Page 387 - Mechanical Engineers' Handbook (Volume 4)
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376   Cooling Electronic Equipment

                          and the Reynolds number, Re, which relates the momentum in the flow to the viscous dis-
                          sipation,
                                                              	VL
                                                          Re

                          Natural Convection
                          In natural convection, fluid motion is induced by density differences resulting from temper-
                          ature gradients in the fluid. The heat-transfer coefficient for this regime can be related to the
                          buoyancy and the thermal properties of the fluid through the Rayleigh number, which is the
                          product of the Grashof and Prandtl numbers,
                                                            2
                                                           	 gc p
                                                                  3
                                                      Ra         L 
T
                                                              k
                          where the fluid properties, 	,  , c ,  , and k, are evaluated at the fluid bulk temperature and
                                                    p
                          
T is the temperature difference between the surface and the fluid.
                             Empirical correlations for the natural convection heat-transfer coefficient generally take
                          the form
                                                h   C         n        2
                                                       k
                                                        fl
                                                       L   (Ra)    (W/m  K)                   (12)
                                                                 3
                                                                           9
                          where n is found to be approximately 0.25 for 10   Ra   10 , representing laminar flow,
                                   9
                                             12
                          0.33 for 10   Ra   10 , the region associated with the transition to turbulent flow, and
                          0.4 for Ra   10 , when strong turbulent flow prevails. The precise value of the correlating
                                      12
                          coefficient, C, depends on the fluid, the geometry of the surface, and the Rayleigh number
                          range. Nevertheless, for common plate, cylinder, and sphere configurations, it has been found
                          to vary in the relatively narrow range of 0.45–0.65 for laminar flow and 0.11–0.15 for
                          turbulent flow past the heated surface. 42
                             Natural convection in vertical channels such as those formed by arrays of longitudinal
                          fins is of major significance in the analysis and design of heat sinks and experiments for this
                          configuration have been conducted and confirmed. 4,5
                             These studies have revealed that the value of the Nusselt number lies between two
                          extremes associated with the separation between the plates or the channel width. For wide
                          spacing, the plates appear to have little influence upon one another and the Nusselt number
                          in this case achieves its isolated plate limit. On the other hand, for closely spaced plates or
                          for relatively long channels, the fluid velocity attains its fully developed value and the Nusselt
                          number reaches its fully developed limit. Intermediate values of the Nusselt number can be
                          obtained from a form of a correlating expression for smoothly varying processes and have
                          been verified by detailed experimental and numerical studies. 19,20
                             Thus, the correlation for the average value of h along isothermal vertical placed sepa-
                          rated by a spacing, z
                                                   h      576    2.873   1/2
                                                      k
                                                       fl
                                                       z  (El) 2     (El) 1 / 2               (13)
                          where El is the Elenbaas number
                                                            2
                                                                 4
                                                           	 gc z 
T
                                                                p
                                                       El
                                                               kL
                                                                fl
                          and 
T   T   T .
                                   s
                                        fl
                             Several correlations for the coefficient of heat transfer in natural convection for various
                          configurations are provided in Section 2.1.
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