AREAL INFILTRATION MODELING OVER SOILS WITH SPATIALLY CORRELATED HYDRAULIC CONDUCTIVITIES

Theoretical analysis of the mean and variance of field scale infiltration downward soils. Analysis of mean infiltration rate time-dependent rainfall. Study soils and Monte-Carlo simulations for natural field: the soil is assumed to be vertically homogeneous while the saturated hydraulic conductivity is considered to vary randomly through the soil surface.