Author
Listed:
- Jie Zhang
(Research Institute of Unconventional Oil & Gas and Renewable Energy, China University of Petroleum (East China), Qingdao 266580, China
School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China)
- Shuangfang Lu
(Research Institute of Unconventional Oil & Gas and Renewable Energy, China University of Petroleum (East China), Qingdao 266580, China)
- Junqian Li
(Research Institute of Unconventional Oil & Gas and Renewable Energy, China University of Petroleum (East China), Qingdao 266580, China)
- Pengfei Zhang
(Research Institute of Unconventional Oil & Gas and Renewable Energy, China University of Petroleum (East China), Qingdao 266580, China
School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China)
- Haitao Xue
(Research Institute of Unconventional Oil & Gas and Renewable Energy, China University of Petroleum (East China), Qingdao 266580, China)
- Xu Zhao
(Exploration & Production Research Institute SINOPEC, Beijing 100083, China
Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Mineral, Shandong University of Science and Technology, Qingdao 266590, China)
- Liujuan Xie
(Research Institute of Unconventional Oil & Gas and Renewable Energy, China University of Petroleum (East China), Qingdao 266580, China
School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China)
Abstract
Adsorption of hydrocarbons may significantly affect hydrocarbon migration in unconventional reservoirs. Clay minerals form the primary adsorbent surfaces for hydrocarbons adsorbed in mudstone/shale. To study the adsorption properties of hydrocarbons (n-decane (C 10 H 22 ), methyl cyclohexane (C 7 H 14 ) and toluene (C 7 H 8 )) on clay minerals (i.e., cookeite, ripidolite, kaolinite, illite, illite/smectite mixed-layer, Na-montmorillonite and Ca-montmorillonite), hydrocarbon vapor adsorption (HVA) tests were conducted at 298.15 K. The results showed that (i) the adsorption amounts of C 10 H 22 , C 7 H 14 and C 7 H 8 ranged from 0.45–1.03 mg/m 2 , 0.28–0.90 mg/m 2 and 0.16–0.53 mg/m 2 , respectively; (ii) for cookeite, ripidolite and kaolinite, the adsorption capacity of C 10 H 22 was less than C 7 H 14 , which was less than C 7 H 8 ; (iii) for illite, Na-montmorillonite and Ca-montmorillonite, the adsorption capacity of C 10 H 22 was greater than that of C 7 H 8 , and the adsorption capacity of C 7 H 14 was the lowest; (iv) for an illite/smectite mixed-layer, C 7 H 14 had the highest adsorption capacity, followed by C 10 H 22 , and C 7 H 8 had the lowest capacity. Adsorption properties were correlated with the microscopic parameters of pores in clay minerals and with experimental pressure. Finally, the weighted average method was applied to evaluate the adsorption properties of C 10 H 22 , C 7 H 14 and C 7 H 8 on clay minerals in oil-bearing shale from the Shahejie Formation of Dongying Sag in the Bohai Bay Basin, China. For these samples, the adsorbed amounts of C 7 H 14 ranged from 18.03–28.02 mg/g (mean 23.33 mg/g), which is larger than that of C 10 H 22 , which ranges from 15.40–21.72 mg/g (mean 18.82 mg/g). The adsorption capacity of C 7 H 8 was slightly low, ranging from 10.51–14.60 mg/g (mean 12.78 mg/g).
Suggested Citation
Jie Zhang & Shuangfang Lu & Junqian Li & Pengfei Zhang & Haitao Xue & Xu Zhao & Liujuan Xie, 2017.
"Adsorption Properties of Hydrocarbons (n-Decane, Methyl Cyclohexane and Toluene) on Clay Minerals: An Experimental Study,"
Energies, MDPI, vol. 10(10), pages 1-14, October.
Handle:
RePEc:gam:jeners:v:10:y:2017:i:10:p:1586-:d:114688
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Cited by:
- Juan Zhao & Hongfu Fan & Qing You & Yi Jia, 2017.
"Distribution and Presence of Polymers in Porous Media,"
Energies, MDPI, vol. 10(12), pages 1-13, December.
- Yanyan Zhang & Shuifu Li & Shouzhi Hu & Changran Zhou, 2023.
"Effects of Inorganic Minerals and Kerogen on the Adsorption of Crude Oil in Shale,"
Energies, MDPI, vol. 16(5), pages 1-19, March.
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