LEADER 05608nam 2200697 a 450 001 9910831048903321 005 20230725053016.0 010 $a1-280-66772-9 010 $a9786613644657 010 $a3-527-63671-4 010 $a3-527-63670-6 010 $a3-527-63669-2 035 $a(CKB)3460000000003449 035 $a(EBL)822723 035 $a(OCoLC)778339411 035 $a(SSID)ssj0000550580 035 $a(PQKBManifestationID)11341226 035 $a(PQKBTitleCode)TC0000550580 035 $a(PQKBWorkID)10509321 035 $a(PQKB)10238001 035 $a(MiAaPQ)EBC822723 035 $a(EXLCZ)993460000000003449 100 $a20120124d2011 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aFlow and transport in porous media and fractured rock$b[electronic resource] $efrom classical methods to modern approaches /$fMuhammad Sahimi 205 $a2nd ed. 210 $aWeinheim, Germany $cWiley-VCH$dc2011 215 $a1 online resource (735 p.) 300 $aDescription based upon print version of record. 311 $a3-527-40485-6 320 $aIncludes bibliographical references (p. 633-700) and index. 327 $aFlow and Transport in Porous Media and Fractured Rock; Contents; Preface to the Second Edition; Preface to the First Edition; 1 Continuum versus Discrete Models; 1.1 A Hierarchy of Heterogeneities and Length Scales; 1.2 Long-Range Correlations and Connectivity; 1.3 Continuum versus Discrete Models; 2 The Equations of Change; 2.1 The Mass Conservation Equation; 2.2 The Momentum Equation; 2.3 The Diffusion and Convective-Diffusion Equations; 2.4 Fluid Flow in Porous Media; 3 Characterization of Pore Space Connectivity: Percolation Theory; 3.1 Network Model of a Porous Medium 327 $a3.2 Percolation Theory3.2.1 Bond and Site Percolation; 3.2.2 Computer Simulation and Counting the Clusters; 3.2.3 Bicontinuous Porous Materials; 3.3 Connectivity and Clustering Properties; 3.4 Flow and Transport Properties; 3.5 The Sample-Spanning Cluster and Its Backbone; 3.6 Universal Properties; 3.7 The Significance of Power Laws; 3.8 Dependence of Network Properties on Length Scale; 3.9 Finite-Size Effects; 3.10 Random Networks and Continuum Models; 3.11 Differences between Network and Continuum Models; 3.12 Porous Materials with Low Percolation Thresholds 327 $a3.13 Network Models with Correlations3.14 A Glance at History; 4 Characterization of the Morphology of Porous Media; 4.1 Porosity; 4.2 Fluid Saturation; 4.3 Specific Surface Area; 4.4 The Tortuosity Factor; 4.5 Correlations in Porosity and Pore Sizes; 4.6 Surface Energy and Surface Tension; 4.7 Laplace Pressure and the Young-Laplace Equation; 4.8 Contact Angles and Wetting: The Young-Dupre? Equation; 4.9 The Washburn Equation and Capillary Pressure; 4.10 Measurement of Capillary Pressure; 4.11 Pore Size Distribution; 4.12 Mercury Porosimetry; 4.12.1 Pore Size Distribution 327 $a4.12.2 Pore Length Distribution4.12.3 Pore Number Distribution; 4.12.4 Pore Surface Distribution; 4.12.5 Particle Size Distribution; 4.12.6 Pore Network Models; 4.12.7 Percolation Models; 4.13 Sorption in Porous Media; 4.13.1 Classifying Adsorption Isotherms and Hysteresis Loops; 4.13.2 Mechanisms of Adsorption; 4.13.3 Adsorption Isotherms; 4.13.4 Distributions of Pore Size, Surface, and Volume; 4.13.5 Pore Network Models; 4.13.6 Percolation Models; 4.14 Pore Size Distribution from Small-Angle Scattering Data; 4.15 Pore Size Distribution from Nuclear Magnetic Resonance 327 $a4.16 Determination of the Connectivity of Porous Media4.17 Fractal Properties of Porous Media; 4.17.1 Adsorption Methods; 4.17.2 Chord-Length Measurements; 4.17.3 The Correlation Function Method; 4.17.4 Small-Angle Scattering; 4.17.5 Porosity and Pore Size Distribution of Fractal Porous Media; 5 Characterization of Field-Scale Porous Media: Geostatistical Concepts and Self-Affine Distributions; 5.1 Estimators of a Population of Data; 5.2 Heterogeneity of a Field-Scale Porous Medium; 5.2.1 The Dykstra-Parsons Heterogeneity Index; 5.2.2 The Lorenz Heterogeneity Index 327 $a5.2.3 The Index of Variation 330 $aIn this standard reference of the field, theoretical and experimental approaches to flow, hydrodynamic dispersion, and miscible displacements in porous media and fractured rock are considered. Two different approaches are discussed and contrasted with each other. The first approach is based on the classical equations of flow and transport, called 'continuum models'. The second approach is based on modern methods of statistical physics of disordered media; that is, on 'discrete models', which have become increasingly popular over the past 15 years. The book is unique in its scope, since (1) the 606 $aPorous materials$xMathematical models 606 $aTransport theory$xMathematical models 606 $aGroundwater flow$xMathematical models 606 $aRocks$xPermeability$xMathematical models 615 0$aPorous materials$xMathematical models. 615 0$aTransport theory$xMathematical models. 615 0$aGroundwater flow$xMathematical models. 615 0$aRocks$xPermeability$xMathematical models. 676 $a530.138 676 $a530.4/15 676 $a530.415 700 $aSahimi$b Muhammad$021514 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910831048903321 996 $aFlow and transport in porous media and fractured rock$91418792 997 $aUNINA