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Corrosion and Alteration of Lead Borate Glass in Bentonite Equilibrated Water

机译:膨润土平衡水中铅硼酸盐玻璃的腐蚀和改变

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The development of an iodine immobilization technique that can fix radioactive iodine in waste form for a long period and constrain its leaching into pore water is necessary in order to secure the long-term safety of geological disposal of transuranic (TRU) waste. Lead borate glass vitrified at a low temperature is regarded as a promising material for immobilizing the Iodine-129 that is recovered from spent AgI filters generated by reprocessing plants in Japan and which may have a significant effect on the long-term safety of geological disposal. Batch leaching tests were conducted to understand glass dissolution behavior in various solutions that account for geological disposal conditions. Boron dissolved at the highest rate in all types of solutions to be used as an index element for measuring the glass dissolution rate. On the other hand, lead dissolved in these solutions at a much lower rate. These results are consistent with an electron micro-probe analysis (EPMA) of the altered glass surfaces that indicated the depletion of boron and enrichment of lead near the surfaces. The altered glass surfaces were further examined by scanning and transmission electron microscopy (SEM/TEM) and X-ray diffraction (XRD). SEM/TEM observation showed formation of a porous altered layer consisting of fine crystallites on the pristine glass and euhedral crystals on the altered layer. XRD analysis indicated that the fine crystallites and euhedral crystals are hydrocerussite, Pb_3 (CO_3)_2(OH)_2, which was predicted by geochemical calculation as the precipitate for the experimental system.
机译:能够在长期内将废物碘固定放射性碘的碘固定化技术,并对其浸入孔隙水来保护其浸入孔隙水中是必要的,以确保经阵挛(Tru)废物的地质处理的长期安全性。在低温下玻璃化的铅硼酸盐玻璃被认为是用于固定从日本再处理植物产生的废富肽过滤器中回收的碘-129的有希望的材料,这可能对地质处置的长期安全性具有显着影响。进行批次浸出试验以了解用于地质处理条件的各种溶液中的玻璃溶解行为。硼以所有类型的溶液中的最高速率溶解用作用于测量玻璃溶解速率的指标元件。另一方面,以更低的速率溶解在这些溶液中的铅。这些结果与了表明硼和的表面附近富集铅的消耗改变的玻璃表面的电子微探针分析(EPMA)是一致的。通过扫描和透射电子显微镜(SEM / TEM)和X射线衍射(XRD)进一步检查改变的玻璃表面。 SEM / TEM观察显示形成多孔改变层,其在原始玻璃和改变层上的Euhedral晶体上组成的细晶体。 XRD分析表明,微晶体和自形晶体hydrocerussite,Pb_3(CO_3)_2(OH)_2,这是由计算地球化学作为实验系统沉淀预测。

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