Topographic and seasonal variations of unsaturated hydraulic conductivity as measured by tension disc infiltrometers at the field scale

Infiltration and sheet flow depend mainly on hydraulic conductivity under nearly saturated conditions which can Vary in space and time. We have studied the variation in relation to the topography at different stages of a cultivation year to understand the origin of sheet flow over the land where maize is grown. The sampling was done to a complete factorial design with two landscape positions, upslope and downslope, two sites in relation to wheeling, no and under wheeling, and three dates in relation to soil surface changes and agricultural operations, June and October 1995 and April 1996. Four measurements were randomly distributed on each of the four sites and each of the three dates. The hydraulic conductivity was measured with a tension disc infiltrometer controlling tension at the soil surface. Steady-state infiltration rates were measured at four soil water tensions: 0.1, 0.3, 0.6 and 1.5 kPa. We also measured bulk density and soil moisture content. Hydraulic conductivity decreased during the year at all tensions by a factor of 2-3 where there was no wheeling, and a factor of 1-6 under wheeling. This decrease was greater downslope than upslope, particularly under traffic. The topographic effect was less than that of time but significant. Whereas the hydraulic conductivity was similar over the field at the beginning of the crop cycle (June), it differed according to the landscape position at the end (April), especially under traffic. These topographic variations of the hydraulic conductivity may be due to slight variations of soil components and hydric conditions in the particular case studied. They are important in relation to the characteristics of rainfall and runoff and help explain the spatial and temporal distributions of sheet flow and erosional processes that themselves may contribute to a redistribution of soil particles and induce feedback effects on sheet flow and infiltration.