Uranium-Thorium Decay Series in the Oceans: Overview


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Michiel.Rutgers.v.d.Loeff [ at ] awi.de

Abstract

Natural radioactivity provides tracers in a wide range of characteristic timescales and reactivities, which can be used as tools to study the rate of reaction and transport processes in the ocean. Apart from cosmogenic nuclides and the long-lived radioisotope K-40, the natural radioactivity in the ocean is primarily derived from the decay series of three radionuclides that were produced in the period of nucleosynthesis preceding the birth of our solar system: Uranium-238, Thorium-232, and Uranium-235 (a fourth series, including Uranium-233, has already decayed away). The remaining activity of these so-called primordial nuclides in the Earth's crust, and the range of half-lives and reactivities of the elements in their decay schemes, control the present distribution of U-series nuclides in the ocean



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Inbook
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Peer-reviewed
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Published
Eprint ID
35600
DOI https://www.doi.org/10.1016/b978-0-12-409548-9.09128-4

Cite as
Rutgers van der Loeff, M. M. (2014): Uranium-Thorium Decay Series in the Oceans: Overview / S. Elias (editor) , In: Earth Systems and Environmental Sciences, (Reference Module in Earth Systems and Environmental Sciences), Amsterdam, Elsevier, 16 p., ISBN: 978-0-12-409548-9 . doi: https://www.doi.org/10.1016/b978-0-12-409548-9.09128-4


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