• Ingen resultater fundet

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 −TTjjj+ 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

εαραjdv=−

˛

∂Ω

εαραjx0αj ·ds+ ˆ

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(εαραα)

αρα∂cαj

∂t +div εαραjuαj

αρααgradcαj (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 −cαjα (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

Dααρα)

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

Dααρα)

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

αjραjbαj +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

αραjbαj + 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

αραjbαj + 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

αj (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

Dαjαj)

Dt −grad(Γαj)uαj

#

= XN

j=1

εαραcαjDαjαj)

Dt −εαραcαjgrad(Γαj)uαj

−Γαjdiv εαραjuαj

+ Γαj ˆrαj+ ˆcαj−cαjα

(A.2.41) The divergence term in (A.2.41) is rewritten by the identity

div εαραjΓαjuαj

αραjgrad 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

εαραcαjDαjαj)

Dt −div εαραjΓαjuαjαjαj+ 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 +x0αjαj + ˆcαj −cαjα

(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 −cαjα x0α

+ XN

j=1

ˆ

rαj+ ˆcαj −cαjα

uαj (A.2.45)

The fact that PN

j=1αjuαj) = 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=1αj + ˆcαj −cαjα

= 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 −cαjα

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!

αραbα

+ 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=1αjuαj) = 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

εαTααTI,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

Dαα)

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) +ΓαααραDαα)

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)

+ ΓαααραDαα) Dt

(A.2.60)

which reduce (A.2.60) to ρD(Γ)

Dt =−div XN

α=1

αραΓαuα) + XN

α=1

Γαα+ XN

α=1

εαραDαα)

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

αραuα⊗uα)−div XN

α=1

αραuα)⊗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=1αραuα) = 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 −TTαjuαjαjeαjuαj

(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

qαjαjeαjuαj

= 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−TTαuααραeαuα

(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

αqααραeαuα)

= qI+ XN

α=1

TTαuα

= q− XN

j=1

−TTααρα1

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

εαραj

eαj+ 12 x0αj

2 dv=

˛

∂Ω

εαραj

eαj +12

x0αj 2

x0αj ·ds +

˛

∂Ω

εα

Tαjx0αj −qαj

·ds +

ˆ

h

εαραjrαjαραjx0αj ·bαj +x0αj · ˆpαj+ˆtαj

+ ˆeαj+ ˆQαj i

dv +

ˆ

ˆ cαj

eαj+ 12

x0αj 2

dv +

ˆ

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

αραjbαj + ˆpαj+ˆtαj

−εαραjDαjx0αj Dt

αραjrαj + 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

αραjrαj

+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

αραrα

+ XN

j=1

ˆ eαj+

XN

j=1

αj (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 −cαjα

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

αραrα

+ XN

j=1

ˆ eαj+

XN

j=1

αj−div XN

j=1

εαραjeαjuαj

+ XN

j=1

ˆ

rαj+ ˆcαj−cαjα

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

αj

+ XN

j=1

ˆ

rαj+ ˆcαj −cαjα

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

εαρα eα+12(x0α)2

dv = −

˛

∂Ω

εαρα eα+ 12(x0α)2

x0α·ds+ +

˛

∂Ω

εα(Tαx0α−qα)·ds+ +

ˆ

αραrααραx0α·bα+ +x0α·ˆtα+ ˆQα

i dv+ +

ˆ

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

αραx0α·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

αραDα

Dteααραx0α·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

·bαjαραbα·x0αα XN

j=1

ραjuαj ·bαj (A.2.90)