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含稀土磷礦酸解動力學及稀土浸出機理

Acidolysis kinetics and RE leaching mechanisms of RE-bearing phosphorite ores

  • 摘要: 對織金新華含稀土磷礦酸解過程動力學及稀土浸出機理進行了研究.結果表明:∑REO轉化率動力學曲線與P2O5轉化率動力學曲線變化趨勢相近,即隨著溫度和溶液酸度的升高,稀土的轉化率提高;∑REO的酸解動力學可用德羅茲多夫方程來很好的描述,擬合曲線的相關系數在0.99以上.根據Arrhenius方程對磷礦酸解過程P2O5的反應表觀活化能計算表明,織金新華磷礦酸解的主要反應為固態膜擴散控制過程,而稀土在磷礦中的類質同象存在形態也決定了其反應屬于固態膜擴散控制過程.織金新華磷礦酸解過程稀土的浸出機理分析表明,稀土主要以RE2(SO4)3形式存在于溶液中,而磷石膏中的稀土以RE2(SO4)3和硫酸鈣晶體包裹的形式存在.

     

    Abstract: The kinetics behaviors and leaching mechanisms of rare earths by acidolysis were studied for Zhijin Xinhua phosphorite ores. It is shown that the ∑REO conversion ratio increases with increasing temperature and sulfuric acid concentration in the reacting solution, which is similar to the kinetics process of P2O5. The acidolysis kinetics of ∑REO reveals that the Drozdov equation can describe the dissolution progress of the ores quite well. The correlation coefficient fitting experimental data is more than 0. 99. The reaction apparent activation energy of P2O5 calculated by the Arrhenius equation indicates that the main reaction of Zhijin Xinhua phosphorire ores dissolved by sulfuric acid is a solid-film diffusion control process, as well as for ∑ REO because of its special presentation in the form of ions in the lattices of collophanite. In addition, studies on the leaching mechanisms of ∑REO dissolved by sulfuric acid show that RE2(SO4)3 is the main existence state in the solution, while RE2(SO4)3 and rare earths enwrapped by calcium sulphate crystals are the main existence state in phosphogypsum.

     

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