中国煤矿区烧变岩地质特征研究进展及趋势

Research progress and trend of geological characteristics of burnt rock in coal mining areas in China

  • 摘要:
    目的 开展烧变岩地质特征系统研究对煤矿区灾害防治及资源充分利用具有重要意义。
    方法 从形成机制、分类特征、矿物学及地球化学特征、物理力学性质、工程地质水文地质特征、地质与环境意义等方面,系统阐述了烧变岩的研究现状,指出了现有研究的不足。
    结果 结果表明,烧变岩性质与煤自燃程度及埋深、含水量等地质环境密切相关,目前逐步形成了岩石学、地球化学、水文地质学和矿物学等多学科融合的综合分类体系,整体上以烧熔岩、烧结岩和烘烤岩为主;有机质、碳酸盐矿物、黏土矿物等原生矿物分解及方石英、磁铁矿、莫来石、玻璃质等高温矿物生成可作为烧变过程和垂向分带的重要依据;烧变岩力学性质和结构在超过温度阈值后快速劣化,引起烧变岩体稳定性下降和富水性激增等工程效应,存在诱发烧变岩体变形过大、突水溃砂和涌水量异常等地质灾害,需根据综合探查、以防为主、分区防治的原则进行治理;现有研究存在烧变岩形成机制不清、环境效应评价不精、资源化利用低、多学科交叉研究不足和工程应用研究弱等主要问题,需深入开展系统研究。
    结论 研究结果可加深对我国煤矿区烧变岩的认识,为其进一步研究和综合利用提供理论依据。

     

    Abstract: Conducting systematic research on the geological characteristics of burnt rock is of great significance for disaster prevention and the full utilization of resources in coal mining areas. This paper comprehensively reviews the current research status of burnt rock from various aspects, including formation mechanisms, classification characteristics, mineralogical and geochemical features, physical and mechanical properties, engineering geological and hydrogeological characteristics, as well as geological and environmental implications. It also highlights the limitations of existing studies. The results indicate that the properties of burnt rock are closely related to the degree of coal spontaneous combustion, burial depth, water content, and other geological conditions. A multidisciplinary integrated classification system, combining petrology, geochemistry, hydrogeology, and mineralogy, has gradually been established, primarily categorizing burnt rock into melted rock, sintered rock, and baked rock. The decomposition of primary minerals such as organic matter, carbonate minerals, and clay minerals, along with the formation of high-temperature minerals like cristobalite, magnetite, mullite, and vitreous materials, can serve as critical indicators for identifying the burning process and vertical zonation. The mechanical properties and structure of burnt rock rapidly deteriorate once temperature thresholds are exceeded, leading to reduced stability of burnt rock masses and a sharp increase in water abundance. These changes can trigger geological disasters such as excessive deformation of burnt rock masses, sudden water inrush and sand outbursts, and abnormal water inflow. Management strategies should follow the principles of comprehensive exploration, prevention-first, and zonal control. Current research faces several major challenges, including unclear formation mechanisms of burnt rock, imprecise evaluation of environmental effects, low resource utilization, insufficient interdisciplinary studies, and weak engineering application research.

     

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