JEQ Journal of Natural Resources and Life Sciences Education
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Published in J Environ Qual 19:302-311 (1990)
© 1990 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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Selenium Immobilization in a Pond Sediment at Kesterson Reservoir

Robert H. B. Long*

Golder Associates, 1451 Harbor Bay Pkwy., Suite 1000, Alameda, CA 94501;

Sally M. Benson, Tetsu K. Tokunaga and Andrew Yee

Earth Sciences Division, Bldg. 50E, Lawrence Berkeley Lab., Berkeley, CA 94720.

* Corresponding author.

ABSTRACT

Kesterson Reservoir, Merced County, CA, a disposal facility for agricultural drain water, became the object of intense scientific investigation following discovery in 1983 that Se-laden agricultural drain water was having serious effects on the reproductive success of waterfowl. A remedial measure involving permanent flooding with low-Se water, aimed at taking advantage of low Se solubility under reducing conditions, was proposed as a means of limiting Se movement into groundwater and biota. A field experiment was undertaken to evaluate the feasibility of the proposed remedial measure, its impact on the quality of shallow groundwater and for quantifying Se immobilization and transport through a newly flooded pond bottom soil. Extensive soil water and groundwater sampling demonstrated that although initial soluble Se concentrations in the top 1.22 m (4 ft) of soil typically ranged from approximately 1000 to 3000 µg L–1, Se concentrations declined dramatically after flooding and elevated concentrations below 1.22 m were observed at only one of five sampling sites. Analysis of the temporal and spatial changes in the distribution of dissolved Se and Cl indicated that 66 to 108% of the initial soluble Se present in the top 1.22 m was immobilized shortly after flooding. These estimates were consistent with the low Se concentrations observed in shallow monitoring wells. The extent to which Se immobilization occurred correlated inversely with average pore water velocity. Data presented suggest that reducing conditions in the newly flooded soils lead to the microbially mediated transformation of selenate to less soluble or mobile forms.


NOTES

Contribution of the Earth Sciences Division, Lawrence Berkeley Lab.

Received for publication November 17, 1988.





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The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Copyright © 1990 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.