ISSN 1000-3665 CN 11-2202/P
    罗伟奇,刘拥军,李同生,等. 湖南省界牌岭矿区矿坑充水途径研究[J]. 水文地质工程地质,2024,51(0): 1-13. DOI: 10.16030/j.cnki.issn.1000-3665.202401054
    引用本文: 罗伟奇,刘拥军,李同生,等. 湖南省界牌岭矿区矿坑充水途径研究[J]. 水文地质工程地质,2024,51(0): 1-13. DOI: 10.16030/j.cnki.issn.1000-3665.202401054
    LUO Weiqi, LIU Yongjun, LI Tongsheng, et al. Study of the hydrogeological boundary conditions in Jiepailing mining area, Hunan Province[J]. Hydrogeology & Engineering Geology, 2024, 51(0): 1-13. DOI: 10.16030/j.cnki.issn.1000-3665.202401054
    Citation: LUO Weiqi, LIU Yongjun, LI Tongsheng, et al. Study of the hydrogeological boundary conditions in Jiepailing mining area, Hunan Province[J]. Hydrogeology & Engineering Geology, 2024, 51(0): 1-13. DOI: 10.16030/j.cnki.issn.1000-3665.202401054

    湖南省界牌岭矿区矿坑充水途径研究

    Study of the hydrogeological boundary conditions in Jiepailing mining area, Hunan Province

    • 摘要: 湖南省界牌岭矿区在深部多金属矿探采结合施工时,出现了矿坑涌水量大和西南部塔下村余家发生了大量岩溶地面塌陷等问题。尽管以往开展过矿区水文地质勘查工作,但对水文地质条件尤其是威胁矿山安全生产及对周边地质环境造成破坏的矿坑潜在充水水源和充水通道不够清楚。文章采用系统整理分析矿区前期各阶段水文地质资料、地面调查、物探、钻探、抽水试验等常规方法对界牌岭矿区水文地质条件进行了研究,并重点分析了矿坑充水的充水途径。结果显示:(1)研究区西南部新发现北东向断层F303。(2)矿坑主要充水途径有2条:①矿区西部F201至F32段隔水层测水组缺失,壶天群、梓门桥组与石蹬子组直接接触,同时受F201、F303、F32的影响,构成矿坑最为主要的充水途径;②矿区西北部沿花岗斑岩岩体与围岩接触带富水性较好,围岩接触带构成矿坑充水途径;主要充水水源为西部壶天群地下水和田尾溪水。建议在F1的西侧梓门桥组壶天群范围内利用下部隔水层测水组对梓门桥组壶天群内的充水途径进行帷幕注浆,阻隔矿区与河水、壶天群地下水水力联系。研究结果可为矿山下一步防治水工作的实施提供参考依据。

       

      Abstract: In the Jiepailing mining area, during the combined exploration and mining of deep polymetallic ores, issues such as large water inflow in the pits and extensive karst ground collapses in the Yujia area occurred. Despite previous hydrogeological surveys and research in the mining area, the hydrogeological conditions, especially the potential water sources and pathways that threaten mine safety and damage the surrounding geological environment, are not sufficiently clear. This paper takes the Jiepailing mining area as the research object to investigate its hydrogeological conditions, employing conventional methods such as systematically organizing and analyzing previous hydrogeological data from various stages, as well as surface investigation, geophysical exploration, drilling, and pumping tests. The study focuses on analyzing the pathways of water filling in the mine pits. The results show: (1) A newly discovered northeastern fault, F303, is located in the southwestern part of the study area. (2) The main pathways for water filling in the mine pits include: ① In the western part of the mining area, the absence of the aquiferous group between F201 and F32 leads to direct contact between the Hutian Group, Zimenqiao Formation, and Shidengzi Formation. Influenced by F201, F303, and F32, this constitutes the most significant pathway for water filling in the mine pits; ② In the northwestern part of the mining area, the contact zone between the granodiorite porphyry body and the surrounding rock has good water-richness, forming a pathway for water filling in the mine pits. The primary sources of water are the groundwater of the western Hutian Group and Tianweixi water.The suggestion proposes execute curtain grouting on the west side of F1, using the lower impermeable layer water measurement group to block water pathways within the Hutian Group of the Zimenqiao Formation, thereby interrupting the hydraulic connection between the mining area and the river water, as well as groundwater within the Hutian Group. The results of the study can provide reference for the implementation of water prevention and control work in the next step of the mine.

       

    /

    返回文章
    返回