废弃矿井水质演化生物地球化学机制及有价元素资源化利用综述

Biogeochemical mechanisms of water quality evolution and the resource utilization of valuable elements in abandoned mine pits: A review

  • 摘要:
    背景 废弃矿井水不仅是矿区主要污染源,也是战略性关键金属与地下空间利用的重要载体。我国矿山影响水污染呈现南方重于北方的空间格局,这是由气候条件、地质背景与采矿历史共同决定的。
    进展 基于环境地球化学前沿视角,系统评述酸性矿山废水(AMD)的形成演化机制及污染阻控−资源回收−能源协同利用技术。废弃矿井闭坑后水质呈现明显的阶段性特征:初期由无机水岩反应主导的重金属浓度高峰,中期微生物驱动的自净化过程,至长期融入区域地下水系统后的动态平衡状态。通过剖析黄铁矿氧化的动力学过程,指出嗜中性微生物在酸化初期的启动作用是控制酸性矿山废水释放速率的关键环节。通过阐明污染物在岩溶−水复杂介质中的源汇演变规律,揭示了碳酸盐岩缓冲作用诱导次生矿物沉淀−老化过程对重金属吸附−解吸的非线性控制机制。
    展望 基于上述阶段性演化特征的认知,有价资源回收技术的路径选择需与水质阶段深度耦合:闭坑初期宜采用电化学活化石灰石系统实现靶向金属回收,闭坑中期可通过硫酸浸出工艺转化富集态沉淀渣中的有价元素,至闭坑长期则需针对不同水质特征构建分类处理与调蓄利用体系。研究成果可为构建废弃矿井水污染治理与有价元素资源化利用新范式提供科学依据与技术路径。

     

    Abstract:
    Background Abandoned mine water is not only a major pollution source in mining areas, but also an important carrier for the recovery of strategic critical metals and the utilization of underground space. In China, water pollution caused by mining activities shows a spatial pattern of being more severe in the south than in the north.
    Advances  This differentiation is jointly shaped by climatic conditions, geological settings and mining history. From the frontier perspective of environmental geochemistry, this paper systematically reviews the formation and evolution mechanisms of acid mine drainage (AMD), as well as the integrated technologies for pollution control, resource recovery and energy utilization. Regarding temporal evolution, water quality in abandoned mines undergoes distinct stages after mine closure: an initial peak of heavy metal concentrations dominated by inorganic water-rock reactions, a microbially driven self-purification process in the medium term, and a dynamic equilibrium state after long-term integration into the regional groundwater system. At the microscopic mechanism level, by analyzing the kinetic process of pyrite oxidation, it is pointed out that the initiation of neutrophilic microbes in the early stage of acidification is a key factor controlling the release rate of acid mine drainage. At the interface process level, by clarifying the source-sink evolution of pollutants in complex karst-water media, the nonlinear control mechanism of heavy metal adsorption-desorption by secondary mineral precipitation and aging induced by the buffering effect of carbonate rocks is revealed.
    Prospects  Based on the above understanding of staged evolution, the selection of technologies for valuable resource recovery should be deeply coupled with water quality stages. In the early closure stage, an electrochemically activated limestone system is suitable for targeted metal recovery; in the middle closure stage, valuable elements in enriched precipitated slags can be extracted via sulfuric acid leaching; in the long-term closure stage, a classified treatment, storage and utilization system should be established according to different water quality characteristics. This paper aims to provide a scientific basis and technical pathway for establishing a new paradigm of water pollution control and valuable element resource utilization in abandoned mines.

     

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