Abstract
Deuteron activation was found to be suitable for analysing geological samples, as no interfering activities are formed from oxygen, silicon and aluminium, which together make up more than 80% by weight of the earth's crust. To test the applicability of this method to geological samples, the mineral tourmaline was activated with 5.5 MeV deuterons obtained from the 6 MV van de Graaff accelerator at the Southern Universities Nuclear Institute. The induced activities were measured and analysed by gammaray spectrometry and the elements Al, Mg, B, Mn, Na, Fe and Li could readily be determined.
Similar content being viewed by others
References
G. E. Gordon, K. Randle, G. G. Goles, J. B. Corlis, M. H. Beeson, S. S. Oxley,Geochim. Cosmochim. Acta, 32 (1968) 369.
H. Higuchi, K. Tamura, H. Takahashi, N. Onuma, H. Hamaguchi, Proc. Modern Trends in Activation Analysis, N.B.S., Gaithersburg, 1969, p. 334.
K. Randle, G. Goles, Proc. Modern Trends in Activation Analysis, N.B.S., Gaithersburg, 1969, p. 347.
J. W. Winchester, Proc. Symp. Nuclear Techniques for Mineral Exploration and Exploitation, Cracow, 1969, I.A.E.A., Vienna, 1969, p. 1.
G. E. Gordon, J. C. Dran, P. A. Baedecker, C. F. L. Anderson, Proc. Modern Trends in Activation Analysis, N.B.S., Gaithersburg, 1969, p. 399.
F. Girardi, Proc. Modern Trends in Activation Analysis, N.B.S., Gaithersburg, 1969, p. 577.
G. H. Morrison,Anal. Chem., 43 (1971) 23A.
Ph. Albert, L'analysis par Radioactivation, Gauthier-Villards, Paris, 1963.
G. H. Morrison, Trace Analysis: Pysical Methods, J. Wiley, New York, 1963, p. 10.
C. Olivier, M. Peisach,J. Radioanal. Chem., 11 (1972) 105.
W. A. Deer, R. A. Howie, J. Zussman, An Introduction to the Rock-forming Minerals, Longmans, 1966, p. 92.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Pretorius, R., Odendaal, F. & Peisach, M. Deuteron activation analysis of geological samples. J. Radioanal. Chem. 12, 139–149 (1972). https://doi.org/10.1007/BF02520983
Issue Date:
DOI: https://doi.org/10.1007/BF02520983