Description and Analysis of a Multiphase Model of Saurel and Abgrall This document describes a multiphase model proposed by Saurel and Abgrall in the article “A Multiphase Godunov Method for Compressible Multifluid and Multiphase flows” [1]. The model is based on the formal theory of Drew and Passman [2] for a fluid with individual densities, pressures, and velocities for each fluid species in the mixture. The Saurel and Abgrall model is based on pressure and velocity relaxation to equilibrium values. The model imposed conservation of individual species mass, total momentum, and total energy. The description here is based on a simple generalization of the model discussed in [1] to multiple space dimensions and more than two fluid species. Notation The basic notation for the description of the fluid motion is given in Table 1. The flow consists of a mixture of N separate fluid species. Table 1 Variable N d t xi , 1 i d Description Number of fluid species. Spatial dimension. The solution time. The spatial coordinate in direction i . Volume fraction of fluid species k. In Units None None Time Length N k , 1 k N general 0 k 1 and k 1 . Here we k 1 assume the flow is saturated so None N that k 1 . k 1 N A A= k =1 k , 1 k N k Mass fraction of fluid species k . None None N w w k None k , 1 k N Micro-density of fluid species k. The quantity k is defined as the ratio of the mass of species k and the volume occupied by species k . It is assumed to be non-negative. Mass/Volume k 1 1 Variable Vk , 1 k N Description The thermodynamic specific volume of species k given byV k 1 . Units Volume/Mass k Total density of the fluid N mixture k k . The volume k 1 fractions and mass fractions are related by the formula k k k so that Mass/Volume N 0 k 1 and k 1. k 1 vk , 1 k N v k2 v ki , 1 k N , 1 i d Velocity of species k . Square of the velocity of species k defined by v k2 v k v k The i th spatial component of the velocity vector v k . The center-of-mass velocity Velocity Energy/Mass Velocity N v k k v k or v k 1 Velocity N equivalently v k v k . k 1 v i , 1 i d vk , 1 k N v ki , 1 k N , 1 i d bk , 1 k N bki , 1 k N , 1 i d The i spatial component of the velocity vector v . The relative velocity or slip of species k defined by v k v k v . th The i spatial component of the velocity slip vector v k . The body force per unit mass acting on species k . th The i spatial component of the body force per unit mass of vector b k . The center-of-mass body force per unit th Velocity Velocity Velocity Force/Mass Force/Mass N mass b k k bk or b k 1 Force/Mass N equivalently b k bk . k 1 bi , 1 i d The i spatial component of the body force per unit mass vector b . The energy body force due to fluid th Force/Mass N r interaction given by r k k v k bk k 1 N or equivalently r k k v kj bkj . k 1 2 Work/Mass Variable Pk , 1 k N Description The thermodynamic pressure of species k . The volume averaged N P pressure P k Pk . Units Pressure Pressure k 1 σ ij The composite Cauchy stress for the mixture defined by N ij P ij k k v ki v kj . Pressure k 1 Tk , 1 k N The pressure fluctuation of species k , defined by Pk Pk P . The thermodynamic specific internal energy of species k . The temperature of species k . Sk , 1 k N The specific entropy of species k . ck , 1 k N k , 1 k N The sound speed of species k . The Grüneisen exponent of species k . The mass averaged specific internal Pk , 1 k N ek , 1 k N Pressure Energy/Mass Temperature Energy/Mass/ Temperature Velocity None N energy e k k ek or e k 1 Energy/Mass N equivalently e k ek . k 1 The composite material specific internal energy given by N e e 21 k k v k v k or e k 1 Energy/mass N equivalently e e 21 k k v ki v ki . k 1 Hk , 1 k N The specific enthalpy for species k given by H k ek PkVk . The heat flux due to fluid interaction defined Energy/mass N q q j by q j k k( H k 21 v k v)k v kj k 1 or equivalent Energy*Velocity/ Volume N q j k k( H k 21 v ki v )ki v kj k 1 Tk , 1 k N Sk , 1 k N The thermodynamic temperature of species k . The thermodynamic specific entropy of species k . The dynamic compaction viscosity. 