摘要
通过杯浸试验确定浸矿的离子交换模型为Kerr模型,得到Kerr模型的选择系数为12.59×10~(-10)L~2/g~2;采用对流-弥散方程描述柱浸过程铵根离子和稀土离子的运移规律,通过Kerr模型确定对流-弥散方程中的源汇项,运用顺序非迭代法解具有强非线性的对流-弥散方程,模拟稀土离子在土柱中的运移过程。与室内一维柱浸试验稀土离子的穿透曲线进行比较,两者的相关系数达到0.8724,说明本方法可以较为准确地模拟风化壳淋积型稀土矿一维柱浸过程。分析硫酸铵溶液浓度对稀土浸取率的影响,结果发现,最优硫酸铵溶液浓度(C_(op)~(NS))与稀土品位(η)满足线性关系。
The ion exchange model of the leaching process was determined via batch leaching experiments using the Kerr model, with the selectivity coefficient experimentally determined to be 12.59×10~(-10) L~2/g~2. Solute transport laws of ammonium ions(NH_4~+) and rare earth ions(RE~(3+)) in column leaching were described by the convection-dispersion equation(CDE). The source and sink in the CDE were determined by the Kerr model. The CDE with strong nonlinearity was solved using the sequential non-iterative method. Compared with the breakthrough curve of RE~(3+), the correlation coefficient between the simulated and experimental curves reached 0.8724. Therefore, this method can simulate the one-dimensional column leaching of weathered crust elution-deposited rare earth ore. Moreover, the effects of different concentrations of ammonium sulfate((NH_4)_2SO_4) solution on the leaching rate of rare earth were analyzed. The optimal concentration of the(NH_4)_2SO_4 solution had a linear relationship with the rare earth grade.
引文
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