Soil and Unsaturated Flow
External reference: https://openalex.org/T10716
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Temporal linearization can bias root water uptake estimates Temporal linearization approximations for estimating root water uptake from soil-water flux gradients fail under dynamic field conditions, introducing substantial systematic errors in hydraulic.
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Freeze–thaw reshapes water, salt, and heat in saline farmland soil Freeze-thaw driven water-salt redistribution in saline farmland soils: quantified hydrothermal parameters and coupled migration mechanisms from field-laboratory verification.

