イルメナイト固溶体(Fe2+, Mn2+, Mg)TiO3と(Fe2+, Mn2+, Mg)Cl2水溶液間におけるイオン交換平衡実験

知裕 久保, 悦生 内田, 容子 古川, 直哉 今井
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引用次数: 3

Abstract

Ion exchange experiments between ilmenite solid solution (Fe2+, Mn2+, Mg)TiO3 and 1 molal aqueous (Fe2+, Mn2+, Mg)Cl2 solution were carried out using standard cold-seal type pressure vessels at 600°C and 1000kg/cm2. The ion exchange reactions can be expressed as follows;FeTiO3+MnCl2aq=MnTiO3+FeCl2aqMnTiO3+MgCl2aq=MgTiO3+MnCl2aqand MgTiO3+FeCl2aq=FeTiO3+MgCl2aq. Under the experimental conditions, FeTiO3, MnTiO3 and MgTiO3 make a perfectly continuous solid solution. Based on thermodynamic analysis using ternary solid solution model of Kakuda et al. (1991), interaction parameters (Wi) for the ternary ilmenite solid solution have been obtained to be WFeFeMn=-0.02, WFeMnMn=-0.19, WMnMnMg=2.99, WMnMgMg=3.34, WMgMgFe=1.23, WMgFeFe=1.03 and WFeMnMg=1.83kcal/mol. FeTiO3-MnTiO3 solid solution is regarded as ideal solution, and MnTiO3-MgTiO3 and MgTiO3-FeTiO3 solid solutions show positive deviations from ideal solution. Ferrous ion is preferably partitioned into ilmenite solid solution. On the other hand, manganese ion tends to concentrate into aqueous chloride solution.
非金属固溶体(Fe2+, Mn2+, Mg)TiO3和(Fe2+, Mn2+, Mg)Cl2水溶液间的离子交换平衡实验
采用标准冷密封型压力容器,在600℃、1000kg/cm2条件下,对钛铁矿固溶体(Fe2+, Mn2+, Mg)TiO3与1mol / l水溶液(Fe2+, Mn2+, Mg)Cl2进行离子交换实验。离子交换反应可以表示为:FeTiO3+MnCl2aq=MnTiO3+FeCl2aqMnTiO3+MgCl2aq=MgTiO3+MnCl2aq和MgTiO3+FeCl2aq=FeTiO3+MgCl2aq。在实验条件下,FeTiO3、MnTiO3和MgTiO3形成了完美连续的固溶体。利用Kakuda et al.(1991)的三元固溶体模型进行热力学分析,得到三元钛铁矿固溶体的相互作用参数(Wi)为WFeFeMn=-0.02, WFeMnMn=-0.19, WMnMnMg=2.99, WMnMgMg=3.34, WMgMgFe=1.23, WMgFeFe=1.03和WFeMnMg=1.83kcal/mol。将FeTiO3-MnTiO3固溶体视为理想溶液,MnTiO3-MgTiO3和MgTiO3-FeTiO3固溶体与理想溶液存在正偏差。亚铁离子优选分区成钛铁矿固溶体。另一方面,锰离子倾向于浓缩到氯水溶液中。
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