Page 302 - Introduction to Computational Fluid Dynamics
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                        APPENDIX A. DERIVATION OF TRANSPORT EQUATIONS
                                     ˙
                                     Q gen = Net volumetric heat generation within the CV,       13:6 281
                                       ˙
                                      W s = Net rate of work done by surface forces, and
                                       ˙
                                      W b = Net rate of work done by body forces.
                           Each term will now be represented by a mathematical expression.
                        Rate of Change
                        The equation for the rate of change is
                                                 o
                                           ∂(ρ m e )           V  2       p    V  2
                                       ˙               o
                                       E =         ,  e = e +     = h −     +    ,        (A.25)
                                              ∂t                2        ρ m   2
                                                                                             2
                        where e represents specific energy (J/kg), h is specific enthalpy (J/kg), and V =
                              2
                                   2
                                                         o
                          2
                        u + u + u . In the expression for e , contributions from other forms of energy
                          1   2    3
                        (potential, chemical, electromagnetic, etc.) are neglected.
                        Convection and Conduction
                        Following the convention that heat energy flowing into the CV is positive (and vice
                        versa), it can be shown that
                                                                     o
                                                           ∂     (N j,k e )
                                                  ˙                  k
                                                 Q conv =−             ,                  (A.26)
                                                               ∂x j
                        where N j,k is given by Equation A.19. Now, since all species have the same
                        velocity,
                                                 ∂
                                       ˙                                    2
                                      Q conv =−          N j,k (h k − p k /ρ k + V /2) ,  (A.27)
                                                ∂x j
                        where p k is the partial pressure of species k. After some algebra, it can be shown
                        that

                                                            o
                                                    ∂(ρ m u j e )  ∂  m    j,k  h k
                                           ˙
                                          Q conv =−           −               .           (A.28)
                                                       ∂x j           ∂x j
                           The conduction contribution is given by Fourier’s law of heat conduction, so
                        that
                                                               ∂      ∂T
                                                       ∂q j
                                              ˙
                                             Q cond =−     =       k m     .              (A.29)
                                                       ∂x j   ∂x j    ∂x j
                        Volumetric Generation
                        Two principal components of volumetric energy generation are chemical energy
                          ˙
                                                    ˙
                        (Q chem ) and radiative transfer (Q rad ). Thus,
                                                          ˙
                                                   ˙
                                                                  ˙
                                                   Q gen = Q chem + Q rad .               (A.30)
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