3 Temperature Entropy Energy/Temperature Time*Length/Mass Variable Description Velocity relaxation coefficient. Units Mass/(Volume*Time) Equations of Motion The equations of motion are based on the conservation of individual species mass, conservation of total momentum and energy, and relaxation to uniform strain. The system is given by k v ∇ k k Pk t A k k ∇ k k v k 0 t k k v k ∇ k k v k v k ∇ k Pk k v k P ∇ k k k b k t W k k e k 21 v k2 t ∇ k k v k e k 21 v k2 ∇ k Pk v k P v ∇ k k k v k b k . k W v vk k A (1) P Pk It is sometimes convenient to write this system using index notation (with no summing over the species index k) k k v j k Pk t x j A k k k kv kj 0 t x j k kv ki k kv ki v kj k Pk k k v ki P k k bki t x j x i W x i k k e k 21 v ki v ki t k kv kj e k 21 v ki v ki x j Pv j k Pkv kj k v j v kj k P Pk x j W A k k kv kj bkj . x j Summing the advection equation for the volume fractions over all species we obtain 4 (2) N k k 1 t N v ∇ 0 , k k 1 (3) N since by definition Pk 0 . Thus is the flow is initially saturated it will remain k 1 N saturated for all time. In the following we thus assume that k 1 . k 1 Summing the second equation corresponding to mass conservation for systems (1) or (2) we obtain the equation for conservation of total mass ∇ v 0 . t (4) This in summation form becomes kv t x j j 0. (5) The conservation of total momentum equation is obtained by summing the third equations in systems (1) and (2): v ∇ v v ∇ σ b t (6) v i v iv j ij b i . t x j x j (7) or in summation form: The conservation of total energy law is obtained by added the fourth equations from systems (1) and (2). e 21 v v ∇ v e 21 v v ∇ σv ∇ q v b r t (8) or in summation form e 21v jv t j v e i x i 1 2 v jv j 5 ijv x i j q i v j b j r . x i (9) It is important to note that even when each individual species is inviscid, the composite flow has a non-isotropic stress tensor and non-trivial heat conduction due to the interactions between species at the subgrid level. Characteristic Analysis The system (1) consists of a set of N *(3 d) coupled partial differential equations in the N *(4 d) unknowns k , k ,v ki 1 i d ,ek , and Pk . The system is closed through the individual species thermodynamic equations of state ek ek Vk ,Sk where Vk 1/ k is the specific volume, and S k is the specific entropy of species k . The pressure and temperature of the species are then given byTk e k S k ,Pk Vk e k V k . This system consists Sk of blocks of equations corresponding to the propagation of volume fractions and each fluid species that are only coupled via source terms, thus we can perform the characteristic analysis on each block separately. The first block of equations corresponding to the time advection of the volume fraction k k v j k Pk t x j A (10) is clearly in characteristic form so that the composite velocity field form a multiplicity N linearly degenerate characteristic field. The derivation of the remaining characteristics proceeds in the usual manner. First it is convenient to rewrite equation (10) in the form k k k v kj v kj k Pk t x j x j A (11) which emphasizes that changes in the k th species volume fraction are driven by velocity and pressure fluctuations from the mean values. Combining equation (11) with the continuity equation for that species we can derive the k th species specific volume update equation Vk k k t v kj Vk x j v kj j k k Pk k v k x j A x j that reduces to the standard equality between the velocity divergence and logarithm derivative of specific volume as the velocity and pressure fluctuations approach zero. 6 (12) Expanding out the momentum species equations we can derive v ki k k t v kj v ki x j P k k v ki k k bki k k Pk x x W i i (13) which again reduces to the standard single component equations