Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

On the continuum-scale simulation of gravity-driven fingers with hysteretic Richards equation: Trucation error induced numerical artifacts

Journal Article · · Water Resources Research
OSTI ID:752074

The authors consider the ability of the numerical solution of Richards equation to model gravity-driven fingers. Although gravity-driven fingers can be easily simulated using a partial downwind averaging method, they find the fingers are purely artificial, generated by the combined effects of truncation error induced oscillations and capillary hysteresis. Since Richards equation can only yield a monotonic solution for standard constitutive relations and constant flux boundary conditions, it is not the valid governing equation to model gravity-driven fingers, and therefore is also suspect for unsaturated flow in initially dry, highly nonlinear, and hysteretic media where these fingers occur. However, analysis of truncation error at the wetting front for the partial downwind method suggests the required mathematical behavior of a more comprehensive and physically based modeling approach for this region of parameter space.

Research Organization:
Sandia National Labs., Albuquerque, NM (US); Sandia National Labs., Livermore, CA (US)
Sponsoring Organization:
US Department of Energy (US)
DOE Contract Number:
AC04-94AL85000
OSTI ID:
752074
Report Number(s):
SAND2000-0608J
Journal Information:
Water Resources Research, Journal Name: Water Resources Research
Country of Publication:
United States
Language:
English

Similar Records

Gravity-driven fingering in unsaturated fractures
Conference · Thu Jan 02 23:00:00 EST 1992 · OSTI ID:5926255

Gravity-driven fingering in unsaturated fractures
Conference · Thu Jan 02 23:00:00 EST 1992 · OSTI ID:10116073

Three-dimensional simulation of unstable gravity-driven infiltration of water into a porous medium
Journal Article · Sun Jan 06 23:00:00 EST 2013 · Journal of Computational Physics · OSTI ID:1557820