Université de Lyon, INSA-Lyon, DEEP (Déchets Eaux Environnement et Pollutions - Wastes Water Environment Pollutions), 20 Avenue Albert Einstein, F-69621, Villeurbanne, France.
Université de Lyon, INSA-Lyon, DEEP (Déchets Eaux Environnement et Pollutions - Wastes Water Environment Pollutions), 20 Avenue Albert Einstein, F-69621, Villeurbanne, France.
J Environ Manage. 2017 May 15;193:567-575. doi: 10.1016/j.jenvman.2017.02.055. Epub 2017 Feb 24.
Phosphogypsum (PPG) is the byproduct of the production of phosphoric acid and phosphate fertilizers from phosphate rocks (PR) by acid digestion. Despite the technical feasibility, the impurities present in this waste make its reuse critical and large amounts of PPG are stockpiled, resulting in the production of polluted acid leachates. The aim of the present study was to characterize the spatial variability and evolution in time of a 20-year-old gypstack and to study the geochemical behavior of the waste in order to assess the best management options. Chemical and mineralogical analyses were performed on core samples taken from 4 different depths of the stack down to 13.5 m. Despite the high homogeneity shown by chemical and mineral characterization, leaching tests revealed a different chemical behavior with depth. pH-dependent leaching tests were also performed to measure the acid neutralization capacity of the studied matrices and to determine the leachability of the elements or pollutants of concern as a function of pH. The study was focused on Ca, Fe Na, Si, Cd and Sr and on F, PO and SO anions. The geochemical modeling of these tests with PHREEQC enabled the identification of the minor phases controlling the solubilization of the elements analyzed. Validation of the model by the simulation of a column leaching test suggested that the model could be used as a predictive tool to assess different management scenarios.
磷石膏(PG)是通过酸浸从磷矿石(PR)中生产磷酸和磷肥的过程中产生的副产品。尽管技术上可行,但这种废物中存在的杂质使其再利用变得至关重要,大量的 PG 被储存起来,导致产生了受污染的酸性浸出液。本研究的目的是描述一个 20 年历史的石膏堆的空间变异性和时间演变,并研究废物的地球化学行为,以评估最佳管理方案。对取自堆体 4 个不同深度直至 13.5 m 的芯样进行了化学和矿物学分析。尽管化学和矿物特性分析表明具有高度的均一性,但浸出试验表明,随着深度的增加,化学行为有所不同。还进行了 pH 依赖性浸出试验,以测量研究基质的酸中和能力,并确定作为 pH 函数的关注元素或污染物的浸出率。该研究集中在 Ca、Fe、Na、Si、Cd 和 Sr 以及 F、PO 和 SO 阴离子上。这些测试的地球化学模型通过 PHREEQC 进行模拟,能够识别出控制所分析元素溶解的次要相。通过柱浸出试验的模拟对模型进行验证表明,该模型可用于作为评估不同管理情景的预测工具。