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Modelling a semi-batch reactive precipitation of ferrihydrite

机译:模拟水铁矿的半间歇反应沉淀

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The reactive precipitation of ferrihydrite was studied in a laboratory semi-batch precipitator, where a highly concentrated sodium hydroxide solution was fed into an iron nitrate solution. Instantaneous hydrolysis of iron[III] takes place when the two reagents are mixed generating supersaturation, and leading to immediate precipitation of ferrihydrite via a primary nucleation mechanism then followed by limited crystallite growth to 3 to 7nm. A mathematical model of the semi-batch laboratory precipitator was used to simulate the pH responses during the precipitation of ferrihydrite at different reagent feed rates. The model comprised of interconnected compartments of averaged hydrodynamic conditions, incorporating physically meaningful turbulent mixing time constants. The precipitation process is described by the solute concentration conservation equation incorporating a postulated ferrihydrite primary nucleation model. It was found that the semi-batch precipitator model predicted the experimental pH response reasonably well. The experimental results demonstrated that the reagent feed rate has a critical effect on the course of the precipitation of ferrihydrite, i.e. it is a rate determining step given the fast hydrolysis and precipitation kinetics.
机译:在实验室半间歇式沉淀器中研究了水铁矿的反应性沉淀,其中将高浓度的氢氧化钠溶液供入硝酸铁溶液中。当两种试剂混合产生过饱和时,铁[III]会发生瞬间水解,并通过主要的成核机制导致亚铁水立即沉淀,然后将晶体生长限制在3至7nm。半批实验室沉淀器的数学模型用于模拟在不同试剂进料速率下水铁矿沉淀过程中的pH响应。该模型由具有平均水动力条件的互连隔室组成,并结合了物理上有意义的湍流混合时间常数。沉淀过程由溶质浓度守恒方程式描述,该方程式结合了假定的三水铁矿一次成核模型。发现半间歇式沉淀器模型可以很好地预测实验的pH响应。实验结果表明,试剂进料速率对水铁矿沉淀过程具有关键影响,即,鉴于快速的水解和沉淀动力学,它是速率确定步骤。

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