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Leaching kinetics and stoichiometry of pyrite oxidation from a pyrite-marcasite concentrate in acid ferric sulfate media

机译:酸性硫酸铁介质中黄铁矿-镁铁矿精矿中黄铁矿氧化的浸出动力学和化学计量

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A pyrite concentrate with minor marcasite was oxidized in an acidic ferric sulfate medium at temperatures from 45 to 75 deg C and at constant potentials corresponding to Fe(III) to Fe(II) ratios from 10 to 300. Potassium permanganate (KmnO_4) was found to be both a suitable oxidant for controlling the solution potential and a convenient and reliable indicator of leaching progress. The stoichiometry of pyrite oxidation was found to be essentially independent of temperature and only slightly dependent on solution potential over the range of conditions studied. Each unit of sulfide sulfur oxidized yielded 64 + - 2 percent sulfate, the rest elemental sulfur as discrete particles approximately 2 um in diameter. The pyrite oxidation rate was very sensitive to the temperature, giving a large activation energy (83 kJ/mol), and was proportional to the Fe(III)/Fe(II) concentration ratio to the power of 0.57. The shrinking sphere model fitted very well the changing grain topology. A single mathematical expression combines the thermal, chemical, and topological functions to predict the pyrite conversion as a function of the known temperature, ferric concentration, ferrous concentration, particle size, and time. The model predictions are excellent over the range of conditions tested.
机译:在酸性硫酸铁介质中,于45至75℃的温度下,以恒定电势(对应于Fe(III)与Fe(II)的比率为10至300),氧化了具有少量马来酸钾的黄铁矿精矿。发现了高锰酸钾(KmnO_4)既是控制溶液电位的合适氧化剂,又是浸出进度的方便可靠的指标。发现黄铁矿氧化的化学计量基本上与温度无关,并且在研究的条件范围内仅略微取决于溶液电势。硫化硫被氧化的每个单元均产生64%-2%的硫酸盐,其余的元素硫为离散颗粒,直径约为2 um。黄铁矿的氧化速率对温度非常敏感,具有很大的活化能(83 kJ / mol),并且与Fe(III)/ Fe(II)浓度比成正比,为0.57的幂。收缩球模型非常适合不断变化的晶粒拓扑。单个数学表达式结合了热,化学和拓扑函数,可根据已知温度,铁浓度,铁浓度,粒径和时间预测黄铁矿转化率。在测试条件范围内,模型预测非常出色。

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