| Title | Water movement through Panoche clay loam soil |
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Water movement through Panoche clay loam is explained on the basis of the soil-water properties within the profile. Laboratory-determined soil water content-tension relations from 3-inch cores taken from the field every 6 inches to 5 feet were shown to provide reliable estimates of soil water behavior. Water management practices relative to favorable plant-available soil water and favorable salt balance within the profile are discussed. |
| Authors |
Nielsen, D. R. : D. R. Nielsen was Associate Professor of Orrigation and Associate Irrigationist, Department of Irrigation, Davis
Davidson, J. M. : J. M. Davidson was Laboratory Technician, Davis
Biggar, J. W. : J. W. Biggar was Associate Irrigationist and Lecturer, Davis
Miller, R. J. : R. J. Miller was Assistant Irrigationist, Five Points.
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| Publication Date | Jul 1, 1964 |
| Date Added | Sep 17, 2014 |
| Copyright | © The Regents of the University of California |
| Copyright Year | 1964 |
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