Cole equation of state: Difference between revisions

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(Derivation complete. Formulas a bit ugly, will make them nicer soon)
(space inserted between 'the' and 'EOS' for friendly reading)
 
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The '''Cole equation of state'''
The '''Cole equation of state'''
<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>
<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>
is the adiabatic version of the [[stiffened equation of state]]. (See ''Derivation'', below.)
is the adiabatic version of the [[stiffened equation of state]] for liquids. (See ''Derivation'', below.)
It has the form
It has the form


Line 45: Line 45:
:<math>  dW= -p dV  = dE .</math>
:<math>  dW= -p dV  = dE .</math>


Taking differences on theEOS,
Taking differences on the EOS,


:<math>  dE = \frac{1}{\gamma-1} [(p+p^*) dV + V dp ] , </math>
:<math>  dE = \frac{1}{\gamma-1} [(p+p^*) dV + V dp ] , </math>
Line 76: Line 76:
:<math> B = p^* / \gamma  </math>
:<math> B = p^* / \gamma  </math>


Moreover, the Cole EOS is slightly incorrect, as it should read (as indeed does in e.g. the book by Courant)
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>
:<math>p = A \left( \frac{\rho}{\rho_0} \right)^\gamma  - B ,</math>
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:<math>  p      =  p_0 +  ( \rho_0 c^2 / \gamma)  ( (\rho/\rho_0)^\gamma - 1) . </math>
:<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]