Unsteady waves

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Moving shock waves

Moving Normal Shock Waves

The starting point is the governing equations for stationary normal shocks (repeated here for convenience).

ρ1u1=ρ2u2(Eq. 6.1)
ρ1u12+p1=ρ2u22+p2(Eq. 6.2)
h1+12u12=h2+12u22(Eq. 6.3)

Shock moving to the right with the constant speed $W$ into a gas that is standing still. Moving with the shock, we would see a gas velocity ahead of the shock u1=W, and the gas behind the shock moves to the right with the velocity u2=Wup. Now, let's insert u1 and u2 in the stationary shock relations \ref{eq:stationary:cont} - \ref{eq:stationary:energy}.

ρ1W=ρ2(Wup)(Eq. 6.4)
ρ1W2+p1=ρ2(Wup)2+p2(Eq. 6.5)
h1+12W2=h2+12(Wup)2(Eq. 6.6)

Rewriting Eqn. \ref{eq:unsteady:cont}

(Wup)=Wρ1ρ2(Eq. 6.7)

Inserting Eqn. \ref{eq:unsteady:cont:mod} in Eqn. \ref{eq:unsteady:mom} gives

p1+ρ1W2=p2+ρ2W2(ρ1ρ2)2p2p1=ρ1W2(1ρ1ρ2)(Eq. 6.8)
W2=p2p1ρ2ρ1(ρ2ρ1)(Eq. 6.9)

From the continuity equation \ref{eq:unsteady:cont}, we get

W=(Wup)(ρ2ρ1)(Eq. 6.10)

Inserting Eqn. \ref{eq:unsteady:cont:modb} in Eqn. \ref{eq:unsteady:mom:mod} gives

(Wup)2=p2p1ρ2ρ1(ρ1ρ2)(Eq. 6.11)

Now, let's insert Eqns. \ref{eq:unsteady:mom:mod} and \ref{eq:unsteady:mom:modb} in the energy equation (Eqn. \ref{eq:unsteady:energy}).

h1+12[p2p1ρ2ρ1(ρ2ρ1)]=h2+12[p2p1ρ2ρ1(ρ1ρ2)](Eq. 6.12)
h=e+pρ(Eq. 6.13)
e1+p1ρ1+12[p2p1ρ2ρ1(ρ2ρ1)]=e2+p2ρ2+12[p2p1ρ2ρ1(ρ1ρ2)](Eq. 6.14)

which can be rewritten as

e2e1=p1+p22(1ρ11ρ2)(Eq. 6.15)

Eqn \ref{eq:unsteady:hugonoit} is the same Hugoniot equation as we get for a stationary normal shock. The Hugoniot equation is a relation of thermodynamic properties over a shock. As the shock in the unsteady case is moving with a constant velocity, the frame of reference moving with the shock is an inertial frame and thus the same physical relations apply in the moving shock case as in the stationary shock case. The fact that the Hugoniot relation does not include any velocities or Mach numbers but only thermodynamic properties, the relation will be unchanged for a moving shock.

Moving Shock Relations

For a calorically perfect gas we have e=CvT. Inserted in the Hugoniot relation above this gives

Cv(T2T1)=p1+p22(ν1ν2)(Eq. 6.16)

where ν=1/ρ

Now, using the ideal gas law T=pν/R and Cv/R=1/(γ1) gives

(1γ1)(p2ν2p1ν1)=p1+p22(ν1ν2)



p2(ν2γ1ν1ν22)=p1(ν1γ1+ν1ν22)
(Eq. 6.17)

From this result, we can derive a relation for the pressure ratio over the shock as a function of density ratio

p2p1=(γ+1γ1)(ν1ν2)1(γ+1γ1)(ν1ν2)(Eq. 6.18)

ν=RT/p and thus

ν1ν2=T1T2p2p1(Eq. 6.19)

Eqn. \ref{eq:unsteady:density:ratio} in Eqn. \ref{eq:unsteady:hugonoit:c} gives

p2p1=(γ+1γ1)(T1T2p2p1)1(γ+1γ1)(T1T2p2p1)(Eq. 6.20)

Now, we can get a relation for calculation of the temperature ratio over the moving shock as function of the shock pressure ratio

T2T1=p2p1[(γ+1γ1)+(p2p1)1+(γ+1γ1)(p2p1)](Eq. 6.21)

