寒旱矿区煤矸石土壤化利用与生态修复:关键过程、工程模式与区域适配性

    Soil-forming utilization of coal gangue and ecological restoration in cold and arid mining areas: key processes, engineering models, and regional adaptability

    • 摘要: 煤矸石是煤炭开采与洗选过程中产生量最大、累积量最高的固体废弃物之一,长期堆存易引发土地占压、风化崩解、渗滤污染、自燃发热和景观破坏等问题。寒旱矿区受降水偏少、蒸发强烈、表土稀缺、冻融扰动和生态恢复缓慢等多重约束,对煤矸石土壤化利用的区域适配性、过程稳定性和长期安全性提出了更高要求。本文系统综述寒旱矿区煤矸石土壤化利用与矿区生态修复研究进展,归纳水分保持与再分配、冻融风化、矿物转化、微生物定殖、植物建植和污染物稳定化等关键过程,并进一步指出:水分-孔隙结构是过程启动的一级控制因子,冻融风化与矿物转化决定类土壤基质形成,生物过程决定功能维持,而污染释放与稳定化构成安全边界。在此基础上,比较种植基质、人工土壤、原位成土、覆土-隔离-回填一体化、高寒参与式重构及多源固废协同等技术路径,结合国内外典型案例提炼其适用场景与量化边界。研究认为,寒旱矿区煤矸石土壤化利用的核心不是单一材料替代,而是围绕气候区、场地约束、材料属性和修复目标建立“分区适配-剖面配置-生物建植-风险监测”闭环。未来应重点验证水分阈值、冻融促成土-促释放双效应、生物定殖滞后补偿和分区参数可迁移性等科学假设,以形成可复制、可预警、可推广的矿区生态修复模式。

       

      Abstract: Coal gangue is one of the solid wastes with the largest generation and accumulation in coal mining and washing processes. Long-term stockpiling may induce land occupation, weathering and disintegration, leachate pollution, spontaneous combustion, and landscape degradation. In cold and arid mining areas, low precipitation, strong evaporation, scarce topsoil, freeze-thaw disturbance, and slow ecological recovery impose higher requirements on regional adaptability, process stability, and long-term safety. This review summarizes recent progress in the soil-forming utilization of coal gangue and ecological restoration in cold and arid mining areas, focusing on moisture retention and redistribution, freeze-thaw weathering, mineral transformation, microbial colonization, vegetation establishment, and pollutant stabilization. It further clarifies that the water-pore structure acts as the primary controlling factor for process initiation, freeze-thaw weathering and mineral transformation determine the formation of soil-like substrates, biological processes govern functional maintenance, and pollutant release and stabilization define the safety boundary. Major technical pathways, including planting substrates, artificial soils, in-situ pedogenesis, integrated covering-isolation-backfilling, participatory soil reconstruction in alpine areas, and synergistic use of multiple solid wastes, are compared with typical domestic and international cases. The review concludes that the core of coal gangue utilization in cold and arid mining areas is no single-material substitution but a closed-loop framework of zoning adaptation, profile configuration, biological establishment, and risk monitoring based on climate zones, site constraints, material properties, and restoration targets. Future studies should test verifiable hypotheses concerning water thresholds, dual effects of freeze-thaw on soil formation and pollutant release, delayed biological compensation, and cross-regional transferability of adaptation parameters, so as to develop replicable,early-warning-capable, and scalable ecological restoration models for mining areas.

       

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