Surface Water-Groundwater Relations for Open Channelsby Herman Bouwer, USDA, United States,
Abstract: For losing channels with clean wetted perimeters (no clogging layers), the seepage rate varies essentially linearly with depth to groundwater if the groundwater is relatively shallow, but is essentially independent of depth to groundwater if the groundwater is relatively deep.
Subject Headings: Water table | Fluid flow | Pipe blockage | Seepage | Linear functions | Surface water | Open channels
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