Page 225 - Introduction to Computational Fluid Dynamics
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P1: IWV
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            0521853265c06
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                               10       0 521 85326 5           2D CONVECTION – COMPLEX DOMAINS
                                          OUTER (COLD)           Ra = 4.8 × 10 4
                                8                               ∈/L = 0.652

                                6
                              K eq                                  INNER (HOT)

                                4



                                2



                                0
                                 0             50           100           150
                                                                    Θ
                            Figure 6.24. K eq versus θ for natural convection in an eccentric annulus.


                            in this region. It must be mentioned, however, that the results with quadrilateral
                            meshes compare extremely favourably with previous curvilinear grid predictions
                            [32, 58]. It is for this reason that many CFD analysts prefer to use quadrilateral
                            elements near curved surfaces while still employing triangular elements away
                            from such surfaces. Thus, they prefer to use mixed elements for the domain as
                            a whole.
                               Figure 6.25 shows the vector plots on the two meshes. It is seen that there is
                            a strong upward flow near the hot inner cylinder where density is lower. Mass
                            conservation, however, requires that circulation be set up with a downwards flow
                            neartheoutercylinder.Thereis,however,aregionofweakcontrarotatingcirculation


                               TRIANGULAR                QUADRILATERAL







                                                                          Figure 6.25. Vector plots for natural
                                                                          convection in an eccentric annulus.
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