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Occurrence of a Tabular Halloysite in a Texas Soil

Published online by Cambridge University Press:  01 January 2024

G. W. Kunze  and
W. F. Bradley
G. W. Kunze
Affiliation:
Agricultural and Mechanical University of Texas and The University of Texas, USA
W. F. Bradley
Affiliation:
Agricultural and Mechanical University of Texas and The University of Texas, USA
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Abstract

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A substantially homogeneous mineral fraction from a Katy soil profile in Fort Bend County, Texas, consists of a tabular kaolin group mineral with the physical and chemical properties characteristic of a nearly dehydrated halloysite, retaining only a small excess of water.

Type
General
Information
Clays and Clay Minerals (National Conference on Clays and Clay Minerals) , Volume 12 , February 1963 , pp. 523 - 527
Copyright
Copyright © The Clay Minerals Society 1963

References

Brindley, G. W. (1951) X-ray Identification and Structure of Clay Minerals. The Mineralogical Society (London), 345 pp.Google Scholar
Radoslovich, E. W. (1962) The cell dimensions and symmetry of layer lattice silicates. II. Regression relations: Am. Mineral v.47, pp. 617–636.Google Scholar
Serratosa, J. M. (1960) Dehydration studies by infrared spectroscopy: Am. Mineral v. 45, pp. 1101–1104.Google Scholar