Fluid flow in porous media using image-based modelling to parametrize Richards' equation

Image-based modelling is used to investigate the relationship between the pore structure and the parameters

Abstract

The parameters in Richards’ equation are usually calculated from experimentally measured values of the soil–water characteristic curve and saturated hydraulic conductivity. The complex pore structures that often occur in porous media complicate such parametrization due to hysteresis between wetting and drying and the effects of tortuosity. Rather than estimate the parameters in Richards’ equation from these indirect measurements, image-based modelling is used to investigate the relationship between the pore structure and the parameters

This works arises from the Sustainable Crop production for International Development (SCPRID) programme.

Citation

Cooper L, Daly K, Hallett P, Naveed M, Koebernick N, Bengough A, George T, Roose T (2017). Fluid flow in porous media using image-based modelling to parametrize Richards’ equation. Proc Math Phys Eng Sci. 473(2207): 20170178

Fluid flow in porous media using image-based modelling to parametrize Richards’ equation

Updates to this page

Published 22 November 2017