DOE BES Geosciences Symposium on Fluid Flow Gaithersburg, MD, March 11–12, 2010 EFFECTIVE STRESS FOR FLUID FLOW IN ANISOTROPIC FRACTURED ROCK: ISOTROPY TO ORTHOTROPY - Rock mechanics - Document - PDFSEARCH.IO

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	DOE BES Geosciences Symposium on Fluid Flow Gaithersburg, MD, March 11–12, 2010 EFFECTIVE STRESS FOR FLUID FLOW IN ANISOTROPIC FRACTURED ROCK: ISOTROPY TO ORTHOTROPY Add to Reading List Document Date: 2015-05-26 20:38:22 Open Document File Size: 81,78 KB Share Result on Facebook Company Layered Systems / / IndustryTerm anisotropic media / granular and other anisotropic porous media / / Organization MIT / ORTHOTROPY James G. Berryman Geophysics Department Earth Sciences Division / / Person Flow Gaithersburg / Lawrence Berkeley / James G. Berryman Geophysics / / Technology ultrasound / / SocialTag Porous media Continuum mechanics Mechanics Materials Aquifers Permeability Poromechanics Porous medium Fluid dynamics Materials science

DOE BES Geosciences Symposium on Fluid Flow Gaithersburg, MD, March 11–12, 2010 EFFECTIVE STRESS FOR FLUID FLOW IN ANISOTROPIC FRACTURED ROCK: ISOTROPY TO ORTHOTROPYAdd to Reading List