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Richards equation
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Definition
Mathematical equation describing water flow in partially saturated soils by relating volumetric soil water content to constitutive relations
Publications (4)
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The effects of spatial and temporal resolution of gridded meteorological forcing on watershed hydrological responses
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On the similarity of hillslope hydrologic function: a clustering approach based on groundwater changes
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Estimation of Evapotranspiration Rates and Root Water Uptake Profiles From Soil Moisture Sensor Array Data
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