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Potential incorporation of transuranics into uranyl phases: Implications for the immobilization of radionuclides in the alteration phases of spent nuclear fuel.

机译:可能将超铀酸类化合物掺入铀基相中:对于将放射性核素固定在乏核燃料的改变相中的意义。

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摘要

The UO2 in spent nuclear fuel is unstable under the moist oxidizing conditions expected in the proposed repository at Yucca Mountain, Nevada and will be altered to secondary uranyl (UO22+) phases. The transuranics released during the corrosion of spent fuel may also be incorporated into the structures of these phases. The incorporation of radionuclides into alteration products will limit their mobility.; A series of precipitation tests were conducted to determine the potential incorporation of Ce4+ and Nd3+ (surrogates for Pu4+ and Am3+, respectively) into uranyl phases. The uranium alteration phases examined in this study include ianthinite ([U24+(UO2)4O6(OH) 4(H2O)]4](H2O)5), becquerelite (Ca(UO2)6O4(OH)6(H2O) 8), Na-compreignacite (Na2(UO2)6O 4(OH)6(H2O)7), boltwoodite (K(UO 2)(SiO3OH)(H2O)1.5), and other unidentified uranyl compounds. The results of these experiments demonstrate that significant quantities of both Ce4+ (up to 800 ppm) and Nd3+ (up to 24,800 ppm) maybe incorporated within the uranium alteration phases. By analogy, it is likely that Pu4+ and Am3+ will behave in a similar fashion. Incorporation of cerium and neodymium by the uranyl phases can be accomplished by co-precipitation of the elements within the crystalline structure, by adsorption of the elements onto surfaces of the solid phases, or by inclusion of the components into the host solids in which they ultimately become absorbed by a process of surface overgrowth. The incorporation of Ce4+ and Nd3+ into or onto the uranium phases appeared to be dependent on the solution pH. The pH dependence for enhancing tetra- and trivalent element incorporation varies with various incorporation reactions and host phases.
机译:在内华达州尤卡山拟建的储存库中,在预期的潮湿氧化条件下,乏核燃料中的UO 2 不稳定,并将被转化为仲铀酰(UO 2 2 + )阶段。在乏燃料腐蚀期间释放的超铀化合物也可以并入这些相的结构中。放射性核素掺入蚀变产物将限制其迁移。进行了一系列降水试验,以确定Ce 4 + 和Nd 3 + (Pu 4 + 和Am <分别是super> 3 + )变成铀酰相。在这项研究中检查的铀蚀变阶段包括堇青石([U 2 4 + (UO 2 4 O 6 (OH) 4 (H 2 O)] 4 ](H 2 O) 5 ),珠光沸石(Ca(UO 2 6 O 4 (OH) 6 (H 2 O) 8 ),钠共镁石(Na 2 (UO 2 6 O 4 (OH) 6 (H 2 O) 7 ) ,芒硝(K(UO 2 )(SiO 3 OH)(H 2 O) 1.5 )和其他未确定的铀酰化合物。这些实验的结果表明,可能在铀蚀变中掺入了大量的Ce 4 + (最高800 ppm)和Nd 3 + (最高24800 ppm)。阶段。以此类推,Pu 4 + 和Am 3 + 的行为可能相似。铀基相中铈和钕的掺入可通过共沉淀晶体结构中的元素,将元素吸附到固相表面上或将组分包含在最终形成主体的固体中来实现被表面过度生长的过程所吸收。 Ce 4 + 和Nd 3 + 掺入铀相的过程似乎取决于溶液的pH值。用于增强四价和三价元素掺入的pH依赖性随各种掺入反应和主体相而变化。

著录项

  • 作者

    Kim, Cheol-Woon.;

  • 作者单位

    University of Missouri - Rolla.;

  • 授予单位 University of Missouri - Rolla.;
  • 学科 Geology.; Geochemistry.; Environmental Sciences.; Chemistry Nuclear.
  • 学位 Ph.D.
  • 年度 2001
  • 页码 152 p.
  • 总页数 152
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;地质学;环境科学基础理论;无机化学;
  • 关键词

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