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Infiltration tests on a granite/bentonite mixture: Influence of water salinity

机译:花岗岩/膨润土混合物的渗透测试:水盐度的影响

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A series of infiltration tests on a 70%/30% granite/bentonite mixture compacted at a dry density of 1.70 g/cm~3 are reported and analysed. This mixture is proposed as backfill material in the Swedish concept for radioactive waste disposal. The tests have been carried out at laboratory temperature for different periods of time, between 10 and 100 days, and with two kinds of infiltration water, to check the influence of the salinity on the hydration behaviour. The water intake has been measured during the tests, and the distributions of water content, dry density and soluble salts of the material have been determined at the end of the tests. It has become patent the difficulty in accurately measuring these parameters in such heterogeneous materials. The influence of the permeant salinity on the intrinsic permeability of the material has been highlighted, as well as the swelling capacity of this mixture. The ionic species distribution depends on the kind of infiltration water and the duration of the test. Dissolution, advection and diffusion are the mechanisms identified.
机译:报道并分析了以70%/ 30%花岗岩/膨润土混合物压实的干密度为1.70 g / cm〜3的一系列渗透测试。在瑞典的概念中,建议将该混合物用作回填材料,以处理放射性废物。该测试已在实验室温度下进行了10到100天的不同时间段测试,并使用两种渗透水进行了测试,以检查盐度对水化行为的影响。在测试过程中已测量了进水量,并在测试结束时确定了水含量,干密度和可溶性盐分的分布。在这样的异质材料中准确测量这些参数的困难已成为专利。渗透盐分对材料固有渗透率的影响以及该混合物的溶胀能力已得到强调。离子种类的分布取决于渗透水的种类和测试的持续时间。溶解,对流和扩散是确定的机制。

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