A.1.5 Second axiom of thermodynamics
A.1.5.1 Entropy inequality for the whole system
The use of the entropy inequality to obtain governing equations is demon-strated in the following. It is shown how Fick's law can be derived from the classical denition of chemical potentialµ, with a specic choice of Helmholtz free energyψ. Consider the entropy inequality for the case with a single tem-perature for the whole system, as
ρDη
Dt ≥ −div (h/θ) +ρr/θ (A.1.171) where the entropy inux vectorhcan be expressed as (A.1.168) and (A.1.107) to yield the form
ρDη
Dt ≥ −div q/θ− XN
j=1
ρj
θ −TTj/ρj +ψj+ 12u2jI uj
!
+ρr/θ (A.1.172) Using the denition of the chemical potentialKjin (A.1.165) reduce (A.1.172) to
ρDη
Dt ≥ −div q/θ− XN
j=1
ρj
θ Kj +12u2jI uj
!
+ρr/θ (A.1.173) The chemical potential Kj is assumed simplied as Kj = µjI, using this in (A.1.173) and rewrite (A.1.173) in terms of the temperature θ, for further use, yields
θρDη
Dt ≥ −θdiv 1 θ q−
XN
j=1
ρj µj+ 12u2j uj
!!
+ρr (A.1.174) The last term in (A.1.174) is found in the energy balance for the system (A.1.113) and inserting this yields
θρDη
Dt −ρDe
Dt ≥ −θdiv 1 θ q−
XN
j=1
ρj µj+ 12u2j uj
!!
−trTL
+ divq− XN
j=1
ρjuj·bj (A.1.175) The terms divq and θdiv qθ
in (A.1.175) can be rewritten as θdivq
θ
=−q
θ ·grad (θ) + divq (A.1.176)
Inserting (A.1.176) in (A.1.175), yields θρDη
Dt −ρDe
Dt ≥ θdiv 1 θ
XN
j=1
ρj µj+ 12u2j uj
!!
−trTL
+q
θ ·grad (θ)− XN
j=1
ρjuj·bj (A.1.177) For the further rewriting of (A.1.177) consider the following relation θdiv 1
θ XN
j=1
ρj µj +12u2j uj
!!
=θ XN
j=1
ρjuj ·grad 1
θ µj +12u2j +
XN
j=1
µj +12u2j
div (ρjuj) (A.1.178) and the mass balance (A.1.47) multiplied by µj+ 12u2j
, which is ρ
XN
j=1
Dcj
Dt µj +12u2j
= − XN
j=1
µj +12u2j
div(ρjuj)
+ XN
j=1
µj+ 12u2j ˆ
cj (A.1.179) Substituting the rst term on the right-hand side of (A.1.177) in (A.1.178) and substituting the last term on the right-hand side of (A.1.178) in (A.1.179), yields the inequality
θρDη
Dt −ρDe Dt +ρ
XN
j=1
Dcj
Dt µj +12u2j
≥ XN
j=1
ρjuj ·
θgrad 1
θ µj +12u2j
−bj
+ XN
j=1
µj +12u2j ˆ
cj −trTL+q
θ ·grad (θ) (A.1.180) For future use consider the relation between the internal energy e and the inner internal energy eI, as shown in (A.1.104), with the expansion u2j = uj·uj. The material derivative of the internal energy DeDt in (A.1.180) is
De
Dt = DeI Dt + 1
2 XN
j=1
Dcj Dt u2j +
XN
j=1
cjDuj
Dt ·uj (A.1.181)
Substituting (A.1.181) into (A.1.180) and using the derivative of (A.1.163) for the inner internal energy eI yields the sought entropy inequality form
0≤ρ −ηDθ
Dt − DψI Dt +
XN
j=1
Dcj Dt µj
!
− XN
j=1
ρjuj ·
θgrad 1
θ µj +12u2j
−bj +Duj Dt
− XN
j=1
µj+ 12u2j ˆ
cj+ trTL−q
θ ·grad (θ) (A.1.182)
A.2 Mixture theory for multispecies in multi phases
The following section will show a detailed review of the derivation of multi-phase and multi-constituent mixture theory also referred to as hybrid mixture theory (HMT). Consider a mixture of R continuous bodies B1, ...BR in a three dimensional physical space, with the possibility of the dierent bodies to occupy common physical space. As a result of thisXaj andXbjare allowed to occupy the the same spatial position in the space.
