Abstract
The theory basic to the solution of problems in infiltration and redistribution of water in porous media has been evolved and experimentally verified. As yet, application of this theory to the solution of field problems has been limited. If comprehensive solutions to hydrologic problems, including water pollution, are to be obtained, the theoretical base established by the soil physicist must be employed. In most instances heterogeneity of the system has been a formidable barrier to the solution of such problems. Therefore, most studies have dealt with homogeneous, isotropic, one-dimension, semi-infinite systems with vertical flow and a constant initial water content throughout the profile. This is documented in a reasonably current review by Freeze (1969).
Contribution from the Southern Branch, Soil and Water Conservation Research Division, Agricultural Research Service, USDA, Watkinsville, Georgia, U.S.A., in cooperation with the University of Georgia Agricultural Experiment Stations.
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References
Bertrand, A. R., Parr, J. F.: Design and operation of the Purdue sprinkling infiltrometer. Indiana Agr. Exp. Sta. Res. Bul. 723 (1961).
Dixon, R. M., Peterson, A. E.: A vacuum system for accumulating runoff from infiltrometers. Soil Sci. Soc. Amer. Proc. 32, 123–125 (1968).
Doering, E. J.: Soil-water diffusivity by the one-step method. Soil Sci. 99, 322–326 (1964).
Freeze, Allen, R.: The mechanism of natural ground-water recharge and discharge. I. One-dimensional, vertical, unsteady, unsaturated flow above a recharging or discharging ground-water flow system. Water Resources Res. 5, 153–171 (1969).
Gardner, W. R.: Note on the separation and solution of diffusion type equations. Soil Sci. Soc. Amer. Proc. 26, 404 (1962).
Green, R. E. et al.: Estimates of field infiltration by numerical solution of the moisture flow equation. Soil Sci. Soc. Amer. Proc. 28, 15–18 (1964).
Hanks, R. J., Klute, A., Bresler, E.: A numeric method for estimating infiltration, redistribution, drainage and evaporation of water from soil. Water Resources Res. 5, 1064–1069 (1969).
Hanks, R. J., Bowers, S. A.: Numerical solution of the moisture flow equation for infiltration into layered soils. Soil Sci. Amer. Proc. 26, 530–534 (1962).
Miller, D. E., Gardner, W. H.: Water infiltration into stratified soil. Soil Sci. Soc. Amer. Proc. 26, 115–119(1962).
Wang, F. C., Lakshiminarayana, V.: Mathematical simulation of water movement through unsaturated-non-homogeneous soil. Soil Sci. Soc. Amer. Proc. 26, 115–119 (1968).
Whisler, F. D., Klute, A.: The numerical analysis of infiltration, considering hysteresis, into a vertical soil column at equilibrium under gravity. Soil Sci. Soc. Amer. Proc. 29, 489–494 (1965).
Whislér, F. D., Klute, A.: Analysis of infiltration into stratified soil columns. In: Proc. symp. water in the unsaturated zone. Wageningen 1966, pp. 451–470. Paris: UNESCO 1969.
Whisler, F. D. Watson, K. K.: Analysis of infiltration into draining porous media. A.S.C.E. J. Irrigation and Drainage 95, 481–491 (1969).
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Bruce, R.R., Whisler, F.D. (1973). Infiltration of Water into Layered Field Soils. In: Hadas, A., Swartzendruber, D., Rijtema, P.E., Fuchs, M., Yaron, B. (eds) Physical Aspects of Soil Water and Salts in Ecosystems. Ecological Studies, vol 4. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-65523-4_9
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DOI: https://doi.org/10.1007/978-3-642-65523-4_9
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