Pore-Scale Simulation of Deep Shale Gas Flow Considering the Dual-Site Langmuir Adsorption Model Based on the Pore Network Model

As a key resource in the oil and gas sector, shale gas development profoundly influences the advancement of the global energy industry. Deep shale gas reservoirs, typically found at depths exceeding 3500 m, represent a significant portion of total shale gas reserves. Currently, pore network models p...

Ausführliche Beschreibung

Bibliographische Detailangaben
Veröffentlicht in:Langmuir : the ACS journal of surfaces and colloids. - 1999. - 40(2024), 43 vom: 29. Okt., Seite 22844-22855
1. Verfasser: Zhao, Chaoyang (VerfasserIn)
Weitere Verfasser: Yang, Yongfei, Sun, Hai, Zhong, Junjie, Zhang, Kai, Wang, Ke, Zhang, Lei, Yao, Jun
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2024
Zugriff auf das übergeordnete Werk:Langmuir : the ACS journal of surfaces and colloids
Schlagworte:Journal Article
LEADER 01000caa a22002652 4500
001 NLM378920103
003 DE-627
005 20241029232454.0
007 cr uuu---uuuuu
008 241016s2024 xx |||||o 00| ||eng c
024 7 |a 10.1021/acs.langmuir.4c02889  |2 doi 
028 5 2 |a pubmed24n1584.xml 
035 |a (DE-627)NLM378920103 
035 |a (NLM)39405521 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Zhao, Chaoyang  |e verfasserin  |4 aut 
245 1 0 |a Pore-Scale Simulation of Deep Shale Gas Flow Considering the Dual-Site Langmuir Adsorption Model Based on the Pore Network Model 
264 1 |c 2024 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Revised 29.10.2024 
500 |a published: Print-Electronic 
500 |a Citation Status PubMed-not-MEDLINE 
520 |a As a key resource in the oil and gas sector, shale gas development profoundly influences the advancement of the global energy industry. Deep shale gas reservoirs, typically found at depths exceeding 3500 m, represent a significant portion of total shale gas reserves. Currently, pore network models primarily simulate middle and shallow shale gas, insufficiently addressing the unique challenges posed by high-temperature and high-pressure conditions in deep shale gas formations. There is an urgent need to explore the microscale flow dynamics of deep shale gas. In this work, we use the pore network model to simulate the flow dynamics of deep shale gas, particularly under nanoconfinement conditions. The simulation integrates adsorption, slip flow, Knudsen diffusion, and bulk flow phenomena. Utilizing the dual-site Langmuir adsorption model tailored for high-temperature and high-pressure conditions enhances the accuracy of gas conductivity calculations for the adsorbed phase, thereby reflecting the specific characteristics of deep shale gas reservoirs. Moreover, this research investigates the flow characteristics of deep shale gas under varying sensitivity parameters, such as water saturation, temperature, and pressure. It explores methane flow dynamics, focusing on effective diffusion coefficients and permeability. The modified approach to calculating adsorption phase conductivity using the dual-site Langmuir adsorption model accurately captures the adsorption behaviors and characteristics of deep shale gas reservoirs 
650 4 |a Journal Article 
700 1 |a Yang, Yongfei  |e verfasserin  |4 aut 
700 1 |a Sun, Hai  |e verfasserin  |4 aut 
700 1 |a Zhong, Junjie  |e verfasserin  |4 aut 
700 1 |a Zhang, Kai  |e verfasserin  |4 aut 
700 1 |a Wang, Ke  |e verfasserin  |4 aut 
700 1 |a Zhang, Lei  |e verfasserin  |4 aut 
700 1 |a Yao, Jun  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Langmuir : the ACS journal of surfaces and colloids  |d 1999  |g 40(2024), 43 vom: 29. Okt., Seite 22844-22855  |w (DE-627)NLM098181009  |x 1520-5827  |7 nnns 
773 1 8 |g volume:40  |g year:2024  |g number:43  |g day:29  |g month:10  |g pages:22844-22855 
856 4 0 |u http://dx.doi.org/10.1021/acs.langmuir.4c02889  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_22 
912 |a GBV_ILN_350 
912 |a GBV_ILN_721 
951 |a AR 
952 |d 40  |j 2024  |e 43  |b 29  |c 10  |h 22844-22855