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Effect of Impurities on the Rheology of Two Kaolins

Published online by Cambridge University Press:  01 January 2024

R. B. Langston
Affiliation:
University of California, Berkeley, California, USA
E. A. Jenne*
Affiliation:
University of California, Berkeley, California, USA
J. A. Pask
Affiliation:
University of California, Berkeley, California, USA
*
*Present address: U.S. Geological Survey, Federal Center, Denver, Colorado.

Abstract

Two kaolins were given five successive processing steps designed to remove a number of impurities: (1) removal of nonclay and soluble fractions; (2) removal of organic material; (3) removal of iron oxides; (4) removal of allophane; and (5) removal of three- layer lattice minerals. After each of these steps, consistency curves were obtained for each of the clays at both 6.5 and 9.0 pH on slurries containing up to 50 weight % solids.

Photomicrographs and electron micrographs showed that Ka-7 from Bath, South Carolina, contained generally smaller particles than Ka-2 from Macon, Georgia. Lowering the pH from 9.0 to 6.5 in Ka-2 produced no change in plastic viscosity at the lower concentrations and a decrease of about 30 per cent at higher concentrations after processing step 1. A comparison of the same evaluations of step-1-treated Ka-7 showed that the decrease in pH reduced the plastic viscosity by 50 per cent at 5 per cent clay concentration and increased the plastic viscosity by 100 per cent at 35 per cent clay concentration. After complete processing, lowering the pH from 9.0 to 6.5 increased the plastic viscosity at all concentrations for both kaolins by 5–20 per cent. At a clay concentration of 30 per cent, complete processing decreased the plastic viscosity of Ka-2 from 0.4 to 0.02 poise and of Ka-7 from 0.4 to 0.06 poise. Ka-7 showed progressive viscosity changes due to the processing, while Ka-2 showed only a marked change in viscosity for processing step 5. The rheological changes of Ka-2 and Ka-7 with processing are supported by the X-ray diffraction data at the various processing stages. X-ray diffraction data confirm that processing step 5 effectively removed a three-layer lattice expandable mineral from Ka-2, while processing step 3 effectively removed a different three-layer expandable mineral from Ka-7.

Type
General Session
Copyright
Copyright © Clay Minerals Society 1964

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References

Hashimoto, I., and Jackson, M. L. (1960) Rapid dissolution of allophane and kaolinite-halloysite after dehydration, Clays and Clay Minerals, 7th Conf. [1958], pp. 102–13, Pergamon Press, New York.Google Scholar
Hauser, E. A., and Reed, C. E. (1937) Studies in thixotropy, XI, The thixotropic behavior and structure of bentonite, J. Phys. Chem. 41, 911–34.CrossRefGoogle Scholar
Henry, E. C. (1955) Clay technology in ceramics, Clays and Clay Technology, Calif. Dep. Nat. Resources, Div. Mines, Bull. 169, 257–66.Google Scholar
Jackson, M. L. (1956) Soil Chemical Analysis—Advanced Course, Published by Author, Madison, Wisconsin.Google Scholar
Johnson, A. L., and Norton, F. H. (1941) Fundamental study of clay: Preparation of a purified kaolinite suspension, J. Am. Ceram. Soc. 24, 61–9.CrossRefGoogle Scholar
Kerr, P. F., Main, M. S., and Hamilton, P. K. (1951) Occurrence and microscopic examination of reference clay mineral specimens, Reference Clay Minerals, American Petroleum Institute Research Project 49, Preliminary Report 5, Columbia University, New York.Google Scholar
Lang-ston, R. V., and Jenne, E. A. (1964) NaOH dissolution of some oxide impurities from kaolins, Clays and Clay Minerals, 12th Conf. [1963], pp. 633–47, Pergamon Press, New York.Google Scholar
Langston, R. V., and Pask, J. A. (1958) Analysis of consistencies of kaolin-water systems below the plastic range, Clays and Clay Minerals, Nat. Acad. Sci.—Nat. Res. Council, Publ. 566, pp. 428.Google Scholar
Langston, R. V., Trask, P D, and Pask, J. A. (1958) Effect of mineral composition on strength of central-California sediments, Cahf. J. Mines Geol. 54, 215–35.Google Scholar
Mitchell, L., and Henry, E. C. (1943) Nature of Georgia kaolin, I, Evidence of chemical and colloidal analysis, J. Am. Ceram. Soc. 26, 105–13.Google Scholar
Mitchell, L., and Poulas, N. E. (1959) The relationship of structure of Georgia kaolin to its viscosity, Georgia Inst. Technol. Eng. Exp. Stat. Bull. 23.Google Scholar