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Changes in b-dimension in relation to potassium exchange and to oxidation of phlogopite and biotite

Published online by Cambridge University Press:  01 July 2024

G. J. Ross  and
C. I. Rich
G. J. Ross
Affiliation:
Soil Research Institute, Research Branch, Canada Agriculture, Ottawa, Ontario, Canada K1A OC6.
C. I. Rich
Affiliation:
Agronomy Department, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061, U.S.A.
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Clays and Clay Minerals , Volume 21 , Issue 3 , June 1973 , pp. 201 - 204
Copyright
Copyright © 1973 The Clay Minerals Society

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References

Farmer, V. C., Russell, J. D. M. Hardy, W. J., Newman, A. C. D. Ahlrichs, J. L. and Rimsaite, J. Y. H., (1971) Evidence for loss of protons and octahedral iron from oxidized biotites and vermiculites Miner. Mag. 38 121–137.CrossRefGoogle Scholar
Jones, J. B., (1958) Dispersion in trioctahedral micas: Ph.D. thesis, Univ. Wisconsin .Google Scholar
Kodama, H. and Ross, G. J., (1972) Structural changes accompanying potassium exchange in a clay-size muscovite Proc. Intern. Clay Conf. 159–171.Google Scholar
Leonard, R. A. and Weed, S. B., (1967) Influence of exchange ions on the b-dimensions of dioctahedral vermiculite Clays and Clay Minerals 15 149–161.CrossRefGoogle Scholar
Leonard, R. A. and Weed, S. B., (1970) Mica weathering rates as related to mica type and composition Clays and Clay Minerals 18 187–195.CrossRefGoogle Scholar
Leonard, R. A. and Weed, S. B., (1970) Effects of potassium removal on the b-dimension of phlogopite Clays and Clay Minerals 18 197–202.CrossRefGoogle Scholar
Le Roux, J., Rich, C. I. and Ribbe, P. H., (1970) Ion selectivity by weathered micas as determined by electron microprobe analysis Clays and Clay Minerals 18 333–338.CrossRefGoogle Scholar
Mathieson, A. M. and Walker, G. F., (1954) Crystal structure of Mg-vermiculite Am. Mineralogist 39 231–255.Google Scholar
Radoslovich, E. W. and Norrish, K., (1962) The cell dimensions and symmetry of layer-lattice silicates—I. Some structural considerations Am. Mineralogist 47 599–616.Google Scholar
Radoslovich, E. W., (1962) The cell dimensions and symmetry of layer-lattice silicates—II. Regression relations Am. Mineralogist 47 617–636.Google Scholar
Radoslovich, E. W., (1963) The cell dimensions of layer silicates — IV. Interatomic forces Am. Mineralogist 48 76–99.Google Scholar
Rich, C. I., (1957) Determination of (060) reflections of clay minerals by means of counter type X-ray diffraction instruments Am. Mineralogist 42 569–570.Google Scholar
Rimsaite, J., (1967) Biotites intermediate between dioctahedral and trioctahedral micas Clays and Clay Minerals 15 375–393.CrossRefGoogle Scholar
Ross, G. J. and Rich, C. I. (1973) Effect of particle thickness on potassium exchange from phlogopite: Clays and Clay Minerals, 21, (in press).CrossRefGoogle Scholar
Wones, D. R., (1963) Physical properties of synthetic biotites on the join phlogopite-annite Am. Mineralogist 48 1300–1321.Google Scholar