#fluid flow

Impact of permeability anisotropy misalignment on flow rates

Permeability is the most critical parameter controlling fluid flow in porous media. The general form of permeability is anisotropic but […]

Novel technique for solving advection-dominated fluid flow in anisotropic and heterogeneous porous media

Advective-dominated diffusion problems in heterogeneous and anisotropic porous media play a critical role in geoscience. These problems inform our understanding […]

Modelling fluid flow in the Glyde sub-basin

Understanding fluid flow pathways in sedimentary basins is critical for predicting the location of sediment-hosted mineral deposits. Fluid flow pathways […]