首页> 外文期刊>Russian Journal of Inorganic Chemistry >Solid-Liquid Metastable Phase Equilibria in the Ternary System (MgCl2 + MgSO4 + H2O) at 323.15 K
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Solid-Liquid Metastable Phase Equilibria in the Ternary System (MgCl2 + MgSO4 + H2O) at 323.15 K

机译:在323.15 k的三元体系(MgCl2 + MgSO4 + H2O)中的固 - 液相稳定相平衡

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摘要

The solubilities and the densities in the aqueous ternary system (MgCl2 + MgSO4 + H2O) at 323.15 K were determined by the isothermal evaporation method. The phase diagram was drawn for this system at 323.15 K. The phase diagram consists of two invariant points, three univariant curves, and three crystallization regions corresponding to bischofite (MgCl2 bold /bold6H(2)O), tetrahydrate (MgSO4 bold /bold4H(2)O) and hexahydrite (MgSO4 bold /bold6H(2)O). Neither double salts nor solid solution was found. Based on the Pitzer and Harvie-Weare (HW) model, the solubility equilibrium constants for the salts were fitted with the solubilities in this research work, and the solubilities of the ternary system at 323.15 K were calculated. Comparisons between the calculated and measured solubilities show that the predicted data agree well with the experimental results.
机译:通过等温蒸发法测定323.15k水溶液(MgCl 2 + MgSO4 + H 2 O)中的溶解度和密度。 在323.15k中为该系统绘制了相图。相图由两个不变焦点,三个单变曲线和三个与双螺杆物(MgCl2粗&& /粗体& 6h(2)o)组成。 四水合物(MgSO4&粗体&& /粗体& 4h(2)o)和六水石(mgso4粗体;& / bold& 6h(2)o)。 没有发现双重盐也不是固溶。 基于皮带和HARVIE-WEATE(HW)模型,盐的溶解度平衡常数在该研究工作中配备了溶解度,并且计算了三元体系的溶解度在323.15 k。 计算和测量溶解度之间的比较表明,预测数据与实验结果很好。

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