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沁水盆地太原组煤层岩石物理性质、镜质组反射率与微观结构实验研究(英文)

Physical properties,vitrinite reflectance,and microstructure of coal,Taiyuan Formation,Qinshui Basin,China

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【作者】 李琼陈杰何建军

【Author】 Li Qiong;Chen Jie;He Jian-Jun;College of Geophysics, Chengdu University of Technology;College of Information Science & Technology, Chengdu University of Technology;

【机构】 成都理工大学地球物理学院成都理工大学信息科学与技术学院

【摘要】 为了分析沁水盆地太原组煤层岩石物理性质、镜质组反射率与微观结构之间的关系,采集了三个不同煤矿井下的11个煤岩样品,利用MTS岩石物理参数测试系统对煤样进行弹性参数测试,通过薄片鉴定和扫描电镜对11个煤样的有机显微组分、镜质组最大反射率和微观结构特征进行了分析。对上述实验结果进行交会分析发现:一些弹性参数之间具有线性关系;纵波速度与横波速度均具有各向异性特征,其各向异性特征与镜质组最大反射率有良好的负相关性;纵横波速度、杨氏模量与微孔含量呈负相关关系。获得的煤岩岩石物理参数之间的关系构成了煤岩地震岩石物理建模和煤层气地震反演技术的基础。

【Abstract】 In this study, we experimentally established the relationship between physical properties, vitrinite reflectance, and microstructure of coal, Taiyuan Formation, Qinshui Basin, China using representative coal samples collected from three different mines via the rock mechanics testing system(MTS). We analyzed the organic macerals, vitrinite reflectance, and microstructure of 11 coal samples using petrography and scanning electron microscopy(SEM). The experimental results suggest that(1) the elastic parameters can be described by linear equations,(2) both P-and S-wave velocities display anisotropy,(3) the anisotropy negatively correlates with vitrinite reflectance, and(4) the acoustic velocities and Young’s modulus are negatively correlated with the volume of micropores. The derived empirical equations can be used in the forward modeling and seismic inversion of physical properties of coal for improving the coal-bed methane(CBM) reservoir characterization.

【基金】 sponsored by the National Natural Science Foundation of China(No.41274129);the National Research Program of China(No.2008ZX05035-001-006HZ and No.2011ZX05035-005-003HZ)
  • 【文献出处】 Applied Geophysics ,应用地球物理(英文版) , 编辑部邮箱 ,2017年04期
  • 【分类号】P618.13;P631.4
  • 【被引频次】5
  • 【下载频次】146
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