TY  - JOUR
AV  - none
KW  - Biot's theory; Coupled equation; Coupled formulation; Darcy's law; Finite Element; Governing equations; Mechanics models; Mixture theory; Non equilibrium thermodynamics; Numerical results; Pore-water pressures; Thermal-osmosis; Very low permeability; Water transport
KW  -  Elasticity; Porous materials; Thermodynamic stability
KW  -  Osmosis
ID  - scholars3746
TI  - Coupled thermo-hydro-mechanical model with consideration of thermal-osmosis based on modified mixture theory
SP  - 1
N2  - A coupled formulation based on non-equilibrium thermodynamics, Biot's elasticity is derived to model thermal-osmotic flow in very low permeability rock. Darcy's law has been modified by incorporating thermal effects from the dissipation process by using standard arguments of non-equilibrium thermodynamics. The relationship of chemical potential of water and pore water pressure has been analysed. Helmholtz free energy is used to construct the structure of the mechanics model. The derived coupled equations can be validated by comparing with those from Mechanics approach. Finally, finite elements are used to solve the governing equations. The numerical results show the thermal-osmosis has an important effect on water transport in very low permeability porous media. © 2013 Elsevier Ltd. All rights reserved.
N1  - cited By 25
SN  - 00207225
Y1  - 2013///
VL  - 64
EP  - 13
UR  - https://www.scopus.com/inward/record.uri?eid=2-s2.0-84872965759&doi=10.1016%2fj.ijengsci.2012.12.005&partnerID=40&md5=1d88796d83e0a0f18159e182b4018e66
JF  - International Journal of Engineering Science
A1  - Chen, X.
A1  - Pao, W.
A1  - Li, X.
ER  -