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Recovery of Magnesium and Recycling of Spent Solution in Chloride-Based Atmospheric Acid Leaching of Nickel Laterite

机译:镍基红土中基于氯的大气酸浸过程中镁的回收和废溶液的回收

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In this work, the equilibrium relationship of MgCl_2-MgSO_4-HCl-H_2SO_4-H_2O system at 75°C was studied. This system is ofinterest because of its relevance to the process designed forrecovery of magnesium and recycling of spent solution inchloride-based atmospheric acid leaching of nickel laterite.Experimental results showed that the concentration of Mg~(2+) iondecreases with the increase of H~+ ion concentration whenmSO_4~(2-)/(0.5m_(Cl~-)+mSO_4~(2-))is the same. With the same H~+concentration, the concentration of Mg~(2+) ion decreases sharply atfirst and then increases slightly when mSO_4~(2-)/(0.5m_(Cl~-)+mSO_4~(2-)changes from 0.1 to 1. And in all experiments, MgSO_4·H_2O wasthe only crystallization phase.
机译:在这项工作中,MgCl_2-MgSO_4-的平衡关系 研究了75°C下的HCl-H_2SO_4-H_2O体系。这个系统是 兴趣,因为它与为 回收镁并回收废旧溶液 氯化物的大气酸浸出红土镍矿。 实验结果表明,Mg〜(2+)离子的浓度 随H〜+离子浓度的增加而降低 mSO_4〜(2-)/(0.5m_(Cl〜-)+ mSO_4〜(2-)) 是一样的用相同的H〜+ 浓度时,Mg〜(2+)离子的浓度在 mSO_4〜(2-)/(0.5m_(Cl〜-)+ mSO_4〜(2-) 从0.1变为1。在所有实验中,MgSO_4·H_2O为 唯一的结晶阶段。

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