MODELING WATER-MOVEMENT IN DRAINED CLAY SOIL .1. DESCRIPTION OF THE MODEL, SAMPLE OUTPUT AND SENSITIVITY ANALYSIS

[1] AITCHISON G. D., 1953, Australian Journal of Applied Science, V4, P244

[2] BEVEN K, 1981, J SOIL SCI, V32, P15

[3] MACROPORES AND WATER-FLOW IN SOILS [J]. WATER RESOURCES RESEARCH, 1982, 18 (05) : 1311 - 1325

[4] BEVEN K, 1980, 65 I HYDR REP

[5] CASE-STUDY ON INFILTRATION INTO DRY CLAY SOIL .1. MORPHOLOGICAL OBSERVATIONS [J]. GEODERMA, 1978, 20 (01) : 27 - 40

[6] FUNCTION OF DIFFERENT TYPES OF MACROPORES DURING SATURATED FLOW THROUGH 4 SWELLING SOIL HORIZONS [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1977, 41 (05) : 945 - 950

[7] CHILDS EC, 1969, INTRO PHYSICAL BASIS

[8] Chong S. K., 1983, Advances in infiltration., P82

[9] NUMERICAL STUDY OF THE EFFECTS OF NON-CAPILLARY-SIZED PORES UPON INFILTRATION [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1979, 43 (05) : 851 - 856

[10] FITZPATRICK E A, 1985, Soil Use and Management, V1, P70, DOI 10.1111/j.1475-2743.1985.tb00660.x

[1] AITCHISON G. D., 1953, Australian Journal of Applied Science, V4, P244

[2] BEVEN K, 1981, J SOIL SCI, V32, P15

[3] MACROPORES AND WATER-FLOW IN SOILS [J]. WATER RESOURCES RESEARCH, 1982, 18 (05) : 1311 - 1325

[4] BEVEN K, 1980, 65 I HYDR REP

[5] CASE-STUDY ON INFILTRATION INTO DRY CLAY SOIL .1. MORPHOLOGICAL OBSERVATIONS [J]. GEODERMA, 1978, 20 (01) : 27 - 40

[6] FUNCTION OF DIFFERENT TYPES OF MACROPORES DURING SATURATED FLOW THROUGH 4 SWELLING SOIL HORIZONS [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1977, 41 (05) : 945 - 950

[7] CHILDS EC, 1969, INTRO PHYSICAL BASIS

[8] Chong S. K., 1983, Advances in infiltration., P82

[9] NUMERICAL STUDY OF THE EFFECTS OF NON-CAPILLARY-SIZED PORES UPON INFILTRATION [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1979, 43 (05) : 851 - 856

[10] FITZPATRICK E A, 1985, Soil Use and Management, V1, P70, DOI 10.1111/j.1475-2743.1985.tb00660.x