Hostname: page-component-5c6d5d7d68-pkt8n Total loading time: 0 Render date: 2024-08-16T01:04:58.405Z Has data issue: false hasContentIssue false

The Use of Salted Pastes of Soil Colloids for X-Ray Analysis

Published online by Cambridge University Press:  01 January 2024

Isaac Barshad*
Affiliation:
University of California, Berkeley, USA

Abstract

A new technique for the x-ray analysis of soil colloids is proposed based on the finding that the interlayer swelling of montmorillonite persists in the presence of salt solutions and that the x-ray reflection representing the d(001) spacings becomes intensified in salted gels. The technique consists in flocculating the colloid from a suspension with sodium chloride, removing the “free” Fe2O3, Al2O3, and SiO2 by means of a solution of sodium citrate and sodium hydrosulfite, separating the cleaned colloid from the solution as a salted paste, and as such subjecting it to x-ray analysis. The method is not only more rapid than other recommended methods for x-ray analysis of soil colloids, but also — and which is of the utmost importance — yields a much more accurate picture of the mineralogical composition, particularly with respect to the content of the mica and the montmorillonite-type clays.

Type
Article
Copyright
Copyright © Clay Minerals Society 1953

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Aldrich, D. G., Hellman, N. N., and Jackson, M. L. (1944) Hydration control of montmorillonite as required for its identification and estimation by x-ray diffraction methods: Soil Sci., v. 57, p. 215231.CrossRefGoogle Scholar
Barshad, I. (1946) A pedologic study of California prairie soils: Soil Sci., v. 61, p. 423442.CrossRefGoogle Scholar
Barshad, I. (1950) The effect of the interlayer cation on the expansion of the mica type of crystal lattice: Amer. Mineral., v. 35, p. 225238.Google Scholar
Beu, K. E. (1951) Improvements in a method for preparing plastic powder sample capillary tubes: Rev. Sci. Instr., v. 22, p. 62.CrossRefGoogle Scholar
Brown, G. (1953) A semi-micro method for the preparation of soil clays for x-ray diffraction studies: Jour. Soil Sci., v. 4, p. 229232.CrossRefGoogle Scholar
Brown, G., and MacEwan, D. M. C. (1950) The interpretation of x-ray diagrams of clays: II. Structures with random inter stratification: Jour. Soil Sci., v. 1, p. 239253.CrossRefGoogle Scholar
Deb, B. C. (1950) The estimation of free iron oxides in soils and clays and their removal: Jour. Soil Sci., v. 1, p. 212220.CrossRefGoogle Scholar
Kelley, W. P., Dore, W. H., and Page, J. B. (1941) The colloidal constituents of American alkali soils: Soil Sci., v. 51, p. 101124.CrossRefGoogle Scholar
Kelley, W. P., Dore, W. H., and Woodford, A. O. (1939) The colloidal constituents of California soils: Soil Sci., v. 48, p. 201255.Google Scholar
MacEwan, D. M. C. (1944) Identification of the montmorillonite group of minerals by x-ray: Nature, v. 154, p. 577.CrossRefGoogle Scholar
MacEwan, D. M. C. (1950) Some notes on the recording and interpretation of x-ray diagrams of soil clays: Jour. Soil Sci., v. 1, p. 90103.CrossRefGoogle Scholar
Nagelschmidt, A. (1941) The identification of clay minerals by means of aggregate diffraction diagrams: Jour. Sci. Instr., v. 18, p. 100101.CrossRefGoogle Scholar
Weymouth, J. H., and Williamson, W. O. (1953) The effects of extrusion and some other processes on the microstructure of clay: Amer. Jour. Sci., v. 251, p. 89108.CrossRefGoogle Scholar