Pages that link to "Item:Q2382516"
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The following pages link to Effective thermal conductivity of partially saturated porous rocks (Q2382516):
Displaying 11 items.
- How interface size, density, and viscosity affect creep and relaxation functions of matrix-interface composites: a micromechanical study (Q255232) (← links)
- Temperature and pressure dependence of the effective thermal conductivity of geomaterials: numerical investigation by the immersed interface method (Q364384) (← links)
- Fundamental study of thermal conduction in dry soils (Q732732) (← links)
- Effect of pore shape on effective porothermoelastic properties of isotropic rocks (Q833860) (← links)
- The effective thermal conductivity of a porous medium with interconnected particles (Q1276685) (← links)
- Equivalent microstructure problem: mathematical formulation and numerical solution (Q1625050) (← links)
- Size- and shape-dependent effective conductivity of porous media with spheroidal gas-filled inclusions (Q1794041) (← links)
- Hierarchical unsymmetrical effective medium approximations for the electrical conductivity of water-saturated porous rocks (Q1975497) (← links)
- Multiscale poro-elasticity of densifying calcium-silicate hydrates in cement paste: an experimentally validated continuum micromechanics approach (Q2295772) (← links)
- Effective thermal conductivity of transversely isotropic media with arbitrary oriented ellipsoidal inhomogeneities (Q2455474) (← links)
- Effective thermal conductivity of inhomogeneous medium containing gas‐filled inclusions (Q4977737) (← links)