2011
DOI: 10.1016/j.ijheatmasstransfer.2010.11.002
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Couette flow with frictional heating in a fluid with temperature and pressure dependent viscosity

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Cited by 11 publications
(3 citation statements)
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“…As pointed out earlier, for highly viscous fluids, the Brinkman number might not be small [30] but of order of unity or greater. Hence, from (4.20), we deduce that equation (4.29) 3 has to be changed to…”
Section: Approximationsmentioning
confidence: 85%
See 1 more Smart Citation
“…As pointed out earlier, for highly viscous fluids, the Brinkman number might not be small [30] but of order of unity or greater. Hence, from (4.20), we deduce that equation (4.29) 3 has to be changed to…”
Section: Approximationsmentioning
confidence: 85%
“…The specific entropy is then not concave and so assumption (1.1) leads also to thermodynamic instability (see also [32] from which one deduces that the speed of sound in the fluid is imaginary, a physically unrealistic situation! It must be acknowledged that, despite the physically unrealistic deductions described above, as long as the ratio between the Eckert number and the second Froude number is of the same order as the Carnot number or smaller, the approximations derived in [17,28,30] under the assumption (1.1) (and valid whenever α ref (θ M − θ m ) is small) coincide, respectively, with the Oberbeck-Boussinesq, Stokes-Oberbeck-Boussinesq and Navier-Stokes with frictional heating approximations derived in §4. In virtue of this remark, the results concerning the onset of convection and the viscous dissipation in fluids with pressure-and temperature-dependent viscosity found in [28,30,33], where the approximations are derived under the assumption (1.1), hold true.…”
Section: Discussionmentioning
confidence: 99%
“…The fluid between them follows the following governing equations (Rajagopal et al , 2010): where ρ represents the density of the fluid, v is the velocity, μ is the viscosity, k is the thermal conductivity, c is the specific heat at constant pressure, Z i is the viscous dissipation and y is the coordinate axis perpendicular to the fluid layer. Under steady state, the velocity distribution at a certain height of the fluid layer can be approximately considered as having the following linear relationship (Kavinprasad et al , 2015): where v 0 represents the linear velocity of the moving wall; δ represents the height of the fluid layer in the z direction.…”
Section: Theoretical Basismentioning
confidence: 99%