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

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ABHOR

Thermal Convection with LTNE,roperties of their solutions. The linear operator which arises in the LTNE equations often belongs to a special class of operators, known as symmetric operators, and this class of linear operator has special mathematical properties in the context of stability. Before we briefly discuss an important

延期

Rotating Convection with LTNE, 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

REP

Double Diffusive Convection with LTNE,bounding the fluid. If the fluid layer additionally has salt dissolved in it then there are potentially two destabilizing sources for the density difference, the temperature field and the salt field. A similar scenario could be witnessed in isothermal conditions but with two dissolved salts such as

砍伐

Vertical Porous Convection with LTNE, in a vertical layer subject to different temperatures on the vertical walls. The problem where the porous medium occupies a vertical layer subject to differential heating from one side to the other has attracted much attention. This problem has much application to insulation, such as in the area of

歹徒

歹徒

淡紫色花

絕種

MANIA

Convection in a Porous Layer with Solid Partitions, of the same thickness interleaved with . identical layers of a rigid heat conducting solid each of the same thickness, where . is an integer greater than or equal to 2. The temperatures of the upper surface of the top layer, at ., and lower surface of the bottom layer, at ., are fixed at constant v