Nano-Scale Pore Structure of Marine-Continental Transitional Shale from Liulin Area, the Eastern Margin of Ordos Basin, China

被引:21
作者
Xi, Zhaodong
Tang, Shuheng [1 ]
Zhang, Songhang
Li, Jun
机构
[1] China Univ Geosci, MOE Key Lab Marine Reservoir Evolut & Hydrocarbon, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Pore Structure; N-2; Adsorption/Desorption; Marine-Continental Transitional Shale; The Eastern Margin of Ordos Basin; GAS-ADSORPTION; SURFACE-AREA; BLACK SHALES; POROSITY; BARNETT; SYSTEMS; SIZE; CLASSIFICATION; DISTRIBUTIONS; POROSIMETRY;
D O I
10.1166/jnn.2017.14501
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Organic shale, which is deposited in marine-continental transitional environments and is found in coal-bearing strata, is well developed in China. This type of shale contains large amounts of shale gas. Here, a series of parallel experiments, including scanning electronic microscopy, low-temperature nitrogen adsorption/desorption, X-ray diffraction and geochemical analyses, were performed on 23 samples of marine-continental transitional shale from the eastern margin of the Ordos Basin in China. The results showed that the dominant minerals in the shale were quartz and clay, with average volumes of 36.31% and 52.07% respectively. The total organic carbon ranged from 0.18% to 31.16%, with a mean value of 2.43%. Based on kerogen stable carbon isotopes and maceral composition analysis, it appears that marine-continental transitional shale is characterized by gas-prone, inertinite-dominated type III kerogen. SEM images showed that the pores in the shale matrix were mainly associated with clay minerals and organic matter (OM). According to the N-2 adsorption analysis, pores of 2.5 nm and 30-50 nm in size were dominant and there were obvious differences in the mesopore (2-50 nm) volumes of the different samples. In summary, we assert that the marine-continental transitional shale pore volume comes primarily from mesopores (2-50 nm) and macropores (50 nm-300 nm) and the specific surface area comes mainly from mesopores and micropores(< 2 nm). Pore structure development is principally controlled by the type of organic matter and the mineral composition, which are different from those of marine systems. The composition of organic matter (i.e., the high inertinite content) in the study area is the main constraint on the development of organic pores. The mesopores are more developed in shales with a high content of mixed-layer illite-smectite. In addition, a higher content of brittle minerals will generate a strong rock resistant compaction ability, which helps reserve more pores.
引用
收藏
页码:6109 / 6123
页数:15
相关论文
共 51 条
  • [1] Comparisons of pore size distribution: A case from the Western Australian gas shale formations
    Al Hinai, Adnan
    Rezaee, Reza
    Esteban, Lionel
    Labani, Mehdi
    [J]. JOURNAL OF UNCONVENTIONAL OIL AND GAS RESOURCES, 2014, 8 (0C) : 1 - 13
  • [2] Synthesis of Zn2SnO4 via a co-precipitation method and its gas-sensing property toward ethanol
    An, Dongmin
    Wang, Qiong
    Tong, Xiaoqiang
    Zhou, Qingjun
    Li, Zepeng
    Zou, Yunling
    Lian, Xiaoxue
    Li, Yan
    [J]. SENSORS AND ACTUATORS B-CHEMICAL, 2015, 213 : 155 - 163
  • [3] [Anonymous], 2008, SPE119892
  • [4] 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
  • [5] STUDIES ON PORE SYSTEMS IN CATALYSTS .13. PORE DISTRIBUTIONS FROM DESORPTION BRANCH OF A NITROGEN SORPTION ISOTHERM IN CASE OF CYLINDRICAL PORES .B. APPLICATIONS
    BROEKHOFF, JC
    DEBOER, JH
    [J]. JOURNAL OF CATALYSIS, 1968, 10 (04) : 377 - +
  • [6] Adsorption of gases in multimolecular layers
    Brunauer, S
    Emmett, PH
    Teller, E
    [J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1938, 60 : 309 - 319
  • [7] Cao Q.Y, 1985, Pet. Explor. Dev, V12, P14
  • [8] Classification and controlling factors of organic pores in continental shale gas reservoirs based on laboratory experimental results
    Cao, Qian
    Zhou, Wen
    Deng, Hucheng
    Chen, Wenling
    [J]. JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING, 2015, 27 : 1381 - 1388
  • [9] 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
  • [10] The organic matter distribution and methane capacity of the lower Cretaceous strata of northeastern British Columbia, Canada
    Chalmers, Gareth R. L.
    Bustin, R. Marc
    [J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY, 2007, 70 (1-3) : 223 - 239