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Fluid Flow in the Subsurface: History, Generalization and Applications of Physical Laws
Kategorie Beschreibung
036aXA-DE
037beng
087q978-3-319-43448-3
100 Liu, Hui-Hai
331 Fluid Flow in the Subsurface
335 History, Generalization and Applications of Physical Laws
410 Cham ; s.l.
412 Springer International Publishing
425 2017
425a2017
433 Online-Ressource (XIII, 230 p. 91 illus., 64 illus. in color, online resource)
451 Theory and Applications of Transport in Porous Media ; 28
501 Description based upon print version of record
527 Druckausg.ISBN: 978-3-319-43448-3
540aISBN 978-3-319-43449-0
700 |RBK
700 |SCI081000
700b|551.4
700c|GB1001-1199.8
750 This book presents a systematic attempt to generalize several fundamental physical laws related to subsurface fluid flow that are important for a number of contemporary applications in the areas of hydrogeology, reservoir engineering and rock mechanics. It also covers the history of discovering these physical laws, their respective scope of validity, and their generalizations or extensions. The physical laws discussed include Darcy’s law, Darcy-Buckingham law and Hooke’s law. Darcy’s law is the fundamental law for subsurface fluid flow. For low-permeability media, it is not always adequate because of the strong fluid-solid interaction. Though the Darcy-Buckingham law is often used for modeling subsurface multiphase flow, it is only valid under the local equilibrium condition. This condition does not hold in many cases, especially when fingering flow occurs. It is well known that subsurface fluid flow is coupled with mechanical deformation of subsurface media; in some applications, this coupling can play a dominant role. The continuum-scale elastic deformation of natural rock, however, does not always follow the traditional form of Hooke’s law. The book also presents applications of the proposed generalizations of the physical laws to several important engineering projects
753 Preface -- 1. Generalization of Darcy Law: Non-Darcian Liquid Flow in Low-permeability Media -- 2. Generalization of Darcy-Buckingham Law: Optimality and water flow in unsaturated media -- 3. Two-Part Hooke Model (TPHM): Theory, Validation and Applications -- 4. A Thermodynamic Hypothesis Regarding Optimality Principles for Flow Processes in Geosystems -- 5. Final Remarks
902s 210077638 Filtergesetz
902s 209071044 Poröser Stoff
902s 208920811 Fluid
902s 208943250 Grundwasser
902s 208965963 Hydraulik
902s 209206705 Strömungsmechanik
907s 209542950 Grundwasserstrom
907s 209861487 Hydrodynamische Gleichungen
907s 208965998 Hydrogeologie
907s 210058048 Wasserdurchlässigkeit
912s 208943277 Grundwasserleiter
912s 476861810 Hookesches Gesetz
912s 209952938 Permeabilität
912s 21214555X Deformation <Geologie>
917s 210077638 Filtergesetz
917s 209071044 Poröser Stoff
917s 208920811 Fluid
917s 208943250 Grundwasser
917s 208965963 Hydraulik
917s 209206705 Strömungsmechanik
922s 209542950 Grundwasserstrom
922s 209861487 Hydrodynamische Gleichungen
922s 208965998 Hydrogeologie
922s 210058048 Wasserdurchlässigkeit
927s 208943277 Grundwasserleiter
927s 476861810 Hookesches Gesetz
927s 209952938 Permeabilität
927s 21214555X Deformation <Geologie>
012 477154417
081 Liu, Hui-Hai: Fluid Flow in the Subsurface
100 Springer E-Book
125aElektronischer Volltext - Campuslizenz
655e$uhttp://dx.doi.org/10.1007/978-3-319-43449-0
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