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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >French SON 68 nuclear glass alteration mechanisms on contact with clay media
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French SON 68 nuclear glass alteration mechanisms on contact with clay media

机译:法国SON 68与黏土介质接触的核玻璃蚀变机制

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The leaching behavior of the nonradioactive French SON 68 (R7T7-type) nuclear glass was investigated in the presence of FoCa7 clay. Static experiments were carried out at 90 degreesC under conditions favorable to convective transfer. Three test environments were compared: a clay medium, the same clay medium doped with 2.5 wt.% silica gel, and pure water. These experiments showed that in raw clay the glass alteration rate remained near the initial value for several hundred days, whereas in pure water at the same temperature and with the same glass-surface-area-to-solution-volume (S/V) ratio the alteration rate quickly dropped by several orders of magnitude after the formation of a protective gel layer. This major difference between the two media can be attributed to transfer of the principal gel-forming elements (Si, Al, Ca) into the clay medium as a result of sorption phenomena and probably the precipitation of silicate phases. The addition of silica gel to the clay not only neutralizes the clay sorption capacity, but also protects the glass from significant alteration (the glass was altered appreciably less than in pure water). This article discusses the mechanisms limiting the glass alteration kinetics in the test media. The gel that forms by reconstitution of hydrolyzed glass species at the glass/clay interface is shown to constitute a diffusion barrier whose effectiveness depends to a large degree on the conditions under which species are removed by the external medium. Interpreting the experimental data from this standpoint leads to a reexamination of the classic model in which the glass alteration kinetics are inhibited by the dissolved silicon content. (C) 2001 Elsevier Science Ltd. All rights reserved. [References: 51]
机译:研究了在FoCa7粘土存在下非放射性法国SON 68(R7T7型)核玻璃的浸出行为。在有利于对流转移的条件下于90°C进行静态实验。比较了三种测试环境:粘土介质,掺有2.5 wt。%硅胶的相同粘土介质和纯水。这些实验表明,在原始黏土中,玻璃的变化率在最初的几百天内保持在初始值附近,而在纯水中,在相同的温度和相同的玻璃表面积与溶液体积比(S / V)下在形成保护性凝胶层后,变化速率迅速下降了几个数量级。两种介质之间的主要区别可以归因于主要的凝胶形成元素(Si,Al,Ca)由于吸附现象以及可能的硅酸盐相沉淀而转移到粘土介质中。向粘土中添加硅胶不仅可以中和粘土的吸附能力,而且还可以保护玻璃免受明显的改变(与纯水相比,玻璃的改变明显更少)。本文讨论了限制测试介质中玻璃变化动力学的机制。通过在玻璃/粘土界面处水解玻璃物质的重构而形成的凝胶显示出构成扩散屏障,其有效性在很大程度上取决于外部介质除去物质的条件。从这个角度解释实验数据导致对经典模型的重新检验,在经典模型中,溶解的硅含量抑制了玻璃的改变动力学。 (C)2001 Elsevier ScienceLtd。保留所有权利。 [参考:51]

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