Once again using the ideal gas law

ρ2ρ1=(γ+1γ1)+(p2p1)1+(γ+1γ1)(p2p1)(Eq. 6.22)

Going back to the momentum equation

p2p1=ρ1W2(1ρ1ρ2)={W=Msa1}=ρ1Ms2a12(1ρ1ρ2)(Eq. 6.23)

with a12=γp1/ρ1, we get

p2p1=γMs2(1ρ1ρ2)+1(Eq. 6.24)

From the normal shock relations, we have

ρ1ρ2=2+(γ1)Ms2(γ+1)Ms2(Eq. 6.25)

Eqn. \ref{eq:unsteady:Mach:b} in \ref{eq:unsteady:Mach:a} gives

p2p1=1+(2γγ+1)(Ms21)(Eq. 6.26)

or

Ms=(γ+12γ)(p2p11)+1(Eq. 6.27)

Eqn. \ref{eq:unsteady:Mach} with Ms=W/a1

W=a1(γ+12γ)(p2p11)+1(Eq. 6.28)

Induced Flow Behind Moving Shock

Let's try to find a relation for calculation of the induced velocity behind the moving shock. Once again, the starting point is the continuity equation for moving shocks (Eqn. \ref{eq:unsteady:cont}) repeated here for convenience

ρ1W=ρ2(Wup)(Eq. 6.29)

The induced velocity appears on the right side of the continuity equation

W(ρ1ρ2)=ρ2up(Eq. 6.30)
up=W(1ρ1ρ2)(Eq. 6.31)

From before we have a relation for $W$ as a function of pressure ratio and one for ρ1/ρ2, also as a function of pressure ratio.

Eqn. \ref{eq:unsteady:up:a} togheter with Eqns. \ref{eq:unsteady:W} and \ref{eq:unsteady:density:ratio} gives

up=a1(γ+12γ)(p2p11)+1I[1(γ+1γ1)+(p2p1)1+(γ+1γ1)(p2p1)]II(Eq. 6.32)

The equation subsets I and II can be rewritten as:

Term I:

(γ+12γ)(p2p11)+1=γ+12γ[(p2p1)+(γ1γ+1)](Eq. 6.33)


Term II:

[1(γ+1γ1)+(p2p1)1+(γ+1γ1)(p2p1)]=1γ(p2p11)(2γγ+1)(γ1γ+1)+(p2p1)(Eq. 6.34)

the rewritten terms I and II implemented, Eqn. \ref{eq:unsteady:up:b} becomes

up=a1γ(p2p11)(2γγ+1)(γ1γ+1)+(p2p1)(Eq. 6.35)

Since the region behind the moving shock is region 2, the induced flow Mach number is obtained as

Mp=upa2=upa1a1a2=upa1γRT1γRT2=upa1T1T2(Eq. 6.36)

With up/a1 from Eqn. \ref{eq:unsteady:up} and T1/T2 from Eqn. \ref{eq:unsteady:temperature:ratio}

Mp=1γ(p2p11)((2γγ+1)(γ1γ+1)+(p2p1))1/2(1+(γ+1γ1)(p2p1)(γ+1γ1)(p2p1)+(p2p1)2)1/2(Eq. 6.37)

There is a theoretical upper limit for the induced Mach number Mp

limp2/p1Mp(p2p1)=2γ(γ1)(Eq. 6.38)

As can be seen, at the upper limit the induced Mach number is a function of γ and for air (γ=1.4) we get

limp2/p1Mp(p2p1)1.89(Eq. 6.39)

Shock Wave Reflection

When the incident shock wave reaches the wall, a shock propagating in the opposite direction is generated with a shock strength such that the velocity of the induced flow behind the incident shock is reduced to zero. The flow can not go through the wall and thus the velocity must be zero in the vicinity of the wall. The properties of the incident shock wave are directly related to the pressure ratio over the shock wave. Therefore, it would be convenient to have a relation between the reflected shock wave and incident shock wave.


The Incident Shock Wave

The pressure ratio over the incident shock in Fig.~\ref{fig:reflection} can be obtained as

p2p1=1+2γγ+1(Ms21)(Eq. 6.40)

where Ms is the wave Mach number, which is calculated as

Ms=Wa1(Eq. 6.41)

In Eqn.~\ref{eq:incident:Mach:def}, W is the speed with which the incident shock wave travels into region 1 and a1 is the speed of sound in region 1 (see Fig.~\ref{fig:reflection}).

