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Published in Soil Sci Soc Am J 32:35-40 (1968)
© 1968 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Solubility and Redox Criteria for the Possible Forms of Selenium in Soils1

Harold R. Geering, Earle E. Cary, L. H. P. Jones and W. H. Allaway2

ABSTRACT

The solubility of Se in seven soils indicate that Se concentration in solution is governed primarily by a ferric oxide-selenite-adsorption complex (Se oxidation state +4). However, under certain conditions Se may also exist in the oxidation states +6, 0, and –2. The proportions of Se in the four oxidation states are treated theoretically as they are affected by the redox potential, soil pH, and ions with which Se combines.


NOTES

1 Contribution from the US Plant, Soil & Nutrition Laboratory, Soil & Water Conservation Research Division, ARS, USDA, Ithaca, New York.

2 Research Assoc., N. Y. S. College of Agriculture, Ithaca, New York; Chemist, USDA, Ithaca, New York; Principal Research Scientist, CSIRO Victoria, Australia; and Research Soil Scientist, USDA, Ithaca, New York, respectively.

Received for publication February 13, 1967. Accepted for publication September 29, 1967.







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Copyright © 1968 by the Soil Science Society of America.