1997
DOI: 10.1306/522b42c1-1727-11d7-8645000102c1865d
|View full text |Cite
|
Sign up to set email alerts
|

Diffusion of Methane and Ethane Through the Reservoir Cap Rock: Implications for the Timing and Duration of Catagenesis: Discussion

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

0
1
0

Year Published

2021
2021
2023
2023

Publication Types

Select...
5

Relationship

0
5

Authors

Journals

citations
Cited by 5 publications
(2 citation statements)
references
References 30 publications
0
1
0
Order By: Relevance
“…In shale reservoirs with ultralow permeability and porosity, nanopore-throats with hydrophilic walls are normally filled with brine originating from high-salinity formation water or low-salinity hydraulic fracturing fluids, ,, leading to the critical pressure that impedes the transport of hydrocarbon. The displacement pressure, also termed breakthrough pressure or critical pressure, which refers to the pressure required for driving nonwetting fluid to break through the capillary resistance of rock and form a continuous fluid flow, could be very high in the nanopore-throat channels. , Therefore, investigations of the displacement pressure are crucial for evaluating the sealing capacity of shale as caprocks and the migration of oil in tight reserviors. Previous studies of the salinity effect ,, show that the capillary resistance is closely related to the water salinity. However, the hydrodynamical behaviors of fluids confined in nanopores are strongly influenced by fluid–pore wall interactions. Nonequilibrium molecular dynamics (NEMD) simulations have been widely utilized and proven as a promising technique for the investigation of pressure-driven fluid transport through nanochannels. …”
Section: Introductionmentioning
confidence: 99%
“…In shale reservoirs with ultralow permeability and porosity, nanopore-throats with hydrophilic walls are normally filled with brine originating from high-salinity formation water or low-salinity hydraulic fracturing fluids, ,, leading to the critical pressure that impedes the transport of hydrocarbon. The displacement pressure, also termed breakthrough pressure or critical pressure, which refers to the pressure required for driving nonwetting fluid to break through the capillary resistance of rock and form a continuous fluid flow, could be very high in the nanopore-throat channels. , Therefore, investigations of the displacement pressure are crucial for evaluating the sealing capacity of shale as caprocks and the migration of oil in tight reserviors. Previous studies of the salinity effect ,, show that the capillary resistance is closely related to the water salinity. However, the hydrodynamical behaviors of fluids confined in nanopores are strongly influenced by fluid–pore wall interactions. Nonequilibrium molecular dynamics (NEMD) simulations have been widely utilized and proven as a promising technique for the investigation of pressure-driven fluid transport through nanochannels. …”
Section: Introductionmentioning
confidence: 99%
“…Its low porosity and permeability play a very important role in the accumulation and preservation of hydrocarbons [2,3]. Currently, the sealing capacity of shale is mainly evaluated by high-pressure mercury intrusion, gas diffusion test, triaxial stress test and breakthrough pressure test [4][5][6], from the perspective of throat size, porosity, permeability, diffusion coefficient and gas breakthrough pressure [7][8][9][10]. Due to experimental limitations (such as high pressure, threshold time, relaxation time and pore size), however, these methods are deficient in some respects, for example, the destructive effects of high-pressure mercury intrusion on pore structure at the high-pressure stage and the dependence on threshold in CT scan identification [11].…”
Section: Introductionmentioning
confidence: 99%