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Quantitative mineralogical analysis of some Bangladesh soils with X-ray, ion exchange and selective dissolution techniques

Published online by Cambridge University Press:  09 July 2018

A. K. M. E. Islam  and
E. G. Lotse
A. K. M. E. Islam
Affiliation:
Department of Soil Sciences, Swedish University of Agricultural Sciences, S-750 07 Uppsala, Sweden
E. G. Lotse
Affiliation:
Department of Soil Sciences, Swedish University of Agricultural Sciences, S-750 07 Uppsala, Sweden
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Abstract

Fine clay, coarse clay, and silt fractions of four Bangladesh soils were studied using XRD, ion exchange, and selective dissolution techniques. Constants for the XRD intensity-weight proportion relationships were derived using these techniques. Smectite and mica were found to be dominant in Batra and Ghior soils, whereas kaolinite and mica were dominant in the Naraibag and Ghatail soils. Other minerals present were vermiculite, vermiculite with hydroxyaluminium interlayers, chlorite, randomly interstratified chlorite-mica, feldspar, quartz, and trace amounts of amphibole. The amorphous material content varied between 1 and 11% and decreased with increasing particle size. No crystalline iron oxides were detected in untreated clay fractions.

Type
Research Article
Information
Clay Minerals , Volume 21 , Issue 1 , March 1986 , pp. 31 - 42
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1986

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References

Alexander, L. & Klug, H.P. (1948) Basic aspects of X-ray absorption. Analyt. Chem. 20, 886–889.Google Scholar
Alexiades, C.A. & Jackson, M.L. (1966) Quantitative clay mineralogical analysis of soils and sediments. Clays Clay Miner. 14, 35–52.CrossRefGoogle Scholar
Brammer, H. (1971) Soil survey project, Bangladesh. Soil Resources. AGL:SF/PAK 6, Tech. Rep. 3. UNDP-FAO, Rome.Google Scholar
Brindley, G.W. (1961) Quantitative analysis of clay mixtures. Pp. 489–516 in: The X-ray Identification and Crystal Structures of Clay Minerals (Brown, G., editor). Mineralogical Society, London.Google Scholar
Drever, J.I. (1973) The preparation of oriented clay mineral specimens for X-ray diffraction analysis by a filter-membrane peel technique. Am. Miner. 58, 553–554.Google Scholar
Gorbunov, N.I. (1971) Status and problems of the X-ray diffraction method for quantitative determination of minerals in soils. Soviet Soil Sci. 3, 229–241.Google Scholar
Hashimoto, I. & Jackson, M.L (1960) Rapid dissolution of allophane and kaolinite-halloysite after dehydration. Clays Clay Miner. 7, 102–113.Google Scholar
Huizing, H.G.J. (1971) A reconnaissance study of the mineralogy of sand fractions from East Pakistan sediments and soils. Geoderma 6, 109–133.Google Scholar
Jackson, M.L. (1965) Soil Chemical Analysis-Advanced Course. Second printing. Published by the author. Dept. of Soil Science, University of Wisconsin, Madison.Google Scholar
Jackson, M.L. (1968) Weathering of primary and secondary minerals in soils. Trans. 9th Int. Congr. Soil Sci. Adelaide 4, 281–292.Google Scholar
Johns, W.D., Grim, R.E. & Bradley, W.F. (1954) Quantitative estimations of clay minerals by diffraction methods. J. Sed. Petrol 24, 242–251.Google Scholar
Karim, Z. & Akhand, N.A. (1982) Net irrigation requirement of rice and evapotranspiration of wheat and potato for different locations of Bangladesh. Soils and Irrigation Publication 11. Bangladesh Agricultural Research Council, Dacca, Bangladesh.Google Scholar
Kiely, P.V. & Jackson, M.L. (1965) Quartz, feldspar, and mica determination for soils by sodium pyrosulfate fusion. Soil Sci. Soc. Am. Proc. 29, 159–163.Google Scholar
Klug, H.P. & Alexander, L.E. (1974) X-ray Diffraction Procedures for Polycrystalline and Amorphous Materials, p. 533. John Wiley and Sons, Inc., New York.Google Scholar
Mehra, O.P. & Jackson, M.L. (1960) Iron oxide removal from soils and clays by a dithionite-citrate system buffered with sodium bicarbonate. Clays Clay Miner. 7, 317–327.Google Scholar
Schultz, L.G. (1960) Quantitative X-ray determinations of some aluminous clay minerals in rocks. Clays Clay Miner. 7, 216–224.Google Scholar
Snäll, S., Persson, C. & Wikström, A. (1979) Mineralogisk undersökning av morän från ett område väister om Katrineholm. Sveriges GeoL Undersökning, Ser C 73, 1–32.Google Scholar
Thorez, J. (1975) Phyllosilicates and Clay Minerals, p. 361. G. Lelotte, Dison, Belgium.Google Scholar
Weaver, C.E. (1958) Geologic interpretation of argillaceous sediments Part I. Origin and significance of clay minerals in sedimentary rocks. Bull Am. Assoc. of Petrol. Geol. 42, 254–271.Google Scholar
Weir, A.H., Ormerod, E.C. & El Mansey, I.M.I. (1975) Clay mineralogy of sediments of the western Nile delta. Clay Miner. 10, 369–386.Google Scholar
Whittig, L.D. (1965) X-ray diffraction techniques for mineral identification and mineralogical composition. Pp. 671–698 in: Methods of Soil Analysis, Part I (Black, C. A., editor). Agronomy 9, American Society of Agronomy Inc., Madison.Google Scholar