dc.contributor.author |
May, F
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|
dc.contributor.author |
Bugan, Richard DH
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|
dc.contributor.author |
Mikes, D
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|
dc.contributor.author |
Jovanovic, Nebojsa
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dc.date.accessioned |
2012-01-06T08:58:13Z |
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dc.date.available |
2012-01-06T08:58:13Z |
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dc.date.issued |
2011-09 |
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dc.identifier.citation |
May, F., Bugan, R., Mikes, D. and Jovanovic, N. 2011. Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments. International Conference on Groundwater: Our source of security in an uncertain future, CSIR International Convention Centre, Pretoria, South Africa, 19-21 September 2011 |
en_US |
dc.identifier.uri |
http://gwd.org.za/sites/gwd.org.za/files/list_papers_posters_accepted_march_2011.pdf
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|
dc.identifier.uri |
http://hdl.handle.net/10204/5440
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|
dc.description |
International Conference on Groundwater: Our source of security in an uncertain future, CSIR International Convention Centre, Pretoria, South Africa, 19-21 September 2011 |
en_US |
dc.description.abstract |
Freshwater availability is being threatened in arid and semi arid areas. As a result of this and the over exploitation of surface freshwater sources, groundwater resources are increasingly receiving more attention as an alternative source of water. This investigation aims to identify preferential flow paths in fractured rock environments. Time-lapse Electrical Resistivity Tomography (TLERT, Lund Imaging System), is regarded as a suitable method for identifying preferential water flow. |
en_US |
dc.language.iso |
en |
en_US |
dc.relation.ispartofseries |
Workflow request;7831 |
|
dc.subject |
Preferential flow |
en_US |
dc.subject |
Time lapse resistivity |
en_US |
dc.subject |
2D electrical resistivity tomography |
en_US |
dc.subject |
Infiltration rate |
en_US |
dc.subject |
Fractured rocks |
en_US |
dc.subject |
Groundwater |
en_US |
dc.subject |
Freshwater |
en_US |
dc.title |
Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments |
en_US |
dc.type |
Conference Presentation |
en_US |
dc.identifier.apacitation |
May, F., Bugan, R. D., Mikes, D., & Jovanovic, N. (2011). Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments. http://hdl.handle.net/10204/5440 |
en_ZA |
dc.identifier.chicagocitation |
May, F, Richard DH Bugan, D Mikes, and Nebojsa Jovanovic. "Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments." (2011): http://hdl.handle.net/10204/5440 |
en_ZA |
dc.identifier.vancouvercitation |
May F, Bugan RD, Mikes D, Jovanovic N, Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments; 2011. http://hdl.handle.net/10204/5440 . |
en_ZA |
dc.identifier.ris |
TY - Conference Presentation
AU - May, F
AU - Bugan, Richard DH
AU - Mikes, D
AU - Jovanovic, Nebojsa
AB - Freshwater availability is being threatened in arid and semi arid areas. As a result of this and the over exploitation of surface freshwater sources, groundwater resources are increasingly receiving more attention as an alternative source of water. This investigation aims to identify preferential flow paths in fractured rock environments. Time-lapse Electrical Resistivity Tomography (TLERT, Lund Imaging System), is regarded as a suitable method for identifying preferential water flow.
DA - 2011-09
DB - ResearchSpace
DP - CSIR
KW - Preferential flow
KW - Time lapse resistivity
KW - 2D electrical resistivity tomography
KW - Infiltration rate
KW - Fractured rocks
KW - Groundwater
KW - Freshwater
LK - https://researchspace.csir.co.za
PY - 2011
T1 - Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments
TI - Using DC electrical resistivity tomography to quantify preferential flow in fractured rock environments
UR - http://hdl.handle.net/10204/5440
ER -
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en_ZA |