Zero-Gradient Rotational Diffusion Constants of Some Polydisperse Clay Mineral Sols

W. T. Granquist* and C. A. Hollingsworth
Department of Chemistry, University of Pittsburgh, Pittsburgh 13, Pa.
* National Lead Follow, Mellon Institute, Pittsburgh 13, Pa.

Abstract: Rotational diffusion constants were determined as a function of shear gradient in a region of low shear (generally, less than 20 sec−1) for various concentrations (generally, less than 0.1 per cent clay by weight) of polydisperse aqueous dispersions of montmorillonite, hectorite, and attapulgite. Extrapolation of these data to zero shear gave concentration dependent zero-gradient rotational diffusion constants. Proper treatment of these results permitted a linear extrapolation to zero concentration to give θG=0, C=0, the zero-gradient zero-concentration rotational diffusion constant, for each of the clay systems.

Particle size distributions were determined for each of the clays by a direct counting technique, based on electron micrographs prepared from dilute (∼0.005 per cent clay dispersions. These distributions were then used to calculate a θG=0, C=0 for each system, on the basis of the relationship θ G=0,  C=0 = ∑ i φ i / θ i ∑ i φ i / θ i , where θi is the rotational diffusion constant and φi is the volume fraction of the ith monodisperse component of the polydisperse system.

Agreement between the calculated and experimental values of θG=0, C=0 was good. Thus, theoretical and experimental considerations both lead to the conclusion that the behavior at low shear of polydisperse systems, such as these, is governed by the relatively few large particles in the distribution.

Clays and Clay Minerals; 1962 v. 11; no. 1; p. 295; DOI: 10.1346/CCMN.1962.0110128
© 1962, The Clay Minerals Society
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