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Quantitative Analysis of Elements in Sediments and Soils by X-Ray Fluorescence

Published online by Cambridge University Press:  01 July 2024

E. R. Tuncer*
Affiliation:
Engineering Research Institute, Department of Civil Engineering, Iowa State University Ames, IA 50011, U.S.A.
T. Demirel
Affiliation:
Engineering Research Institute, Department of Civil Engineering, Iowa State University Ames, IA 50011, U.S.A.
R. A. Lohnes
Affiliation:
Engineering Research Institute, Department of Civil Engineering, Iowa State University Ames, IA 50011, U.S.A.
*
Present address: Civil Engineering Department, Middle East Technical University, Ankara, Turkey.
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Abstract

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Previous applications of the method of known additions for quantitative X-ray fluorescent analysis have assumed a linear relationship between peak intensity and concentration of the element being analyzed. This assumption is true for soils or sediments containing small amounts of the element in question. In this paper, an equation is derived which takes into account both absorption and enhancement and thus is applicable to samples containing high concentrations of the element. The equation was tested by analyzing an artificial soil sample containing 60% kaolinite and 40% hematite, i.e. the sample contained 28% by weight iron. The fluorescent analysis utilizing the equation derived here resulted in an iron content of 27%. In addition, nine soils from Hawaii were analyzed by this method and the results of these analyses compared with analyses by atomic absorption. The agreement between the two methods is good. It is concluded that the method and equations proposed here provides a reliable measurement of elements in a soil sample which contains high concentrations of the elements in question.

Type
Research Article
Copyright
Copyright © Clay Minerals Society 1977

Footnotes

*

Investigations sponsored by U.S. Army Research Office and the Engineering Research Institute, Iowa State University.

References

Adler, I. (1966) X-ray Emission Spectrography in Geology. Methods in Geochemistry and Geophysics, 4: Elsevier, Amsterdam.Google Scholar
Beattie, H. J. and Brissey, R. M. (1954) Calibration method for X-ray fluorescence spectrometry: Anal. Chem. 26, 980.CrossRefGoogle Scholar
Birks, L. S. (1959) X-ray Spectrochemical Analysis: Interscience, New York.Google Scholar
Blokhin, M. A. (1965) Methods of X-ray Spectroscopic Research: Pergamon Press, Oxford.Google Scholar
Cullity, B. D. (1967) Elements of X-ray Diffraction: Addison–Wesley, Reading, MA.Google Scholar
Diehl, H. (1970) Quantitative Analysis: Oakland Street Press, Ames, Iowa.Google Scholar
Handy, R. L. and Rosauer, E. A. (1959) X-ray fluorescence analysis of total iron and manganese in soils: Proc. Iowa Acad. Sci. 66, 237247.Google Scholar
Jenkins, R. and deVries, J. L. (1967) Practical X-ray Spectrometry: Phillips Technical Library.Google Scholar
Lee, R. W. and Güven, N. (1975) Chemical interferences in atomic absorption spectrometric analysis of silicates in the fluoboric–boric acids matrix: Chem. Geol. 16, 5358.CrossRefGoogle Scholar
Müller, R. O. (1972) Spectrochemical Analysis by X-ray Fluorescence: Plenum Press, New York.CrossRefGoogle Scholar
Tuncer, E. R. (1976) Engineering behavior and classification of lateritic soils in relation to soil genesis: Unpublished Ph.D. thesis, Iowa State University, Ames.Google Scholar