JEQ Journal of Natural Resources and Life Sciences Education
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Published in J Environ Qual 4:73-79 (1975)
© 1975 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Calculated Drainage Water Compositions and Salt Burdens Resulting from Irrigation with River Waters in the Western United States1

J. D. Oster and J. D. Rhoades2

ABSTRACT

Drainage water compositions were calculated with a computer simulation model from irrigation water compositions, leaching fractions, aragonite and gypsum solubilities, and measured partial pressure of CO2. The calculated compositions were compared with measured values obtained from lysimeters filled with Pachappa soil, cropped with alfalfa, and irrigated with eight synthetic waters typical of rivers in the western U. S. Linear regression analysis of predicted vs. measured values for Na+ and SO42- concentrations, sodium-adsorption-ratio, electrical conductivity, and salt burden resulted in essentially one-to-one relationships. The gain in salt burden of drainage water at high leaching fractions due to mineral dissolution was adequately described by assuming the soil solution was saturated with respect to aragonite. Some evidence for Mg2+ precipitation was found.

The utility of the simulation model is demonstrated for evaluating the salinity, sodicity, and pollution hazards of irrigation waters. The evaluation of irrigation water quality in terms of minimum leaching fractions commensurate with maintaining satisfactory salinity, and sodicity levels is illustrated using recent crop tolerance data for alfalfa and the hydraulic conductivity characteristics of several representative soils. For salt-tolerant plants leaching fractions between 0.05 to 0.1 should be safe for six of the eight waters. Salt burdens of drainage waters are predicted to decrease with decreasing leaching fraction and partial pressure of CO2. The predicted relative decrease in salt burden ranged from 0.32 to 0.85 for a decrease in leaching fraction from 0.33 to 0.04.

Key Words: mineral dissolution • leaching fraction • salinity and sodicity hazard • carbon dioxide • environmental pollution • computer modeling


NOTES

1 Contribution from the U. S. Salinity Laboratory, Agricultural Research Service, USDA, Riverside, Calif. 92502.

2 Soil Scientists.

Received for publication March 4, 1974.





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1975 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.