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Interstratified Layer Silicates in Some Soils of Northern Wisconsin

Published online by Cambridge University Press:  01 January 2024

L. D. Whittig
Affiliation:
University of Wisconsin, USA
M. L. Jackson
Affiliation:
University of Wisconsin, USA
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Abstract

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Examination of the silt and clay fractions of two northern Wisconsin soils, Omega loamy sand of the Brown Podzolic group and Ahmeek loam of the Brown Forest group, revealed considerable quantities of interstratified layer silicates. The two soils contained montmorin, vermiculite, chlorite, and illite both as discrete and interstratified components. Regularly alternating montmorin-illite structures, which registered a 28 Å first order diffraction peak, and vermiculite-illite structures, which yielded a 24 Å first order peak, were observed in the fine silt fractions of the Ahmeek loam A3 and B22 horizons, respectively. Weak diffraction peaks in general and lack of binary mixture average spacings was suggestive of ternary or quarternary interstratification of illite, chlorite, vermiculite, and montmorin in the medium and fine clay fractions of the Ahmeek loam horizons. Randomly interstratified vermiculite-chlorite and vermiculite-montmorin, as revealed by comparative basal diffraction peaks before and after heating potassium saturated samples, were evidenced in the fine silt and clay fractions of the Omega profile.

Mixed layer components in the Omega and Ahmeek soils originated from illite and chlorite in the? horizons with a progressive increase in proportions of first vermiculite and finally montmorin with proximity to the soil surface. The observed weathering transitions within the mixed layer structures illustrates the effects of accelerated leaching which has taken place in these coarse textured soil profiles, even though these soils are relatively young (late Pleistocene).

Type
Article
Copyright
Copyright © The Clay Minerals Society 1954

References

Aguilera, N. H., and Jackson, M. L. (1953) Iron oxide removal from soils and clays: Soil Sci. Soc. Amer. Proc., vol. 17, pp. 359364; (1954) vol. 18, pp. 223 and 350.CrossRefGoogle Scholar
Barshad, I. (1948) Vermiculite and its relation to biotite as revealed by base exchange reactions, X-ray analyses, differential thermal curves and water content: Am. Mineral., vol. 33, pp. 655678.Google Scholar
Bradley, W. F. (1950a) The alternating layer sequence of reciorite: Am. Mineral., vol. 35, pp. 590595.Google Scholar
Bradley, W. F. (1950b) Inter stratified growths in clays and clay-like minerals: Trans. Fourth Intern. Cong. Soil Sci., vol. 1, pp. 101103.Google Scholar
Brindley, G. W., and Ali, S. E. (1950) Thermal transformation in magnesian chlorites: Acta Cryst., vol. 3, pp. 2530.CrossRefGoogle Scholar
Brindley, G. W., and Youell, R. F. (1950) Thermal and X-ray studies of chamosite and chlorites (cited in Brindley, G. W., and Robinson, K., in X-ray identification and crystal structures of clay minerals: Mineralogical Society of Great Britain Monograph, Ch. 6, pp. 173198).Google Scholar
Brown, G., and MacEwan, D. M. C, (1951) X-ray diffraction by structures with random interstratification: In X-ray identification and crystal structures of clay minerals: Mineralogical Society of Great Britain Monograph, Ch. 11, pp. 266284.Google Scholar
Gruner, J. W. (1934) Vermiculite and hydrobiotite structures: Am. Mineral., vol. 19, pp. 557575.Google Scholar
Gruner, J. W. (1948) Progress in silicate structures: Am. Mineral., vol. 33, p. 679691.Google Scholar
Hendricks, S. B., and Alexander, L. T. (1939) Minerals present in soil colloids: Soil Sei., vol. 48, pp. 257267.CrossRefGoogle Scholar
Hendricks, S. B., and Teller, E. (1942) X-ray interference in partially ordered layer lattices: Jour. Chem. Phys., vol. 10, pp. 147167.10.1063/1.1723678CrossRefGoogle Scholar
Hseung, Y., and Jackson, M. L. (1952) Mineral composition of the clay fraction. III. Of some main soil groups of China: Soil Sci. Soc. Amer. Proc., vol. 16, pp. 294297.Google Scholar
Jackson, M. L., Tyler, S. A., Willis, A. L., Bourbeau, G. A., and Pennington, R. P. (1948) Weathering sequence of clay-size minerals in soils and sediments. I. Fundamental generalisations: Jour. Phys. Coll. Chem., vol. 52, pp. 12371260.CrossRefGoogle Scholar
Jackson, M. L., Whittig, L. D., and Pennington, R. P. (1950) Segregation procedure for the mineralogical analyses of soils: Soil Sci. Soc. Amer. Proc., vol. 14, pp. 7781.CrossRefGoogle Scholar
Jackson, M. L., Hseung, Y., Corey, R. B., Evans, E. J., and Vanden Heuvel, R. C. (1952) Weathering sequence of clay-size minerals in soils and sediments. II. Chemical weathering of layer silicates: Soil Sci. Soc. Amer. Proc., vol. 16, pp. 36.CrossRefGoogle Scholar
Jackson, M. L., and Sherman, G. D. (1953) Chemical weathering of minerals in soils: Adv. in Agron., vol. 5, pp. 219318.10.1016/S0065-2113(08)60231-XCrossRefGoogle Scholar
Jackson, M. L., Whittig, L. D., Kaufman, A., Vanden Heuvel, R. C, and Brown, B. E. (1954) Some analyses of soil montmorin, vermiculite, micas, chlorites, and inter- stratified 2:1 layer silicates: Proc. Second Conf. on Clays and Clay Minerals, Natl. Res. Council Publication 327.Google Scholar
Jeffries, C. D., and Jackson, M. L. (1949) Mineralogical analysis of soils: Soil Sei., vol. 67, pp. 5773.CrossRefGoogle Scholar
MacEwan, D. M. C. (1949) Some notes on the recording and interpretation of X-ray diagrams of soil clays: Jour. Soil Sei., vol. 1, pp. 90103.10.1111/j.1365-2389.1950.tb00721.xCrossRefGoogle Scholar
Mackenzie, R. C., Walker, G. F., and Hart, R. (1949) Illite occurring in decomposed gramte at Ballater, Aberdeenshire: Mineral. Mag., vol. 48, pp. 704713.Google Scholar
Pauling, L. (1930) The structure of the chlorites: Proc. Nat. Acad. Sci., vol. 16, pp. 578582.10.1073/pnas.16.9.578CrossRefGoogle ScholarPubMed
Walker, G. F. (1950) Trioctahedral minerals in the soil-clays of North-East Scotland: Mineral. Mag., vol. 49, pp. 7284.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 of Great Britain Monograph, Chap. 7, pp. 199223.Google Scholar