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Clay Formation and Accumulation in Selected Oklahoma Soils

Published online by Cambridge University Press:  01 January 2024

Fenton Gray ,
L. W. Reed  and
H. D. Molthan
Fenton Gray
Affiliation:
Oklahoma State University, Stillwater, Okla, USA
L. W. Reed
Affiliation:
Oklahoma State University, Stillwater, Okla, USA
H. D. Molthan
Affiliation:
Oklahoma State University, Stillwater, Okla, USA
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Abstract

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The clay minerals were studied from eleven soil profiles representing three Great Groups of eastern and central Oklahoma. Montmorillonite and illite type clay minerals were found to be the dominant minerals; montmorillonite dominates the fine clays; illite is the chief constituent of the coarse clays. The fine clays dominated the clay fraction of most horizons, including the parent material. The results of the investigation indicate that the present régime of soil formation has had little effect in altering the clay minerals of the soil from those present in the original sediments.

Type
General Session
Information
Clays and Clay Minerals (National Conference on Clays and Clay Minerals) , Volume 11 , February 1962 , pp. 211 - 224
Copyright
Copyright © The Clay Minerals Society 1962

Footnotes

Research reported in this publication was done under Oklahoma Agricultural Experiment Station Project Number 868, and was presented at the Eighth Conference, in Norman, Okla.

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