Titlebook: Convection with Local Thermal Non-Equilibrium and Microfluidic Effects; Brian Straughan Book 2015 Springer International Publishing Switze

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冒失

Anisotropic Inertia Effect,ly transversely isotropic. One may expect properties like the permeability and the thermal diffusivity to vary strongly with changes of direction in a porous material. With wood or layered rocks one may expect strong permeability variation along the grain lines as opposed to directions orthogonal to

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mercenary

Resonance in Thermal Convection,reshold for the onset of convection, which in turn is of interest to the energy industry. In particular, with modern heat transfer devices being increasingly employed on a microscale there is much need to understand penetrative and resonant convection on a nanoscale. MEMS (micro-electro-mechanical-s

Brain-Imaging

Thermal Convection in Nanofluids,oparticles and the stability of the suspension and prevention of particle settlement has been achieved in the laboratory. There are many types of nanofluids but typical examples might involve a suspension of copper, Cu, copper oxide, CuO, or aluminium oxide, Al.O., in water or ethylene glycol. Other

STERN

https://doi.org/10.1007/978-3-319-13530-4Convection; Hydrodynamic Stability; Local Thermal Non-Equilibrium; Nanofluids; Slip Boundary; partial dif

STING

978-3-319-37240-2Springer International Publishing Switzerland 2015

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Lecture Notes in Networks and Systemsial configuration of the phenomenon are very small, although not exclusively so since some of the topics will be of interest in their own right at the macro scale. In particular, much attention is directed at thermal convection flow problems in a porous medium where the fluid temperature, ., may be

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出處

Blessing Leonard,Giovanni Vincenti and in the opposite direction to gravity. Before we consider the LTNE case we briefly describe thermal convection in a rotating layer with a single temperature. We begin with a layer of viscous, incompressible fluid contained in the horizontal layer between the planes . and ., such that the layer i