Modifying the Feddes plant water uptake function to retain a small non-zero water loss rate under anaerobic conditions fixes systematic soil moisture over-prediction in waterlogged Irish grasslands.
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A systematic evaluation of the Richards equation for predicting soil moisture in Irish grasslands
Modifying the Feddes plant water uptake function to retain a small non-zero water loss rate under anaerobic conditions fixes systematic soil moisture over-prediction in waterlogged Irish grasslands.