Solving Eqn.~\ref{eq:incident:pr} for Ms, we get

Ms=γ+12γ(p2p11)+1(Eq. 6.42)

Anderson derives the relations for calculation of the ratio T2/T1

T2T1=p2p1(γ+1γ1+p2p11+γ+1γ1p2p1)(Eq. 6.43)

From Eqn.~\ref{eq:incident:tr} it is easy to get the corresponding relation for ρ2/ρ1

ρ2ρ1=1+γ+1γ1p2p1γ+1γ1+p2p1(Eq. 6.44)

Anderson also shows how to obtain the induced velocity, up, behind the incident shock wave, {\emph{i.e.}} the velocity in region 2 (see Fig.~\ref{fig:reflection}).

up=W(1ρ1ρ2)=Msa1(1ρ1ρ2)(Eq. 6.45)

The Reflected Shock Wave

The pressure ratio over the reflected shock can be obtained from Eqn.~\ref{eq:incident:pr} by analogy

p5p2=1+2γγ+1(Mr21)(Eq. 6.46)

where Mr is the Mach number of the reflected shock wave defined as

Mr=Wr+upa2(Eq. 6.47)

where Wr is the speed of the reflected shock wave and a2 is the speed of sound in region 2 (see Fig.~\ref{fig:reflection}).

Solving Eqn.~\ref{eq:reflected:pr} for Mr gives

Mr=γ+12γ(p5p21)+1(Eq. 6.48)

The ratios T5/T2 and ρ5/ρ2 can be obtained from Eqns.~\ref{eq:incident:tr} and \ref{eq:incident:rr} by analogy

T5T2=p5p2(γ+1γ1+p5p21+γ+1γ1p5p2)(Eq. 6.49)
ρ5ρ2=1+γ+1γ1p5p2γ+1γ1+p5p2(Eq. 6.50)

The velocity in region 2 which is the same as the induced flow velocity behind the incident shock wave can be obtained as

up=Wr(ρ5ρ21)=Mra2(1ρ2ρ5)(Eq. 6.51)

Reflected Shock Relation

With the relations for the incident shock wave and reflected shock wave defined, we now have the tools to derive a relation between the incident and reflected shock waves. The induced flow velocity $u_p$ calculated using the relation obtained for the incident shock wave must of course be the same as when calculated using reflected wave properties, {\emph{i.e.}} the result of Eqn.~\ref{eq:incident:up} is identical to that of Eqn.~\ref{eq:reflected:up}

Mra2(1ρ2ρ5)=Msa1(1ρ1ρ2)(Eq. 6.52)

rewriting gives

Mr(1ρ2ρ5)=Ms(1ρ1ρ2)a1a2(Eq. 6.53)

Assuming calorically perfect gas gives a=γRT and thus

Mr(1ρ2ρ5)=Ms(1ρ1ρ2)T1T2(Eq. 6.54)

Let's first look at the term on the left hand side of Eqn.~\ref{eq:relation:c}

Mr(1ρ2ρ5)(Eq. 6.55)

Using the ρ5/ρ2 and p2/p5 from Eqns.~\ref{eq:reflected:rr} and~\ref{eq:reflected:pr} and simplifying gives

Mr(1ρ2ρ5)=(2γ+1)(Mr21Mr)(Eq. 6.56)

Using the same approach on the corresponding term for the incident shock wave on the right hand side of Eqn.~\ref{eq:relation:c} gives

Ms(1ρ1ρ2)=(2γ+1)(Ms21Ms)(Eq. 6.57)

Now, inserting~\ref{eq:relation:d} and~\ref{eq:relation:e} in Eqn.~\ref{eq:relation:c} gives

(2γ+1)(Mr21Mr)=(2γ+1)(Ms21Ms)T1T2(Eq. 6.58)

Simplifying and inverting gives

(MrMr21)=(MsMs21)T2T1(Eq. 6.59)

The rightmost term in Eqn.~\ref{eq:relation:g} (T2/T1) needs to be rewritten. Inserting~\ref{eq:incident:pr} in~\ref{eq:incident:tr} and expanding all terms gives

