Research Article
Sep 1963
Separation of Evapotranspiration and Deep Percolation
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VIEW THE REPLYPublication: Journal of the Irrigation and Drainage Division
Volume 89, Issue 3
Abstract
Deep percolation losses of water from the root zone under a growing crop continue for a considerable time. Soil moisture depletion methods of determining evapotranspiration include these deep percolation losses. By assuming that deep percolation rate is a function of soil moisture content for a given soil profile, soil moisture depletion data can be separated into components of evapotranspiration and deep percolation. Data from two crops and two soils when separated also show that evapotranspiration rates decrease as soils become drier. Measurements of soil moisture depletions from covered areas and adjacent cropped areas are needed for the analysis. On a sandy loam planted to alfalfa, one-third of the soil moisture depletion for an 18-day period was due to deep percolation. Frequent irrigations that completely wet the soil profile increase evapotranspiration and deep percolation.
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Published In
Journal of the Irrigation and Drainage Division
Volume 89 • Issue 3 • September 1963
Pages: 77 - 88
Copyright
© 1963 American Society of Civil Engineers.
History
Published in print: Sep 1963
Published online: Feb 11, 2021
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Authors
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Lyman S. Willardson, AM.ASCE
Agric. Engr., Southwest Branch, Soil and Water Conservation Research Div., Agric. Research Service, U. S. Dept. of Agric., Washington, D. C.
Wendell L. Pope
Asst. Prof., Mathematics, Computer Services Supervisor, Dept. of Applied Statistics and Computer Science, Utah State Univ., Logan, Utah
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.