Revisiting total, matric, and osmotic suction in partially saturated geomaterials

DOI10.1007/S00033-011-0168-6zbMath1255.74045OpenAlexW2071476920MaRDI QIDQ422317

Zachary C. Grasley, Kumbakonam R. Rajagopal

Publication date: 16 May 2012

Published in: ZAMP. Zeitschrift für angewandte Mathematik und Physik (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s00033-011-0168-6

zbMATH Keywords

suctiontheoretical analysispartial saturationpore pressurestemperature effects

Mathematics Subject Classification ID

Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Stefan problems, phase changes, etc. (80A22) Flows in porous media; filtration; seepage (76S05) Soil and rock mechanics (74L10) Chemically reacting flows (80A32)

Related Items (1)

The significance of pore liquid pressure and disjoining pressure on the desiccation shrinkage of cementitious materials

Cites Work

• A thermodynamical framework for chemically reacting systems
• Equilibrium of partially dried porous media influenced by dissolved species and the development of new interfaces
• A constitutive equation for nonlinear solids which undergo deformation induced microstructural changes
• A thermodynamic framework for the study of crystallization in polymers
• Mechanics of the inelastic behavior of materials. I: Theoretical underpinnings
• Toward a thermodynamics and mechanics of mixtures
• A thermodynamic theory of mixtures of fluids
• Diffusion in mixtures of elastic materials
• Effects of Holistic Nursing Course
• ON BASIC EQUATIONS FOR MIXTURES
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