Volume 46 Issue 12
Dec.  2021
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Liang Zhengwei, Tian Shihong, 2021. Uranium 'Stable' Isotope Fractionation and Its Applications in Earth Science. Earth Science, 46(12): 4405-4426. doi: 10.3799/dqkx.2021.091
Citation: Liang Zhengwei, Tian Shihong, 2021. Uranium "Stable" Isotope Fractionation and Its Applications in Earth Science. Earth Science, 46(12): 4405-4426. doi: 10.3799/dqkx.2021.091

Uranium "Stable" Isotope Fractionation and Its Applications in Earth Science

doi: 10.3799/dqkx.2021.091
  • Received Date: 2021-05-02
  • Publish Date: 2021-12-15
  • Uranium isotope (238U/235U, usually expressed as δ238U) has been the research hotspot in the field of non-traditional stable isotopes. In the last century, it was thought that uranium isotope fractionation did not exist, so the development of uranium isotope research was very slow. However, with the development of the analytical technology, it has been found that there exists significant fractionation between238U and 235U in nature, which makes uranium isotopes an ideal tracer in Earth science. Indeed, overwhelming amounts of studies of uranium isotopes as a paleo-redox proxy have been published so far, most of which use uranium isotope to track the evolution of oxygen levels of Earth's subaerial environments through time and, furthermore, the potential relationship between the several big mass extinctions and the redox conditions of the oceans. Although researches on uranium isotope have achieved progresses in the co-evolution of the hydrosphere and biosphere, some problems still remain some unsolved. For example, the effects of microcosmic pathways of biological and abiotic reduction reactions on uranium isotope fractionation, and how the 238U/235U can trace the source of uranium ore deposits. Here, in this paper, it provides an overview of the uranium and its isotope geochemistry over the last decades, aiming at promoting applications of uranium isotopes in the genesis of uranium polymetallic deposits and high-temperature geochemistry in the future.

     

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