as the pressure and velocity fluctuations approach zero. A somewhat long but straightforward computation using the energy equations and equations (11), (12), and (13) allow us to derive the entropy equation Sk k kTk t v kj Sk x j Pk k k j j v kj k v v k t x W j (14) We observe that equation (14) is in characteristic form so that each of the N species velocities corresponds to a linearly degenerate characteristic field. We also observe that it is fluctuations in pressure and velocity that break the thermal isolation of a fluid species. If we use the thermodynamic relation dVk 1 k c k 2 2 dPk k k c k2 Tk dSk to replace the specific volume derivative with pressure and entropy derivatives in equation (12) and use equation (14) to replace entropy derivatives with volume fraction derivatives, we obtain Pk v kj k t Pk x j j k 2 v k j j k c k2 k Pk k v kj k k c k k k v v k . t x x W j j (15) Combining equations(10),(13),(14), and (15) we get the quasi-linear system k k v j k Pk t x j A S k k k j j v kj k v v k t t x W j j Pk Pk k 2 v k k v kj k c k2 k Pk k v kj k k c k t t x x x j j j v i v i P k k k v kj k k k Pk k k v ki k k bki . x j x i x i W t k kTk v kj S k x j Pk j j k k v v k W (16) System (16) is block structured for each material species, so the characteristics for the complete multi-material equation consist of the union of the characteristics for each block. Given a spatial direction ξ 1, ,d and a characteristic speed the symbol for the system consists of a block diagonal matrix formed by the single species symbol given by the 3 d 3 d matrix 7 0 0 0 v ξ Pk v k ξ k kTk v k ξ 0 0 Mk 2 c k Pk v k ξ 0 k v k ξ k k c k2 ξ k k Pk ξT 0d d k ξT k k v k ξ Id d (17) in terms of the state representation Sk k ,Sk ,Pk , vTk . It is easy to shown that T d 2 det Mk k3 k2Tk v ξ v k ξ v k ξ c k2ξ ξ and thus the total system is hyperbolic with characteristic speeds v ξ of multiplicity N , v k ξ of multiplicity d for 1 k N and vk ξ ck ξ , 1 k N . The eigenvectors correspond to the characteristic field corresponding to the center of mass velocity are then given by v ξ r v k ξ 2 k kTk P 2 k c k2 ξ kTk Pk 0d v ξ c 2 1 P T k k k k k k l 1 0 0 0d 0 0 k v k ξ ξT (18) In order to determine the characteristic type of this field (genuinely nonlinear or linearly degenerate) we need to compute the derivative of the composite velocity with respect to N N k 1 k 1 the state variable. Using k k , v k k , and k k Pk ,Sk we find that v ξ k v ξ S k v ξ Pk v ξ v k k v k ξ T k k2 k v k ξ ck k 2 v k ξ k c k (19) k ξ Using (18) and (19) you can then calculate that for the center of mass velocity field r 0 so that this characteristic family is linearly degenerate. Just as for the single material Euler equations, we see that the eigenvectors corresponding to the velocity of the k th material field are given by 8 vk ξ 0 0 1 0 r span , , ξη 0 0 0 0 η l span 0 1 0 0 , 0 0 0 ηT (20) , ξη 0 Since v k ξ k v k ξ S k v k ξ Pk v k ξ v k 0 0 (21) 0 ξ we easily check that this characteristic family is also linearly degenerate. Finally for the k th material sonic wave families with speeds vk ξ ck ξ we get eigenvectors vk ξ ck ξ 0 0 r k c k ξ T ξ 2 2 c k 1 Pk l ck ξ k k vk ξ ck ξ (22) 0 ξ c k ξ Computing vk ξ ck ξ k vk ξ ck ξ S k vk ξ ck ξ Pk vk ξ ck ξ v k 0 c k S k c k Pk ξ 9 ξ Pk ξ Sk Gk 1 k c k (23) ξ where Gk is the fundamental derivative of gas dynamics [3, 4] for the k th material field and we compute for this family r Gk ξ which will be genuinely non-linear for nonzero Gk . 1. Saurel, R. and R. Abgrall, A Multiphase Godunov Method for Compressible Multifluid and Multiphase Flows. Jour. Comp. Phys, 1999. 150: p. 425-467. 2. Drew, D. and S. Passman, Theory of Multicomponent Fluids. 1999, New York: Springer-Verlag. 3. Thompson, P., Compressible-Fluid Dynamics. 1972, New York: McGraw-Hill. 4. Menikoff, R. and B. Plohr, The Riemann Problem for Fluid Flow of Real Materials. Rev. Mod. Phys., 1989. 61: p. 75-130. 10