Published September 1980
| Version v1
Report
Flow in fractured porous media
Description
The equations governing fluid flow through fractured porous media consist of two equations of motion and two continuity equations. These equations are coupled by an interaction term that represents the mass flux of fluid from the primary pores into the fractures. Numerical (finite element) solution of the governing equations was used to investigate the relative magnitude of some of the terms of the equations. The acceleration term in the equation of motion for the fractures was found to be small and for the cases investigated can be neglected. Elimination of this acceleration term allows the governing equations to be greatly simplified, a simplification that allows for the numerical solution of the governing equations on a larger region
Additional details
Publishing Information
- Imprint Title
- Proceedings of the workshop on numerical modeling of thermohydrological flow in fractured rock masses
- Journal Page Range
- p. 33-36.
- Report number
- LBL--11566
Conference
- Title
- Workshop on numerical modeling of thermohydrological flow in fractured rock masses.
- Dates
- 19 - 20 Feb 1980.
- Place
- Berkeley, CA, USA.
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 12641460
- Subject category
- S61: RADIATION PROTECTION AND DOSIMETRY;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- FINITE ELEMENT METHOD; FLUID FLOW; GEOLOGIC DEPOSITS; MATHEMATICAL MODELS; PERMEABILITY; POROUS MATERIALS; RADIOACTIVE WASTE DISPOSAL; RADIONUCLIDE MIGRATION
- Descriptors DEC
- MANAGEMENT; NUMERICAL SOLUTION; WASTE DISPOSAL; WASTE MANAGEMENT