The Clay Mineral Composition of Representative Soils from Five Geological Regions of Texas*

G. W. Kunze, E. H. Templin and J. B. Page
Agricultural and Mechanical College of Texas
* Contribution from the Agronomy Department of the Texas Agr. Exp. Sta., College Station, Texas, as Technical Article No. 2113.

Abstract: Mineralogical studies for the <2 µ fractions are presented for seventeen soil profiles and two surface horizon samples, which represent eight soil types and five geological regions in the state. There was no evidence of clay mineral formation in the upper 6 feet or more of soil. X-ray diffraction data from the Lufkin, Ruston and Katy soils suggested some decomposition of montmorillonite and kaolinite in the upper horizon. However, the overall picture is one of little change in clay mineral composition between the soils and parent sediments.

Clays and Clay Minerals; 1954 v. 3; no. 1; p. 373-383; DOI: 10.1346/CCMN.1954.0030129
© 1954, The Clay Minerals Society
Clay Minerals Society (www.clays.org)