sensitivity analysis of different infiltration equations and their coefficients under various initial soil moisture and ponding depth

infiltration is a complex process that changed by initial moisture and water head on the soil surface. the main objective of this study was to estimate the coefficients of infiltration equations, kostiakov-lewis, philip and horton, and evaluate the sensitivity of these equations and their coefficients under various initial conditions (initial moisture soil) and boundary (water head on soil surface). therefore, one-and two-dimensional infiltration for basin (or border) irrigation were simulated by changing the initial soil moisture and water head on soil surface from irrigation to other irrigation using the solution of the richards’ equation (hydrus model). to determine the coefficients of infiltration equations, outputs of the hydrus model (cumulative infiltration over time) were fitted using the excel solver. comparison of infiltration sensitivity equations and their coefficients in one-and two-dimensional infiltration showed infiltration equations and their sensitivity coefficients were similar function but quantitatively in most cases sensitive two-dimensional equations and their coefficients were greater than one dimension. in both dimensions the soil adsorption coefficient philip equation as the sensitive coefficient and horton equation as the sensitive equation under various initial moisture soil and water head on soil surface were identified.