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Measurement of the steady and non-steady-state chloride diffusion coefficients in a migration test by means of monitoring the conductivity in the anolyte chamber. Comparison with natural diffusion tests

机译:通过监测阳极电解液室中的电导率,在迁移测试中测量稳态和非稳态氯化物扩散系数。与自然扩散测试的比较

摘要

The precise calculation of steady-state chloride diffusion coefficients is laborious, expensive, and time consuming due to the fact that it is necessary to take liquid samples for the chlorides to be analysed. In this paper, the concentration of chlorides is monitored by measuring the conductivity of the anolyte which initially is distilled water. Additionally, the calculation of Ds and Dns is made from the same test using the concept of “time-lag” and of the “equivalent time” between diffusion and migration experiments. The correlation between Ds and the conductivity has been done by testing 10 different cementitious matrixes (concrete and mortar) with different binders, and considering the influence of the type of solution that is the source of chloride ions as well as the variation of the electrodes and the effect of the kind of matrix. The results obtained have been compared with natural diffusion results in order to validate them. As a result, for the possibility of making it automatic, the calculation of Ds and Dns diffusion coefficients has been verified.
机译:稳态氯化物扩散系数的精确计算是费力,昂贵和耗时的,这是因为必须为分析的氯化物采集液体样品这一事实。在本文中,通过测量最初是蒸馏水的阳极电解液的电导率来监控氯化物的浓度。另外,Ds和Dns的计算是使用扩散和迁移实验之间的“时滞”和“等效时间”的概念,通过同一测试进行的。 Ds和电导率之间的相关性是通过测试10种具有不同粘合剂的不同水泥基(混凝土和砂浆),并考虑作为氯离子来源的溶液类型的影响以及电极和电极的变化而完成的。矩阵的效果。为了验证它们,已将获得的结果与自然扩散结果进行了比较。结果,为了使其具有自动化的可能性,已经验证了Ds和Dns扩散系数的计算。

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