h M SD S CS t ruc t ureCom pos i t i onG ue s t  di s t ri but i onG a s / w a t e r ra t i o (m a s s i ve )S a t ura t i on (i n-por e )Com pone nt sO ri gi nS t a bi l i t yre gi m eD i s s oc i a t i on TCoe xi s t i ng pha s eD e c om pos i t i on be ha vi orof c om pl e x hydra t e sConc e nt ra t i onD i s s oc i a t i on Figure 1.  General scheme for the laboratory analysis of recovered natural gas hydrate samples.   HYDRATE CHARACTERIZATION A general scheme of the laboratory analysis of natural gas hydrate and the information that becomes available is given in Fig. 1.   Macroscopic When recovered core sections reach the laboratory, a close examination, either by eye or microscope, of the sample cooled in liquid nitrogen will often reveal the hydrate which then can be classified according to its appearance – massive, nodules, veins, etc. If there is only pore hydrate, often invisible to the naked eye, a bubble test will reveal the presence of hydrate and the amount of hydrate can be assessed by the vigour of the gas release.  If sufficient sample is available, quantitative measurements can be carried out on the amount of gas, water and solids.  This will give the water saturation and, eventually, the level of conversion of water to hydrate can be estimated once the nature of the hydrate is known.  Before such an analysis is carried out, it is important to remove any adsorbed gas, for instance, the N2 gas that remains on the surface of the samples after storage in liquid nitrogen.  Exposing the sample to a dynamic vacuum at ~ 120K is sufficient to remove adsorbed gas, and under these conditions the hydrate will not decompose.  If enough hydrate is present, the hydrate can be placed in a small-volume pressure cell and after removal of air and adsorbed gas it is 0102030405060702 5 0 2 6 0 2 7 0 2 8 0 2 9 0 3 0 0 3 1 0P (bar)T  ( K )1234561 .  C H4 ( s I )2 .  C H4- m e t h y l c y c l o p e n t a n e  ( s H )3 .  n a t u r a l  g a s  h y d r a t e s  ( s I I - s H )4 .   9 5 . 2 %  C H4- p r o p a n e  ( s I I )5 .  C H4- 6 %  i s o b u t a n e  ( s I I )6 .  C H4- c y c l o p e n t a n e  ( s I I )P (bar) Figure 2. Left -small pressure vessel for temperature-programmed decomposition of hydrate; Right - data obtained – curve 3 is for mixed sII – sH hydrate from Barkley Canyon, Cascadia.  possible to follow the pressure-temperature behaviour of the hydrate by heating the sample in increments. After each heating step, the pressure in the cell is allowed to come to equilibrium, thus mapping out a P-T stability zone for the hydrate (Fig.2). The gas from decomposed hydrate can be captured and subjected to composition analysis by GC-MS as well as high resolution mass spectrometry for isotope analysis to give information on the origins of the gas.  The sediment should be examined to determine mineralogy, particle and pore sizes and water content. Once the structure and composition of the hydrate are known, the degree of conversion of the water to hydrate can be calculated.   Microscopic Hydrate characterization requires a determination of both the hydrate structure and composition, as these materials are non-stoichiometric and they may contain a variety of guest molecules distributed over different sites.  The appropriate techniques include various powder diffraction (usually X-ray) methods to give the structure and unit cell parameters and spectroscopic methods to measure cage populations.  For many recovered natural hydrates it is possible to isolate enough hydrate for study by several techniques.  In cases where only pore hydrates are present it sometimes is possible to crush the hydrate/sediment composite in liquid nitrogen and harvest the finely powdered hydrate that rises to the top of the sediment for further study.    Figure 3. Single crystal of sII hydrate found in a recovered core from Cascadia – Bullseye vent (left); Structure determined by single crystal diffraction (SCD), showing location of methane, ethane and propane.  Butane and isobutene were also found to be present from GC –MS, but in quantities too small to be seen by SCD (< 5% of the guest in the sII large cage) Although powder diffraction usually yields only the unit cell parameters of the various phases present, recent work has shown that, with some assumptions, hydrate cage occupancies can be obtained in the case of simple hydrates (generally not more than one type of guest/cage) [9].  As well, in some circumstances it is possible to find single crystals of hydrate in recovered core samples [10].  Excellent structural information is available in such cases (Fig.3).  