A comparison of deep and shallow drain tile for reduction of soil salinity in Imperial Valley
Authors
F. E. RobinsonJ. N. Luthin
Authors Affiliations
Frank E. Robinson is Assistant Water, Scientist, Imperial Valley Field Station El Centro; James N. Luthin is Professor of Irrigation and Civil Engineering, Department of Water Science and Engineering, University of California Davis.Publication Information
Hilgardia 21(2):2-4. DOI:10.3733/ca.v021n02p2. February 1967.
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Abstract
In these tests, more salt was removed per unit of time by constant flooding than with intermittent flooding — indicating this treatment would be preferred where land values are higher or water is inexpensive. However, intermittent irrigation removed more salt per unit of water applied—indicating that where water is expensive, or land values low, this would be the better treatment. The shallow tile increased the rate of salt removal from the first and fourth foot of soil in the intermittent treatment, and for all depths except the fourth foot, under the constant flooding treatment. For soils having a less permeable layer at shallow depths, the use of shallow drain lines in addition to deep lines will increase the leaching of the soil and will help salinity control.
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