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The Generation and Treatment of Acid Rock Drainage

机译:酸性岩排水的产生与处理

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摘要

This review of the chemistry of acid rock drainage (ARD) concentrates on what the author thinks are important but not obvious geochemical principles in the generation and treatment of ARD. In ARD generation, the role Fe(Ⅲ) plays in the oxidation of sulfides, the generation of further acidity, and the release of minor constituents of concern (COCs) is explained. In ARD treatment, three geochemical principles are described. Of most importance, is the concept of mineral acidity and the prominent role iron and aluminum play in the treatment of ARD. Second in importance is the role oxidation and reduction play in the sequence of treatment steps and in the difficulty of removing minor constituents such as arsenic and selenium. Finally, how complex ion formation can frustrate the removal of some metals such as aluminum and zinc is explained. For the removal of trace COCs in ARD, the role of adsorption and co-precipitation onto the oxyhydroxide precipitates is important to the achievement of environmental guidelines.
机译:本文对酸性岩石排泄(ARD)的化学过程进行了综述,重点在于作者认为在ARD的产生和处理中重要但并不明显的地球化学原理。在ARD的产生中,解释了Fe(Ⅲ)在硫化物的氧化,进一步的酸度的产生以及所关注的次要成分(COCs)的释放中的作用。在ARD处理中,描述了三个地球化学原理。最重要的是矿物酸度的概念以及铁和铝在ARD的治疗中起的重要作用。其次,重要的是氧化和还原在处理步骤的顺序中以及在去除次要成分(例如砷和硒)的难度方面所起的作用。最后,解释了复杂的离子形成如何会阻碍某些金属(例如铝和锌)的去除。为了除去ARD中的痕量COC,在羟基氧化物沉淀物上的吸附和共沉淀作用对于实现环境准则至关重要。

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