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首页> 外文期刊>Journal of Nuclear Materials: Materials Aspects of Fission and Fusion >Thermal diffusion of chlorine in uranium dioxide studied by secondary ion mass spectrometry and X-ray absorption spectroscopy
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Thermal diffusion of chlorine in uranium dioxide studied by secondary ion mass spectrometry and X-ray absorption spectroscopy

机译:通过二次离子质谱和X射线吸收光谱研究氯在二氧化铀中的热扩散

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摘要

In a nuclear reactor, Cl-35 present as an impurity in the nuclear fuel is activated by thermal neutron capture. During interim storage or geological disposal of the nuclear fuel, Cl-36 may be released from the fuel to the geo/biosphere and contribute significantly to the 'instant release fraction'. In order to elucidate the diffusion mechanisms, both irradiation and thermal effects must be assessed. This paper deals with the thermal diffusion of chlorine in depleted UO2. For this purpose, sintered UO2 pellets were implanted with Cl-37 at an ion fluence of 10(13) cm(-2) and successively annealed in the 1175-1475 K temperature range. The implanted chlorine is used to simulate the behaviour of the displaced one due to recoil and to interactions with the fission fragments during reactor operation. The behaviour of the pristine and the implanted chlorine was investigated during thermal annealing. SIMS and p-XAS (at the G-K edge) analyses show that: (1) the thermal migration of implanted chlorine becomes significant at 1275 K; this temperature and the calculated activation energy of 4.3 eV points out the great ability of chlorine to migrate in UO2 at relatively low temperatures, (2) the behaviour of the implanted chlorine which aggregates into 'hot spots' during annealing before its effusion is clearly different from that of the pristine one which remains homogenously distributed after annealing, (3) the 'hot spot' and the pristine chlorine seem to be in different structural environments. Both types of chlorine are assumed to have a valence state of -I, (4) the comparison between an U2O2Cl5 reference compound and the pristine chlorine environment shows a contribution of the U2O2Cl5 to the pristine chlorine. (C) 2007 Elsevier B.V. All rights reserved.
机译:在核反应堆中,作为杂质存在于核燃料中的Cl-35通过热中子捕获而被激活。在核燃料的临时存储或地质处置期间,Cl-36可能会从燃料中释放到地球/生物圈中,并对“即时释放率”做出重大贡献。为了阐明扩散机理,必须同时评估辐射和热效应。本文探讨了氯在贫乏UO2中的热扩散。为此,将烧结的UO2球团以10(13)cm(-2)的离子通量注入Cl-37,并在1175-1475 K温度范围内连续退火。注入的氯用于模拟由于反冲和在反应堆运行过程中与裂变碎片的相互作用而置换的氯的行为。在热退火过程中研究了原始和注入的氯的行为。 SIMS和p-XAS(在G-K边缘)分析表明:(1)注入的氯的热迁移在1275 K时变得显着;该温度和4.3 eV的计算活化能表明,氯在相对较低的温度下在UO2中迁移的能力很强,(2)注入的氯的行为在退火之前在退火之前聚集成“热点”,而渗出之前明显不同与原始材料相比,原始材料在退火后仍保持均匀分布,(3)“热点”和原始氯似乎处于不同的结构环境中。假定这两种类型的氯的价态均为-I,(4)U2O2Cl5参考化合物与原始氯环境之间的比较表明,U2O2Cl5对原始氯的贡献。 (C)2007 Elsevier B.V.保留所有权利。

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