Water movement through Panoche clay loam soil

V Nielsen, J. M. Davidson, J. W. Biggar and R. J. Miller

Hilgardia, 1964, vol. 35, issue 17

Abstract: 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.

Keywords: Resource/Energy; Economics; and; Policy (search for similar items in EconPapers)
Date: 1964
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