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Susceptibility of Interlayer Potassium in Micas to Exchange with Sodium

Published online by Cambridge University Press:  01 July 2024

A. D. Scott
Affiliation:
Department of Agronomy, Iowa State University, Ames, Iowa
S. J. Smith
Affiliation:
Department of Agronomy, Iowa State University, Ames, Iowa
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Abstract

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Interlayer K in muscovite, biotite, phlogopite, illite and vermiculite-hydrobiotite samples was replaced by cation exchange with Na. The rate and amount of exchange varied with the mineral and the level of K in solution.

Essentially, all the K in muscovite, biotite, phlogopite and vermiculite was exchangeable when the mass-action effect of the replaced KT was reduced by maintaining a very low level of K in solution. The time required for this exchange varied from < 10 hr with vermiculite to > 45 weeks with muscovite. Only 66% of the K in the illite was exchangeable under these conditions. When the replaced K was allowed to accumulate in the solution, the amount of exchange was determined by the level of K in solution required for equilibrium. These levels decreased with the degree of K-depletion and with the selectivity of the mica for K. The order of selectivity was muscovite > illite > biotite > phlogopite > vermiculite. Decreasing the K in solution from 10 to 7 ppm increased the exchangeable K in biotite from 30 to 100%. A K level of only 0.1 ppm restricted the exchange of K in muscovite to 17%.

A decrease in layer charge was not required for K exchange, but a decrease did occur in K-depleted biotite and vermiculite. Muscovite with the highest layer charge (247 meq/100 g), least expansion with Na (12.3Å), and least sensitivity to solution pH had the highest selectivity for K and the slowest rate of exchange. The K in vermiculite was the most readily exchangeable.

Type
Research Article
Copyright
Copyright © Clay Minerals Society 1966

Footnotes

*

Journal Paper No. J-5216 of the Iowa Agricultural and Home Economics Experiment Station, Ames, Iowa, Project No. 1234.

References

Arnold, P. W. (1960) Nature and mode of weathering of soil-potassium reserves, J. Sci. Food Agr. 11, 285–92.10.1002/jsfa.2740110601CrossRefGoogle Scholar
Barshad, I. (1954) Cation exchange in micaceous minerals, II. Replaceability of ammonium and potassium from vermiculite, biotite and montmorillonite, Soil Sci. 78, 5776.10.1097/00010694-195407000-00007CrossRefGoogle Scholar
Bassett, W. A. (1960) Role of hydroxyl orientation in mica alteration, Bull. Geol. Soc. Am. 71, 449–56.10.1130/0016-7606(1960)71[449:ROHOIM]2.0.CO;2CrossRefGoogle Scholar
Bolt, G. H., Sumner, M. E. and Kamphorst, A. (1963) A study of the equilibria between three categories of potassium in an illitic soil, Proc. Soil Sci. Soc. Amer. 27, 294–99.10.2136/sssaj1963.03615995002700030024xCrossRefGoogle Scholar
Flaschka, H. and Barnard, A. J. Jr. (1960) Tetraphenylboron (TRB) as an analytical reagent, Advan. Anal. Chem. Instr. 1, 1117.Google Scholar
Hanway, J. J., Scott, A. D. and Stanford, G. (1957) Replaceability of ammonium fixed in clay minerals as influenced by ammonium or potassium in the extracting solution, Proc. Soil Sci. Soc. Amer. 21, 2934.10.2136/sssaj1957.03615995002100010008xCrossRefGoogle Scholar
Heltferich, F. (1962) Ion Exchange, McGraw-Hill, New York.Google Scholar
Jackson, M. L. and Sherman, G. D. (1953) Chemical weathering of minerals in soils, Advan. Agron. 5, 219318.10.1016/S0065-2113(08)60231-XCrossRefGoogle Scholar
Marshall, C. E. (1964) The Physical Chemistry and Mineralogy of Soils, Vol. I., Soil Materials, John Wiley, New York.Google Scholar
Marshall, C. E. and McDowell, L. L. (1965) The surface reactivity of micas, Soil Sci. 99, 115–31.10.1097/00010694-196502000-00009CrossRefGoogle Scholar
Mortland, M. M. and Lawton, K. (1961) Relationships between particle size and K release from biotite and its analogues, Proc. Soil Sci. Soc. Amer. 25, 473–6.10.2136/sssaj1961.03615995002500060017xCrossRefGoogle Scholar
Reed, M. G. and Scott, A. D. (1962) Kinetics of potassium release from biotite and muscovite in sodium tetraphenylboron solutions, Proc. Soil Sci. Amer. 26, 437–40.10.2136/sssaj1962.03615995002600050010xCrossRefGoogle Scholar
Reed, M. G. and Scott, A. D. (1966) Chemical extraction of potassium from soils and micaceous minerals with solutions containing sodium tetraphenylboron, IV, Muscovite, Proc. Soil Sci. Soc. Amer, (in press).10.2136/sssaj1966.03615995003000020014xCrossRefGoogle Scholar
Rich, C. I. and Black, W. R. (1964) Potassium exchange as affected by cation size, pH, and mineral structure. Soil Sci. 97, 384–90.10.1097/00010694-196406000-00004CrossRefGoogle Scholar
Scott, A. D., Hasway, J. J. and Edwards, A. P. (1958) Replaceability of ammonium in vermiculite with acid solutions, Proc. Soil Sci. Soc. Amer. 22, 388–92.10.2136/sssaj1958.03615995002200050006xCrossRefGoogle Scholar
Scott, A. D., Hunziker, R. R. and Hanway, J. J. (1960) Chemical extraction of potassium from soils and micaceous minerals with solutions containing sodium tetraphenylboron, I, Preliminary experiments, Proc. Soil Sci. Soc. Amer. 24, 191–4.10.2136/sssaj1960.03615995002400030020xCrossRefGoogle Scholar
Scott, A. D. and Reed, M. G. (1962) Chemical extraction of potassium from soils and micaceous minerals with solutions containing sodium tetraphenylboron, II, Biotite, Proc. Soil Sci. Soc. Amer. 26, 41–5.Google Scholar
Scott, A. D. and Reed, M. G. (1965) Expansion of potassium-depleted muscovite, Clays and, Clay Minerals, Proc. 13th Conf. Pergamon Press, New York (in press).Google Scholar
Smith, S. J. and Scott, A. D. (1966) Extractable potassium in Grundite illite, I, Method of extraction, Soil Sci. (in press).10.1097/00010694-196608000-00006CrossRefGoogle Scholar
Tucker, B. M. (1964) The solubility of potassium from soil illites, II, Mechanisms of potassium release, Australian Jour. Soil Research. 2, 6775.10.1071/SR9640067CrossRefGoogle Scholar