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Volume 34 Issue 6
Dec 2023
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Xiaowen Guo, Tao Luo, Tian Dong, Rui Yang, Yuanjia Han, Jizheng Yi, Sheng He, Zhiguo Shu, Hanyong Bao. Quantitative Estimation on Methane Storage Capacity of Organic-Rich Shales from the Lower Silurian Longmaxi Formation in the Eastern Sichuan Basin, China. Journal of Earth Science, 2023, 34(6): 1851-1860. doi: 10.1007/s12583-020-1394-7
Citation: Xiaowen Guo, Tao Luo, Tian Dong, Rui Yang, Yuanjia Han, Jizheng Yi, Sheng He, Zhiguo Shu, Hanyong Bao. Quantitative Estimation on Methane Storage Capacity of Organic-Rich Shales from the Lower Silurian Longmaxi Formation in the Eastern Sichuan Basin, China. Journal of Earth Science, 2023, 34(6): 1851-1860. doi: 10.1007/s12583-020-1394-7

Quantitative Estimation on Methane Storage Capacity of Organic-Rich Shales from the Lower Silurian Longmaxi Formation in the Eastern Sichuan Basin, China

doi: 10.1007/s12583-020-1394-7
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  • Corresponding author: Xiaowen Guo, E-mail: guoxw@cug.edu.cn
  • Received Date: 02 Sep 2020
  • Accepted Date: 15 Dec 2020
  • Available Online: 08 Dec 2023
  • Issue Publish Date: 30 Dec 2023
  • The assessment of gas storage capacity is crucial to furthering shale gas exploration and development in the eastern Sichuan Basin, China. Eleven organic-rich shale samples were selected to carry out the high pressure methane sorption, low-pressure N2/CO2 gas adsorption, and bulk and skeletal density measurements to investigate the methane storage capacity (MSC). Based on the relative content of clay, carbonates, quartz + feldspar, we grouped the 11 samples into three lithofacies: silica-rich argillaceous shale (CM-1), argillaceous/siliceous mixed shale (M-2), and clay-rich siliceous shale (S-3). The total porosity of the shale samples varies from 3.4% to 5.6%, and gas saturation ranges from 47% to 89%. The measured total gas amount ranges from 1.84 mg/g to 4.22 mg/g with the ratio of free gas to total gas amount ranging from 52.7% to 70.8%. Free gas with high content in the eastern Sichuan Basin may be the key factor controlling amount of shale gas production. The TOC content critically controls the MSC of shales, because micropore, mesopore volumes and the specific surface areas associated with organic matter provide the storage sites for the free and adsorbed gas. The methane sorption capacities of samples from different lithofacies are also affected by clay minerals and moisture content. Clay minerals can provide additional surface areas for methane sorption, and water can cause a 7.1%–42.8% loss of methane sorption capacity. The total porosity, gas-bearing porosity, water saturation, free gas and adsorbed gas number of samples from different lithofacies show subtle differences if the shale samples had similar TOC contents. Our results suggest that, in the eastern Sichuan Basin, clay-rich shale lithofacies is also prospecting targets for shale gas production.

     

  • Electronic Supplementary Materials: Supplementary materials (Figs. S1–S4) are available in the online version of this article at https://doi.org/10.1007/s12583-020-1394-7.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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