The notation of the derivatives is extended compared to the single phase mixture in order to include multiple phases. The velocity of the constituents, the phases and the whole mixture are dened as
x0αj = ∂χαj Xαj, t
∂t ; x0α = ∂χα(Xα, t)
∂t ; x0 = ∂χ(X, t)
∂t (A.2.1) The material time derivatives are also extended to include multiple phases whereΓ is an arbitrary property. The material time derivative following the j constituent in the α phase is
Dαj(Γ) Dt = ∂Γ
∂t +grad(Γ)x0αj (A.2.2) The material time derivative following the α phase is
Dα(Γ) Dt = ∂Γ
∂t +grad(Γ)x0α (A.2.3) The material time derivative for the whole mixture is given as
D(Γ) Dt = ∂Γ
∂t +grad(Γ)x0 (A.2.4)
The diusion velocity is dened in two levels, one for the constituents with respect to a phase and one for the phases with respect to the whole mixture, these are dened as
uαj =x0αj−x0α; uα =x0α−x0 (A.2.5) The denitions of the material derivatives and the diusion velocities, leads to the following relations between the material derivatives
(a) : Dαj(Γ)
Dt −Dα(Γ)
Dt =grad(Γ)uαj (b) : Dα(Γ)
Dt − D(Γ)
Dt =grad(Γ)uα
(A.2.6)
which is used in the the following derivations.
The dierence between describing multiple-phases and multiple-species is that a clear boundary exist between phases, whereas the species do not have clear physical boundaries. In HMT a volume ratio εα of the phases α in a bodyB is dened as
εα = dvα
dv (A.2.7)
where va is the volume of the phase α and v is the volume of the whole mixture. The denition (A.2.7) implies that
XN
α=1
εα = 1 (A.2.8)
must be satised. The density of the whole mixture determined from the summation of the phase masses dm = PN
α=1ραdvα is the mass of the total mixture, determines as
dm=ρdv= XM
α=1
ραdvα (A.2.9)
which yields the density of the whole mixture as ρ=
XM
α=1
εαρα (A.2.10)
The density of the whole mixture is described by summation of the den-sities of the phases, recall from Sec. A.1.1 that the density of a phase is described by the summation of densities of the species, see equation (A.1.19)
and repeated here with the phase indexα andj = 1...N as the total number of species in the phase
ρα = XN
j=1
ραj (A.2.11)
The equations (A.2.10) and (A.2.11) relates the phases and species to the mixture.
A.2.1 Mass balance
The mass balance postulate for an M - phase and N - species mixture is given as
∂
∂t ˆ
Ω
εαραjdv=−
˛
∂Ω
εαραjx0αj ·ds+ ˆ
Ω
ˆ
rαj+ ˆcαj
dv (A.2.12) where rˆαj is the mass exchange term between the phases. Using the diver-gence theorem for the rst term on the right hand side of (A.2.12), yields the local form of mass balance as
∂εαραj
∂t +div
εαραjx0αj
= ˆrαj+ ˆcαj α = 1, ..., M j = 1, .., N (A.2.13) The local form of the mass balance for the phase α given as
∂εαρα
∂t +div(εαραx0α) = ˆrα (A.2.14) where the summation of the mass exchange termrˆαj yields the left-hand side of (A.2.14)
ˆ rα =
XN
j=1
ˆ
rαj (A.2.15)
Summation of the constituents in (A.2.13), together with (A.1.19) and (A.1.22) enables the comparison of (A.2.13) and (A.2.14), Using (A.2.15) yeilds the summation of the chemical interactions in the α phase as
XN
j=1
ˆ
cαj = 0 (A.2.16)
which is equal to the result obtained in (A.1.43) for the single phase system.
The further derivation to include multiple phases in the mixture is similar to
the constituent derivation. The postulate for the mass balance of the mixture
is ∂ρ
∂t +div(ρx0) = 0 (A.2.17) summation of (A.2.14), over the phases and use
x0 = 1 ρ
XR α=1
ραx0α(x, t) (A.2.18) with (A.2.8), (A.2.10) and nally compare with (A.2.17), yields
XN
α=1
ˆ
rα = 0 (A.2.19)
With the results in (A.2.16) and (A.2.19), it is shown that a summation over the constituents and the phases yields the result for the mixture as a whole.