T2T1=2(γ+1)+(γ+1)(γ1)Ms2+4γ(Ms21)+2γ(γ1)Ms2(Ms21)(γ+1)2Ms2=
=2(γ+1)+(γ+1)(γ1)Ms2+4γ(Ms21)(γ+1)2Ms2+2(γ1)(γ+1)2(Ms21)γ=
=2(γ+1)+(γ+1)(γ1)Ms2+4γ(Ms21)(2(γ1)(Ms21))(γ+1)2Ms2
2(γ1)(γ+1)2(Ms21)(γ+1Ms2)(Eq. 6.60)

Finally we end up with the following relation

T2T1=1+2(γ1)(γ+1)2(Ms21)(γ+1Ms2)(Eq. 6.61)

The temperature ratio over the incident shock wave is now totally defined by the incident Mach number Ms and the ratio of specific heats γ. With~\ref{eq:relation:tr} in~\ref{eq:relation:g} we get the sought relation between the reflected and incident Mach numbers.

(MrMr21)=(MsMs21)1+2(γ1)(γ+1)2(Ms21)(γ+1Ms2)(Eq. 6.62)

It should be noted that Eqn.~\ref{eq:relation:final} is valid for calorically perfect gases only.

Acoustic theory

In the following we are going to derive the linear acoustic wave equation starting from the continuity and momentum equations on non-conservation differential form. The equations are repeated here for convenience.

DρDt+ρ(𝐯)=0(Eq. 6.63)
ρD𝐯Dt+p=0(Eq. 6.64)

Remember that D/Dt denotes the substantial derivative operator defined as follows

DDt=t+𝐯(Eq. 6.65)

where /t is the local temporal derivative and 𝐯 is the convective derivative.

We are going to analyze acoustic waves in one dimension, which means that the equations above reduces to

ρt+uρx+ρux=0(Eq. 6.66)
ρut+ρuux+px=0(Eq. 6.67)

Pressure is a thermodynamic property and thus it can be expressed as a function of two other thermodynamic properties. Let's express pressure as a function of density (ρ) and entropy (s).

p=p(ρ,s)dp=(pρ)sdρ+(ps)ρds(Eq. 6.68)

Since weak acoustic waves are considered, entropy will be constant and thus ds=0, which means that

dp=(pρ)sdρ=a2dρ(Eq. 6.69)
ρut+ρuux+a2ρx=0(Eq. 6.70)

The acoustic perturbations can be described as small deviations around a reference state

ρ=ρ+Δρp=p+ΔpT=T+ΔTu=u+Δu={u=0}=Δu

Inserted in Eqns.~\ref{eq:unstady:acoustic:wave:cont} and \ref{eq:unstady:acoustic:wave:mom:b} and using the fact that derivatives of the constant reference state flow quantities are zero, we get

t(Δρ)+Δux(Δρ)+(ρ+Δρ)x(Δu)=0(Eq. 6.71)
(ρ+Δρ)t(Δu)+(ρ+Δρ)Δux(Δu)+a2x(Δρ)=0(Eq. 6.72)

In the same way as pressure, being a thermodynamic variable, can be expressed as a function of two other thermodynamic variables, so can the speed of sound. Once again we will select density and entropy as the two thermodynamic variables

a2=a2(ρ,s)(Eq. 6.73)

and since entropy is constant

a2=a2(ρ)(Eq. 6.74)

Taylor expansion of a2 around the reference state a with Δρ=ρρ gives

a2=a2+(ρ(a2))Δρ+(2ρ2(a2))(Δρ)2+ (Eq. 6.75)

Inserted in Eqn.~\ref{eq:unstady:acoustic:wave:mom:pert}, we get


(ρ+Δρ)t(Δu)+(ρ+Δρ)Δux(Δu)+[a2+(ρ(a2))Δρ+ ]x(Δρ)=0(Eq. 6.76)

The perturbations Δu and Δρ are small, which implies that Δua and Δρρ. This means that products of perturbations can be canceled and so can higher-order terms in the Taylor expansion of a2. This means that the continuity and momentum equations reduces to

t(Δρ)+ρx(Δu)=0(Eq. 6.77)
ρt(Δu)+a2x(Δρ)=0(Eq. 6.78)

