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Effects of Effluent Irrigation on Seal Formation, Infiltration, and Soil Loss during Rainfall

Institute of Soil, Water and Environmental Sciences, the Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel

View larger version (32K): [in a new window]   Fig. 1. Mean infiltration rates as functions of cumulative rainfall for the two soils irrigated with fresh-water or effluent at two initial conditions. Bars indicate one standard deviation.

View larger version (22K): [in a new window]   Fig. 2. Mean concentrations of clay in the leachate for the two soils irrigated with fresh-water and effluent at two initial conditions vs. the cumulative leachate depth. Bars indicate one standard deviation.

View larger version (22K): [in a new window]   Fig. 3. Mean concentration of dissolved organic matter (DOM) in the leachate for the two soils irrigated with fresh-water and effluent at two initial conditions vs. cumulative leachate depth. Bars indicate standard deviation.

View larger version (21K): [in a new window]   Fig. 4. Sodium adsorption ratio (SAR) in the leachate for the two soils irrigated with fresh-water and effluent at two initial conditions vs. cumulative leachate depth. Bars indicate one standard deviation.

View larger version (17K): [in a new window]   Fig. 5. Total soil loss during the entire rainstorm for the two soils irrigated with effluent or fresh-water at two initial conditions. Bars indicate standard deviation. Different lowercase letters indicate statistically significant (at 0.05% level) differences between irrigation water quality within soil type and initial condition, and different uppercase letters indicate statistically significant (at 0.05% level) differences between initial conditions within soil type and irrigation water quality.