As described earlier, it is convenient to work with the concentrations of the species due to the fact no direct boundary exist between the species. The mass balance for a single phase written in terms of species concentrations is given in (A.1.47) and extended in the following to include multiple-phases.
The equation (A.2.13) written in terms of the diusion velocity (A.1.23), yields
∂εαραj
∂t +div εαραjuαj
+div εαραjx0α
= ˆrαj + ˆcαj (A.2.20) The rst term on the left-hand side of (A.2.20) written in terms of the species concentration,cαj, is
∂εαραj
∂t = ∂εαcαjρα
∂t =cαj∂εαρα
∂t +εαρα∂cαj
∂t (A.2.21)
The divergence product rule used on the third term in (A.2.20) together with (A.1.20) gives the result
div cαjεαραx0α
=cαjdiv(εαραx0α) +εαραx0αgradcαj (A.2.22) Inserting (A.2.21) and (A.2.22) into (A.2.20) and collect the terms including cαj, yields
ˆ
rαj+ ˆcαj = cαj
∂εαρα
∂t +div(εαραx˙α)
+εαρα∂cαj
∂t +div εαραjuαj
+εαραx˙αgradcαj (A.2.23)
where the mass balance for the phase (A.2.14) is identied in the square bracket. Using (A.1.33) with Γ =cαj simplies (A.2.24) to
εαραDαcαj
Dt +div εαραjuαj
= ˆrαj + ˆcαj −cαjrˆα (A.2.24) which is the material derivative of the mass balance for the species, expressed in terms of the diusion velocity and the concentration of the species.
The mass balance for the phase can be rewritten in terms of the diusion velocity of the phase, using Γ =εαρα in (A.2.3) to obtain
Dα(εαρα)
Dt = ∂εαρα
∂t +grad(εαρα)x0α (A.2.25) and the identity
div(εαραx0α) = εαραdiv(x0α) +grad(εαρα)x0α (A.2.26) Combining (A.2.25) and (A.2.26) with (A.2.14), yields
Dα(εαρα)
Dt +εαραdiv(x0α) = ˆrα (A.2.27) The equation (A.2.27) written in terms of the diusion velocity, with respect to the whole mixture is
D(εαρα)
Dt +div(εαραuα) +εαραdiv(x0) = ˆrα (A.2.28) The mass balance for the whole mixture is obtained by using ρin (A.2.4) to get
D(ρ) Dt = ∂ρ
∂t +grad(ρ)x0 (A.2.29)
and using the identity
div(ρx0) = ρdiv(x0) +grad(ρ)x0 (A.2.30) Combining (A.2.29) and (A.2.30) yields the mass balance of the whole mix-ture, that is
D(ρ)
Dt +ρdiv(x0) = 0 (A.2.31)
A.2.2 Momentum balance
The momentum balance for a mixture, withαphases andj species is derived.
