“…In this equation, D ( θ , t ) and K ( θ , t ) are time‐dependent soil hydraulic parameters, cm 2 ·min −1 ; S ( z,t ) is the RWU source/sink term, cm 3 ·cm −3 ·d −1 ; θ is the soil moisture content, cm 3 ·cm −3 ; z is the depth of soil, cm; and t is the experimental duration, d. The forms of D ( θ , t ) and K ( θ , t ) can be determined through continuous soil experiments described in a previous study (Liao, Wu, Ren, & Yang, ), and the parameters for equation θ = θ re + ( θ sa − θ re ) ∕ [1 + ( αh ) d ] f fitted by the soil water retention curve are listed in Table . We ignored the changes in soil volume affected by the SAP; therefore, the SAP‐treated soil was regarded as a rigid soil with time‐dependent soil hydraulic parameters.…”