The Influence of Heat-Stable Intercalate on the Rate of Dehydroxylation of Smectite1

R. H. Loeppert Jr. and M. M. Mortland
Department of Crop and Soil Science, Michigan State University East Lansing, Michigan 48824
1 Journal article No. 8890, Michigan State Experiment Station. Work partially supported by National Science Foundation Grant CHE-76-80370.

Abstract: The rates of dehydroxylation of smectites intercalated with the decomposition products of Ni(phen)3SO4 are from 2 to 4 times greater than those of clays without the heat-stable intercalate. These results suggest that the intercalated material, in keeping the clay sheets separated, provides a more ready avenue for water loss during the dehydroxylation process.

Key Words: Activation energy • Dehydroxylation • Intercalate • Reaction rate constant • Smectite

Clays and Clay Minerals; October 1979 v. 27; no. 5; p. 373-376; DOI: 10.1346/CCMN.1979.0270508
© 1979, The Clay Minerals Society
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