Page 301 - Introduction to Computational Fluid Dynamics
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                                                  APPENDIX A. DERIVATION OF TRANSPORT EQUATIONS
                               Under certain restricted circumstances of interest in this book, the diffusion flux
                            is given by Fick’s law of mass diffusion
                                                                    ∂ρ k
                                                         m     i,k  =− D  ,                   (A.20)
                                                                    ∂x i
                                       2
                                                               5
                            where D (m /s) is the mass diffusivity. Substituting Equations A.19 and A.20 in
                            Equation A.18, we can show that
                              ∂(ρ k )  ∂(ρ k u 1 )  ∂(ρ k u 2 )  ∂(ρ k u 3 )  ∂     ∂ρ k     ∂     ∂ρ k
                                    +         +         +          =       D      +        D
                                ∂t      ∂x 1      ∂x 2       ∂x 3    ∂x 1    ∂x 1    ∂x 2    ∂x 2
                                                                        ∂      ∂ρ k
                                                                     +       D       + R k .  (A.21)
                                                                       ∂x 3    ∂x 3
                               It is a common practise to refer to species k via its mass fraction ω k defined as
                                                         ρ k
                                                    ω k =             ω k = 1.                (A.22)
                                                         ρ m
                                                               all species
                            Using this definition, Equation A.21 can be compactly written as
                                         ∂(ρ m ω k )  ∂(ρ m u j ω k )  ∂     ∂ω k
                                                  +            =       ρ m D      + R k .     (A.23)
                                            ∂t          ∂x j      ∂x j       ∂x j
                               Note that when the mass transfer equation is summed over all species of the
                            mixture, the mass conservation equation for the bulk fluid (Equation A.5) is re-

                            trieved. This is because  R k = 0. That is, when some species are generated by
                            a chemical reaction, others are destroyed so that there is no net mass generation in
                            the bulk fluid.



                            A.5    Energy Equation
                                                                                           3
                            The first law of thermodynamics, when considered in rate form (W/m ), can be
                            written as
                                                                          ˙
                                                           ˙
                                                                               ˙
                                                                   ˙
                                                    ˙
                                               ˙
                                               E = Q conv + Q cond + Q gen − W s − W b ,      (A.24)
                            where
                                           ˙
                                           E = Rate of change of energy of the CV,
                                        ˙
                                        Q conv = Net rate of energy transferred by convection,
                                        ˙
                                        Q cond = Net rate of energy transferred by conduction,
                            5  The mass diffusivity is defined only for a binary mixture of two fluids 1 and 2 as D 12 . In mul-
                              ticomponent gaseous mixtures, however, diffusivities for pairs of species are nearly equal and a
                              single symbol D suffices for all species. Incidentally, in turbulent flows, this assumption of equal
                              (effective) diffusivities has even greater validity.
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