• Aucun résultat trouvé

Compressible Fluids: the discontinuity of the vorticity vector on a shock wave in thermodynamical variables.

N/A
N/A
Protected

Academic year: 2021

Partager "Compressible Fluids: the discontinuity of the vorticity vector on a shock wave in thermodynamical variables."

Copied!
7
0
0

Texte intégral

(1)

HAL Id: hal-00276736

https://hal.archives-ouvertes.fr/hal-00276736

Submitted on 1 May 2008

HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

Compressible Fluids: the discontinuity of the vorticity vector on a shock wave in thermodynamical variables.

Henri Gouin

To cite this version:

Henri Gouin. Compressible Fluids: the discontinuity of the vorticity vector on a shock wave in thermodynamical variables.. Comptes rendus hebdomadaires des séances de l’Académie des sciences, Gauthier-Villars, 1973, 276 (Serie A), pp.1377-1380. �hal-00276736�

(2)

hal-00276736, version 1 - 1 May 2008

Compressible Fluids:

The discontinuity of the vorticity vector on a shock wave in thermodynamical variables

Translation of C. R. Acad. Sci. Paris t. 276, A, p. 1377-1380 (1973)

Henri Gouin

Universit´e d’Aix-Marseille & C.N.R.S. U.M.R. 6181,

Case 322, Av. Escadrille Normandie-Niemen, 13397 Marseille Cedex 20 France

Abstract

The discontinuity of the vorticity is written as a function of the vector Tgrads, (whereT is the temperature andsthe specific entropy). The expression is obtained thanks to potential equations and independently of the mass conservation and the equation of momentum balance.

Key words: Instationary perfect fluids; shock waves; vorticity vector.

PACS:47.40.Nm; 47.15.ki; 47.32.C-

1 Introduction

The aim of this note is to prove that, in the most general instationary case of perfect compressible fluids, across a shock wave we have the relations:

[u(rot v)tg] =n∧[T grad s]

[(rot v)n] = 0 (1)

where v is the velocity vector of the fluid, uis the fluid velocity with respect to the shock wave, T is the temperature, s is the specific entropy, the indices tg andn indicate the tangential and normal components to the shock wave of the vector rot v and the discontinuity of a tensorial quantityα is denoted by [α] (see[1]).

Email address: henri.gouin@univ-cezanne.fr(Henri Gouin).

(3)

We take into account the following shock conditions:

[vtg] = 0 (2)

1

2u2+h

= 0 (3)

where h denotes the specific enthalpy (dh=T ds+dp ρ ).

We do not use the following shock conditions:

[ρu] = 0 (4)

hp+ρu2i= 0 (5)

where ρ is the density andp the pression of the fluid.

We will use the potential equations obtained by P. Casal [2] or J. Serrin [3]

and expressing another form of the equations of the motions of compressible perfect fluids.

The motion of a compressible fluid is represented by a continuous mapping of a reference three-dimensional space Do in the physical space Dt occupied by the fluid at time t:

x=ϕt(X), x∈Dt, X∈Do,

or equivalently by a continuous mapping Φ :Wo −→W, z= Φ(Z) where Wo

is a four-dimensional reference space andW the physical time-space,

z=

t x

∈W and Z =

t X

∈Wo.

We assume the motion has a shock wave localized on a surfaceS(t) propagating inDt, image byϕt of a surfaceSo(t) propagating inDo. We denote by no and n the unit normal vectors to So(t) and S(t) respectively, and go and g their respective velocities; then u=nTv−g, where T denotes the transposition.

Equivalently, Σo and Σ are respectively the two corresponding surfaces prop- agating in Wo and W; No and Nare the associated normal vectors,

NT=(−g,nT).

Consequently, Φ is a differential mapping on Wo, except on Σo; its Jacobian matrix is denoted by∂z/∂Z, F denotes the Jacobian matrix ofϕt:

dx=vdt+F dX.

2

(4)

2 Exterior derivative

The covector C=vT has an inverse imageCo inDo such that Co =CF

The exterior derivative of the form C is a 2-form which is isomorph to the vector rot v. It the image of the 2-form which is the exterior derivative ofCo

isomorph to the vector rotoCoT

: rotv= F

det F rotoCoT

(6) roto is the rotational on Do (see reference[4]).

The discontinuity of the vorticity vector comes from to parts: one part comes from the discontinuity of its image roto

CoT

, and the other part comes from the discontinuity of the JacobianF.

3 Discontinuity of the Jacobian F

∂z/∂Z is a linear mapping transforming any tangent vector to So(t) in a tangent vector to S(t). If we denote by no =−no/go, we obtain:

[F] = [v]noT, noT =nTF1

u1 =nTF2

u2

where indices 1,2 indicate quantities upstream and downstream the shock.

Consequently,

nT

F u

= 0 Taking into account Eq. (2) we obtain

[v] = [u]n, (7)

[F] = [u]n noT, (8)

F det F

= [u]

u2det F1

n nT −IF1. (9)

where Iis the identity matrix.

