-15℃下Na+， K+， Mg2+//Cl-， NO3-， SO42——H2O体系相平衡研究

新疆卤水硝酸盐矿主要含有Na⁺、K⁺、Mg²⁺、Cl^-、NO₃^-、SO₄^2-六种离子，属于高元复杂体系，其合理利用和开发需要不同温度下的相平衡研究作为理论支撑。采用等温溶解平衡法，对Na⁺， K⁺， Mg²⁺//Cl^-， NO₃^-， SO₄^2--H₂O体系在-15℃、NaCl·2H₂O饱和条件下的相平衡进行了研究，并构建了相图。相图中有六个零变量点和八个两盐结晶区，只存在一种复盐KCl·MgCl₂·6H₂O。八个两盐结晶区，分别对应于NaCl·2H₂O+Na₂SO₄·10H₂O、NaCl·2H₂O+NaNO₃、NaCl·2H₂O+KCl、NaCl·2H₂O+KNO₃、NaCl·2H₂O+MgSO₄·7H₂O、NaCl·2H₂O+MgCl₂·8H₂O、NaCl·2H₂O+Mg(NO₃)₂·6H₂O和NaCl·2H₂O+KCl·MgCl₂·6H₂O，其中NaCl·2H₂O+Na₂SO₄·10H₂O共晶区最大，在低温时，硫酸钠的溶解度最小，降温过程中较易结晶析出。与该体系在25℃下的相图相比，复盐种类减少5种，零变量点减少19个，相关系得以极大简化。

Study on phase equilibrium of system Na+, K+, Mg2+//Cl-, NO3-, SO42--H2O at-15℃

Xinjiang brine nitrate mine mainly contains six kinds of ions: Na⁺, K⁺, Mg²⁺, Cl^-, NO₃^-, and SO₄^2-, belonging to a high-element complex system, and its rational utilization and development require phase equilibrium studies at different temperatures as theoretical support. The phase equilibrium of the system Na⁺, K⁺, Mg²⁺//Cl^-, NO₃^-, SO₄^2--H₂O saturated with NaCl·2H₂O at -15℃ was investigated using the isothermal solution equilibrium method. According to the measured data, the phase diagrams were constructed. Only one double salt KCl·MgCl₂·6H₂O was found in the system. There are six invariant points and eight two-salt crystallization fields corresponding to NaCl·2H₂O+Na₂SO₄·10H₂O, NaCl·2H₂O+NaNO₃, NaCl·2H₂O+KCl, NaCl·2H₂O+KNO₃, NaCl·2H₂O+MgSO₄·7H₂O, NaCl·2H₂O+MgCl₂·8H₂O, NaCl·2H₂O + Mg(NO₃)₂·6H₂O and NaCl·2H₂O+KCl·MgCl₂·6H₂O. The crystallization area of NaCl·2H₂O+Na₂SO₄·10H₂O occupies the largest part because of its low solubility, and they will crystallize out easily from the mixed solution in the cooling process. Compared with the phase diagram of the system at 25℃, there are 5 types of double salts reduced, 19 zero variable points reduced, and the phase relationship is greatly simplified.