首页|信湖煤矿DF19断层带岩性特征及采动影响分析

信湖煤矿DF19断层带岩性特征及采动影响分析

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通过资料收集,结合取样测试、水文试验及FLAC3D数值模拟分析等,对信湖煤矿82采区DF19断层带岩性特征、含导水性及采动影响下围岩破坏特征进行了分析.分析结果表明:1.DF19断层为张扭性断层,形成时代较早;2.断层带岩性以泥岩、粉砂岩为主,岩体较破碎,岩石质量指标较低,成分以石英、石膏为主,岩石强度较高;3.DF19断层带渗透系数为0.0026m/d~0.0398 m/d,透水率为0.0246Lu~0.0475Lu,含水性弱,导水性差;4.数值模拟分析采动影响下DF19断层下盘留设防水煤柱小于55m时断层"活化".
Analysis of Lithological Characteristics and Mining Impact of DF19 Fault Zone in Xinhu Coal Mine
Based on data collection,sampling tests,hydrological experiments,and FLAC3D nu-merical simulation analysis,the lithological characteristics,water permeability,and surrounding rock failure characteristics of the DF19 fault zone in the 82nd mining area of Xinhu Coal Mine were analyzed.The research results indicate that:1.The DF19 fault is a tensional and torsional fault,formed at an ear-lier age.2.The lithology of the fault zone is mainly composed of mudstone and siltstone,with relatively fractured rock mass and low rock quality indicators.The composition is mainly quartz and gypsum,and the rock strength is relatively high.3.The permeability coefficient of the DF19 fault zone is 0.0026~0.0398 m/d,with a permeability rate of 0.0246~0.0475 Lu.It has weak water content and poor hydrau-lic conductivity.4.Numerical simulation analysis shows that under the influence of mining,the DF19 fault is activated when a waterproof coal pillar less than 55m is left in the lower wall.

Xinhu Coal Minefault zonelithologic structurewater-bearing propertychar-acteristics of mining damage

黄河、牛浩荣、张治、王来斌、谢君

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矿山地质灾害防治安徽省高校重点实验室,安徽淮南 232001

安徽理工大学地球与环境学院,安徽淮南 232001

安徽省亳州煤业有限公司信湖煤矿,安徽亳州 235000

信湖煤矿 断层带 岩性结构 含导水性 采动破坏特征

2024

佳木斯大学学报(自然科学版)
佳木斯大学

佳木斯大学学报(自然科学版)

影响因子:0.159
ISSN:1008-1402
年,卷(期):2024.42(11)