Early stage infiltration of water into horizontal and vertical soil columns
Authors
T. MiyazakiD. R. Nielsen
J. L. MacIntyre
Authors Affiliations
T. Miyazaki was former Visiting Scientist, is presently an Agricultural Engineer, Shikoku Agricultural Experiment Station, Ikano-cho, Zentsuji-shi, Kagawa-ken, Japan; D. R. Nielsen was Professor of Soil and Water Science, Land, Air, and Water Resources, and Soil and Water Scientist in the Experiment Station, University of California, Davis; J. L. MacIntyre was Staff Research Associate, Land, Air, and Water Resources, University of California, Davis.Publication Information
Hilgardia 52(6):1-24. DOI:10.3733/hilg.v52n06p024. June 1984.
PDF of full article, Cite this article
Abstract
Water content distributions during horizontal, vertical-up, and vertical-down infiltration into air-dry soil, were measured experimentally using gamma radiation attenuation equipment. A sufficient number of soil columns were analyzed to ascertain fiducial limits of both measured and calculated soil water properties and parameters. The first three coefficient functions of Philip’s solution of the Richards’ flow equation applied to infiltration as well as to the soil hydraulic conductivity and soil water diffusivity as functions of soil water content were ascertained from the measured water content distributions.
Literature Cited
Fritton D. D. Resolving time, mass absorption coefficient and water content with gamma-ray attenuation. Soil Sci. Soc. Am. Proc. 1969. 33:651-655.
Nielsen D. R., Kirkham D., Van Wijk W. R. Diffusion equation calculations of field soil water infiltration profiles. Soil Sci. Soc. Am. Proc. 1961. 25:165-168.
Nielsen D. R., Vachaud G. Infiltration of water into vertical and horizontal soil columns. J. Indian Soc. Soil Sci. 1965. 13:15-23.
Philip J. R. Numerical solution of equation of the diffusion type with diffusivity concentration-dependent. Trans. Faraday Soc. 1955. 51:885-892. DOI: 10.1039/tf9555100885 [CrossRef]
Philip J. R. Numerical solution of equation of the diffusion type with diffusivity concentration-dependent. Australian J. Phys. 1957a. 10:29-42. DOI: 10.1039/tf9555100885 [CrossRef]
Philip J. R. The theory of infiltration; 1. The infiltration equation and its solution. Soil Sci. 1957b. 83:345-357. DOI: 10.1097/00010694-200606001-00009 [CrossRef]
Philip J. R. Theory of infiltration. Adv. Hydrosci. 1969a. 5:215-290. DOI: 10.1097/00010694-195806000-00007 [CrossRef]
Philip J. R. The dynamics of capillary rise 1969b. pp.559-564. Proc. Symposium Water in the Unsaturated Zone Wageningen (1966), IASH/UNESCO, II
Reginato R. J., Van Bavel C. H. M. Soil water measurement with gamma attenuation. Soil Sci. Soc. Am. Proc. 1964. 28:721-724.
Selim H. M., Kirkham D., Amemiya M. A comparison of two methods for determining soil water diffusivity. Soil Sci. Soc. Am. Proc. 1970. 34:14-18.
Youngs E. G. Moisture profiles during vertical infiltration. Soil Sci. 1957. 84:283-290. DOI: 10.1097/00010694-195710000-00003 [CrossRef]
Also in this issue:
Biotechnology: New benefits, new questionsScience briefs
UC contributes biotech breakthroughs
Public germplasm development at a crossroads: Biotechnology and intellectual property
Transgenic Bt crops and resistance: Broadscale use of pest-killing plants to be true test
Success of mite-fighting tactics evaluated: In Central Valley, early-season release of Willamette mites confers resistance on wine grapes
Native gray ant has beneficial role in peach orchards
Feasibility of producing pear wine: Pears produce premium sparkling wine
Cost analysis: Méthod champenoise sparkling pear wine costs most, but offers highest quality