Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Kangsheng Xue"'
Publikováno v:
Water, Vol 16, Iss 19, p 2860 (2024)
The main objective of this paper is to investigate the evolution of rock fracture slug structures and decongestion strategies for natural gas extraction processes. For this purpose, the level set method was used to simulate the evolution of the slug
Externí odkaz:
https://doaj.org/article/796f8e67c9c24bc288d9fdba11083490
Publikováno v:
Water, Vol 15, Iss 23, p 4110 (2023)
Understanding the fluid pattern is of special significance for estimating the hydraulic conductivity of fractured rock masses. The nonlinearity of fluid flow in discrete fracture networks (DFNs) originates from inertial effects and is enhanced by com
Externí odkaz:
https://doaj.org/article/352a40641fee465bb797ecef66157bf6
Publikováno v:
Geofluids, Vol 2022 (2022)
Equivalent hydraulic aperture and fracture surface roughness are two significant factors affecting the fluid flow behaviors in rock fractures. To understand the role of fracture surface roughness and aperture in the fluid flow through 3D self-affine
Externí odkaz:
https://doaj.org/article/dcc9d52ad8be4c98b0f719cc839edb55
Publikováno v:
Sustainability; Volume 15; Issue 12; Pages: 9744
Geothermal recovery involves a coupled thermo-hydro-mechanical (THM) process in fractured rocks. A fluid transient equilibrium equation, considering thermal conduction, convection, and heat exchange, is established. The evolution of the reservoir per
Publikováno v:
The European Physical Journal Plus. 137
Publikováno v:
Geomechanics and Geophysics for Geo-Energy and Geo-Resources. 8
Publikováno v:
Advances in Water Resources. 175:104426
Estimating the permeability of fractured rocks using topological characteristics of fracture network
Publikováno v:
Computers and Geotechnics. 157:105337
Publikováno v:
SSRN Electronic Journal.
Publikováno v:
Physics of Fluids. 34:125114
Fluid flow regimes affect the determination of hydraulic conductivity of fractured rocks, and the critical criteria for the onset of nonlinear fluid flow transitions in discrete fracture networks (DFNs) of rocks have yet to be established. First, the