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Theoretical Calculation of Background in X-Ray Spectrometry for the Determination of Some Heavy Trace Elements

Published online by Cambridge University Press:  06 March 2019

Jean-Jacques Gruffat*
Affiliation:
Département de Géologie - Ecole des Mines 158 Cours Fauriel 42023 SAINT-ETIENNE CEDEX 2 - FRANCE
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Abstract

The Kulenkampff-Kramers formula giving the spectral distribution of the continuum as a function of wavelength allows a correct calculation of background under the peak. It is only necessary to measure two backgrounds, one on each side of the peak, The true background under the peak is given by multiplying them by adequate coefficients and adding them up. This method has been applied to the determination of low amounts of Ce, La, Ba and Cs in geological samples.

Type
X. Mathematical Methods in X-Ray Spectrometry (XRS)
Copyright
Copyright © International Centre for Diffraction Data 1991

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References

1. Vié Le Sage, R. et al. Utilisation du Rayonnement Primaire Diffusé par l’Enchantillon pour une Determination Rapide et Precisé des Elements Traces dans les Roches. X-Ray Spectrom. 8, 121 (1979).10.1002/xrs.1300080309Google Scholar
2. Tertian, R., Claisse, F., Principles of Quantitative X-Ray Fluorescence Analyses. Heyden, London (1982).Google Scholar