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Porcwater in Compacted Water-Saturated MX-80 Bentonite

机译:压实水饱和MX-80膨润土中的猪水

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Bentonite is planned to be used in many countries as a buffer material in repositories for spent nuclear fuel. The proper understanding and modelling of the functioning of the water-saturated bentonite requires knowledge about the bentonite microstructure and also the way water is distributed between different phases. This paper presents experimental results from our studies of water in compacted, water-saturated MX-80 bentonite at dry densities in the range 0.7-1.6 g/cm~3. Three techniques, Cl-porosity, SAXS and proton NMR measurements, were applied to samples kept at room temperature, while TEM imaging was applied to high pressure frozen samples. The combined results of these techniques strongly indicate that the two major water phases in the compacted MX-80 bentonite samples are 'interlayer' and 'non-interlayer' water. The results of the relative amounts of different water types by SAXS and NMR are very similar. The results by Cl-porosity measurement indicate that only part of the non-interlayer water is available for anions. Those observations are discussed in comparison to TEM micrographs. Our study provides solid experimental evidence for the presence of two major water phases in water-saturated bentonite and estimates their relative proportions and pore sizes.
机译:膨润土计划在许多国家用作乏核燃料储存库中的缓冲材料。对水饱和膨润土功能的正确理解和建模需要有关膨润土微观结构以及水在不同相之间分配方式的知识。本文介绍了我们在致密,水饱和的MX-80膨润土中以0.7-1.6 g / cm〜3的干密度对水进行研究的实验结果。将三种技术(Cl孔隙率,SAXS和质子NMR测量)应用于保持在室温下的样品,而TEM成像应用于高压冷冻样品。这些技术的综合结果强烈表明,压实的MX-80膨润土样品中的两个主要水相是“夹层”和“非夹层”水。通过SAXS和NMR对不同水类型的相对量的结果非常相似。 Cl-孔隙率测量的结果表明,只有一部分非夹层水可用于阴离子。与TEM显微照片相比,对这些观察结果进行了讨论。我们的研究为水饱和膨润土中存在两个主要水相提供了可靠的实验证据,并估计了它们的相对比例和孔径。

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