Consider a system ofα phases and j species which expands the postulate of momentum balance (A.1.48) to include momentum gain for the j species from other phases in the mixture by ˆtαj. The local form of the momentum balance is
∂
εαjραjx0αj
∂t = −div
εαjραjx0αj⊗x0αj
+div εαjTαj
+εαjραjbαj +ˆtαj + ˆpαj + ˆcαjx0αj + ˆrαjx0αj (A.2.32) where the mass balance (A.2.13) can be identied by similar mathematical steps as shown from (A.1.53) to (A.1.55) and therefore (A.2.25) reduces to
εαραjDαjx0αj
Dt =div εαTαj
+εαραjbαj + ˆtαj+ ˆpαj (A.2.33) The local postulate for the momentum balance of the phases is dened as
εαραDαx0α
Dt =div(εαTα) +εαραbα+ ˆtα (A.2.34) Summation over the species of (A.2.33) yields
XN
j=1
εαραjDαjx0αj Dt =
XN
j=1
div εαTαj
+εαραjbαj + ˆtαj+ ˆpαj
(A.2.35) where the inner stress tensorTI,α of the α phase is dened as
TI,α= XN
j=1
Tαj (A.2.36)
and the body force for the phase is dened as bα = 1
ρα XN
j=1
ραjbαj (A.2.37)
Inserting (A.2.36) and (A.2.37) into (A.2.35), yields XN
j=1
εαραjDαjx0αj
Dt =div(εαTI,α) +εαραbα+ XN
j=1
ˆtαj + XN
j=1
pˆαj (A.2.38)
General relation 2:
A general relation for a arbitrary property Γ(x, t) is shown in order to com-pare the summation of the species (A.2.38) to the postulate of the phase (A.2.34). Consider the property Γ(x, t) and assume that the relation be-tween the species level and the phase level is described by
Γα = 1 ρα
XN
j=1
ραjΓαj = XN
j=1
cαjΓαj (A.2.39) The material time derivative of the general property is
DαΓα Dt =
XN
j=1
Dα cαjΓαj
Dt =
XN
j=1
"
ΓαjDα cαj
Dt +cαjDα Γαj Dt
#
(A.2.40) For the further derivation, consider (A.2.6)-(a) with Γ = Γαj which yields the time derivative of the last term in the square brackets in (A.2.40). Mul-tiplying (A.2.40) by εαρα, shows that a part of the rst term in the square brackets is equal to the mass balance shown in (A.2.24). Inserting these relation into (A.2.40) yields the form
εαραDαΓα
Dt =εαρα XN
j=1
"
ΓαjDα cαj
Dt +cαjDα Γαj Dt
#
= XN
j=1
"
ΓαjεαραDα cαj
Dt +εαραcαj
Dαj(Γαj)
Dt −grad(Γαj)uαj
#
= XN
j=1
εαραcαjDαj(Γαj)
Dt −εαραcαjgrad(Γαj)uαj
−Γαjdiv εαραjuαj
+ Γαj ˆrαj+ ˆcαj−cαjrˆα
(A.2.41) The divergence term in (A.2.41) is rewritten by the identity
div εαραjΓαjuαj
=εαραjgrad Γαj
uαj+ Γαjdiv εαραjuαj
(A.2.42) Combining (A.2.41) and (A.2.42) yields the desired nal relation as
εαραDαΓα
Dt =
XN
j=1
εαραcαjDαj(Γαj)
Dt −div εαραjΓαjuαj +Γαj rˆαj+ ˆcαj−cαjˆrα
(A.2.43)
Using the general relation (A.2.43), with Γ =x0, yields εαραDαx0α
Dt =
XN
j=1
εαραcαjDαj(x0αj)
Dt −div εαραjx0αj ⊗uαj +x0αj rˆαj + ˆcαj −cαjrˆα
(A.2.44) Applying the diusion velocity for the j'th species, x0αj = uαj +x0α in the divergence term of (A.2.44) yields
εαραDαx0α
Dt =
XN
j=1
εαραcαjDαj(x0αj) Dt −div
XN
j=1
εαραju0αj⊗uαj
−div XN
j=1
εαραjuαj
⊗x0α+ XN
j=1
ˆ
rαj + ˆcαj −cαjrˆα x0α
+ XN
j=1
ˆ
rαj+ ˆcαj −cαjrˆα
uαj (A.2.45)
The fact that PN
j=1(ραjuαj) = 0 is used to reduce (A.2.45) further, which eliminates the second divergence term in (A.2.45). Furthermore, it is noted that PN
j=1 rˆαj + ˆcαj −cαjrˆα
= 0 is obtained for the mass balance and the fact thatPN
j=1cαj = 1, which yields a reduced form of (A.2.45), as εαραDαx0α
Dt =
XN
j=1
εαραcαjDαj(x0αj) Dt −div
XN
j=1
εαραjuαj ⊗uαj
+ XN
j=1
ˆ
rαj + ˆcαj −cαjrˆα
uαj (A.2.46)
by substituting the rst term on right-hand side of (A.2.46) with (A.2.38), to get
εαραDαx0α
Dt = div εαTI,α− XN
j=1
εαραju0αj⊗uαj!
+εαραbα
+ XN
j=1
ˆtαj+ XN
j=1
ˆ pαj +
XN
j=1
ˆ
rαju0αj + XN
j=1
ˆ cαju0αj
−rˆα ρα
XN
j=1
ραju0αj (A.2.47)
where the last term is eliminated by PN
j=1(ραjuαj) = 0 with the use of the expansion ofcαj.
