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主办单位:煤炭科学研究总院有限公司、中国煤炭学会学术期刊工作委员会
地质构造及水动力条件对瓦斯赋存的控制作用
  • Title

    Controlling effects of geological structure and hydrodynamics on gas occurrence

  • 作者

    赵俊山陈亮李瑞敬郭建行刘桂凤

  • Author

    ZHAO Junshan,CHEN Liang,LI Ruijing,GUO Jianhang,LIU Guifeng

  • 单位

    冀中能源股份有限公司峰峰集团大社矿煤炭科学技术研究院有限公司〓安全分院冀中能源股份有限公司

  • Organization
    1.Dashe Coal Mine of Fengfeng Group Co.,Ltd.,Jizhong Energy Resources Co.,Ltd.,Handan ,China;2.Mine Safety Technology Branch of China Coal Research Institute,Beijing ,China; 3.Jizhong Energy Resources Co.,Ltd.,Xingtai ,China
  • 摘要

    为了掌握唐家河井田地质构造与水动力条件对瓦斯赋存的影响,基于大量瓦斯参数测试及瓦斯地质资料,深入总结了8号煤层瓦斯赋存区域分布特征,系统分析了地质构造演化、构造应力场及地质构造形态对瓦斯赋存逐级控制作用,采用数据统计和非线性拟合方法定量分析了水动力条件对瓦斯的生气-富集-存储全过程的影响。结果表明:唐家河井田8号煤层东翼瓦斯含量为西翼的1.7倍,且其挥发分小于西翼、镜质组反射率略大于西翼。煤层埋深东翼大于西翼,且与瓦斯涌出量线性相关性较好,其煤层顶板岩性变化较大,西翼则以泥岩为主,相应煤层倾角为西翼的1.5倍,相应煤层厚度及其完整性均强于西翼。研究发现受控于地质构造演化,成煤时期煤层东翼围岩透气性条件较好,并发育有0.2~0.4 m厚的构造煤,煤层埋深整体东深西浅;煤层东翼位于大两会背斜翼部,埋深较深,倾角相对平缓,其构造应力场主要呈现为挤压作用,利于瓦斯保存。成煤时期西翼煤层的水动力活动性较强,导致煤储层古地温略低于东翼,相应煤变质程度稍低,且其煤层完整性相对较差;后期东、西翼瓦斯运移与水流方向相反,分别呈现为水力封堵和水力运移作用,故西翼水动力条件不利于瓦斯的产生及保存。研究发现该井田工作面含水层涌水量与瓦斯涌出量满足对数函数关系,有助于揭示涌水量与瓦斯赋存之间的定量关系。

  • Abstract
    This paper is devoted to study the influence of geological structure and hydrodynamics on gas occurrence in Tangjiahe coalfield.Based on tests of gas parameters and geological data,the gas distributions of No.8 coal seam are analyzed.The analysis includes the controlling effects of geological structure evolution,tectonic stress field,and geological structure form on gas distributions.Also,hydrodynamic impact on gas generation-enrichment-storage process is analyzed using descriptive statistics and nonlinear regression.The results show that the gas content of east flank is 1.7 times of gas content of west flank.Gas of east flank contains lower volatile contents and higher vitrinite reflectance contents than the west flank.The depth of the east flank if larger than the depth of the west flank and is correlated with gas emission linearly.The roof lithology for east flank varies greatly while the roof of west flank is mainly composed of mudstone.The coal seam dip angle of east flank is 1.5 times of the dig angle of west flank.Gas permeability in east flank is higher than west flank because the geological tectonic evolution developed 0.2~0.4 m thick tectonic coal during coal-forming period.The east flank is located at an anticline flank in Dalianghui anticline and the main tectonic stress is compression,which is conducive to gas storage.During the coal-forming period,the hydrodynamic activity in west flank was strong,which results in slightly lower ground temperature of coal reservoir,slightly lower coal metamorphism,and poorer coal seam integrity than the east flank.In reserving period,due to gas migration opposite to water flow direction,hydraulic sealing occurred in east flank while hydraulic migration occurred in west flank.The hydrodynamic conditions of west flank go against gas storage.The study also found that the aquifer water inflow is related to face gas emission with a logarithmic relationship,which helps to reveal the mathematical relationship between water inflow and gas occurrence.
  • 关键词

    地质构造水动力大两会背斜热致因成气变质程度

  • KeyWords

    geological structure; hydrodynamic force; Dalianghui anticline; thermogenic gas; degree of metamorphism

  • 基金项目(Foundation)
    国家重点研发计划资助项目(2017YFC0804206-002);国家科技重大专项资助项目(2016ZX05067005-005);国家自然科学基金资助项目(51604154)
  • 相关专题
  • 图表
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    • 唐家河煤矿8号煤层的埋藏与成气史

    图(4) / 表(0)

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主办单位:煤炭科学研究总院有限公司 中国煤炭学会学术期刊工作委员会

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