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010   $a3-319-43449-7
024 7 $a10.1007/978-3-319-43449-0
035   $a(CKB)3710000000837664
035   $a(EBL)4662192
035   $a(DE-He213)978-3-319-43449-0
035   $a(MiAaPQ)EBC4662192
035   $a(PPN)194804488
035   $a(EXLCZ)993710000000837664
100   $a20160831d2017      u|             0
101 0 $aeng
135   $aur|n|---|||||
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aFluid Flow in the Subsurface$b[electronic resource] $eHistory, Generalization and Applications of Physical Laws  /$fby Hui-Hai Liu
205   $a1st ed. 2017.
210  1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2017.
215   $a1 online resource (241 p.)
225 1 $aTheory and Applications of Transport in Porous Media,$x0924-6118 ;$v28
300   $aIncludes index.
311   $a3-319-43448-9 
327   $aPreface -- 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.
330   $aThis book presents a systematic attempt to generalize several fundamental physical laws related to subsurface fluid flow that are important for a number of contemporary applications in the areas of hydrogeology, reservoir engineering and rock mechanics. It also covers the history of discovering these physical laws, their respective scope of validity, and their generalizations or extensions. The physical laws discussed include Darcy?s law, Darcy-Buckingham law and Hooke?s law. Darcy?s law is the fundamental law for subsurface fluid flow. For low-permeability media, it is not always adequate because of the strong fluid?solid interaction. Though the Darcy-Buckingham law is often used for modeling subsurface multiphase flow, it is only valid under the local equilibrium condition. This condition does not hold in many cases, especially when fingering flow occurs. It is well known that subsurface fluid flow is coupled with mechanical deformation of subsurface media; in some applications, this coupling can play a dominant role. The continuum-scale elastic deformation of natural rock, however, does not always follow the traditional form of Hooke?s law. The book also presents applications of the proposed generalizations of the physical laws to several important engineering projects.
410  0$aTheory and Applications of Transport in Porous Media,$x0924-6118 ;$v28
606   $aHydrogeology
606   $aEngineering geology
606   $aEngineering?Geology
606   $aFoundations
606   $aHydraulics
606   $aGeophysics
606   $aGeology
606   $aGeotechnical engineering
606   $aFluids
606   $aHydrogeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G19005
606   $aGeoengineering, Foundations, Hydraulics$3https://scigraph.springernature.com/ontologies/product-market-codes/T23020
606   $aGeophysics/Geodesy$3https://scigraph.springernature.com/ontologies/product-market-codes/G18009
606   $aGeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17002
606   $aGeotechnical Engineering & Applied Earth Sciences$3https://scigraph.springernature.com/ontologies/product-market-codes/G37010
606   $aFluid- and Aerodynamics$3https://scigraph.springernature.com/ontologies/product-market-codes/P21026
615  0$aHydrogeology.
615  0$aEngineering geology.
615  0$aEngineering?Geology.
615  0$aFoundations.
615  0$aHydraulics.
615  0$aGeophysics.
615  0$aGeology.
615  0$aGeotechnical engineering.
615  0$aFluids.
615 14$aHydrogeology.
615 24$aGeoengineering, Foundations, Hydraulics.
615 24$aGeophysics/Geodesy.
615 24$aGeology.
615 24$aGeotechnical Engineering & Applied Earth Sciences.
615 24$aFluid- and Aerodynamics.
676   $a550
700   $aLiu$b Hui-Hai$4aut$4http://id.loc.gov/vocabulary/relators/aut$01063136
906   $aBOOK
912   $a9910254009603321
996   $aFluid Flow in the Subsurface$92530695
997   $aUNINA