Geoscience Reference
In-Depth Information
Ibrahim, H. A. and Brutsaert, W. (1968). Intermittent infiltration into soils with hysteresis.
J. Hydraul.
Div., Proc. ASCE
,
94
, 113-137.
Irmay, S. (1954). On the hydraulic conductivity of unsaturated soils.
Trans. Amer. Geophys. Un.
,
35
,
463-467.
Jackson, R. D., Reginato, R. J. and VanBavel, C. H. M. (1965). Comparison of measured and calculated
hydraulic conductivities of unsaturated soils.
Water Resour. Res.
,
1
, 375-380.
Jackson, R. D., Reginato, R. J., Kimball, B. A. and Nakayama, F. S. (1974). Diurnal soil-water
evaporation: comparison of measured and calculated soil-water fluxes.
Soil Sci. Soc. Amer. Proc.
,
38
, 861-866.
Jacob, C. E. (1940). The flow of water in an elastic artesian aquifer.
Eos Trans. AGU
,
21
, 574-586.
(1950). Flow of ground water. In
Engineering Hydraulics
, ed. H. Rouse. New York: John Willey,
pp. 321-386.
Katul, G. G., Wendroth, O., Parlange, M. B., Puente, C. E., Folegatti, M. V. and Nielsen, D. R. (1993).
Estimation of in situ hydraulic conductivity function from nonlinear filtering theory.
Water
Resour. Res.
,
29
, 1063-1070.
Kimball, B. A., Jackson, R. D., Nakayama, F. S. and Idso, S. B. (1976). Comparison of field-measured
and calculated soil-heat fluxes.
Soil Sci. Soc. Amer. J.
,
40
, 18-25.
Klute, A. (1952). A numerical method for solving the flow equation for water in unsaturated materials.
Soil Sci.
,
73
, 105-116.
Kozeny, J. (1927). Uber kapillare Leitung des Wassers im Boden,
Sitzungsberichte. Akad. der
Wissensch. Wien, Math.-Naturw. Klass. Abt. 2a
,
136
, 271-306.
Lamb, H. (1932).
Hydrodynamics
, sixth edition. New York: Cambridge University Press.
Le Van Phuc and Morel-Seytoux, H. J. (1972). Effect of soil air movement and compressibility on
infiltration rates.
Soil Soc. Amer. Proc.
,
36
, 237-241.
Leamer, R. W. and Lutz, J. F. (1940). Determination of pore-size distribution in soils.
Soil Sci.
,
49
,
347-360.
Libardi, P. L., Reichardt, K., Nielsen, D. R. and Biggar, J. W. (1980). Simple field methods for
estimating soil hydraulic conductivity.
Soil Sci. Soc. Amer. J.
,
44
, 3-7.
Marshall, T. J. (1958). A relation between permeability and size distribution of pores.
J. Soil Sci.
,
9
,
1-8.
McMurdie, J. L. and Day, P. R. (1960). Slow tests under soil moisture suction.
Soil Sci. Soc. Amer.
Proc.
,
24
, 441-444.
Miller, R. D. and Bresler, E. (1977). A quick method for estimating soil water diffusivity functions.
Soil
Sci. Soc. Amer. Proc.
,
41
, 1021-1022.
Miller, R. J. and Low, P. F. (1963). Threshold gradient for water flow in clay systems.
Soil Sci. Soc.
Amer. Proc.
,
27
, 605-609.
Millington, R. J. and Quirk, J. P. (1964). Formation factor and permeability equations.
Nature
,
202
,
143-145.
Milly, P. C. D. (1984). A simulation analysis of thermal effects on evaporation from soil.
Water Resour.
Res.
,
20
, 1087-1098.
Morel-Seytoux, H. J. (1973). Two-phase flows in porous media.
Advan. Hydrosci.
,
9
, 119-202.
Mualem, Y. (1976). A new model for predicting the hydraulic conductivity of unsaturated porous
media.
Water Resour. Res.
,
12
, 513-522.
(1978). Hydraulic conductivity of unsaturated porous media: generalized macroscopic approach.
Water Resour. Res.
,
14
, 325-334.
Mualem, Y. and Miller, E. E. (1979). A hysteresis model based on an explicit domain-dependence
function.
Soil Sci. Soc. Amer. J.
,
43
, 1067-1073.