The momentum balance for the species (A.2.47) and the phase (A.2.34) are compatible which yields the criteria
εαTα =εαTI,α− XN
j=1
εαραjuαj ⊗uαj
(A.2.48)
ˆtα = XN
j=1
ˆtαj + XN
j=1
ˆ
rαjuαj (A.2.49)
and
XN
j=1
ˆ pαj+
XN
j=1
ˆ
cαjuαj = 0 (A.2.50) where the second order tensor ραju0αj⊗u0αj is the so-called Reinholds stress tensor.
A similar approach is used to show that the summation of the phases is compatible with the postulate for the whole mixture. The local postulate for the momentum balance of the whole mixture is
ρDx0
Dt =divT+ρb (A.2.51)
Direct denition for summations over the phases are given for the stress tensor and the body force as
TI = XN
α=1
εαTα (A.2.52)
and
b= 1 ρ
XN
α=1
εαραbα (A.2.53)
where (A.2.8) is used. By use of the denitions (A.2.52) and (A.2.53) in (A.2.34) yields
XN
α=1
εαραDαx0α
Dt =divTI+ρb+ XN
α=1
ˆtα (A.2.54)
General relation 3:
A relation similar to (A.2.43), is established between the phase description an the whole mixture description. First consider the arbitrary variable Γ, with the denition
ρΓ = XN
α=1
εαραΓα (A.2.55)
The material derivative of (A.2.55) with respect to the mixture is D(ρΓ)
Dt = XN
α=1
ΓαD(εαρα)
Dt +εαραD(Γα) Dt
(A.2.56) The rst term on the left-hand side of (A.2.56) is (A.2.28), substituting this and using (A.2.6)-(b) with Γ = Γα, yields
D(ρΓ)
Dt =
XN
α=1
Γα(−div(εαραuα)−εαραdiv(x0) + ˆrα) +εαρα
Dα(Γα)
Dt −grad(Γα)uα
(A.2.57) The rst divergence term and the gradient term on the left-hand side, is equivalent to the divergence of the product of the variables
div(εαραΓαuα) =εαραgrad(Γα)uα+ Γαdiv(εαραuα) (A.2.58) Substituting (A.2.58) into (A.2.57), yields
D(ρΓ)
Dt =
XN
α=1
−div(εαραΓαuα)−εαραΓαdiv(x0) +Γαrˆα+εαραDα(Γα)
Dt
(A.2.59) Applying the product rule to the right-hand side of (A.2.59) and by using PN
α=1εαραΓαdiv(x0) = ρΓdiv(x0), show that the mass balance for the whole mixture (A.2.31) is identied in the below square brackets, that is
Γ
D(ρ)
Dt +ρdiv(x0)
+ρD(Γ) Dt =
XN
α=1
−div(εαραΓαuα)
+ Γαrˆα+εαραDα(Γα) Dt
(A.2.60)
which reduce (A.2.60) to ρD(Γ)
Dt =−div XN
α=1
(εαραΓαuα) + XN
α=1
Γαrˆα+ XN
α=1
εαραDα(Γα)
Dt (A.2.61) Using the general relation (A.2.61) with Γ =x0and the denition of the diusion velocity for the phase x0α =uα+x0, yields
ρD(x0)
Dt = −div XN
α=1
(εαραuα⊗uα)−div XN
α=1
(εαραuα)⊗x0
+ XN
α=1
ˆ rαuα+
XN
α=1
ˆ rαx0+
XN
α=1
εαραDα(x0α)
Dt (A.2.62)
The relation between the momentum for the whole mixture and the summa-tion of the momentum of the phases is established in (A.2.62). The second di-vergence term in (A.2.62) is eliminated by the denitionPN
α=1(εαραuα) = 0 and it is shown by the compatible mass balance terms that PN
α=1ˆrα = 0. Furthermore, combining (A.2.62) and (A.2.54) reduces (A.2.62) to
ρD(x0) Dt =div
XN
α=1
(Tα−εαραuα⊗uα) +ρb+ XN
α=1
ˆtα+ XN
α=1
ˆ
rαuα (A.2.63) Comparing (A.2.63) with (A.2.51) show that
T= XN
α=1
(Tα−εαραuα⊗uα) (A.2.64)
and XN
α=1
ˆtα+ XN
α=1
ˆ
rαuα = 0 (A.2.65)
A.2.3 Angular momentum balance
The angular momentum is derived for the whole mixture in Sec. A.1.3, where it is shown that the stress tensor must be symmetric T=TT and also that the inner stress tensor must be symmetric TI = TIT. Since the symmetry condition is decduced from the whole mixture, then it is directly transferable to the multi-phase and multi-species approach. The summation over the species yields
XN
j=1
Mαj = XN
j=1
Tαj −TT
αj
= 0 (A.2.66)
and with summation over the phases yields XN
α=1
XN
j=1
Mαj = XN
α=1
XN
j=1
Tαj−TT
αj
= 0 (A.2.67)
A.2.4 Energy balance
Energy balance postulates are given in Sec. A.2.4.2 where compatible ver-sions of the postulates between the whole mixture, the phases and the species are obtained. The compatible versions is deduced with help from, among other things, relations given in Sec. A.2.4.1.