For example, the structure of a sI methane hydrate crystal was refined to an R value of an order of magnitude better than for laboratory prepared crystals. Presumably this was possible because annealing of the crystal on a geological time scale removed the defects usually encountered in samples prepared in the laboratory. However, if there are a variety of guests distributed over one of the cage sites there are limits on how low cage occupancies can be before their signatures are lost in the noise.  5 10 15 20 25 30050100150200250300IceII ( 400 )H ( 201 )II ( 222 )H ( 002 )II ( 311 )H ( 111 )H ( 200 )II ( 220 )H ( 001 )II ( 111 )R6 9 4Intensity2  T h eta (deg re es)PXR D (d etail ) of  n at ur al  h y dra te samp le fromBa rkle y Can yonUnit c el l  par amete rs (nm )sIIa= 1. 7259(8)sHa= 1. 2482(1)      c= 1. 0064(4)IntensityIntensityIntensity Figure 4. Detail of powder X-ray diffraction pattern of mixed sII-sH hydrate from Barkley Canyon, Cascadia Similarly, if mixed phases are present it is necessary to examine the powder patterns carefully in order to track the minor component. Fig. 4 shows that some reflections needed to be indexed as sH hydrate with sII being the major component.  A useful innovation in the study of hydrates is the availability of a sample cell for in-situ high pressure work.   Not only is it possible to follow hydrate formation by PXRD, but also processes such as hydrate decomposition.   13C NMR and Raman spectroscopy have been developed to provide information on both hydrate structure and cage occupancies (Fig. 5) [1][2][3][4][11].  Each technique has its advantages and disadvantages, including ease of use and the capital investment required. An important distinction between the two lies in the actual sampling of the hydrate: NMR gives an average over the bulk of the sample – usually from tens to a few hundred mg, whereas Raman gives a localized response from a spot of a few microns in diameter on the surface. NMR spectroscopy is inherently quantitative, as it counts the number of spins of a certain type, each at a characteristic chemical shift. The Raman spectrum is more difficult to interpret and the line intensities depend on the cross section for Raman scattering. This means that quantitative analysis requires calibration of Raman with another technique such as NMR.  On the other hand, the spot analysis of natural hydrates by Raman is able to give information on sample homogeneity. A recent application in this area is that of Raman mapping [4]. A sI hydrate recovered by IODP 311 containing mainly methane and a small quantity of H2S, indicating that the latter can be present either in a mixed CH4/H2S hydrate or isolated H2S and CH4 hydrates.     Differential Scanning Calorimetry of recovered samples is another technique that can give information on the nature of the hydrate present by following the differential thermal input during decomposition of the hydrate. Quantitative measurement of the thermal events is not trivial as the mass and heat capacity of the sample may   - 9- 8- 7- 6- 5- 4- 3- 2- 10123456789( p p m )4 6 0 - 4 8 1  cm  bsf2 6 4 - 2 8 4  cm  bsf2 8 4 - 2 9 4  cm  bsf- 4 . 2  p p m- 6 . 6  p p m7 8 . 9 %7 5 . 2 %7 9 . 5 %2 0 . 5 %2 1 . 1 %2 4 . 8 %T=  173KHP DEC MAS  3 000 HzStr . I  Figure 5. 13C NMR spectrum of a sI methane hydrate samples recovered from a cold vent field, Barkley canyon, showing the signal of methane in small and large cages.   change when gas evolves  during decomposition.  However, sometimes by comparing the thermal profile of different samples, including synthetic ones, can give some valuable insight into the nature of the hydrate.  Figure 6 shows that pure methane and H2S hydrates have very different thermal profiles during decomposition, reflecting their different stabilities.  The natural samples contain up to a percent of H2S, yet the traces show remarkably different thermal profiles. Some (marked with arrows) show a two step process, others a single step, suggesting that the samples with the marked traces have distinct regions of hydrate – perhaps pure methane hydrate as well as mixed CH4-H2S hydrate [5].     U 1 3 2 8 B  2 H 1 -9- 10 0 - 80 - 60 - 40 - 20 0 20T (oC)CH4 hy dr a teU 1 3 2 8 B  2 H 1 X- 5  # 2U 1 3 2 8 B  2 H 1 X- 5  # 3U 1 3 2 8 B  2 H 1 X- 5  # 1U 1 3 2 8 E 2 X- 2  8 0 -9 0  c mH2S hy dr a te- 80 ° C- 23 ° C Figure 6. Differential Scanning Calorimetry traces of sI hydrates pure H2S hydrate (top) samples recovered by IODP 311 and pure methane hydrate (bottom).                     Table 1 Summary of techniques and information   ACKNOWLEDGEMENTS   We acknowledge funding support from NRCan through the Climate Change Technology and Innovation Initiative (Unconventional Gas).  