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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Kaolinite as an in situ dosimeter for past radionuclide migration at the Earth's surface
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Kaolinite as an in situ dosimeter for past radionuclide migration at the Earth's surface

机译:高岭石作为原位剂量计,用于过去放射性核素在地球表面的迁移

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The origin of 3 types of point defects (A-, A'- and B-centers) in kaolinite, due to natural irradiation and detected by electron paramagnetic resonance spectroscopy (EPR), has been demonstrated by artificial irradiation. The potential use of tracing the dynamics of the transfer of radionuclides through A-centers (i.e. the most stable centers) was qualitatively tested on different low-temperature alteration systems, some associated with U-concentrations. This paper proposes a quantitative approach to the reconstruction of the past migration of radionuclides by dosimetry of A-centers. With this aim in mind, the efficiency of alpha- and gamma-radiations to produce A-centers was determined by experimental irradiation. Parameters extracted from A-center growth curves, together with their relationship with a parameter describing the degree of order of kaolinite, permitted (i) a definition to be made of the dose range in which a given kaolinite could be used as a dosimeter and (ii) the quantitative derivation of U-concentration from the cumulative dose (paleodose) of kaolinites. This was achieved by a formalism that accounted for the contribution of natural radiosources to the production of A-centers. The formalism was applied to the Nopal I U-deposit (Chihuhua, Mexico), considered as a natural analogue of a high level nuclear waste repository. Irrespective of the scenario considered, in terms of kaolinite age and of degree of isotopic disequilibrium in the system, A-center dosimetry permitted the determination of past occurrences of U which were several orders of magnitude higher than the present-day measured U-concentrations. Furthermore, this approach also provided evidence for several previous episodes of U-migration. EPR spectroscopy is thus a unique tool for the quantitative, indirect assessment of past radionuclide migration in the geosphere and kaolinite is a reliable in-situ dosimeter. (C) 1998 Elsevier Science Ltd. All rights reserved. [References: 45]
机译:高岭石中的三种类型的点缺陷(A-,A'-和B-中心)的起源是由于自然辐照和通过电子顺磁共振波谱(EPR)检测到的,已通过人工辐照得到了证明。在不同的低温蚀变系统(其中一些与U浓度相关)上定性测试了跟踪放射性核素通过A中心(即最稳定的中心)转移动力学的潜在用途。本文提出了一种定量方法,可通过A中心的剂量测定法重建放射性核素的过去迁移。出于这个目的,通过实验辐射确定了α和γ辐射产生A中心的效率。从A中心生长曲线中提取的参数及其与描述高岭石有序程度的参数的关系允许(i)定义给定高岭石可用作剂量计的剂量范围和( ii)从高岭石的累积剂量(古剂量)定量推导U浓度。这是通过形式主义实现的,这种形式解释了自然无线电源对A中心生产的贡献。形式主义应用于Nopal I U矿床(墨西哥奇胡瓦),被认为是高级核废料矿床的自然类似物。无论考虑哪种情况,就高岭石年龄和系统中同位素不平衡程度而言,A中心剂量测定法都可以确定过去发生的U量,其比当前测得的U浓度高几个数量级。此外,这种方法还为以前的几次U迁移事件提供了证据。因此,EPR光谱学是定量,间接评估过去放射性核素在地球圈中迁移的独特工具,而高岭石是可靠的原位剂量计。 (C)1998 Elsevier ScienceLtd。保留所有权利。 [参考:45]

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