Cole equation of state: Difference between revisions

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The '''Cole equation of state''' <ref>R. H. Cole "Underwater Explosions", Princeton University Press (1948) ISBN 9780691069227</ref><ref>
The '''Cole equation of state'''
G. K. Batchelor "An introduction to fluid mechanics", Cambridge University Press (1974) ISBN  0521663962</ref>
<ref>[http://www.archive.org/details/underwaterexplos00cole Robert H Cole "Underwater explosions", Princeton University Press, Princeton (1948)]</ref><ref>G. K. Batchelor "An introduction to fluid mechanics", Cambridge University Press (1974) ISBN  0521663962</ref><ref>[http://www.archive.org/details/supersonicflowsh00cour Richard Courant "Supersonic flow and shock waves a manual on the mathematical theory of non-linear wave motion", Courant Institute of Mathematical Sciences, New York University, New York (1944)]</ref>
can be written, when atmospheric pressure is negligible, has the form
is the adiabatic version of the [[stiffened equation of state]] for liquids. (See ''Derivation'', below.)
It has the form


:<math>p = B \left[ \left( \frac{\rho}{\rho_0} \right)^\gamma  -1 \right]</math>.
:<math>p = B \left[ \left( \frac{\rho}{\rho_0} \right)^\gamma  -1 \right]</math>


In it, <math>\rho_0</math> is a reference density around which the density varies
In it, <math>\rho_0</math> is a reference density around which the density varies,
<math>\gamma</math> is an exponent and <math>B</math> is a pressure parameter.
<math>\gamma</math> is the [[Heat capacity#Adiabatic index | adiabatic index]], and <math>B</math> is a pressure parameter.


Usually, the equation is used to model a nearly incompressible system. In this case,
Usually, the equation is used to model a nearly incompressible system. In this case,
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where <math>v</math> is the largest velocity, and <math>c</math> is the speed of
where <math>v</math> is the largest velocity, and <math>c</math> is the speed of
sound (the ratio <math>v/c</math> is [[Mach's number]]). The speed of sound can
sound (the ratio <math>v/c</math> is [[Mach's number]]). The [[speed of sound]] can
be seen to be
be seen to be


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Therefore, if <math>B=100 \rho_0 v^2 / \gamma</math>, the relative density fluctuations
Therefore, if <math>B=100 \rho_0 v^2 / \gamma</math>, the relative density fluctuations
will be of about 0.01.
will be about 0.01.
 
If the fluctuations in the density are indeed small, the
[[Equations of state | equation of state]] may be approximated by the simpler:
 
:<math>p = B \gamma \left[
\frac{\rho-\rho_0}{\rho_0}
\right]</math>
 
 
It is quite common that the name "[[Tait equation of state]]" is improperly used for this EOS. This perhaps stems for the classic text by Cole calling this equation a "modified Tait equation" (p. 39).
 
==Derivation==
 
Let us write the stiffened EOS as
 
:<math>p+ p^* = (\gamma -1) e \rho = (\gamma -1) E / V ,</math>
 
where ''E'' is the internal energy. In an adiabatic process, the work is the only responsible of a change in internal energy. Hence the
first law reads
 
:<math>  dW= -p dV  = dE .</math>
 
Taking differences on the EOS,
 
:<math>  dE = \frac{1}{\gamma-1} [(p+p^*) dV + V dp ] , </math>
 
so that the first law can be simplified to
 
:<math>  - (\gamma p + p^*)  dV  = V dp.</math>
 
This equation can be solved in the standard way, with the result
 
:<math>  ( p + p^* / \gamma)  V^\gamma  = C ,</math>
 
where ''C'' is a constant of integration. This derivation closely follows the standard derivation of the adiabatic law
of an ideal gas, and it reduces to it if <math>  p^*  =0 </math>.
 
