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RATE OF DECOMPOSITION OF PHOSPHORITE IN SULPHURIC ACID-SODIUM SULPHATE SOLUTIONS

机译:硫酸-硫酸钠溶液中亚磷酸酯的分解速率

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This article presents a series of studies on the rate of decomposition of phosphorite in H_2SO_4 - Na_2SO_4 solutions of various concentrations at temperatures of 40 to 80 deg C in order to elucidate the mechanism of phosphorus dissolution from this mineral. The dissolution rate was directly influenced by the reagent concentration and temperature but was inversely proportional to the average initial particle size of the phosphorite grains. The reaction rate was significantly improved by the addition of sodium sulphate and by stirring. The experimental data fitted well into an expression based on a kinetic model for diffusion-controlled reactions. The enhanced kinetics in H_2SO_4 - Na_2SO_4 solutions could be attributed to the relatively lower activation energy obtained, compared to that in H_2SO_4 alone. In both cases, the activation energy was less than 20 kJ.mol~(-1), suggesting a transport process to be the rate controlling step.
机译:本文提出了一系列研究,说明了在40至80摄氏度的温度下,不同浓度的H_2SO_4-Na_2SO_4溶液中亚磷酸盐的分解速率,以阐明磷从这种矿物中溶解的机理。溶解速度直接受试剂浓度和温度影响,但与磷矿颗粒的平均初始粒径成反比。通过加入硫酸钠和搅拌,反应速率得到显着提高。实验数据很好地拟合了基于扩散控制反应动力学模型的表达式。与单独的H_2SO_4相比,H_2SO_4-Na_2SO_4溶液中增强的动力学可以归因于所获得的相对较低的活化能。在这两种情况下,活化能均小于20 kJ.mol〜(-1),表明传输过程是速率控制的步骤。

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