Before making the assumption that the perturbations are small compared to the corresponding reference state flow quantities and thus justifying the cancelation of products of perturbations from the equations, the flow equations were still the exact fully non-linear equations. Eqns.~\ref{eq:unstady:acoustic:wave:cont:linear}. and \ref{eq:unstady:acoustic:wave:mom:linear}, however, are approximations as several terms has been removed. The equations are linear and are good approximations as long as the perturbations are small. The smaller the perturbations, the better the approximation are the linear equations. Eqns.~\ref{eq:unstady:acoustic:wave:cont:linear} and \ref{eq:unstady:acoustic:wave:mom:linear} describes the motion induced in a gas by the passage of a sound wave. By combining the temporal derivative of Eqn.~\ref{eq:unstady:acoustic:wave:cont:linear} with the divergence of Eqn.~\ref{eq:unstady:acoustic:wave:mom:linear}, it is possible to obtain a wave equation describing the propagation of acoustic waves in a quiescent surrounding.

The temporal derivative of the continuity equation:

2t2(Δρ)+ρ2xt(Δu)=0(Eq. 6.79)

The divergence of the momentum equation:

ρ2xt(Δu)+a22x2(Δρ)=0(Eq. 6.80)

The second term in the first equation is the same as the first term in the second equation. Substituting the term, the two equations reduces to one single equation

2t2(Δρ)=a22x2(Δρ)(Eq. 6.81)

which is a one-dimensional form of the classic wave equation with the general solution

Δρ=F(xat)+G(x+at)(Eq. 6.82)

F and G are arbitrary functions. The function F describes the shape of a wave traveling in the positive x-direction at the speed of sound of the ambient gas and the function G describes the shape of a wave traveling in the negative x-direction at the same speed. In Eqn.~\ref{eq:wave} Δρ appears with second derivatives in space and time. Let's differentiate the proposed solution (Eqn.~\ref{eq:wave:solution}) two times in time and space, respectively, and check that it is actually a valid solution to Eqn.~\ref{eq:wave}.

t(Δρ)=F(xat)(xat)t+G(x+at)(x+at)t(Eq. 6.83)
t(Δρ)=aF+aG(Eq. 6.84)
2t2(Δρ)=aF(xat)(xat)t+aG(x+at)(x+at)t(Eq. 6.85)
2t2(Δρ)=a2F+a2G(Eq. 6.86)
x(Δρ)=F(xat)(xat)x+G(x+at)(x+at)x(Eq. 6.87)
x(Δρ)=F+G(Eq. 6.88)
2x2(Δρ)=F(xat)(xat)x+G(x+at)(x+at)x(Eq. 6.89)
2x2(Δρ)=F+G(Eq. 6.90)

Eqns. \ref{eq:wave:ddt} and \ref{eq:wave:ddx} inserted Eqn. \ref{eq:wave} gives

a2F+a2G=a2(F+G)(Eq. 6.91)

which shows that Eqn. \ref{eq:wave:solution} is a valid solution to the wave equation.

F and G are arbitrary functions and thus G=0 is a valid solution, which gives

Δρ(x,t)=F(xat)(Eq. 6.92)

If Δρ is constant, i.e. a wave with constant amplitude, we see from Eqn.~\ref{eq:wave:solution:F} that (xat) is constant and thus

x=at+cdxdt=a(Eq. 6.93)

From Eqn.~\ref{eq:wave:solution:F}, we get

t(Δρ)=aF(Eq. 6.94)
x(Δρ)=F(Eq. 6.95)

and thus

x(Δρ)=1at(Δρ)(Eq. 6.96)

which gives a relation between the temporal derivative of Δρ and the spatial derivative of Δρ. With Eqn.~\ref{eq:wave:solution:F:b}, the linearized momentum equation Eqn.~\ref{eq:unstady:acoustic:wave:mom:linear} can be rewritten as follows

t(Δu)=a2ρx(Δρ)={x(Δρ)=1at(Δρ)}=aρt(Δρ)(Eq. 6.97)
t(ΔuaρΔρ)=0ΔuaρΔρ=const(Eq. 6.98)

In an undisturbed gas Δu=Δρ=0 and thus

ΔuaρΔρ=0(Eq. 6.99)

or

Δu=aρΔρ(Eq. 6.100)

If instead F is set to zero and G is non-zero, we get

Δu=aρΔρ(Eq. 6.101)
(pρ)s=a2Δp=a2Δρ(Eq. 6.102)

