Microscopic analysis of macroscopic transport properties of single natural fractures using graph theory algorithms
- 1 June 1995
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 22 (11) , 1429-1432
- https://doi.org/10.1029/95gl01498
Abstract
Given an aperture distribution for a single fracture, a graph theory model has been employed to simulate the transport properties of the fracture. In the processes of imbibition and drainage, the connectivity of each phase at a particular capillary pressure can be sought out by the priority‐first search algorithm of graph theory. Then, the flow path in each phase can be identified, and flow equations can be established and solved in an optimal manner. It was observed that in a simulated rough fracture, a few flow “channels” can dominate the permeability of the whole system.This publication has 4 references indexed in Scilit:
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- Tracer movement in a single fissure in granitic rock: Some experimental results and their interpretationWater Resources Research, 1982