Journal of Applied Mathematics
Volume 2003 (2003), Issue 7, Pages 327-364
doi:10.1155/S1110757X03205143
Abstract
A derivation of a multiple-porosity model for the flow of a single phase, slightly compressible fluid in a multiscale, naturally fractured reservoir is presented by means of recursive use of homagnetization theory. We obtain a model which generalizes the double-porosity model of Arbogast et al. (1990) to a flow system with an arbitrary finite number of scales.