Hydrogeologic controls on underflow in alluvial valleys : implications for Texas water law
Groundwater flow in alluvial valleys consists of two components, baseflow and underflow. The baseflow component of the Darcy flux flows normal to the river and contributes to the surface flow. The underflow component moves downstream in the same direction as the river but at a much slower rate. Unde...
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| Format: | Others |
| Language: | English |
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2013
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| Online Access: | http://hdl.handle.net/2152/20847 |