Other
Scientific paper
Dec 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30xsde7k&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 24, pp. SDE 7-1, CiteID 2268, DOI 10.1029/2003GL018838
Other
Physical Properties Of Rocks: Fracture And Flow, Physical Properties Of Rocks: Permeability And Porosity, Physical Properties Of Rocks: Thermal Properties, Physical Properties Of Rocks: General Or Miscellaneous, General Or Miscellaneous: New Fields (Not Classifiable Under Other Headings)
Scientific paper
The partial differential equations governing non-isothermal flow and deformation in an elastic medium with double porosity are presented. The governing equations satisfy an effective stress concept, Darcy's law, Fourier' law and the equations of Hookean thermoelasticity. The equations are derived using a systematic macroscopic approach that satisfies conservation laws applicable to balance of linear momentum, mass and energy. The Thermo-Hydro-Mechanical coupling take into account processes associated with: thermal expansion, thermal convection by moving fluid, fluid flux due to temperature gradients, heat flux due to pressure gradients, fluid and heat exchange between the two pore system, and the heat of phase compression.
Khalili Nasser
Selvadurai P. S. A.
No associations
LandOfFree
A fully coupled constitutive model for thermo-hydro-mechanical analysis in elastic media with double porosity does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with A fully coupled constitutive model for thermo-hydro-mechanical analysis in elastic media with double porosity, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and A fully coupled constitutive model for thermo-hydro-mechanical analysis in elastic media with double porosity will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-879862