| Mathematical Modeling for Flow and Transport Through Porous Media 1991 Edition Contributor(s): Dagan, Gedeon, Hornung, Ulrich, Knabner, Peter |
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ISBN: 0792316169 ISBN-13: 9780792316169 Publisher: Springer OUR PRICE: $161.49 Product Type: Hardcover Published: January 1992 Annotation: This book contains a selection of articles presented at an International Workshop on Mathematical Modeling for Flow and Transport Through Porous Media'. The major topics of the meeting were free and moving boundary problems, structured media, multiphase flow, scale problems, stochastic aspects, parameter identification and optimization problems. The volume also represents a few contributions on the incorporation of chemical and biological processes in mathematical models for transport in porous media. The book is directed at researchers active in porous media, mathematical modeling, petroleum and geotechnical engineering and environmental sciences. |
| Additional Information |
| BISAC Categories: - Science | Earth Sciences - Geology - Mathematics | Applied - Science | Mechanics - Fluids |
| Dewey: 551.490 |
| LCCN: 91046824 |
| Physical Information: 0.87" H x 6.28" W x 9.7" (1.39 lbs) 298 pages |
| Descriptions, Reviews, Etc. |
| Publisher Description: 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. |