Contaminant transport through abandoned boreholes in fractured rock
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 contamina...
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ndltd-UBC-oai-circle.library.ubc.ca-2429-105302018-01-05T17:35:24Z Contaminant transport through abandoned boreholes in fractured rock Burns, Sean Raymond Patrick 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. Science, Faculty of Earth, Ocean and Atmospheric Sciences, Department of Graduate 2009-07-09T21:30:10Z 2009-07-09T21:30:10Z 2000 2000-11 Text Thesis/Dissertation http://hdl.handle.net/2429/10530 eng 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. 7492989 bytes application/pdf |
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English |
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Others
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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. === Science, Faculty of === Earth, Ocean and Atmospheric Sciences, Department of === Graduate |
author |
Burns, Sean Raymond Patrick |
spellingShingle |
Burns, Sean Raymond Patrick Contaminant transport through abandoned boreholes in fractured rock |
author_facet |
Burns, Sean Raymond Patrick |
author_sort |
Burns, Sean Raymond Patrick |
title |
Contaminant transport through abandoned boreholes in fractured rock |
title_short |
Contaminant transport through abandoned boreholes in fractured rock |
title_full |
Contaminant transport through abandoned boreholes in fractured rock |
title_fullStr |
Contaminant transport through abandoned boreholes in fractured rock |
title_full_unstemmed |
Contaminant transport through abandoned boreholes in fractured rock |
title_sort |
contaminant transport through abandoned boreholes in fractured rock |
publishDate |
2009 |
url |
http://hdl.handle.net/2429/10530 |
work_keys_str_mv |
AT burnsseanraymondpatrick contaminanttransportthroughabandonedboreholesinfracturedrock |
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1718588580366909440 |