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准东大井矿区巨厚煤层开采覆岩含水层渗透特性研究 被引量:1
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作者 曾强 李根生 +2 位作者 杨洁 赵龙辉 高坡 《中国矿业》 北大核心 2019年第5期116-124,共9页
基于准东大井矿区赋岩柱状及岩性,构建了赋岩物理模型与数值模型。基于该模型,开展了赋岩位移与含水层渗透特性的模拟研究。结果表明:开采首分层覆岩含水层各测点位移随开挖长度的增加而增加;测点1~#物理模拟开挖至70~250m及数值模拟... 基于准东大井矿区赋岩柱状及岩性,构建了赋岩物理模型与数值模型。基于该模型,开展了赋岩位移与含水层渗透特性的模拟研究。结果表明:开采首分层覆岩含水层各测点位移随开挖长度的增加而增加;测点1~#物理模拟开挖至70~250m及数值模拟开挖至100~300m时,位移呈快速增加,其后位移变化稳定;测点2~#物理模拟开挖至70~420m及数值模拟开挖至250~500m时,位移呈快速增加,其后位移稳定;测点3~#物理模拟开挖至430~600m及数值模拟开挖至450~600m时,位移快速增加。物理相似模拟及数值模拟各测点变化趋势基本一致;覆岩含水层各测点有效应力与孔隙介质渗透率呈负相关;覆岩含水层各测点有效应力与裂隙介质渗透率呈正相关。开挖1~5分层渗透率大小为:测点1~#>测点3~#>测点2~#;开挖6~8分层渗透率大小为:测点3~#>测点1~#>测点2~#;覆岩含水层渗透特性与覆岩孔隙-裂隙双重介质动态变化特征有关,与采动覆岩应力变化具有耦合效应。 展开更多
关键词 准东矿区 巨厚煤层开采 覆岩含水层 渗透特性 数值模拟
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覆岩含水层采动破坏机理流固耦合分析及保护措施研究
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作者 董立军 张国红 吴洪胜 《中国矿业》 北大核心 2014年第9期95-101,共7页
为了研究煤层开采对覆岩含水层的破坏机理,采用岩石破裂过程流固耦合分析系统UDECFlow,根据老三沟井田6煤工作面地质条件,对覆岩含水层(砂砾岩、细砾岩和粗砂岩含水层)的破坏过程进行数值模拟。模拟结果显示,随着工作面的推进,裂隙不断... 为了研究煤层开采对覆岩含水层的破坏机理,采用岩石破裂过程流固耦合分析系统UDECFlow,根据老三沟井田6煤工作面地质条件,对覆岩含水层(砂砾岩、细砾岩和粗砂岩含水层)的破坏过程进行数值模拟。模拟结果显示,随着工作面的推进,裂隙不断向上发育,直接顶、基本顶的相继破断和垮落导致了导水裂隙的形成;同时随着工作面的推进,先前生成的一些裂隙出现了闭合,而工作面附近又产生新的裂隙。以6煤为例,对上覆含水层的保水开采难度进行分级,并提出了相应的保水开采技术,如加快工作面推进速度、注浆加固、降低采高、充填开采及部分开采等,将指导6煤开采时覆岩含水层保护,对同类开采地质条件下的矿井有较好的指导借鉴意义。 展开更多
关键词 覆岩含水层 数值模拟 采动破坏机理 保护措施
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泥岩超压层封闭煤层气能力分析 被引量:2
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作者 王翰锋 《煤炭科学技术》 CAS 北大核心 2015年第6期81-84,共4页
覆岩(盖层)密闭性是煤层气储层资源量决定条件之一。通过对泥岩超压层的成因和性质分析,建立煤层气储层渗流的数学方程,探讨稳定地质条件下煤层气运移的约束条件。研究发现,泥岩超压的形成具有阶段性,受地质条件变化控制;超压层封闭一... 覆岩(盖层)密闭性是煤层气储层资源量决定条件之一。通过对泥岩超压层的成因和性质分析,建立煤层气储层渗流的数学方程,探讨稳定地质条件下煤层气运移的约束条件。研究发现,泥岩超压的形成具有阶段性,受地质条件变化控制;超压层封闭一定压力气体需达到一定深度,随着埋深增加和地温升高,覆岩孔隙度递减导致超压变化,覆岩对孔隙水的吸附阻力与底部岩层的排替压力也随之发生改变,逐步提高覆岩对煤层气的封闭能力。 展开更多
关键词 煤层气 运移 超压 覆岩含水层
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Overburden failure and the prevention of water and sand inrush during coal mining under thin bedrock 被引量:7
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作者 Yang Weifeng Xia Xiaohong Zhao Guorong Ji Yubin Shen Dingyi 《Mining Science and Technology》 EI CAS 2011年第5期733-736,共4页
Coal mining under thin bedrock or thick unconsolidated soil layers brings mining problems related to these special geological conditions. The meaning of the term ''thin bedrock'' is defined through the... Coal mining under thin bedrock or thick unconsolidated soil layers brings mining problems related to these special geological conditions. The meaning of the term ''thin bedrock'' is defined through the thick- ness statistics of the coal seam and the bedrock layer. The coal-bearing strata having thick, unconsoli- dated aquifers and thin bedrock located at the Taiping Coal Mine in Shandong province were taken as a geological prototype for subsequent study. The geological, hydro-geological and engineering character- istics of the thin bedrock were analyzed. An engineering geological model was than established. Overbur- den failure and the development of ''Three Zones'' were studied by physical model tests. The rupture pattern and rock failure were analyzed for mining conditions under thin bedrock. The height of the caving zone and the freely flowing water fractured zone of different mining thicknesses were separately calcu- lated. The results show that a mining thickness greater than 3.5 m causes the height of the freely flowing water fractured zone to be sufficient to touch the weathered zone and the bottom of the Quaternary sys- tem aquifer, to various degrees. This, then, would lead to water and sand inrush into the working face. Measures to prevent water and sand flow inrush disasters by eliminating the power source are put fore- word. A field dewatering scheme was designed and observational data were obtained. The dewatering project had an obvious effect and the water level at working face number 8309 dropped to a safe level. The average draw down of the groundwater was observed to be 7.86 m. This showed that the dewatering project played a role in decreasing the hydraulic pressure and ensuring safety mining. 展开更多
关键词 Thin bedrockMining failureWater and sand flow inrushDewatering
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