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and infiltrates to the water table or if permeability varies laterally travels downslope. Throughflow usually occurs during peak hydrologic events (such as high precipitation). Flow rates are dependent on the hydraulic conductivity of the geologic medium.
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zone, typically through a highly permeable geologic unit overlying a less permeable one. Water thus returns to the surface, as return flow, before or on entering a stream or groundwater. Once water infiltrates into the soil, it is still affected by
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66:Applied Hydrogeology
64:Fetter, C. (2001).
126:Physical geography
89:Selby, M. (2005).
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136:Hydrogeology
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115:Categories
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46:References
121:Hydrology
26:interflow
18:hydrology
39:gravity
32:in the
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30:water
95:ISBN
70:ISBN
34:soil
16:In
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