A.2.4.1 Denitions for energy balances
The relation for summation of the external heat rα and the inner internal energy eI,α for the α phase is
rα = 1 ρα
XN
j=1
ραjrαj; eI,α= 1 ρα
XN
j=1
ραjeαj (A.2.68) The internal energy of the phase is related to the energy density eα for the phase, as
eα =eI,α− 1 2ρα
XN
j=1
ραj uαj2
(A.2.69)
where uαj2
=uαj·uαj.
The inner heat ux qI,α for the α phase is dened as
qI,α= XN
j=1
qαj −TTαjuαj +ραjeαjuαj
(A.2.70)
which is related to the heat uxqα for the phase as
qα =qI,α+1 2
XN
j=1
ραj uαj2
uαj (A.2.71)
A quantity kα related to the heat ux is introduced as kα =
XN
j=1
qαj+ραjeαjuαj
= qI,α+ XN
j=1
TTαjuαj
= qα− XN
j=1
ραj
− 1
ραjTTαj+ 1
2 uαj2
I
uαj (A.2.72) Similar denitions is given for the whole mixture, The denition for the external heat rα and the inner internal energy eI,α for the whole mixture is given as
r = 1 ρ
XN
α=1
εαραrα; eI = 1 ρ
XN
α=1
εαραeα (A.2.73) The internal energy eI is related to the energy density e the whole mixture as
e=eI− 1 2ρ
XN
α=1
εαρα(uα)2 (A.2.74) where (uα)2 =uα·uα.
The inner heat ux for the mixture is dened as qI =
XN
α=1
qα−TTαuα+εαραeαuα
(A.2.75) which is related to the heat ux qfor the whole mixture as
q=qI +1 2
XN
α=1
εαρα(uα)2uα (A.2.76) A quantity k related to the heat ux qis introduced as
k = XN
α=1
(εαqα+εαραeαuα)
= qI+ XN
α=1
TTαuα
= q− XN
j=1
−TTα+εαρα1
2(uα)2I
uα (A.2.77)
A.2.4.2 Energy balance for constituents
The energy balance postulate for the j'th specie in the α phase is
∂
∂t ˆ
Ω
εαραj
eαj+ 12 x0αj
2 dv=
−
˛
∂Ω
εαραj
eαj +12
x0αj 2
x0αj ·ds +
˛
∂Ω
εα
Tαjx0αj −qαj
·ds +
ˆ
Ω
h
εαραjrαj +εαραjx0αj ·bαj +x0αj · ˆpαj+ˆtαj
+ ˆeαj+ ˆQαj i
dv +
ˆ
Ω
ˆ cαj
eαj+ 12
x0αj 2
dv +
ˆ
Ω
ˆ rαj
eαj +12 x0αj
2
dv (A.2.78) Using the mathematical operations similar to (A.1.86)-(A.1.98) yields the local form of the energy balance for the species, that is
εαραjDαjeαj
Dt = tr εαTαjLαj
−div εαqαj + +x0αj ·
div εjTαj
+εαραjbαj + ˆpαj+ˆtαj
−εαραjDαjx0αj Dt
+εαραjrαj + ˆeαj+ ˆQαj (A.2.79) The momentum balance for the species is identied in the square brackets in (A.2.79) and cancels out. The reduced form of (A.2.79) is
εαραjDαjeαj
Dt = tr εαTαjLαj
−div εαqαj
+εαραjrαj
+ˆeαj+ ˆQαj (A.2.80)
The summation over the species of (A.2.80) where the denition (A.2.68)-(b) is used, is
εα XN
j=1
ραjDαjeαj
Dt = tr XN
j=1
εαTαjLαj
−div XN
j=1
εαqαj
+εαραrα
+ XN
j=1
ˆ eαj+
XN
j=1
