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现代矿业 ›› 2025, Vol. 41 ›› Issue (12): 137-144,151.

• 岩土工程 • 上一篇    下一篇

铜陵市新桥矿岩溶塌陷特征及影响因素分析

陈 彬1 吴 岳2 王义霞2 赵 建3   

  1. 1. 铜陵化学工业集团有限公司;2. 铜陵化工集团新桥矿业有限公司; 3. 安徽省地质矿产勘查局321地质队
  • 出版日期:2025-12-25 发布日期:2026-01-23

Analysis of the Development Characteristics and Patterns of Karst Collapse in Xinqiao Mine, Tongling City

  1. 1. Tongling Chemical Industry Group Co.,Ltd.;2. TCIGCL Xinqiao Mining Co.,Ltd.; 3. 321 Geological Team,Anhui Bureau of Geology and Mineral Resources
  • Online:2025-12-25 Published:2026-01-23

摘要: 为分析新桥矿岩溶塌陷特征及影响因素,通过收集矿山基础地质、水工环地质、防治 水、历史岩溶塌陷数据、岩溶塌陷地质灾害勘查及地下水监测等资料,掌握了矿山地质环境背景条 件,总结了岩溶塌陷的特征,分析了岩溶塌陷影响因素。通过数理统计分析,明确了下伏岩溶发育 的基岩地层、上覆松散土层和地下水活动是岩溶塌陷的主要影响因素。研究表明,下伏栖霞组、孤 峰组上段岩溶发育的灰岩地层是岩溶塌陷发生的基本条件,断层破碎带、接触带等地质构造薄弱 地带控制岩溶塌陷的分布及塌陷程度,上覆松散地层影响岩溶塌陷进程及规模,并提供塌陷物源, 矿山疏排水为诱发岩溶塌陷的主要动力因素。矿区岩溶塌陷多呈圆形、椭圆形,直径和深度多小 于 5 m,90% 以上为矿山疏干排水诱发,且随地下水活动增强而加剧,塌陷具有沿灰岩岩溶发育区 与断层、接触带构造复合地段集中分布的特征。研究结果明确了矿区岩溶塌陷影响因素,为矿区 岩溶塌陷防治提供了科学依据,建议工程建设避开构造薄弱带,并优化矿山排水管理以降低塌陷 风险。

关键词: 岩溶塌陷, 岩溶发育, 地质构造, 影响因素

Abstract: To analyze the characteristics and influencing factors of karst collapse in Xinqiao Mine, by collecting data on the mine's basic geology,water conservancy,engineering and environmental geolo‐ gy,water prevention and control,historical karst collapse,karst collapse geological disaster investigation and groundwater monitoring of the mine,The background conditions of the mine geological environment were mastered,the characteristics of karst collapse were summarized,and the influencing factors of karst collapse were analyzed. Through mathematical and statistical analysis,it has been clearly identified that the underlying karst developed bedrock strata,the overlying loose soil layers and groundwater activities are the main influencing factors of karst collapse. Research shows that the limestone strata with karst develop‐ ment in the lower Qixia Formation and the upper section of the Gufeng Formation are the basic conditions for the occurrence of karst collapse. Weak geological structures such as fault zones and contact zones con‐ trol the distribution and degree of karst collapse. The overlying loose strata affect the process and scale of karst collapse and provide the source of collapse materials. Mine drainage is the main dynamic factor that induces karst collapse. Karst collapses in mining areas are mostly circular or oval in shape,with diameters and depths mostly less than 5 m. Over 90% of them are induced by mine drainage and dewatering,and they intensify with the increase of groundwater activity. The collapses are characterized by concentrated dis‐tribution along the complex sections of limestone karst development areas and fault and contact zone struc‐ tures. The research results have clarified the influencing factors of karst collapse in the mining area,pro‐ viding a scientific basis for the prevention and control of karst collapse in the mining area. It is suggested that the engineering construction avoid the weak structural zone and optimize the mine drainage manage‐ ment to reduce the risk of collapse.

Key words: karst collapse, karst development, geological structure, influencing factors