(5)

4 Discontinuity of the 1-form Co

Due to the fact that Co =vTF and by using Eq. (7) and Eq. (8), we obtain:

[Co] =hu2+guinoT. (10)

5 Discontinuity of potentials

The dot denotes the material derivative, Ω is the body force potential. We consider the two quantitiesϕ(t,X) andψ(t,X) (denoted potentials) such that

˙

ϕ=β(t,X), (11)

ψ˙ =γ(t,X). (12)

β and γ are two scalar fields defined in each point of the flow and such that β(t,X) = 1

2v2−h−Ω, γ(t,X) =T.

There exists a covector B function only of X such that Co = ∂ϕ

∂X +ψ ∂s

∂X +B. (13)

We can verify that Eq. (13) together with Eq. (11) and Eq. (12) are equivalent topotential equations proposed by P. Casal in [2] and J. Serrin in [3].

With the condition of adiabaticity

˙ s= 0, and the equation of balance of mass

∂ρ

∂t + div(ρv) = 0, we obtain the complete set of motion equations.

We can choose ϕ and ψ null on the shock wave and continuous through the shock surface in the following manner:

ϕ =

Z t

f(X)β(τ ,X)dτ, ψ =

Z t

f(X)γ(τ ,X)dτ, (14) where t = f(X) is the equation of the shock surface So(t) which is assumed regular.

4

(6)

Potential ϕ being continuous through the shock surface,

"

∂ϕ

∂X

#

= [ ˙ϕ] noT =

1

2v2−h

noT.

By using Eq. (2), Eq. (3) and Eq. (10) we get:

"

∂ϕ

∂X

#

= [Co]. (15)

Due to the fact that ψ is null on the shock wave, Eq. (13) expresses B is continuous through the shock:

[B] = 0 (16)

6 Discontinuity of the image of the vorticity

Let us consider

Wo =CoT − ∂ϕ

∂X

!T

, then rotoWo = rotoCoT

.

Eq. (13) yields W˙o =T grados, the value of grados being defined on Wo. Due to Eq. (15), Wo is continuous through the shock and we get:

"

∂Wo

∂X

#

=ho

i noT, [rotoWo] =noho

i,

hrotoCoTi

=no∧[T grados]. (17) The discontinuity of the image of the vorticity is only tangential. Using the previous results and application Φ, we can verify that this property of the vorticity remains true.

7 Discontinuity of the vorticity

The results obtained by Eqs (6), (9) and (17) allow to obtain Formulae (1).

This expression general for non stationary perfect compressible fluids is dif- ferent from the result given by Hayes [5]. This is due to the fact the result is obtained thanks to Eq. (3) of conservation of energy. It neither uses Eq. (5) of the balance of the quantity of motion nor Eq. (4) of the conservation of mass.

(7)

To obtain Formulae (1), the knowledge of the enthalpy field is only necessary.

In the special case of a stationary, iso-energetic, irrotational motion upstream of the shock, the relation can be expressed with the help of the curvature tensor of the shock surface [6].

References

[1] J. Hadamard, Le¸cons sur la propagation des ondes et les ´equations de l’hydrodynamique, Chelsea Publ., New York (1949).

[2] P. casal, Journal de M´ecanique, 5, no 2, 1986, p. 149-161.

[3] J. Serrin, Mathematical principle of classical fluid mechanics, Fluid dynamics 1, Encyclopedia of Physics, VIII/1, Springer, New York (1959).

[4] H. Cartan, Calcul diff´erentiel, Hermann, Paris (1967).

[5] W.D. Hayes, Journal of Fluid Mechanics, 2, 1957, p. 595.

[6] A.L. Jaumotte and P. Carri`ere, Chocs et ondes de chocs, Masson, Paris (1971), p. 67-68.

6

Références

Documents relatifs

Selecting the 120 kHz frequency bandwidth of the filter it is ¾ spectrum magnitude of the analysis signals and central frequencies of the filter are left the same: 150 kHz,

It can be seen that when the VDF has an enhanced tail of suprathermal particles approximated by a kappa or Lorentzian function, the total density in the exosphere is

• Does agreement reduce need for

Subject to the conditions of any agreement between the United Nations and the Organization, approved pursuant to Chapter XVI, States which do not become Members in

This algorithm is important for injectivity problems and identifiability analysis of parametric models as illustrated in the following. To our knowledge, it does not exist any

L’enquête par entretiens avec les seules mères minore le rôle des conjoints dans le « choix » du homeschooling, comme l’illustre un entretien exceptionnellement mené en

Studying approximations deduced from a Large Eddy Simulations model, we focus our attention in passing to the limit in the equation for the vorticity.. Generally speaking, if E(X) is

2. b) Derive the least squares solution of the unknown parameters and their variance-covariance matrix.. Given the angle measurements at a station along with their standard