Abstract
A radioisotope-excited X-ray fluorescence technique is applied for the determination of thorium and rare earth elements in britholite ore from Canada. An annular source of57Co is employed for excitation of characteristic K X-rays of thorium and rare earth elements. The peak ratios of lanthanides were used to remove the difficulties because of overlapping lines at the 33–50 keV energy region. Matrix effects are examined also in detail and compensated for infinitely thick powdered ore sample. Results obtained in the analysis agree well with recommended values of Canada.
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References
J.J. Labrecque, J.M. Beusen, R.E. Van Grieken,X-Ray Spectrom., 15 /1986/ 13.
P. Arikan, I. Alkan,J. Radioanal. Chem., 67 /1981/ 403.
P. Van Espen, L. Van T'Dack, F. Adams, R.E. Van Grieken,Anal. Chem., 51 /1979/ 961.
A. Şaplakoĝlu, I. Özoĝlu, M. Tan, H. Erdoĝan,A.N.R.C. Tech. Journal., 1 /1974/ 47.
P. Arikan, H. Demirel,J. Radioanal. Nucl. Chem., 90 /1985/ 317.
V. Machacek, D. Weiss,X-Ray Spectrom., 14 /1985/ 317.
R. Tertian, F. Claisse, Principles of Quantitative XRF Analysis, Heyden, London, 1982.
P. Arikan, A. Zararsiz, N. Efe,J. Radioanal. Nucl. Chem., 100 /1986/ 303.
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Efe, N., Akman, S. & Arikan, P. Determination of rare earth elements and thorium in britholite ore by energy dispersive X-ray fluorescence spectrometry. Journal of Radioanalytical and Nuclear Chemistry Letters 117, 1–9 (1987). https://doi.org/10.1007/BF02165544
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DOI: https://doi.org/10.1007/BF02165544