Cole equation of state: Difference between revisions

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:<math>c^2 = \frac{\gamma B}{\rho_0}. </math>
:<math>c^2 = \frac{\gamma B}{\rho_0}. </math>


where <math>\gamma</math> is the [[Heat capacity#Adiabatic index | adiabatic index]].
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.

Revision as of 16:02, 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.

where γ is the adiabatic index. 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 equation of state 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