Acoustic wave traveling in the positive x-direction:

Δu=aρΔρ=1aρΔp(Eq. 6.103)

Acoustic wave traveling in the negative x-direction:

Δu=aρΔρ=1aρΔp(Eq. 6.104)

Finite non-linear waves

Starting point: the governing flow equations on partial differential form

Continuity equation:

ρt+uρx+ρux=0(Eq. 6.105)

Momentum equation:

ut+uux+1ρpx=0(Eq. 6.106)

Any thermodynamic property can be expressed as a function of two other thermodynamic properties. This means that we can get density as a function of pressure and entropy: ρ=ρ(p,s) and therefore

dρ=(ρp)sdp+(ρs)pds(Eq. 6.107)

Assuming isentropic flow ds=0 gives

dρ=(ρp)sdp(Eq. 6.108)
ρt=(ρp)spt=1a2ptρx=(ρp)spx=1a2px(Eq. 6.109)

Now, insert \ref{eq:rhotop} in \ref{eq:pde:cont} gives

pt+upx+ρa2ux=0(Eq. 6.110)

Dividing \ref{eq:pde:cont:b} by ρa gives

1ρa(pt+upx)+aux=0(Eq. 6.111)

A slightly modified form of the momentum equation is obtained by multiplying and dividing the last term by a

ut+uux+1ρa(apx)=0(Eq. 6.112)

If the continuity equation on the form \ref{eq:pde:cont:c} is added to the momentum equation on the form \ref{eq:pde:mom:c}, we get

[ut+(u+a)ux]+1ρa[pt+(u+a)px]=0(Eq. 6.113)

If, instead, the continuity equation on the form \ref{eq:pde:cont:c} is subtracted from the momentum equation on the form \ref{eq:pde:mom:c}, we get

[ut+(ua)ux]+1ρa[pt+(ua)px]=0(Eq. 6.114)

Since u=u(x,t), we have from the definition of a differential

du=utdt+uxdx=utdt+uxdxdtdt(Eq. 6.115)

Now, let dx/dt=u+a

du=utdt+(u+a)uxdt=[ut+(u+a)ux]dt(Eq. 6.116)

which is the change of u in the direction dx/dt=u+a

In the same way

dp=ptdt+pxdx=ptdt+pxdxdtdt(Eq. 6.117)

and thus, in the direction dx/dt=u+a

dp=ptdt+(u+a)pxdt=[pt+(u+a)px]dt(Eq. 6.118)

If we go back and examine Eqn. \ref{eq:nonlin:a}, we see that Eqns. \ref{eq:du:b} and \ref{eq:dp:b} appear in the equation and thus it can now be rewritten as follows

dudt+1ρadpdt=0du+dpρa=0(Eq. 6.119)

Eqn. \ref{eq:nonlin:a:ode} applies along a C+ characteristic, i.e., a line in the direction dx/dt=u+a in xt-space and is called the compatibility equation along the C+ characteristic. If we instead chose a C characteristic, i.e., a line in the direction dx/dt=ua in xt-space, we get

du=[ut+(ua)ux]dt(Eq. 6.120)
dp=[pt+(ua)px]dt(Eq. 6.121)

which can be identified as subsets of Eqn. \ref{eq:nonlin:b} and thus

dudt1ρadpdt=0(Eq. 6.122)

In order to fulfil the relation above, either du=dp=0 or

dudpρa=0(Eq. 6.123)

Eqn. \ref{eq:nonlin:b:ode} applies along a C characteristic, i.e., a line in the direction dx/dt=ua in xt-space and is called the compatibility equation along the C characteristic.


So, what we have done now is that we have have found paths through a point (x1, t1) along which the governing partial differential equations Eqns. \ref{eq:nonlin:a} and \ref{eq:nonlin:b} reduces to the ordinary differential equations \ref{eq:nonlin:a:ode} and \ref{eq:nonlin:b:ode}. The C+ and C characteristic lines are physically the paths of right- and left-running sound waves in the xt-plane.

Riemann Invariants

If the compatibility equations are integrated along respective characteristic line, i.e., integrate \ref{eq:nonlin:a:ode} along the C+ characteristic and \ref{eq:nonlin:b:ode} along the C characteristic, we get the Riemann invariants J+ and J.

J+=u+dpρa=const(Eq. 6.124)
J=udpρa=const(Eq. 6.125)

The Riemann invariants are constants along the associated characteristic line.