We also acknowledge the essential role played by those who recovered samples and ensured their intact transfer to our laboratory: Scott Dallimore, Fred Wright, Ross Chapman, Michael Riedel, George Spence, Tim Collett, Bob Hunter, Rick Coffin, John Pohlman, Pushpendra Kumar, Ryo Matsumoto, et al.    REFERENCES:  [1] Tulk CA, Ratcliffe CI, Ripmeester JA. Chemical and physical analysis of Natural Gas Hydrate from the JNOC/JAPEX/GSC Mallik 2L-38 research well, Technique  Information  1. Visual observation Hydrate morphology 2. Bubble test Presence of hydrate 3. Temperature programmed decomposition in small pressure cell P- T stability curve 4. Gas capture–  (from 3)                               GC – MS Isotope analysis                                                Gas composition Origin of gas 5. Water content of sediment  6. Sediment particle/pore sizes Pore saturation 7. Total gas measurement Provisional estimate of water conversion to hydrate 8. Powder X-ray diffraction Structure of hydrate, unit cell 9. Single crystal X-ray diffrcation Structure and composition of hydrate 10. Raman spectroscopy Composition of hydrate Sample heterogeneity 11. NMR spectroscopy Structure and composition of hydrate,  cage occupancies 12. Results from 5 – 11,  Amounts of hydrate, water conversion 13 Differential scanning calorimetry Thermal hydrate decomposition characteristics 14 High pressure calorimetry – mass spectrometry Thermal hydrate decomposition and produced gas identification – simulated field conditions Bull. Geological Survey of Canada 1999; 544: 251-263. [2] Ripmeester JA, Lu H, Moudrakovski IL, Dutrisac R, Wilson LD, Wright F, Dallimore S. Structure and composition of hydrate in sediment recovered from Mallik 5L-38, Mackenzie Delta, NWT, Canada: X-ray diffraction, Raman and Solid-state NMR spectroscopy, Geological Survey of Canada Bulletin 2005; 585: 89. [3] Lu H, Seo YT, Lee JW, Moudrakovski IL, Ripmeester JA, Chapman NR, Coffin RB, Gardner G, Pohlman J. Complex gas hydrate from the Cascadia margin. Nature 2007; 445: 303-306. [4] Schicks, JM, Ziemann MA, Lu H, Ripmeester, JA. Raman spectroscopic investigations on natural samples from IODP Expedition 311: indications for heterogeneous compositions in hydrate crystals. Submitted to Geophysical Research Letters.  [5] Lu H, Schicks JM, Moudrakovski IL, Udachin K, Ripmeester JA, Zhang M, Naumann R, Dutrisac R, Luzi M, Erzinger J. Laboratory-based characterization of gas hydrate samples recovered from northern Cascadia by IODP Expedition 311. Submitted to J. Geophys. Res.   [6] Lu H, Kawasaki T, Zeng H, Fujii T, Nakamizu M, Ripmeester JA. Sediment control on the saturation level of gas hydrate in natural environments. ICGH 6, Vancouver, July, 2008. [7] Tulk CA, Wright F, Ratcliffe CI, Ripmeester JA. Storage and handling of Natural Gas Hydrate. Bull. Geological Survey of Canada 1999; 544: 263-268. [8] Lu H, Dutrisac R, Ripmeester JA, Wright F, Uchida T. Gas hydrate saturation and its distribution in the sediments of Mallik 5L-38, MacKenzie Delta, 2004, N.W.T. Canada. Bulletin of the Geological Survey of Canada 2005; 585: 106. [9] Takeya S, Udachin KA, Ripmeester JA. Ab initio structure determination of gas hydrates and refinement of guest molecule positions by powder x-ray diffraction. ICGH 2008; this volume. [10] Udachin K, Lu H, Enright G, Ratcliffe CI, Chapman R, Riedel M, Spence G, Ripmeester, JA. Single-crystals of naturally occurring gas hydrates: the structures of methane and methane-mixed hydrocarbon hydrates. Angewandte Chemie International Edition 2007; 46: 8220-8222. [11] Moudrakovski IL, Luzi M, Kumar R, Lu H, Ripmeester JA. Experimental Solid State NMR of Gas Hydrates: Problems and Solutions. ICGH-2008; this volume. Schicks JM, Lu H, Ziemann M, Ripmeester JA. The characteristics of gas hydrates formed from H2S and CH4 under various conditions. ICGH 2008; this volume.  


Citation Scheme:


Citations by CSL (citeproc-js)

Usage Statistics

Country Views Downloads
United States 1 0
City Views Downloads
Ashburn 1 0

{[{ mDataHeader[type] }]} {[{ month[type] }]} {[{ tData[type] }]}
Download Stats



Customize your widget with the following options, then copy and paste the code below into the HTML of your page to embed this item in your website.
                            <div id="ubcOpenCollectionsWidgetDisplay">
                            <script id="ubcOpenCollectionsWidget"
                            async >
IIIF logo Our image viewer uses the IIIF 2.0 standard. To load this item in other compatible viewers, use this url:


Related Items