Mathematical Modeling for Flow and Transport Through Porous Media

. Ed(s): Dagan, Gedeon; Hornung, U.; Knabner, Peter

ISBN 10: 0792316169 / ISBN 13: 9780792316169

Published by Kluwer Academic Publishers, 1992

About this Item

A selection of papers presented at an international workshop on mathematical modelling for flow and transport, this work covers free and moving boundary problems, structured media, multiphase flow, scale problems, stochastic aspects, parameter identification and optimization problems. Editor(s): Dagan, Gedeon; Hornung, U.; Knabner, Peter. Num Pages: 302 pages, biography. BIC Classification: RBGG; TGM. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly. Dimension: 297 x 210 x 19. Weight in Grams: 609. . 1992. Reprinted from 'TRANSPORT IN POROUS MEDIA', 6:5/6. Hardback. . . . . Books ship from the US and Ireland.

Seller Inventory # V9780792316169

Bibliographic Details

• Title: Mathematical Modeling for Flow and Transport Through Porous Media
• Publisher: Kluwer Academic Publishers
• Publication Date: 1992
• Language: English
• ISBN 10: 0792316169
• ISBN 13: 9780792316169
• Binding: Hardcover
• Condition: New

About this title

Synopsis

The main aim of this paper is to present some new and general results, ap­ plicable to the the equations of two phase flow, as formulated in geothermal reservoir engineering. Two phase regions are important in many geothermal reservoirs, especially at depths of order several hundred metres, where ris­ ing, essentially isothermal single phase liquid first begins to boil. The fluid then continues to rise, with its temperature and pressure closely following the saturation (boiling) curve appropriate to the fluid composition. Perhaps the two most interesting theoretical aspects of the (idealised) two phase flow equations in geothermal reservoir engineering are that firstly, only one component (water) is involved; and secondly, that the densities of the two phases are so different. This has led to the approximation of ignoring capillary pressure. The main aim of this paper is to analyse some of the consequences of this assumption, especially in relation to saturation changes within a uniform porous medium. A general analytic treatment of three dimensional flow is considered. Pre­ viously, three dimensional modelling in geothermal reservoirs have relied on numerical simulators. In contrast, most of the past analytic work has been restricted to one dimensional examples.