Published September 1980 | Version v1
Report

Flow in fractured porous media

Creators

  • 1. Battelle Memorial Inst., Columbus, OH

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