首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Redistribution of fissiogenic and non-fissiogenic REE, Th and U in and around natural fission reactors at Oklo and Bangombe, Gabon
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Redistribution of fissiogenic and non-fissiogenic REE, Th and U in and around natural fission reactors at Oklo and Bangombe, Gabon

机译:在加蓬Oklo和Bangombe的自然裂变反应堆中及其周围,裂变和非裂变的REE,Th和U重新分布

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摘要

Elemental abundances and isotopic compositions of rare earth elements (REE), Th and U of twenty eight samples from four kinds of natural fission reactors at the Oklo and Bangombe uranium ores were determined by mass spectrometry. Fissiogenic and non-fissiogenic REE components of each sample were calculated from the isotopic compositions. The geochemical distribution of both fissiogenic and non-fissiogenic REE differs among the four reactors. Each reactor shows the following features possibly associated with the local geochemical conditions. (I) Reactor 9 at the shallow depth of the Oklo deposit contains higher amounts of non-fissiogenic REE than the other reactors. The distribution of non-fissiogenic REE does not reflect the primordial REE abundance patterns, and might have been disturbed in and around the reactor due to supergene alteration. Our results suggest that significant amounts of fissiogenic lighter REE (LREE), such as La, Cc and Pr, were mobile in the reactor; (2) Reactors 10 and 13 located deep underground have much lower contents of non-fissiogenic REE than reactor 9. All fissiogenic REE show high retention in the reactors. Non-fissiogenic REE of reactor 10 inform of the primordial ore formation without any geochemical disturbance. Little redistribution of both fissiogenic and non-fissiogenic REE in the reactor 10 was observed; and (3) The Bangombe reactor located at shallow depth has apparently well preserved fissiogenic REE. Non-fissiogenic REE in the Bangombe reactor might have been disturbed, possibly by hydrothermal processes. The distribution behavior of fissiogenic REE is considered to be related with physico-chemical reactor conditions such as nuclear reaction temperature and chemical compositions of each reactor, but clear relationship between nuclear parameters and the REE distribution could not be obtained in this study. Copyright (C) 2000 Elsevier Science Ltd. [References: 44]
机译:通过质谱法测定了Oklo和Bangombe铀矿中四种自然裂变反应堆的28个样品的稀土元素(REE),Th和U的元素丰度和同位素组成。从同位素组成中计算出每个样品的致裂和非裂变稀土元素。在这四个反应堆中,裂变和非裂变稀土元素的地球化学分布都不同。每个反应堆均显示以下特征,可能与当地的地球化学条件有关。 (I)Oklo矿床浅层的反应堆9含有比其他反应堆更多的非裂变稀土元素。非裂变稀土元素的分布不能反映原始稀土元素的丰度模式,并且可能由于超基因改变而在反应堆内部和周围受到干扰。我们的结果表明,大量的易裂化轻质稀土元素(LREE),如La,Cc和Pr在反应堆中可移动。 (2)位于地下深处的反应堆10和13具有比反应堆9低得多的非裂变稀土元素含量。所有裂变稀土元素在反应堆中均显示出较高的保留率。反应堆10的非裂变稀土元素可在无任何地球化学干扰的情况下通知原始矿石的形成。观察到在反应器10中几乎没有重新产生裂变和非裂变的REE。 (3)位于浅层的Bangombe反应堆显然保存得很好,具有成岩性REE。 Bangombe反应堆中的非裂变稀土元素可能已经受到水热过程的干扰。裂变稀土元素的分布行为被认为与物理化学反应器条件有关,例如核反应温度和每个反应器的化学组成,但在这项研究中无法获得清晰的核参数与稀土元素分布之间的关系。版权所有(C)2000 Elsevier Science Ltd. [参考:44]

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