000 | 03436nam a22005295i 4500 | ||
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001 | 978-3-319-04010-3 | ||
003 | DE-He213 | ||
005 | 20160302172650.0 | ||
007 | cr nn 008mamaa | ||
008 | 140219s2014 gw | s |||| 0|eng d | ||
020 |
_a9783319040103 _9978-3-319-04010-3 |
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024 | 7 |
_a10.1007/978-3-319-04010-3 _2doi |
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050 | 4 | _aQC801-809 | |
072 | 7 |
_aPHVG _2bicssc |
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072 | 7 |
_aSCI032000 _2bisacsh |
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082 | 0 | 4 |
_a550 _223 |
082 | 0 | 4 |
_a526.1 _223 |
100 | 1 |
_aGray, William G. _eauthor. |
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245 | 1 | 0 |
_aIntroduction to the Thermodynamically Constrained Averaging Theory for Porous Medium Systems _h[electronic resource] / _cby William G. Gray, Cass T. Miller. |
264 | 1 |
_aCham : _bSpringer International Publishing : _bImprint: Springer, _c2014. |
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300 |
_aXXXIV, 582 p. 12 illus., 11 illus. in color. _bonline resource. |
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336 |
_atext _btxt _2rdacontent |
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337 |
_acomputer _bc _2rdamedia |
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338 |
_aonline resource _bcr _2rdacarrier |
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347 |
_atext file _bPDF _2rda |
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490 | 1 |
_aAdvances in Geophysical and Environmental Mechanics and Mathematics, _x1866-8348 |
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505 | 0 | _aChapter 1 Elements of Thermodynamically Constrained Averaging Theory -- Chapter 2 Microscale Conservation Principles -- Chapter 3 Microscale Thermodynamics -- Chapter 4 Microscale Equilibrium Conditions -- Chapter 5 Microscale Closure for a Fluid Phase -- Chapter 6 Macroscale Conservation Principles -- Chapter 7 Macroscale Thermodynamics -- Chapter 8 Evolution Equations -- Chapter 9 Single-Fluid-Phase Flow -- Chapter 10 Single-Fluid-Phase Species Transport -- Chapter 11 Two-Phase Flow -- Chapter 12 Modeling Approach and Extensions -- Appendix A Considerations on Calculus of Variations -- Appendix B Derivations of Averaging Theorems -- Appendix C Constrained Entropy Inequality Derivations -- Index. | |
520 | _aThermodynamically constrained averaging theory provides a consistent method for upscaling conservation and thermodynamic equations for application in the study of porous medium systems.� The method provides dynamic equations for phases, interfaces, and common curves that are closely based on insights from the entropy inequality.�All larger scale variables in the equations are explicitly defined in terms of their microscale precursors, facilitating the determination of important parameters and macroscale state equations based on microscale experimental and computational analysis.�The method requires that all assumptions that lead to a particular equation form be explicitly indicated, a restriction which is useful in ascertaining the range of applicability of a model as well as potential sources of error and opportunities to improve the analysis. | ||
650 | 0 | _aEarth sciences. | |
650 | 0 |
_aGeology _xStatistical methods. |
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650 | 0 | _aMineralogy. | |
650 | 0 | _aGeophysics. | |
650 | 0 | _aThermodynamics. | |
650 | 1 | 4 | _aEarth Sciences. |
650 | 2 | 4 | _aGeophysics/Geodesy. |
650 | 2 | 4 | _aQuantitative Geology. |
650 | 2 | 4 | _aMineralogy. |
650 | 2 | 4 | _aThermodynamics. |
700 | 1 |
_aMiller, Cass T. _eauthor. |
|
710 | 2 | _aSpringerLink (Online service) | |
773 | 0 | _tSpringer eBooks | |
776 | 0 | 8 |
_iPrinted edition: _z9783319040097 |
830 | 0 |
_aAdvances in Geophysical and Environmental Mechanics and Mathematics, _x1866-8348 |
|
856 | 4 | 0 | _uhttp://dx.doi.org/10.1007/978-3-319-04010-3 |
912 | _aZDB-2-EES | ||
999 |
_c207052 _d207052 |