Possibility of using a mixture of calcium salts to decrease sulphate concentration and total mineralisation of Surface and mine waters

Yuliia Trach, R. Trach
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引用次数: 0

Abstract

Natural limestone may be an option for removing sulphates from water. Such waters, which contain high concentrations of sulphate ions, are surface and mine waters. In this work, the removal of sulphate from model solutions (pH 6–8) by their sorption and chemical binding with calcium salts was studied. For experimental studies, natural limestone was taken, which was crushed to 1–10 μm. Such limestone was modified with acetic acid. A mixture of grinding limestone with the obtained calcium acetate was used for research. Experiments conducted in static conditions showed a decrease in sulphate concentration from 1.2 to 0.38 mg·dm–3 for a duration of 3 days and adding CaСО3:Са(СН3СОО)2 in a ratio of 1 : 1. The analysis of various scientific studies allowed us to assume that when such a mixture of calcium salts is used to reduce sulphate ions in natural surface waters, the formed acetate ion will undergo biological degradation. Thus, it is possible to achieve a reduction in the total mineralisation of surface waters.
使用钙盐混合物降低地表水和矿井水的硫酸盐浓度和总矿化的可能性
天然石灰石可能是去除水中硫酸盐的一种选择。这些水中含有高浓度的硫酸根离子,是地表水和矿井水。在这项工作中,研究了通过吸附和与钙盐化学结合从模型溶液(pH 6-8)中去除硫酸盐的方法。在实验研究中,采用了天然石灰石,将其压碎至1–10μm。用乙酸对这种石灰石进行改性。使用研磨石灰石和获得的乙酸钙的混合物进行研究。在静态条件下进行的实验表明,硫酸盐浓度在3天内从1.2降至0.38 mg·dm–3,并以1:1的比例添加CaСО3:Са(СН3СОО)2。对各种科学研究的分析使我们能够假设,当使用这种钙盐混合物来减少天然地表水中的硫酸根离子时,形成的乙酸根离子将发生生物降解。因此,可以减少地表水的总矿化。
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