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Uptake and retention of molybdenum in cementitious systems

机译:水泥系统中钼的吸收与保留

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摘要

The uptake of molybdenum, present in aqueous cementitious environments in the form of the molybdate ion (MoO42-), by various cement hydration phases such as calcium-silicate-hydrates (C-S-H), monosulphate (AFm), ettringite (AFt), as well as hardened cement paste made from Ordinary Portland cement (OPC), was studied in batch-type sorption experiments under anoxic conditions. Uptake kinetics were generally fast, leading to sorption equilibrium in less than 30 days. In particular, a strong uptake of molybdate by AFm phases was observed as well as a distinct contribution of C-S-H phases to the molybdate retention in cementitious systems, the latter depending on the Ca/Si-ratio of the C-S-H and the alkali content in solution. In systems containing hydmgarnet, the neo-formation of a molybdate-bearing AFm phase was identified as an additional process contributing to molybdate retention. The findings have implications for selecting grouts for the immobilisation of radioactive waste streams containing Mo-93 and also enhance the data available on molybdate sorption and retention in cementitious systems.
机译:通过各种水泥水合相(Moo42-)的钼水合水合物(Moo42-)的形式存在于钼水溶性环境中的钼,如钙 - 硅酸钙 - 水合物(CSH),单硫酸盐(AFM),Ettringite(AFT),也是如此作为由普通波特兰水泥(OPC)制成的硬化水泥浆料,在缺氧条件下进行了分批式吸附实验。摄取动力学通常很快,导致吸附均衡在不到30天内。特别地,观察到通过AFM阶段的强烈吸收钼酸盐,以及C-S-H相对于水泥系统中的钼酸盐潴留的不同贡献,后者根据C-S-H的Ca / Si比和溶液中的碱含量。在含有HydMGARNET的系统中,鉴定了钼酸盐的AFM相的新形成作为有助于钼酸盐保留的额外过程。该研究结果对选择含有MO-93的放射性废料流的固定的灌浆具有意义,并且还增强了钼酸盐吸附的数据,并在水泥系统中保持保留。

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