A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface
The Edwards aquifer in south-central Texas, U.S., composed of faulted carbonate bedrock, contains freshwater and saline water. In aquifers that are used as a source of drinking water and that contain fresh and saline waters, saline-water intrusion can result in degradation of water quality. Yet, in...
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| Format: | Others |
| Language: | en |
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LSU
2012
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| Online Access: | http://etd.lsu.edu/docs/available/etd-05312012-212545/ |