Soil and Unsaturated Flow

External reference: https://openalex.org/T10716

  1. 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.
  2. 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.