We have assumed isentropic flow and thus we may use the isentropic relations

p=C1Tγ/(γ1)=C2a2γ/(γ1)(Eq. 6.126)

where C1 and C2 are constants. Differentiating Eqn. \ref{eq:isentropic:a} gives

dp=C2(2γγ1)a[2γ/(γ1)1]da(Eq. 6.127)

Now, if we further assume the gas to be calorically perfect

a2=γRT=γpρρ=γpa2(Eq. 6.128)

Eqn. \ref{eq:isentropic:a} in \ref{eq:isentropic:c} gives

ρ=C2γa[2γ/(γ1)2](Eq. 6.129)

and thus

J+=u+C2(2γγ1)a[2γ/(γ1)1]C2γa[2γ/(γ1)2]ada=u+(2γ1)da(Eq. 6.130)
J+=u+2aγ1(Eq. 6.131)
J=u2aγ1(Eq. 6.132)

Eqns. \ref{eq:riemann:a:b} and \ref{eq:riemann:b:b} are the Riemann invariants for a calorically perfect gas. The Riemann invariants are constants along C+ and C characteristics and if the situation shown in Fig. \ref{fig:characteristics} appears, that fact can be used to calculate the flow velocity and speed of sound in the location (x1, t1).

J++J=u+2aγ1+u2aγ1=2uu=12(J++J)(Eq. 6.133)
J+=u+2aγ1=12(J++J)+2aγ1a=γ14(J+J)(Eq. 6.134)

Moving expansion waves

Moving Expansion Waves

The expansion wave propagation into the driver section in a shock tube can be described using characteristic lines.


The expansion is propagating into stagnant fluid in region four (the driver section), which means that the flow properties ahead of the expansion wave are constant.

Ja+=Jb+(Eq. 6.135)

J+ invariants constant along C+ characteristics

Ja+=Jc+=Je+(Eq. 6.136)
Jb+=Jd+=Jf+(Eq. 6.137)

Since Ja+=Jb+ this also implies Je+=Jf+. In fact, since the flow properties ahead of the expansion are constant, all C+ lines will have the same J+ value.

J invariants constant along C characteristics

Jc=Jd(Eq. 6.138)
Je=Jf(Eq. 6.139)
ue=12(Je++Je)uf=12(Jf++Jf)Je=JfJe+=Jf+}ue=ufae=af(Eq. 6.140)

Due to the fact the J+ is constant in the entire expansion region, u and a will be constant along each C line.

The constant J+ value can be used to obtain relations for the variation of flow properties through the expansion region. Evaluation of the J+ invariant at any position within the expansion region should give the same value as in region 4.

u+2aγ1=u4+2a4γ1=0+2a4γ1(Eq. 6.141)

and thus

aa4=1γ12(ua4)(Eq. 6.142)

Eqn. \ref{eq:expansion:a} and a=γRT gives

TT4=[1γ12(ua4)]2(Eq. 6.143)

Using isentropic relations, we can get pressure ratio and density ratio

pp4=[1γ12(ua4)]2γ/(γ1)(Eq. 6.144)
ρρ4=[1γ12(ua4)]2/(γ1)(Eq. 6.145)

Shock-tube relations

From the analysis of the incident shock, we have a relation for the induced flow behind the shock

u2=up=a1γ1(p2p11)((2γ1γ1+1)(γ11γ1+1)+(p2p1))1/2(Eq. 6.146)

The velocity in region 3 can be obtained from the expansion relations

p3p4=[1γ412(u3a4)]2γ4/(γ41)(Eq. 6.147)

Solving for u3 gives

u3=2a4γ41[1(p3p4)(γ41)/(2γ4)](Eq. 6.148)

There is no change in pressure or velocity over the contact surface, which means u2=u3 and p2=p3.

u2=2a4γ41[1(p2p4)(γ41)/(2γ4)](Eq. 6.149)

Now, we have two ways of calculating u2. Setting Eqn. \ref{eq:shocktube:up:a} equal to Eqn. \ref{eq:shocktube:up:d} leads to the shock tube relation

p4p1=p2p1{1(γ41)(a1/a4)(p2/p11)2γ1[2γ1+(γ1+1)(p2/p11)]}2γ4/(γ41)(Eq. 6.150)