Abstract
In the geochemical analysis of charnockite matrix, PIXE results do not show either the minor or traces of thorium and uranium even though they are present in that charnockite composition. Because of a continuous range of elements in charnockite composition and characteristic X-rays of some elements present at similar to characteristic X-rays of thorium and uranium. Therefore, Th and U traces quantification are limited due to the interferences in the PIXE spectrum at similar characteristic X-ray energies of the elements. Otherwise, it is possible for quantification, if the composition does not contain the elements at similar characteristic X-rays of Th and U or using complementary techniques.
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Acknowledgements
I wish to thank to Prof. Y. Rama Krishna, Department of Engineering Physics, Andhra University, and Visakhapatnam and for his support and help in the geochemical analysis of the experimental data. I am grateful to Prof. A. Durga Prasad Rao, senior professor and Head of the Department, Department of Nuclear Physics, Andhra University, Visakhapatnam. I thank Dr. D. P. Mahapatra, Director, Institute of Physics, and Bhubaneswar, providing accelerator facility to carry out the research work and for all amenities provided during our stay at the ion beam laboratory.
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Satayanarayana, A.V.S., Rao, M.J. & Mouli, K.C. Limitation of uranium and thorium traces in charnockite matrix-PIXE analyses at 3 MeV with Si (Li) detector. J Radioanal Nucl Chem 328, 83–87 (2021). https://doi.org/10.1007/s10967-021-07623-0
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DOI: https://doi.org/10.1007/s10967-021-07623-0