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Study on strontium isotope abundance-ratio measurements by using a 13-MeV proton beam
The Rb-Sr dating method is used in dating Paleozoic and Precambrian rocks. This method measures the 87 Rb and the 87 Sr concentrations by using thermal ionization mass spectrometry (TIMS) [J. Hefne et al ., Inter. J. Phys. Sci. 3 (1), 28 (2008)]. In addition, it calculates the initial 87 Sr/ 86 Sr r...
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Published in: | Journal of the Korean Physical Society 2016, 69(6), , pp.1121-1124 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The Rb-Sr dating method is used in dating Paleozoic and Precambrian rocks. This method measures the
87
Rb and the
87
Sr concentrations by using thermal ionization mass spectrometry (TIMS) [J. Hefne
et al
., Inter. J. Phys. Sci.
3
(1), 28 (2008)]. In addition, it calculates the initial
87
Sr/
86
Sr ratio to increase the reliability of Rb-Sr dating. In this study, the
87
Sr/
86
Sr ratio was measured by using a 13-MeV proton accelerator. Proton kinetic energies are in the range of tens of megaelectronvolts, and protons have large absorption cross-sections for (
p
,
n
) reactions with most substances. After absorbing a proton with such a high kinetic energy, an element is converted into a nuclide with its atomic number increased by one via nuclear transmutation. These nuclides usually have short half-lives and return to the original state through radioactive decay. When a strontium sample is irradiated with protons, nuclear transmutation occurs; thus, the strontium isotope present in the sample changes to a yttrium isotope, which is an activated radioisotope. Based on this, the
87
Sr/
86
Sr ratio was calculated by analyzing the gamma-rays emitted by each yttrium isotope. The KIRAMS-13 cyclotron at the Cyclotron Center of Chosun University, where 13-MeV protons can be extracted, was utilized in our experiment. The
87
Sr/
86
Sr isotope ratio was computed for samples irradiated with these protons, and the result was similar to the isotope ratio for the Standard Reference Material,
i.e
., 98.2 ± 3.4%. As part of the analysis, proton activation analyses were performed using 13-MeV protons, and the experimental results of this research suggest a possible approach for measuring the strontium-isotope abundance ratio of samples. |
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ISSN: | 0374-4884 1976-8524 |
DOI: | 10.3938/jkps.69.1121 |