2018
DOI: 10.1016/j.petrol.2018.08.061
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Insight into the pore structure of Wufeng-Longmaxi black shales in the south Sichuan Basin, China

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Cited by 18 publications
(13 citation statements)
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“…Molecular simulation is the common effective method to study shale gas adsorption behavior because of the characteristics of shale pores, whose average pore size is 3–5 nm. Based on realistic kerogen model, Zhao et al studied the effects of water content on methane adsorption capacity using the molecular dynamics (MD) and Monte Carlo (MC) simulation methods . Although some molecular dynamics-based shale kerogen pores were constructed to investigate the adsorption of methane in shale, Huang et al considered the factors of pressures, temperatures, geological depths, kerogen maturity, moisture content, and kerogen organic type on adsorption of CH 4 and CO 2 using GCMC and MC methods. ,, Zhou and Collell et al figured out the effect of pore size on adsorption.…”
Section: Introductionmentioning
confidence: 99%
“…Molecular simulation is the common effective method to study shale gas adsorption behavior because of the characteristics of shale pores, whose average pore size is 3–5 nm. Based on realistic kerogen model, Zhao et al studied the effects of water content on methane adsorption capacity using the molecular dynamics (MD) and Monte Carlo (MC) simulation methods . Although some molecular dynamics-based shale kerogen pores were constructed to investigate the adsorption of methane in shale, Huang et al considered the factors of pressures, temperatures, geological depths, kerogen maturity, moisture content, and kerogen organic type on adsorption of CH 4 and CO 2 using GCMC and MC methods. ,, Zhou and Collell et al figured out the effect of pore size on adsorption.…”
Section: Introductionmentioning
confidence: 99%
“…For the Wufeng-Longmaxi shale, Guo et al reported that the organic pores have a positive contribution to porosity if Ro is less than 2.8% in the Sichuan Basin . Huang and Zhu et al have reported that the Ro of OM in Wufeng-Longmaxi formation in the study area is in the range from 0.7% to greater than 3.0%, with an averafe of 2.19%, among which the samples with Ro between 1.3 and 3.0% take the largest part. Thus, a large number of organic pores flourish in the study area because the R o of the Wufeng-Longmaxi shale is less than 2.2%. The study unveiled a positive correlation between thermal maturity and the specific surface area in the study area (Figure b).…”
Section: Discussionmentioning
confidence: 91%
“…The results showed a significant influence of mineral content on pore occurrence. As shown in the figures, the correlation coefficient of clay mineral content and porosity is 0.5, and the 45 and the triangular pattern refers to the amount data of Sun et al, 42 and in (b), the square pattern refers to Zhu et al's data, 46 while the triangular pattern refers to Yang et al 43 Figure 9. Relationship between TOC and porosity (a) and the specific surface area (b).…”
Section: Discussionmentioning
confidence: 95%
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