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Influence of concentration change of calcium ions over time on their diffusion through sandstone

机译:钙离子浓度变化随时间对砂岩扩散的影响

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Diffusion is one of the most important salt transport mechanisms.The knowledge of the rate of transport of ions in the pore system of building materials is thus of primary importance for their service life prediction.In this paper, the transport of Ca~(2+)` in sandstone Msene was studied as a model system;two types of experiment were performed: a)without addition of Ca~(2+)ions for the achievement of original initial concentration and b)continuous addition of Ca~(2+)ions.The experiment was performed under laboratory conditions in a two-side plexiglass box at the ambient temperature of(20±2)°C for a period of 426 hours.Calcium concentrations were analyzed chelatometrically.
机译:扩散是最重要的盐运输机制之一。因此,建筑材料孔系统中离子运输速率的了解是对其使用寿命预测的主要重要性。本文的运输,CA〜(2+ )在砂岩MSENE中被研究为模型系统;进行两种类型的实验:a)在不添加Ca〜(2+)离子,用于实现原始初始浓度的成就,b)连续添加Ca〜(2+)离子在实验室条件下在两侧有润滑袋的实验室条件下在(20±2)℃的两侧有润滑袋的情况下进行426小时的时间。逐逐酸钙分析。

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