Research Article
Jun 1977
Effect of Leaching Fraction on River Salinity
Authors: Donald L. Suarez and James D. RhoadesAuthor Affiliations
Publication: Journal of the Irrigation and Drainage Division
Volume 103, Issue 2
Abstract
The effects of 0.10 and 0.40 irrigation leaching fraction management on amounts of salt precipitated in the soil and river channel and compositions of drainage and river water have been calculated for each of the three river types routed through nine successive hypothetical irrigated valleys. These calculations assume dissolution of CaCO3 (in the soil) and return of irrigation drainage waters. Rivers undersaturated with CaCO3 were slightly less saline under low versus high leaching. Rivers saturated with CaCO3 were unaffected by irrigation management. Rivers saturated with CaCO3 and approaching saturation with gypsum experienced substantial reductions in salinity under low leaching compared to high leaching. For CaCO3-saturated rivers, a change from high to low leaching results in a rootzone soil porosity reduction of 0.008% more per year. For rivers that result in the precipitation of gypsum, soil porosity was reduced about 0.08% more per year for low as compared to high leaching.
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Published In
Journal of the Irrigation and Drainage Division
Volume 103 • Issue 2 • June 1977
Pages: 245 - 257
Copyright
© 1977 American Society of Civil Engineers.
History
Published in print: Jun 1977
Published online: Feb 11, 2021
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Authors
Affiliations
Donald L. Suarez
Geochemist, U.S. Salinity Lab., Agricultural Research Service, U.S. Dept. of Agr., Riverside, Calif
James D. Rhoades
Supervisory Soil Scientist, U.S. Salinity Lab., Agricultural Research Service, U.S. Dept. of Agr., Riverside, Calif.
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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.