Geochemical Characteristics of an Ancient Nuclear Reactor ^|^ldquo;Oklo^|^rdquo;

  • Hidaka H.
    Department of Earth and Planetary Systems Science, Hiroshima University

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タイトル別名
  • Geochemical Characteristics of an Ancient Nuclear Reactor “Oklo”

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The Oklo uranium deposit at the Republic of Gabon, central Africa, had partly functioned as natural fission reac-tors. Many elements of the Oklo reactor zones and the related samples show the variations in the isotopic compo-sition caused by a combination of nuclear fission, neutron capture, and radioactive decay. Isotopic studies provide useful information to estimate reactor conditions and to understand behavior of radionuclides in geological media. In my recent work, in-situ REE, Pb, and U isotopic analyses of individual tiny minerals in and around reactor zones have been performed using a Sensitive High Resolution Ion Micro-Probe (SHRIMP). The data suggest the adsorption property of apatite in trapping fissiogenic LREE and Pu migrated from the reactor zone, and distribution of fissiogenic REE under oxidizing atmosphere.

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詳細情報 詳細情報について

  • CRID
    1390282679457477248
  • NII論文ID
    10021102008
  • NII書誌ID
    AA11948402
  • DOI
    10.14494/jnrs2000.8.99
  • COI
    1:CAS:528:DC%2BD2sXhsVCgtb3L
  • ISSN
    18835813
    13454749
  • 本文言語コード
    en
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
    • KAKEN
  • 抄録ライセンスフラグ
    使用不可

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