Sentence examples for media flow simulation from inspiring English sources
Therefore, the method of MD used in fluid solid interaction force calculation incorporated into LBM is reasonable in porous media flow simulation.
Such a synchronous calculation method is extremely time-consuming in porous media flow simulation because of the large amount of calculation of MD simulation on both gas liquid and rock fluid interfaces.
In addition, the proposed method shows very low sensitivity to mesh orientation, in contrast with classical finite volume approximation used in porous media flow simulations.
Several numerical results on 1D and 2D test-cases of interest for flow simulation in porous media are presented, some of them exhibiting sharp contrasts in diffusion coefficients.
Discrete Element Method (DEM) simulations of dry media flow in a pilot-scale tower mill are performed for four cases with different shaped grinding media, in order to understand how flow and energy utilisation within a stirred mill depend on media shape.
This paper introduces a new approach to construct an efficient reduced order model for fluid flow simulation and optimization in porous media.
We present a new approach to the simulation of gravity-driven viscous fingering instabilities in porous media flow.
The dual porosity/permeability approach has a lot of limitations which include (1) the fluid distribution within the matrix blocks remains constant during the simulation period, (2) the model cannot be applied to disconnected and discrete fractured (oriented fractures) media and a small number of large scale fractures can be considered for flow simulation.
The limitations of dual-porosity/permeability approach are as follow: (1) the fluid distribution within the matrix blocks remains constant during the simulation period, (2) the model cannot be applied to disconnected and discrete fratured (oriented fractures) media and (3) a small number of large-scale fractures can be considered for flow simulation.
We present the first simulation of linked turbulent-oscillatory flow of the water column, porous media flow, and solute transport in the sediment with oxygen consumption, nitrification, denitrification, and ammonification, informed by field- and/or experimentally-derived parameters.
