Adsorption and diffusion of shale gas in kerogen matrix: Insights from molecular simulations

被引:2
作者
Zhang, Yingchun [1 ,2 ]
He, Kun [3 ]
Wang, Xiaomei [3 ]
Zhang, Xi [1 ,2 ]
Liu, Xiandong [1 ,2 ]
Lu, Xiancai [1 ,2 ]
机构
[1] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China
[2] Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Nanjing 210023, Jiangsu, Peoples R China
[3] PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Kerogen; Adsorption; Diffusion; Methane; Isotope fractionation; Molecular simulations; ISOTOPE FRACTIONATION; METHANE ADSORPTION; THERMAL MATURITY; DYNAMICS; MODEL; TRANSPORT; NANOPORES; CHEMISTRY; MIXTURES; RECOVERY;
D O I
10.1016/j.fuel.2024.134246
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The low recovery rate of shale gas highlights the necessity of understanding how it interacts with and diffuses in kerogen matrices. In this study, by using molecular simulation techniques, the adsorption and diffusion of shale gas in kerogen matrices were systematically investigated. Five kerogen models (i.e., I-A, II-A, II-B, II-C, and II-D) were constructed. I-A and II-D type kerogens were found to exhibit the lowest and highest densities, respectively, and the porosity of kerogens increased monotonically with the thermal maturity. Furthermore, a linear correlation was found between methane adsorption capacity and porosity. The diffusivity of methane in I-A type kerogen was significantly higher than that in type II kerogen, which was attributed to the flexibility of I-A kerogen. Additionally, isotope fractionation for methane diffusion was characterized and it was found that the negative isotope fractionation can be explained by the slightly higher diffusion activation energy of 13CH4. The findings presented in this study provide a molecular-level insight into methane adsorption and diffusion in kerogen and can help understand the methane-kerogen interactions in the production field.
引用
收藏
页数:9
相关论文
共 75 条
[1]   The Impact of Pore Structure on Kerogen Geomechanics [J].
Alafnan, Saad .
GEOFLUIDS, 2021, 2021
[2]   Petrophysics of Kerogens Based on Realistic Structures [J].
Alafnan, Saad .
ACS OMEGA, 2021, 6 (14) :9549-9558
[3]   Effect of Kerogen Thermal Maturity on Methane Adsorption Capacity: A Molecular Modeling Approach [J].
Alafnan, Saad ;
Solling, Theis ;
Mahmoud, Mohamed .
MOLECULES, 2020, 25 (16)
[4]  
Alavi S., 2020, Molecular Simulations: Fundamentals and Practice
[5]  
ALLEN MP, 1989, COMPUTER SIMULATIONS
[6]   Simulating the Geological Fate of Terrestrial Organic Matter: Lignin vs Cellulose [J].
Atmani, Lea ;
Valdenaire, Pierre-Louis ;
Pellenq, Roland J-M ;
Bichara, Christophe ;
Van Damme, Henri ;
van Duin, Adri C. T. ;
Ulm, Franz J. ;
Leyssale, Jean-Marc .
ENERGY & FUELS, 2020, 34 (02) :1537-1547
[7]   From cellulose to kerogen: molecular simulation of a geological process [J].
Atmani, Lea ;
Bichara, Christophe ;
Pellenq, Roland J. -M. ;
Van Damme, Henri ;
van Duin, Adri C. T. ;
Raza, Zamaan ;
Truflandier, Lionel A. ;
Obliger, Amael ;
Kralert, Paul G. ;
Ulm, Franz J. ;
Leyssale, Jean-Marc .
CHEMICAL SCIENCE, 2017, 8 (12) :8325-8335
[8]   Diffusion Behavior of Methane in 3D Kerogen Models [J].
Bin Yu, Kai ;
Bowers, Geoffrey M. ;
Loganathan, Narasimhan ;
Kalinichev, Andrey G. ;
Yazaydin, A. Ozgur .
ENERGY & FUELS, 2021, 35 (20) :16515-16526
[9]  
Bousige C, 2016, NAT MATER, V15, P576, DOI [10.1038/NMAT4541, 10.1038/nmat4541]
[10]   COMPUTER-SIMULATION USING PARTICLES - HOCKNEY,RW, EASTWOOD,JW [J].
BUNEMAN, O .
SIAM REVIEW, 1983, 25 (03) :425-426