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Leaching experiments on a Mn-rich slag from the recycling of alkaline batteries - Solid phase characterization and geochemical modeling

机译:碱性电池回收中富锰渣的浸出实验-固相表征和地球化学模型

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Square sections of a Mn-rich slag from an alkaline battery recycling plant were submitted to 6-month batch leaching procedures. High-Purity Water (HPW), acidic (pH 4) and alkaline (pH 12) conditions were used in order to observe the behavior of primary solid phases as well as the constituent elements (Mn, Mg, Al, Si, Ca). The experiments were coupled with both KINDIS(P) modeling and mineralogical study (SEM-EDS). Experimental results showed that the Mn-rich slag was sensitive to acidic conditions which induced the dissolution of primary phases. Moreover, pH 4 conditions did not result in the formation of newly formed solid products, leading to the greatest mobilization of metallic elements (especially Mn). Alkaline conditions favored the precipitation of secondary phases, especially rhodochrosite, calcite and Mg-saponite, inducing low mobilization of the contained elements. The KINDIS(P) modeling allowed the stability of primary phases and newly formed products to be predicted. Although the modeled results have to be considered with caution, they allow the assessment and understanding of future environmental behavior of the solid material in given conditions. In this case, the reuse of Mn-rich slag in acidic conditions has to be avoided because of the acidic dissolution of the primary phases.
机译:来自碱性电池回收厂的富锰渣的方形截面经过6个月的分批浸提程序。为了观察主要固相以及组成元素(Mn,Mg,Al,Si,Ca)的行为,使用了高纯水(HPW),酸性(pH 4)和碱性(pH 12)条件。实验与KINDIS(P)建模和矿物学研究(SEM-EDS)结合在一起。实验结果表明,富锰渣对酸性条件敏感,酸性条件引起初生相的溶解。而且,pH 4条件没有导致新形成的固体产物的形成,从而导致了金属元素(尤其是Mn)的最大迁移。碱性条件有利于第二相的沉淀,尤其是菱锰矿,方解石和镁皂石的沉淀,从而导致所含元素的低动员。 KINDIS(P)模型可以预测主要相和新形成产物的稳定性。尽管必须谨慎考虑建模结果,但它们可以评估和了解给定条件下固体材料的未来环境行为。在这种情况下,由于主要相的酸性溶解,必须避免在酸性条件下富锰渣的再利用。

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