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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
煤层底板复合岩层微观缝隙结构复杂程度定量辨识
  • Title

    Quantitative identification of complexity of microscopic fracture structure of coal seam floor composite rock layer

  • 作者

    王心义陈博田世元邹宇张波

  • Author

    WANG Xinyi;CHEN Bo;TIAN Shiyuan;ZOU Yu;ZHANG Bo

  • 单位

    河南理工大学 资源环境学院河南省焦作市中站区农业农村局煤炭安全生产与清洁高效利用省部共建协同创新中心广东省水文局江门水文分局中国平煤神马集团能源化工研究院

  • Organization
    Institute of Resources & Environment, Polytechnic University
    Henan Jiaozuo zhongzhan Agriculture and Rural Affairs Bureau
    Collaborative Innovation Center of Coal Work Safety and Clean-efficiency Utilization
    Jiangmen Branch Bureau of Hydrology, Guangdong Provincial Bureau of Hydrology
    Institute of Energy and Chemical Industry, China Pingmei Shenma Group
  • 摘要

    采动条件下煤层底板复合岩层微观缝隙结构影响着下伏高水压含水层地下水的导升和渗流,其复杂程度对于煤层底板水害预测预警具有重要意义。以平顶山煤田东部3个相邻矿井提取的57组岩样为对象,基于SEM图像采集和N2吸附试验的综合信息,选取岩层面积缝隙率、等效缝隙直径、缝隙面积分维值、比表面积、缝隙体积及其分维值为主控因子,利用熵权-TOPSIS数学模型定量评价了己16-17煤层至寒武灰岩顶界面之间复合岩层微观缝隙结构的复杂程度。结果表明:己16~17煤层底板复合岩层微观缝隙结构极简单、简单、中等、复杂、极复杂等级占比分别为25.00%、21.43%、39.29%、7.14%、7.14%,研究地段复合岩层的微观缝隙结构相对不复杂;4个岩段相比,岩层微观缝隙结构复杂程度量化均值排序为L1~L2灰岩段>L5~L7灰岩段>砂岩段>铝土质泥岩段,岩层微观缝隙结构复杂程度较好地反映了岩层缝隙发育程度。研究考虑了多因素对复合岩层的耦合影响,实现了复合岩层垂直段微观缝隙结构的定量分级分区判别,对精准刻画煤层底板复合岩层的含隔水层性能和科学指导煤层底板水害防治具有重要的意义。

  • Abstract

    Under mining conditions, the micro crack structure of the composite strata of the coal seam floor affects the uplift and seepage of the groundwater in the underlying high water pressure aquifer, and its complexity is of great significance for the prediction and early warning of the water disaster in the coal seam floor. In this paper, a total of 57 groups of rock samples extracted from three adjacent mines in the east of Pingdingshan Coalfield are taken as the object. Based on the comprehensive information of SEM image acquisition and N2 adsorption test, the fissure ratio of rock stratum area, equivalent crack diameter of rock stratum, fractal dimension value of fissure area, specific surface area, crevice volume and its fractal dimension are the main controlling factors. Using entropy weighted TOPSIS mathematical model, the complexity of the micro fracture structure of the composite rock stratum between the Ji16-17 coal seam and the Cambrian limestone top interface is quantitatively evaluated. The results show that the micro crack structure of the composite strata in the floor of the Ji16-17 coal seam is very simple, simple, medium, complex and extremely complex, accounting for 25.00%, 21.43%, 39.29%, 7.14% and 7.14% respectively. The micro crack structure of the composite strata in the study section is relatively uncomplicated; Compared with the four rock sections, the order of the quantitative mean value of the complexity of the rock stratum micro fracture structure is: L1−L2 limestone section>L5−L7 limestone section>sandstone section>bauxite mudstone section. The complexity of the rock stratum micro fracture structure better reflects the development of the rock stratum fracture. The paper considers the coupling effect of multiple factors on the composite rock stratum, realizes the quantitative classification and zoning discrimination of the micro crack structure in the vertical section of the composite rock stratum, which is of great significance for accurately describing the aquifer performance of the composite rock stratum in the coal seam floor and scientifically guiding the prevention and control of the water hazard in the coal seam floor.

  • 关键词

    复合岩层微观缝隙结构复杂程度熵权-TOPSIS模型定量辨识

  • KeyWords

    composite strata;microstructure;complexity;entropy weight-TOPSIS model;duantitative identification

  • 基金项目(Foundation)
    国家自然科学基金资助项目(41972254);河南省创新型科技人才队伍建设工程资助项目(CXTD2016053);河南省高校基本科研业务费专项资金资助项目(NSFRF200103)
  • DOI
  • 引用格式
    王心义,陈 博,田世元,等. 煤层底板复合岩层微观缝隙结构复杂程度定量辨识[J]. 煤炭科学技术,2023,51(7):53−63
  • Citation
    WANG Xinyi,CHEN Bo,TIAN Shiyuan,et al. Quantitative identification of complexity of microscopic fracture structure of coal seam floor composite rock layer[J]. Coal Science and Technology,2023,51(7):53−63
  • 相关专题
  • 图表
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    • 己16-17煤底板复合岩层柱状图

    图(13) / 表(0)

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