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Acidic dissolution of magnetite in mixtures of oxalic and sulfuric acid

机译:磁铁矿在草酸和硫酸混合物中的酸性溶解

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摘要

Thermodynamic and kinetic dissolution experiments were performed at different temperatures and different oxalic and sulfuric acid ratios by using synthetic magnetite powder. The Kabai model was the most appropriate one for describing the dissolution kinetics of magnetite in mixtures of sulfuric and oxalic acid. The reaction rate constant, k, at 35 degrees C was found to vary between 4.1.10(-5) and 5.6.10(-4) s(-1) for the different acid ratios. The solid specific constant of the Kabai model, a, was also found to vary in the different acid systems, suggesting that changes in the solid take place during dissolution in different media. Increasing the oxalic acid content in the solution phase yielded higher solubilities, as well as accelerated kinetics. Whereas kinetics was significantly improved when increasing the oxalic acid fraction from 50 to 70, solubility no longer increased markedly. (C) 2016 Published by Elsevier B.V.
机译:使用合成磁铁矿粉在不同温度,不同草酸和硫酸比下进行了热力学和动力学溶解实验。 Kabai模型是描述磁铁矿在硫酸和草酸混合物中的溶解动力学的最合适模型。对于不同的酸比率,发现在35摄氏度下的反应速率常数k在4.1.10(-5)和5.6.10(-4)s(-1)之间变化。还发现Kabai模型a的固体比常数在不同的酸体系中有所不同,这表明固体在溶解于不同介质期间会发生变化。溶液相中草酸含量的增加产生更高的溶解度,并加快动力学。当草酸分数从50增加到70时,动力学得到显着改善,而溶解度不再显着提高。 (C)2016由Elsevier B.V.发布

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