Qˆαj (A.2.81)
The left-hand side of (A.2.81) is the rst term of the right-hand side of (A.2.43) with Γ = e. The summation of eαj over the species is (A.2.68) which is the internal energy of the phase eI,α, which change the notation of the left-hand side of (A.2.39) to ΓI,α with Γ = e and further into (A.2.43), which is
εα XN
j=1
ραjDαjeαj
Dt = εαραDαeI,α Dt +div
XN
j=1
εαραjeαjuαj
− XN
j=1
ˆ
rαj + ˆcαj −cαjrˆα
eαj (A.2.82)
Combining (A.2.81) and (A.2.82) yields
εαραDαeI,α
Dt = tr XN
j=1
εαTαjLαj
−div XN
j=1
εαqαj
+εαραrα
+ XN
j=1
ˆ eαj+
XN
j=1
Qˆαj−div XN
j=1
εαραjeαjuαj
+ XN
j=1
ˆ
rαj+ ˆcαj−cαjrˆα
eαj (A.2.83)
wherekαis identied by combining the divergence terms and (A.2.83) reduces to
εαραDαeI,α
Dt = tr XN
j=1
εαTαjLαj
−div(εαkα) +εαραrα+ XN
j=1
ˆ eαj +
XN
j=1
Qˆαj
+ XN
j=1
ˆ
rαj+ ˆcαj −cαjrˆα
eαj (A.2.84)
In the following, the energy balance postulate for the α phase is brought to a form, which is compatible with (A.2.84). The postulate for the energy
balance for theα phase is
∂
∂t ˆ
Ω
εαρα eα+12(x0α)2
dv = −
˛
∂Ω
εαρα eα+ 12(x0α)2
x0α·ds+ +
˛
∂Ω
εα(Tαx0α−qα)·ds+ +
ˆ
Ω
[εαραrα+εαραx0α·bα+ +x0α·ˆtα+ ˆQα
i dv+ +
ˆ
Ω
ˆ
rα eα+ 12(x0α)2
dv (A.2.85) Using the divergence theorem on the rst and second term on the right-hand side and rewrite the left-right-hand side by mathematical steps similar to (A.1.86)-(A.1.96), yields a reduced local form of (A.2.81) as
εαραDα
Dt eα+12 (x0α)2
= div(εα(Tαx0α−qα)) +εαραrα
+εαραx0α·bα+x0α·ˆtα+ ˆQα (A.2.86) Note that the momentum balance for theα phase has not been identied in (A.2.86). The left-hand side of (A.2.86), where the velocity term is written by its denition (x0α)2 =x0α·x0α and expanded by the product rule is
εαραDαeα
Dt +εαραDα Dt
1
2x0α·x0α
=εαραDα
Dteα+εαραx0α·Dαx0α
Dt (A.2.87) The rst part of divergence term on the right-hand side of (A.2.86), expanded by the product rule and using the denition of the velocity gradient, Lα = grad(x0α), is
div(εαTαx0α) =x0α·div(εαTα) +εαtr(TαLα) (A.2.88) The third term in (A.2.86), expressed in terms of the phase velocity and the diusion velocity (A.2.5)-(a), is
XN
j=1
εαραjx0αj·bαj = XN
j=1
εαραj uαj +x0α
·bαj (A.2.89) It is shown in (A.2.37) that summation over the species of the body force bαj yields the body force of the phasebα. Using this condition with (A.2.89) results in
XN
j=1
εαραj uαj +x0α
·bαj =εαραbα·x0α+εα XN
j=1
ραjuαj ·bαj (A.2.90)