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Examining the Binding Mechanism of Chloride Ions in Sea Sand Mortar

机译:检查海砂砂浆中氯离子的结合机制

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The adsorption and binding mechanisms of chloride ion in sea sand mortars were investigated through measuring the water-soluble chloride ion content in this paper. In addition, the microstructure of Friedel's salt were characterized by three approaches: X-ray diffraction (XRD), thermal analysis method (TG/DTA) and scanning electron microscopy (SEM). The results show that water soluble chloride ion concentration in the sea sand mortar is closely related to the extraction temperature. The water soluble chloride ion concentration increases with the extraction temperature increasing. When extraction temperature is 65°C, the concentration of water soluble chloride ion is about the double of mortars at 15°C. Physically bound chloride ion in fly ash mortar shows low dissolution in lower temperatures. In the sea sand mortar, the endothermic peak of Friedel's salt does not appear on the TG/DTA curve, while the existence of Friedel's salt was determined by SEM and XRD picture. This is probably owing to the small amount of instable Friedel's salt content in the sea sand mortar.
机译:本文测量水溶性氯离子含量研究了海砂砂浆中氯离子的吸附和结合机制。此外,通过三种方法表征了Friedel盐的微观结构:X射线衍射(XRD),热分析方法(TG / DTA)和扫描电子显微镜(SEM)。结果表明,海砂砂浆中的水溶性氯离子浓度与提取温度密切相关。水溶性氯离子浓度随着提取温度的增加而增加。当提取温度为65℃时,水溶性氯离子的浓度约为15℃的砂浆。粉煤灰砂浆中的物理上氯离子显示出低温溶解。在海砂砂浆中,Friedel的盐的吸热峰不会出现在Tg / DTA曲线上,而Friedel盐的存在是通过SEM和XRD图片确定的。这可能是由于海沙砂浆中少量的不稳定炸薯条含量。

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