Page 382 - Modelling in Transport Phenomena A Conceptual Approach
P. 382

362       CHAPTER 9.  STEADY MICROSCOPIC BALANCES  WITH GEN.
                             Convection in -                                 (9.3-8)
            Substitution of Eqs. (9.3-2) and (9.3-3) into Eq. (9.3-7) yields
                                                            d2T



                                                         z-direction
                              r-direction   r-direction   Conduction   in
            Note that in the z-direction  energy is transported both by convection and conduc-
            tion.  As stated by Eq.  (2.4-8), conduction can be considered negligible with respect
            to convection when PeH  >> 1. Under these circumstances, Eq.  (9.3-8) reduces to

                                                                             (9.3-9)


               As an engineer, we axe interested in the variation of the bulk fluid temperature,
            Tb, rather than the local temperature, T. For forced convection heat transfer in a
            circular pipe of  radius R, the bulk fluid temperature defined by Eq.  (4.1-2) takes
            the form
                                          I"" Jd"  v,T  r drd6
                                     Tb =                                   (9.3-10)
                                              1" v, r drd0
            Note that while the fluid temperature, T, depends on both the radial and the axial
            coordinates, the bulk temperature, Tb, depends only on the axial direction.
               To determine the governing equation for the bulk temperature, it is necessary
            to integrate Eq.  (9.3-9) over the cross-sectional area of  the pipe, i.e.,




            Since v, # v,(z),  the integral on the left-side of Eq.  (9.3-11) can be rearranged as
                         1'"Jd" - drd6 = 1'" 1"              r drd6
                                    E
                                 v,
                                       r

                                             = 2 (rlRv,Trdrd6)              (9.3-12)
                                               dz

            Substitution of Eq. (9.3-10) into Eq.  (9.3-12) yields








                                                                            (9.3-13)
   377   378   379   380   381   382   383   384   385   386   387