WebOct 15, 2024 · The topics covered by this Special Issue include but are not limited to: fluid flow and heat transfer in porous media, drying technology, insulation of buildings, conventional and compact heat exchangers, design of nuclear reactors, geothermal systems, microfluidics, nanofluidics, multiphase flows, wind tunnels, turbulence modelling … WebJan 1, 2009 · @article{osti_1233817, title = {Modeling and simulation of pore-scale multiphase fluid flow and reactive transport in fractured and porous media}, author = {Meakin, Paul and Tartakovsky, Alexandre M.}, abstractNote = {In the subsurface fluids play a critical role by transporting dissolved minerals, colloids and contaminants (sometimes …
A Two-Phase Flow Simulation of Discrete-Fractured Media using …
WebMay 15, 2024 · The last decade has seen a strong increase of research into flows in fractured porous media, mainly related to subsurface processes, but also in materials … WebFeb 1, 1985 · Abstract. A multiple interacting continua (MINC) method is presented, which is applicable for numerical simulation of heat and multiphase fluid flow in multidimensional, fractured porous media. This method is a generalization of the double-porosity concept. The partitioning of the flow domain into computational volume elements is based on. the … high bnb
Modelling Flow through Fractures in Porous Media - COMSOL …
WebJan 6, 2024 · The microfluidic model can visually present the fluid flow process in porous media, ... Su et al. used a fractured 2.5D micromodel to further research the blocking effects of ... Zhu, P.; Qi, P.; Lu, J.; Huh, C.; Balhoff, M. A 2.5-D glass micromodel for investigation of multi-phase flow in porous media. Lab Chip 2024, 17, 640–646 ... WebJun 1, 2010 · Transverse and longitudinal fluid flow modelling in fractured porous media with non-matching meshes. ... According to the figure, the results agree well with those obtained by [50] with a discrete ... WebNov 1, 2024 · Section snippets Coupled Stokes–Darcy model. The flow system of interest Ω ¯ = Ω ¯ 1 ∪ Ω ¯ f ∪ Ω ¯ 2 ⊂ R n contains two porous medium domains Ω 1 and Ω 2 separated by the fracture Ω f (Fig. 1, left). The fracture is filled with an incompressible fluid having also constant viscosity and the pore space in the rock matrix Ω 1 ∪ Ω 2 is fully … how far is montgomery al from pensacola fl