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赵楼煤矿1000m深孔水压致裂地应力测量及其应力场研究

RESEARCH ON STRESS FIELD AND HYDRAULIC FRACTURING IN-SITU STRESS MEASUREMENT OF 1000 M DEEP HOLE IN ZHAOLOU COAL MINE

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【作者】 彭华马秀敏姜景捷彭立国

【Author】 PENG Hua1,2,MA Xiumin1,2,JIANG Jingjie1,2,PENG Liguo1(1.Key Laboratory of Neotectonic Movement and Geohazards of Ministry of Land and Resources,Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China;2.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China)

【机构】 中国地质科学院地质力学研究所国土资源部新构造运动与地质灾害重点实验室中国地质科学院地质力学研究所

【摘要】 赵楼煤矿是目前国内开采最深的非金属矿山之一,处于曹县—郓城活动断裂带上,区内地质构造较为复杂。为了掌握矿区原岩应力场分布规律,应用深孔水压致裂地应力测量技术开展地应力测量工作,获得该矿区2个钻孔中16个测段的应力状态。测量结果表明:矿区最大主应力随深度增加基本呈线性增大,且在800 m深度处应力值有所变化,最大水平主应力为28.45~45.75 MPa,方向NEE,反映出矿区地应力场以水平应力为主导的特点,测量结果可为矿山建设和开采设计提供科学依据。

【Abstract】 Zhaolou coal mine is one of the deepest mines in China.Its geological structure is more complex because it is located in Caoxian—Yuncheng active fault.In order to master the distribution law of in-situ stress field in the mine,the in-situ stress measurement is carried out by means of the hydraulic fracturing in-situ stress measurement technique.The stress states are obtained for 16 measuring sections in 2 holes.The measurement results show that the maximum principal stress increases linearly as the depth increases;and the in-situ stresses are varied around the depth of 800 m.The maximum horizontal principal stresses are 28.45–45.75 MPa;and their directions are NEE.It reflects that the horizontal stress is dominant in the stress field of the mine area.The proposed measurement results provide scientific basis for the mine construction and mining design.

【基金】 国土资源大调查项目(1212010916064);“十一五”国家科技支撑计划项目
  • 【文献出处】 岩石力学与工程学报 ,Chinese Journal of Rock Mechanics and Engineering , 编辑部邮箱 ,2011年08期
  • 【分类号】TD326
  • 【被引频次】16
  • 【下载频次】539
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