Author:
Whalley W. R.,Mullins C. E.
Abstract
AbstractCentrifugal photosedimentation was used to determine the size distribution of dilute bentonite suspensions as a function of saturating cation. This method is shown to give a better estimate of the effect of saturating cation on tactoid size than the techniques that are currently used. The results indicate that tactoids may occur in preferred size ranges.
Subject
Geochemistry and Petrology
Cited by
21 articles.
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