Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-23T02:00:28.175Z Has data issue: false hasContentIssue false

Stability of Soil Smectite From a Houston Black Clay

Published online by Cambridge University Press:  01 July 2024

C. D. Carson
Affiliation:
Department of Soil and Crop Sciences, Texas A & M University, College Station, TX 77843, U.S.A.
J. A. Kittrick*
Affiliation:
Department of Soil and Crop Sciences, Texas A & M University, College Station, TX 77843, U.S.A.
J. B. Dixon
Affiliation:
Department of Soil and Crop Sciences, Texas A & M University, College Station, TX 77843, U.S.A.
T. R. McKee*
Affiliation:
Department of Soil and Crop Sciences, Texas A & M University, College Station, TX 77843, U.S.A.
*
Present address: Department of Agronomy and Soils, Washington State University, 99163, Pullman, WA, U.S.A.
Present address: Department of Oceanography, Texas A & M University, U.S.A.
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

The stability of smectite separated from a Houston Black clay soil was studied by solubility methods in an acid environment. High Silicon levels (supersaturated with respect to amorphous Si) probably were due to dissolution of the smectite and slow precipitation of amorphous Silicon. Also, mica and vermiculite impurities may have contributed to high solution Si values. Solubility data from equilibrium solutions of various treatments and chemical structural analyses permitted the formulation of a solubility equation. The ΔG°f for the Houston Black smectite computed from pK values was —2433.9 ± 0.8 kcal/mole. The stability of this clay could then be determined by calculations for any desired solution environment. It was found that under some conditions this soil smectite could be more stable than Belle Fourche and Aberdeen montmorillonites. Therefore, it appears that this soil clay has the required stability area in which it can form in nature.

Type
Research Article
Copyright
Copyright © 1976 The Clay Minerals Society

Footnotes

*

Investigations supported by Texas Agricultural Experiment Station, College Station.

References

American Public Health Association (1960) Standard Methods for the Examination of Water and Waste Water: 11th Edn., New York.Google Scholar
Bernas, B. (1968) A new method for decomposition and comprehensive analysis of silicates by atomic absorption spectrometry: Analyt. Chem. 40, 16821686.CrossRefGoogle Scholar
Carson, C. D. and Dixon, J. B. (1972) Potassium selectivity in certain montmorillonitic soil clays: Soil Sci. Soc. Am. Proc. 36, 838843.CrossRefGoogle Scholar
Garrels, R. M. (1957) Some free energy values from geologic relations: Am. Mineralogist 42, 780791.Google Scholar
Garrels, R. M. (1967) Genesis of some ground waters from igneous rocks: In Researches in Geochemistry (Edited by Abelson, P. H.) . Vol. 2, pp. 405420. Wiley, New York.Google Scholar
Hashimoto, I. and Jackson, M. L. (1960) Rapid dissolution of allophane and kaolinite–halloysite after dehydration: Clays and Clay Minerals 7, 102113.Google Scholar
Hsu, P. H. (1963) Effect of initial pH, phosphate, and silicate on the determination of aluminum with aluminon: Soil Sci. 96, 230235.CrossRefGoogle Scholar
Jackson, M. L. (1956) Soil Chemical Analysis-Advanced Course: Published by the author, Dept. of Soil Sci., University of Wisconsin, Madison, pp. 33–36, 47.Google Scholar
Kittrick, J. A. (1966) Free energy of formation of kaolinite from solubility measurements: Am. Mineralogist 51, 14571466.Google Scholar
Kittrick, J. A. (1969) Soil minerals in the Al2O3–SiO2–H2O system and a theory of their formation: Clays and Clay Minerals 17, 157167.CrossRefGoogle Scholar
Kittrick, J. A. (1971a) Montmorillonite equilibria and the weathering environment: Soil Sci. Soc. Am. Proc. 35, 815820.CrossRefGoogle Scholar
Kittrick, J. A. (1971b) Stability of montmorillonites—I. Belle Fourche and Clay Spur montmorillonites: Soil Sci. Soc. Am. Proc. 35, 140145.CrossRefGoogle Scholar
Kittrick, J. A. (1971c) Stability of montmorillonites—II. Aberdeen montmorillonites: Soil Sci. Soc. Am. Proc. 35, 820823.CrossRefGoogle Scholar
Klotz, I. (1964) Chemical Thermodynamics: W. A. Benjamin, New York.Google Scholar
Mackenzie, F. T. and Gees, R. (1971) Quartz: synthesis at earth surface conditions: Science 173, 533534.CrossRefGoogle ScholarPubMed
McKeague, J. A. and Cline, M. G. (1963) I—The form and concentration of dissolved silica in aqueous extracts of some soils: Can. J. Soil Sci. 43, 7082.CrossRefGoogle Scholar
Robie, R. A. and Waldbaum, D. R. (1968) Thermodynamic properties of minerals and related substances at 298.15°K (25.0°C) and one atmosphere (1.013 Bars) pressure and at higher temperatures: Geol. Survey Bull. 1259, 265 pp.Google Scholar
Weaver, R. M., Jackson, M. L. and Syers, J. K. (1971) Magnesium and silicon activities in matrix solutions of montmorillonite-containing soils in relation to clay mineral stability: Soil Sci. Soc. Am. Proc. 35, 823830.CrossRefGoogle Scholar