- Library Home /
- Search Collections /
- Open Collections /
- Browse Collections /
- UBC Theses and Dissertations /
- Contaminant transport through abandoned boreholes in...
Open Collections
UBC Theses and Dissertations
UBC Theses and Dissertations
Contaminant transport through abandoned boreholes in fractured rock Burns, Sean Raymond Patrick
Abstract
Abandoned exploration boreholes are commonly found around mine sites in a fractured crystalline rock environment. If the abandoned boreholes have not been properly decommissioned they have the potential to create connections through the rock fractures and influence ground water flow and contaminant transport. A fully three-dimensional discrete fracture model is used to investigate the impact of abandoned boreholes on contaminant transport from a waste-rock pile overlying a fractured rock mass. Dissolved contaminants travel through the fractured rock mass under the influence of a subhorizontal regional hydraulic gradient towards a downstream compliance boundary. A number of different fracture geometries are investigated to gain an understanding of the field situations in which abandoned boreholes can be expected to have an impact. The effect of fracture density, transmissivity contrasts, and borehole diameter and location are studied. The simulation results show that vertical abandoned boreholes are most likely to have an impact when large, sub-horizontal, high-transmissivity features are present in the network. Low fracture density, aperture variability, relatively high horizontal transmissivity, and the presence of major features in the fracture network all lead to abandoned boreholes having a greater overall influence. If an abandoned borehole is transversely offset from the central flow line passing through the source zone the contaminant plume can migrate towards the borehole in a direction not predicted by the average regional hydraulic gradient. In field-scale fracture networks smaller borehole diameters leads to shorter breakthrough times and higher contaminant concentrations at the downstream boundary due to the interplay between the fracture network and borehole void space. The presence of abandoned boreholes can be expected to have important implications in the design of monitoring networks to detect ground water contamination when these fracture network and abandoned borehole properties exist.
Item Metadata
Title |
Contaminant transport through abandoned boreholes in fractured rock
|
Creator | |
Publisher |
University of British Columbia
|
Date Issued |
2000
|
Description |
Abandoned exploration boreholes are commonly found around mine sites in a fractured
crystalline rock environment. If the abandoned boreholes have not been properly
decommissioned they have the potential to create connections through the rock fractures
and influence ground water flow and contaminant transport. A fully three-dimensional
discrete fracture model is used to investigate the impact of abandoned boreholes on
contaminant transport from a waste-rock pile overlying a fractured rock mass. Dissolved
contaminants travel through the fractured rock mass under the influence of a subhorizontal
regional hydraulic gradient towards a downstream compliance boundary. A
number of different fracture geometries are investigated to gain an understanding of the
field situations in which abandoned boreholes can be expected to have an impact. The
effect of fracture density, transmissivity contrasts, and borehole diameter and location are
studied. The simulation results show that vertical abandoned boreholes are most likely to
have an impact when large, sub-horizontal, high-transmissivity features are present in the
network. Low fracture density, aperture variability, relatively high horizontal
transmissivity, and the presence of major features in the fracture network all lead to
abandoned boreholes having a greater overall influence. If an abandoned borehole is
transversely offset from the central flow line passing through the source zone the
contaminant plume can migrate towards the borehole in a direction not predicted by the
average regional hydraulic gradient. In field-scale fracture networks smaller borehole
diameters leads to shorter breakthrough times and higher contaminant concentrations at
the downstream boundary due to the interplay between the fracture network and borehole
void space. The presence of abandoned boreholes can be expected to have important
implications in the design of monitoring networks to detect ground water contamination
when these fracture network and abandoned borehole properties exist.
|
Extent |
7492989 bytes
|
Genre | |
Type | |
File Format |
application/pdf
|
Language |
eng
|
Date Available |
2009-07-09
|
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 |
10.14288/1.0089516
|
URI | |
Degree | |
Program | |
Affiliation | |
Degree Grantor |
University of British Columbia
|
Graduation Date |
2000-11
|
Campus | |
Scholarly Level |
Graduate
|
Aggregated Source Repository |
DSpace
|
Item Media
Item Citations and Data
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.