Cole equation of state: Difference between revisions

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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 of about 0.01.
If the fluctuations in the density are indeed small, the
EOS may be rewritten thus:
:<math>p = B \gamma \left[
\frac{\rho-\rho_0}{\rho_0}
\right]</math>


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

Revision as of 12:59, 23 May 2012

The Cole equation of state [1][2] can be written, when atmospheric pressure is negligible, has the form

p=B[(ρρ0)γ−1].

In it, ρ0 is a reference density around which the density varies γ is an exponent 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 of about 0.01.

If the fluctuations in the density are indeed small, the EOS may be rewritten thus:

p=Bγ[ρ−ρ0ρ0]


References

  1. ↑ R. H. Cole "Underwater Explosions", Princeton University Press (1948) ISBN 9780691069227
  2. ↑ G. K. Batchelor "An introduction to fluid mechanics", Cambridge University Press (1974) ISBN 0521663962