Advance Search
Volume 49 Issue 8
Aug.  2021
Turn off MathJax
Article Contents
YANG Peng, YANG Weifeng, MA Rongkun. Study on microscopic pore structure types of Jurassic sandstone and water abundance in Jinjie Coal Mine[J]. COAL SCIENCE AND TECHNOLOGY, 2021, 49(8): 188-194.
Citation: YANG Peng, YANG Weifeng, MA Rongkun. Study on microscopic pore structure types of Jurassic sandstone and water abundance in Jinjie Coal Mine[J]. COAL SCIENCE AND TECHNOLOGY, 2021, 49(8): 188-194.

Study on microscopic pore structure types of Jurassic sandstone and water abundance in Jinjie Coal Mine

More Information
  • Available Online: April 02, 2023
  • Published Date: August 24, 2021
  • The water abundance of sandstone is one of the important indexes for the risk assessment of roof water inrush. It is of great significance to study the microscopic pore structure of sandstone for understanding its relationship with the water abundance of aquifer.In this paper,taking the Jurassic sandstone of 3-1 coal roof in Jinjie Coal Mine as an example. The microscopic pore structure of sandstone was studied by thin section identification and mercury porosimeter method. Finally,the relationship between the microscopic pore structure and water abundance of sandstone in the study area was analyzed by comparing the unit water inflow of borehole. The results show that the clay content(25.5% on average) in Yan’an formation of Jurassic is much higher than that in Zhiluo formation(4% on average).According to the shape of capillary pressure curve and displacement pressure,the pore structure of sandstone can be divided into three types:low displacement pressure type Ⅰ,medium displacement pressure type Ⅱ and high displacement pressure type Ⅲ. The low displacement pressure type Ⅰ sandstone is mainly composed of intergranular and intercrystal pores which is larger than 10 μm. If the pores in the study area larger than 10 meters were regarded as effective pores,the ratio of effective pore volume would reach 61.68%. The confined water head of the aquifer is about 66.30 m,with a certain pressure head,and a large number of gravity water in the pores moves freely under a certain confined water head,which is an important reasons of mediumwater abundance. In the medium displacement pressure type Ⅱ sandstone are dominated by intragranular and intergranular pores between 0.1 μm and 10.0 μm,The pore volume of this type accounts for 51.44%. In the high displacement pressure type Ⅲ sandstone,the intergranular pores are mainly less than 0.1 μm,The pore volume of this class accounts for 45.32%. In the medium displacement pressure type Ⅱ and in the high displacement pressure type Ⅲ,the effective pore volume are only 21.92%,which are weak water abundance.
  • Cited by

    Periodical cited type(8)

    1. 李建新,黄侨,刘寅,高小雷. 锦界煤矿3111运输顺槽进口掘锚机侧帮支护能力适应性研究. 煤炭技术. 2024(03): 255-258 .
    2. 李舒,杨泽元,马雄德,刘胜祖,方楚婧,张奥奇. 神府南区延安组含水层富水性对矿井涌水量的影响研究. 煤田地质与勘探. 2023(06): 92-102 .
    3. 徐智敏,陈天赐,刘栓栓,孙亚军,任冬冬,郇博程,张盼杰. 新疆伊犁矿区侏罗系含水介质特征与地下水赋存运移规律. 煤炭科学技术. 2023(07): 140-151 . 本站查看
    4. 周对对,龙良良,刘家鹏,何静,汪庆国,罗旭东. 大佛寺井田洛河组含水层微观孔隙结构及富水性研究. 中国煤炭. 2023(09): 43-50 .
    5. 方楚婧,杨泽元,范立民,马雄德,孙魁,郭人泰,张奥奇,李舒,刘胜祖. 神府南区直罗组含水层富水性研究. 灾害学. 2022(03): 219-226 .
    6. 范立民,迟宝锁,王宏科,马雄德,焦养泉,孙魁,苗彦平,王建文,胡俭,马万超. 鄂尔多斯盆地北部直罗组含水层研究进展与水害防治建议. 煤炭学报. 2022(10): 3535-3546 .
    7. 孙魁,苗彦平,陈小绳,王宏科,范立民,杨磊,马万超,路波,李成,陈建平,高帅. 鄂尔多斯盆地北部直罗组赋存特征及富水性. 煤炭学报. 2022(10): 3572-3598 .
    8. 李回贵,李化敏,许国胜. 神东矿区不同埋深弱胶结砂岩的孔隙结构特征研究. 中国矿业. 2021(09): 126-131 .

    Other cited types(3)

Catalog

    Article views (64) PDF downloads (264) Cited by(11)
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return