Hydrological processes inferred from water table fluctuations, Walnut Creek, Iowa
In a shallow aquifer underlain by low permeable material, groundwater recharge (R), discharge to rivers or stream as baseflow (BF), and discharge to the atmosphere as evapotranspiration (ET) are related by a simple water balance equation, R - ET - BF = ΔS. Gathering information about these processes...
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Language: | English |
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University of Iowa
2009
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Online Access: | https://ir.uiowa.edu/etd/430 https://ir.uiowa.edu/cgi/viewcontent.cgi?article=1615&context=etd |