Pore Structure Characterization of Shale Using Gas Physisorption: Effect of Chemical Compositions

被引:20
作者
Han, Yosep [1 ]
Kwak, Daewoong [1 ]
Choi, Siyoung Q. [2 ]
Shin, Changhoon [3 ]
Lee, Youngsoo [1 ]
Kim, Hyunjung [1 ]
机构
[1] Chonbuk Natl Univ, Dept Mineral Resources & Energy Engn, 567 Baekje Daero, Jeonju 54896, Jeonbuk, South Korea
[2] Korea Adv Inst Sci & Technol, Dept Chem & Biomol Engn, Daejeon 305701, South Korea
[3] Korea Gas Corp, Gas Resource Technol Ctr, 1248 Suin Ro, Ansan 15328, Kyounggi Do, South Korea
来源
MINERALS | 2017年 / 7卷 / 05期
关键词
shale; pore structure; gas physisorption; micropore volume; chemical composition; SURFACE-AREA; METHANE ADSORPTION; RESERVOIRS; POROSIMETRY; ISOTHERMS; MARCELLUS; AMERICAN; BARNETT; SYSTEMS; BASIN;
D O I
10.3390/min7050066
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In this study, the pore structure characteristics of Canadian Horn River basin shales with various chemical compositions were evaluated using gas physisorption analyses. The samples used in this research were obtained from two different regions (shallow and deep regions) of rock cuttings during the drilling of the shale gas field located in Horn River basin. The pore size, specific surface area, total pore volume, micropore surface area, and micropore volume of the shale samples were measured using both nitrogen and CO2. The results indicated that the pore size was not a function of chemical composition, while distinct trends were observed for other macroscopic and microscopic pore-related properties. In particular, the greatest specific surface area and total pore volume were observed for silica-rich carbonate shales, while clay-rich siliceous shales exhibited the greatest micropore volume and micropore surface area. The trends clearly suggested that macroscopic and microscopic pore-related properties of the Canadian Horn River basin shales were closely related to their chemical composition. Furthermore, a stronger correlation was observed between the quartz content and the micropore-related physical properties of shales (i.e., the micropore surface area and micropore volume) in comparison to other properties.
引用
收藏
页数:11
相关论文
共 31 条
  • [1] Abbaszadeh M., 2016, ENVIRON EARTH SCI, V75, P1
  • [2] THE DETERMINATION OF PORE VOLUME AND AREA DISTRIBUTIONS IN POROUS SUBSTANCES .1. COMPUTATIONS FROM NITROGEN ISOTHERMS
    BARRETT, EP
    JOYNER, LG
    HALENDA, PP
    [J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1951, 73 (01) : 373 - 380
  • [3] Adsorption of gases in multimolecular layers
    Brunauer, S
    Emmett, PH
    Teller, E
    [J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1938, 60 : 309 - 319
  • [4] Importance of rock properties on the producibility of gas shales
    Bustin, Amanda M. M.
    Bustin, R. Marc
    [J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY, 2012, 103 : 132 - 147
  • [5] Characterization of gas shale pore systems by porosimetry, pycnometry, surface area, and field emission scanning electron microscopy/transmission electron microscopy image analyses: Examples from the Barnett, Woodford, Haynesville, Marcellus, and Doig units
    Chalmers, Gareth R.
    Bustin, R. Marc
    Power, Ian M.
    [J]. AAPG BULLETIN, 2012, 96 (06) : 1099 - 1119
  • [6] Shale gas reservoir characterisation: A typical case in the southern Sichuan Basin of China
    Chen, Shangbin
    Zhu, Yanming
    Wang, Hongyan
    Liu, Honglin
    Wei, Wei
    Fang, Junhua
    [J]. ENERGY, 2011, 36 (11) : 6609 - 6616
  • [7] Chiou W., 2012, MICROSTRUCTURE FINE
  • [8] Pore structure characterization of North American shale gas reservoirs using USANS/SANS, gas adsorption, and mercury intrusion
    Clarkson, C. R.
    Solano, N.
    Bustin, R. M.
    Bustin, A. M. M.
    Chalmers, G. R. L.
    He, L.
    Melnichenko, Y. B.
    Radlinski, A. P.
    Blach, T. P.
    [J]. FUEL, 2013, 103 : 606 - 616
  • [9] HOMOGENEOUS AND HETEROGENEOUS MICROPORE STRUCTURES IN CARBONACEOUS ADSORBENTS
    DUBININ, MM
    STOECKLI, HF
    [J]. JOURNAL OF COLLOID AND INTERFACE SCIENCE, 1980, 75 (01) : 34 - 42
  • [10] Ferri F., 2012, GEOSCIENCE REPORTS, V2012, P1