Fig. 5 Variation in the observed hydraulic conductivity values at a depth of 0–38 mm at different water potentials with different rates of sludge application in a silty clay soil, estimated during the second draining cycle
Fig. 5 Variation in the observed hydraulic conductivity values at a depth of 0–38 mm at different water potentials with different rates of sludge application in a silty clay soil, estimated during the second draining cycle