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Nanoscale Pores in Coal Related to Coal Rank and Deformation Structures
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  • 作者:Jienan Pan (1) (2)
    Yanqing Zhao (1) (2)
    Quanlin Hou (3) (4)
    Yi Jin (1) (2)

    1. School of Resources and Environment
    ; Henan Polytechnic University ; Jiaozuo ; 454000 ; China
    2. The Collaborative Innovation Center for Coalbed Methane and Shale Gas
    ; Henan Polytechnic University ; Jiaozuo ; 454000 ; China
    3. Key Lab of Computational Geodynamics
    ; Chinese Academy of Sciences ; Beijing ; 100049 ; China
    4. College of Earth Sciences
    ; University of Chinese Academy of Sciences ; Beijing ; 100049 ; China
  • 关键词:Nanoscale pore ; Tectonically deformed coal ; Normal structure coal ; Coal rank ; Deformation structure
  • 刊名:Transport in Porous Media
  • 出版年:2015
  • 出版时间:March 2015
  • 年:2015
  • 卷:107
  • 期:2
  • 页码:543-554
  • 全文大小:346 KB
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  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geotechnical Engineering
    Industrial Chemistry and Chemical Engineering
    Civil Engineering
    Hydrogeology
    Mechanics, Fluids and Thermodynamics
  • 出版者:Springer Netherlands
  • ISSN:1573-1634
文摘
Experimental results show that nanoscale pores in coal are affected by coal rank and deformation structures. In terms of pore volume, the transitional pores occupy the largest proportion, and in terms of specific surface area, the sub-micropores take up the largest proportion. For weak brittle deformed coal (including normal structured coal), when the coal rank increases, the volume and specific surface area of pores in different sizes firstly decrease and then increase. The volume and specific surface area of transitional pores and micropores in coal reach the minimum at about \({R}_\mathrm{O, ran} = 2.0\,\%\) . After that, a slow increasing trend is observed. The volume of sub-micropores reaches the minimum at about \({R}_\mathrm{O, ran}= 1.5\,\%\) and then shows a trend of rapid growth as coal rank increases. As the degree of coal deformation increases, both pore volume and specific surface area have a significant increase. Under strong tectonic deformation, both the volume and total specific surface area of the nanoscale pores and of sub-micropores increase significantly; the volume of transitional pores increases moderately, and their specific surface area shows a decreasing trend; the volume and specific surface area increments of micropores decline rapidly as the degree of metamorphism increases.

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