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Earth Sciences & Geography - Geophysics & Geodesy | Introduction to the Thermodynamically Constrained Averaging Theory for Porous Medium Systems

Introduction to the Thermodynamically Constrained Averaging Theory for Porous Medium Systems

Gray, William G., Miller, Cass T.

2014, XXXIV, 582 p. 12 illus., 11 illus. in color.

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  • Self-contained introduction to the derivation of conservation, thermodynamic, and evolution equations for modeling multiphase porous media systems
  • Formulates entropy inequalities that can be used to guide the closure of governing equation systems
  • Includes detailed applications to formulate models for flow and transport consistent across scales
  • Presents a forward-looking discussion of open research problems in multi-scale porous medium systems
Thermodynamically 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.

Content Level » Research

Keywords » Averaging Theory - Groundwater - Multiphase Flow - Porous Media - Thermodynamics

Related subjects » Classical Continuum Physics - Geology - Geophysics & Geodesy

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