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Surface Area Changes of a Vermiculite by Acid and Thermal Treatment

Published online by Cambridge University Press:  01 January 2024

Juan de D. Lopez-Gonzalez*
Affiliation:
Laboratorios de Quimica Inorganica de la Universidad de Granada y Estacion, Experimental del Zaidin, Granada, Spain
Jesus Cano-Ruiz
Affiliation:
Laboratorios de Quimica Inorganica de la Universidad de Granada y Estacion, Experimental del Zaidin, Granada, Spain
*
1Present address: Department of Soils and Plant Nutrition, University of California at Berkeley.
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Abstract

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A Vermiculite from Beni-Uxera, North Africa, was refluxed with HC1 solutions of various concentrations to determine the effect of such a treatment on its surface area. The treated vermiculite was analyzed for “free” SiO2 and by x-ray diffraction, and the refluxing solutions were analyzed for the cations removed from the vermiculite. Surface areas were determined by means of adsorption isotherms of n-butane at 0°C.

The surface area of the acid-treated vermiculite increases with increase in concentration of the acid. Heating of the acid-treated samples or the natural samples decreases the surface area.

The increase in surface area by acid treatment is due to destruction of the vermiculite and its conversion to a “free” form of SiO2 which possesses a large surface area. x-Ray analysis indicated that this “free” SiO2 was not present in the interlayer positions of the crystal lattice of vermiculite.

Type
Article
Copyright
Copyright © Clay Minerals Society 1957

References

Adams, C. R. and Vogue, H. H. (1957) Aging of silica-alumina cracking catalyst. II Electron microscope studies: J. Phys. Chem., v. 61, pp. 722727.CrossRefGoogle Scholar
Brunauer, S., Emmett, P. H. and Teller, E. (1938) Adsorption of gases in multimolecular layers: J. Amer. Chem. Soc., v. 60, p. 309.CrossRefGoogle Scholar
Davis, R. T. and DeWitt, T. W. (1948) The adsorption of butane on glass spheres: J. Amer. Chem. Soc., v. 70, pp. 11351141.CrossRefGoogle Scholar
Dyal, R. S. and Hendricks, S. B. (1950) Total surface of clays in polar liquids as a characteristic index: Soil Sci., v. 69, pp. 421432.CrossRefGoogle Scholar
Escard, J. (1950) Influence de la deshydration progressive sur l'aire de surface de mont- morillonites: J. Chim. Phys., v. 47, no. 1-2, pp. 113117.CrossRefGoogle Scholar
Gutierrez-Rios, E. and Lopez-Gonzalez, J. de D. (1952) Accion de los acidos fuertes sobre los silicatos de la serie isomorfa montmoriłlonitar-beidellita: Anal. Edaf., v. 11, p. 225; ibid., pp. 527-538.Google Scholar
Hoyos de Castro, A., Gonzalez-Garcia, F. and Martin-Vivaldi, J. L. (1950) Anal. Real Soc. Esp. Fis. Quim., v. 46 (B), p. 715.Google Scholar
Lopez-Gonzalez, J. de D. and Deitz, V. R. (1952) Surface changes in an original and activated bentonite: J. Res. Natl. Bur. Stand., v. 48, pp. 325333.Google Scholar
Lopez-Gonzalez, J. de D. and Gonzalez-Garcia, S. (1954) Modifications en la superficie total y externa de una bentonita por activacion acida: Anal. Real Soc. Esp. Fis. Quirn., v. 50 (B), pp. 465470.Google Scholar
Mills, G. A., Holmes, J. and Cornelius, E. B. (1950) Acid activation of some bentonite clays: J. Phys. Colloid Chem., v. 54, pp. 11701185.CrossRefGoogle ScholarPubMed
Nutting, P. G. (1935) Technical basis of bleaching-clay industry: Amer. Assoc. Petroleum Geologists Bull., v. 19, pp. 10431052.Google Scholar
Schlaffer, W. G., Morgan, C. Z. and Wilson, J. N. (1957) Aging of silicas-alumina cracking catalyst. I Kinetics of structural changes by heat and steam: J. Phys. Chem., v. 61, pp. 714722.CrossRefGoogle Scholar
Travers, A. (1933) Sur l'activation dos terres: Douzieme Congrès de Chemie Industrielle, Chim. Ind., p. 794.Google Scholar
Walker, G. F. (1951) Vermiculites and some related mixed-layer minerals: in X-Ray Identification and, Crystal Structures of Clay Minerals, Mineralogical Society, London, pp. 199223.Google Scholar