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The Surface Coulomb Energy and Proton Coulomb Potentials of Pyrophyllite {010}, {110}, {100}, and {130} EDGES

Published online by Cambridge University Press:  28 February 2024

William F. Bleam ,
Gereon J. Welhouse  and
Mark A. Janowiak
William F. Bleam
Affiliation:
Department of Soil Science, 1525 Observatory Drive, University of Wisconsin-Madison, Madison, Wisconsin 53706-1299
Gereon J. Welhouse
Affiliation:
Department of Soil Science, 1525 Observatory Drive, University of Wisconsin-Madison, Madison, Wisconsin 53706-1299
Mark A. Janowiak
Affiliation:
Department of Soil Science, 1525 Observatory Drive, University of Wisconsin-Madison, Madison, Wisconsin 53706-1299
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Abstract

This paper describes structural models of four pyrophyllite edge faces: {010}, {110}, {100}, and {130}. Water molecules chemisorbed to Lewis acid sites stabilize edge faces both crystallochemically and electrostatically. The detailed assignment of protons to surface oxygens and the orientation of OH bond-vectors both influence the surface Coulomb energy.

The geometry chosen for the electrostatic calculations was infinite pyrophyllite ribbon the thickness of a single phyllosilicate layer and the width of 50 to 70 unit cells. Such a phyllosilicate ribbon has only two edges, a top and bottom, which were simulated using the edge-face models mentioned above. About 94% of the surface Coulomb energy is confined to the edge-face repeat unit. The surface Coulomb energies of the four edge faces are on the order of 2–3 nJ/m, varying ± 1 nJ/m with proton assignment. The Coulomb potential, measured either within the layer or parallel to the layer, has a distinct negative trend near the edge face that can be traced to chemisorbed water molecules. Finally, the correlation between proton Coulomb potentials at the edge face and the coordination environment of the protons is poor, obscured by long-range interactions.

Keywords

Edge structureElectrostatic potentialLattice sumPyrophyllite

Information

Type
Research Article
Information
Clays and Clay Minerals , Volume 41 , Issue 3 , June 1993 , pp. 305 - 316
Copyright
Copyright © 1993, The Clay Minerals Society

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