“…This is typical for the upper, ploughed layer of agricultural soils. Temporal variation in hydraulic conductivity is caused by the growth and decay of plant roots (Meek et al, 1992), activity of soil organisms (Beven and Germann, 1982;Willoughby et al, 1996), precipitation that forms surface crusts (Messing and Jarvis, 1993), alternate shrinking and swelling processes (Messing and Jarvis, 1990;Bagarello et al, 1999), and agricultural activities, such as tillage and wheel-traffic compaction (Ankeny et al, 1990;Logsdon and Jaynes, 1996). Because many factors influence the hydraulic conductivity, a temporal pattern is usually difficult to observe (Logsdon, 1993).…”