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首页> 外文期刊>Cement and Concrete Research >Physico-chemical investigation of clayey/cement-based materials interaction in the context of geological waste disposal: Experimental approach and results
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Physico-chemical investigation of clayey/cement-based materials interaction in the context of geological waste disposal: Experimental approach and results

机译:地质废物处置中黏土/水泥基材料相互作用的物理化学研究:实验方法和结果

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摘要

Within the concepts under study for the geological disposal of intermediate-level long-lived waste, cementbased materials are considered as candidate materials. The clayey surrounding rock and the cement-based material being considered differ greatly in their porewater composition. Experiments are conducted on the diffusion of solutes constituting those porewaters in a confined clay/cement composite system using cells. The test temperature was set at 25 °C and 2, 6 and 12 months. Results supply new information: carbonation is low and not clog the interface. Such absence of carbonation allows for the diffusion of aqueous species and, thus, for the degradation of the cement paste and the illitisation of illite/smectite interstratifications. The cement material is subjected to a decalcification: portlandite dissolution and a CaO/SiO_2 reduction in the calcium silicate hydrate. The sulphate in diffusion induces non-destructive ettringite precipitation in the largest pores. After 12 months, about 800 um of cement material is concerned by ecalcification.
机译:在研究中级长寿命废物的地质处置概念中,水泥基材料被视为候选材料。所考虑的粘土质围岩和水泥基材料的孔隙水成分差异很大。使用细胞在封闭的粘土/水泥复合系统中进行了构成这些孔隙水的溶质的扩散实验。测试温度设定为25°C以及2、6和12个月。结果提供了新的信息:碳酸化程度低且不会阻塞界面。这种没有碳酸化的现象允许水性物质的扩散,并因此导致水泥浆的降解和伊利石/蒙脱石层化的伊利石化。对水泥材料进行脱钙处理:硅酸钙的溶解和硅酸钙水合物中CaO / SiO_2的还原。扩散中的硫酸盐会在最大的孔隙中引起非破坏性钙矾石沉淀。 12个月后,约有800um的水泥材料被钙化。

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