The model is based on a hybrid methodology to simulate fluid flow by combining a single continuum and discrete fracture network approaches.
This may help us establish a physically reasonable methodology to systemically assess fluid flow in soft rocks.
The philosophy of the arbitrary Lagrangian Eulerian (ALE) methodology for solving multidimensional fluid flow problems is to move the computational grid, using the flow as a guide, to improve the accuracy and efficiency of the simulation.
The developed hybrid methodology used to simulate fluid flow and rock deformation to improve the characterization of the fractured basement by simulating the pressure transient testing.
The pseudo-spectral methodology that is typically employed to simulate fluid flow in spherical geometry exhibits, among other limitations, a severe degradation of performance at high resolution.
Following the methodology developed by Lu et al. [1996. Fluid flow through basic weaves of monofilament filter cloth.
The described methodology allows for the observation of cellular responses to fluid flow.
In this article we discuss a methodology that allows the direct numerical simulation of incompressible viscous fluid flow past moving rigid bodies.
The predictive accuracy of the methodology is governed by the correspondence between the computational model of fluid flow, whose main parameters are the fluid resistances of the inlet and outlet channels, and the actual microfluidic device.
A prescribed methodology has the advantage of significantly reducing the computational time, in this case by a factor 3. Although some agreement between the methodologies can be achieved, it is important to note the effects of the fluid flow on the acoustic sources and acoustic pressure.
A methodology for simulating magmatic and metamorphic fluid production coupled with mechanical deformation, fluid flow and heat transport is presented.