If the values of the thermodynamic variables are known at some reference state, we may write
 
:<math>  ( p + p^* / \gamma)  V^\gamma  =  ( p_0 + p^* / \gamma)  V_0^\gamma , </math>
 
which can be written as
 
:<math>  p      =  p_0 +  ( p_0 + p^* / \gamma) ( (V_0/V)^\gamma - 1 )  . </math>
 
Going back to densities, instead of volumes,
 
:<math>  p      =  p_0 +  ( p_0 + p^* / \gamma)  ( (\rho/\rho_0)^\gamma - 1) . </math>
 
Comparing with the Cole EOS, we can readily identify
 
:<math> B = p^* / \gamma  </math>
 
Moreover, the Cole EOS differs slightly, as it should read (as indeed does in e.g. the book by Courant)
 
:<math>p = A \left( \frac{\rho}{\rho_0} \right)^\gamma  - B ,</math>
 
with
 
:<math> A = p^* / \gamma  + p_0 . </math>
 
This difference is negligible for liquids but for an ideal gas <math>p^*=0</math> and there is a huge
difference, ''B'' being zero and ''A'' being equal to the reference pressure.
 
Now, the speed of sound is given by
 
:<math>  c^2=\frac{dp}{d\rho}  </math>
 
with the derivative taken along an adiabatic line. This is precisely our case, and we readily obtain
 
:<math>  c^2=  ( p_0 + p^* / \gamma) \gamma /\rho_0 . </math>
 
From this expression a value of <math>p^*</math> can be deduced. For water, <math>p^*\approx 23000</math> bar,
from which <math>B\approx 3000</math> bar. If the speed of sound is used in the EOS one obtains the rather
elegant expression
 
 
:<math>  p      =  p_0 +  ( \rho_0 c^2 / \gamma)  ( (\rho/\rho_0)^\gamma - 1) . </math>


==References==
==References==
<references/>
<references/>
[[category: equations of state]]
[[category: equations of state]]

Latest revision as of 14:16, 5 December 2015

The Cole equation of state [1][2][3] is the adiabatic version of the stiffened equation of state for liquids. (See Derivation, below.) It has the form

p=B[(ρρ0)γ−1]

In it, ρ0 is a reference density around which the density varies, γ is the adiabatic index, and B is a pressure parameter.

Usually, the equation is used to model a nearly incompressible system. In this case, the exponent is often set to a value of 7, and B is large, in the following sense. The fluctuations of the density are related to the speed of sound as

δρρ=v2c2,

where v is the largest velocity, and c is the speed of sound (the ratio v/c is Mach's number). The speed of sound can be seen to be

c2=γBρ0.

Therefore, if B=100ρ0v2/γ, the relative density fluctuations will be about 0.01.

If the fluctuations in the density are indeed small, the equation of state may be approximated by the simpler:

p=Bγ[ρ−ρ0ρ0]


It is quite common that the name "Tait equation of state" is improperly used for this EOS. This perhaps stems for the classic text by Cole calling this equation a "modified Tait equation" (p. 39).

Derivation[edit]

Let us write the stiffened EOS as

p+p*=(γ−1)eρ=(γ−1)E/V,

where E is the internal energy. In an adiabatic process, the work is the only responsible of a change in internal energy. Hence the first law reads

dW=−pdV=dE.

Taking differences on the EOS,

dE=1γ−1[(p+p*)dV+Vdp],

so that the first law can be simplified to

−(γp+p*)dV=Vdp.

This equation can be solved in the standard way, with the result

(p+p*/γ)Vγ=C,

where C is a constant of integration. This derivation closely follows the standard derivation of the adiabatic law of an ideal gas, and it reduces to it if p*=0.

If the values of the thermodynamic variables are known at some reference state, we may write

(p+p*/γ)Vγ=(p0+p*/γ)V0γ,

which can be written as

p=p0+(p0+p*/γ)((V0/V)γ−1).

Going back to densities, instead of volumes,

p=p0+(p0+p*/γ)((ρ/ρ0)γ−1).

Comparing with the Cole EOS, we can readily identify

B=p*/γ

Moreover, the Cole EOS differs slightly, as it should read (as indeed does in e.g. the book by Courant)

p=A(ρρ0)γ−B,

with

A=p*/γ+p0.

This difference is negligible for liquids but for an ideal gas p*=0 and there is a huge difference, B being zero and A being equal to the reference pressure.

Now, the speed of sound is given by

c2=dpdρ

with the derivative taken along an adiabatic line. This is precisely our case, and we readily obtain

c2=(p0+p*/γ)γ/ρ0.

From this expression a value of p* can be deduced. For water, p*≈23000 bar, from which B≈3000 bar. If the speed of sound is used in the EOS one obtains the rather elegant expression


p=p0+(ρ0c2/γ)((ρ/ρ0)γ−1).

References[edit]