期刊论文详细信息
FUEL 卷:219
Multifractal analysis of gas adsorption isotherms for pore structure characterization of the Bakken Shale
Article
Liu, Kouqi1  Ostadhassan, Mehdi1  Zou, Jie2  Gentzis, Thomas3  Rezaee, Reza2  Bubach, Bailey1  Carvajal-Ortiz, Humberto3 
[1] Univ North Dakota, Dept Petr Engn, Grand Forks, ND 58202 USA
[2] Curtin Univ, Dept Petr Engn, Perth, WA 6151, Australia
[3] Reservoir Geol Grp, Core Labs, 6316 Windfern Rd, Houston, TX 77040 USA
关键词: Bakken Shale;    Gas adsorption;    Multifractal analysis;    Heterogeneity;   
DOI  :  10.1016/j.fuel.2018.01.126
来源: Elsevier
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【 摘 要 】

Understanding pore heterogeneity can enable us to obtain a deeper insight into the flow and transport processes in any porous medium. In this study, multifractal analysis was employed to analyze gas adsorption isotherms (CO2 and N-2) for pore structure characterization in both a source (Upper-Lower Bakken) and a reservoir rock (Middle Bakken). For this purpose, detected micropores from CO2 adsorption isotherms and meso-macropores from N-2 adsorption isotherms were analyzed separately. The results showed that the generalized dimensions derived from CO2 and the N-2 adsorption isotherms decrease as q increases, demonstrating a multifractal behavior followed by f(alpha) curves of all pores exhibiting a very strong asymmetry shape. Samples from the Middle Bakken demonstrated the smallest average H value and largest average alpha(10-)-alpha(10+) for micropores while samples from the Upper Bakken depicted the highest average alpha(10-)-alpha(10+) for the meso-macropores. This indicated that the Middle Bakken and the Upper Bakken have the largest micropore and meso-macropore heterogeneity, respectively. The impact of rock composition on pore structures showed that organic matter could increase the micropore connectivity and reduce micropore heterogeneity. Also, organic matter will reduce meso-macropore connectivity and increase meso-macropore heterogeneity. We were not able to establish a robust relationship between maturity and pore heterogeneity of the source rock samples from the Bakken.

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