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Published in Soil Sci Soc Am J 24:165-168 (1960)
© 1960 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Cobalt Reactions with Montmorillonite1

J. F. Hodgson2

ABSTRACT

Specific reactions between montmorillonite and Co in low concentrations were studied in the presence of excess CaCl2. Two forms of bound Co were distinguished. One form, characterized as being slowly dissociable, appears to be bound in a monolayer by chemisorption and will exchange with Cu++, Zn++, or other Co++ and to a lesser extent with ions of other transition metals but not with Ca++, Mg++, or NH4+. A second form of Co did not dissociate and could not be extracted from the mineral with 2.5% acetic acid. This fraction, which was not characterized, is thought to either enter the crystal lattice or be occluded in the precipitation of another phase.


NOTES

1 Contributed from the U. S. Plant, Soil and Nutrition Laboratory, ARS, USDA, Ithaca, New York. Presented before Div. II, Soil Science Society of America, Nov. 19, 1959, at Cincinnati, Ohio.

2 Soil Scientist.

Received for publication November 10, 1959. Accepted for publication December 15, 1959.







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