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首页> 外文期刊>Russian Journal of Inorganic Chemistry >Phase Equilibria in the Na,K,Mg,Ca||SO_4,Cl-H_2O System at 25 deg C in the Mirabilite and Thenardite Crystallization Regions
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Phase Equilibria in the Na,K,Mg,Ca||SO_4,Cl-H_2O System at 25 deg C in the Mirabilite and Thenardite Crystallization Regions

机译:25℃下钠镁钙石和芒硝结晶区域中Na,K,Mg,Ca || SO_4,Cl-H_2O体系中的相平衡

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摘要

Phase equilibria in the Na,K,Mg,Ca||SO_4,Cl-H_2O System at 25 deg C in the mirabilite Na_2SO_4 o 10H_2O and thenardite Na_2SO_4 crystallization regions are studied using the translation method. Mirabilite and thenardite, which are the equilibrium solids of the system at 25 deg C, are involved in the formation of one and two invariant points, four and seven monovariant curves, and six and nine divariant fields, respectively. Fragments of the phase equilibrium diagram of the title system are designed in the mirabilite and thenardite crystallization regions.
机译:利用平移法研究了在25℃下在芒硝Na_2SO_4 o 10H_2O和芒硝石Na_2SO_4结晶区中Na,K,Mg,Ca || SO_4,Cl-H_2O体系中的相平衡。闪长岩和芒硝是系统在25摄氏度时的平衡固体,分别参与形成一个和两个不变点,四个和七个单变曲线以及六个和九个二变场。标题系统的相平衡图的片段设计在芒硝和芒硝结晶区域中。

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