A Simplified Moisture Model
Computationally efficient _-based model
Capillary rise during drying events
Gravity drainage during wetting events
Lateral redistribution
No assumption of water table
Amenable to the Kalman-filter
Buckingham Darcy Equation
q = K___+K
Approximate Buckingham Darcy Equation
q = K_VDF+K
where VDF = Vertical Distribution Factor
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