Long-term transient regional groundwater flow in a heterogeneous mature basin with large hydraulic conductivity contrasts
A finite element model is developed to solve the two-dimensional, transient, groundwater flow equation for the purpose of describing the development of regional flow over geologic time, in response to erosional modifications of the land surface, in a mature basin with large hydraulic conductivity co...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/25879 |