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</ref><ref>
The '''Cole equation of state''' <ref>R. H. Cole "Underwater Explosions", Princeton University Press (1948) ISBN 9780691069227</ref><ref>
G.K. Batchelor, An introduction to fluid mechanics. Cambridge University Press 1974 </ref>
G. K. Batchelor "An introduction to fluid mechanics", Cambridge University Press (1974) ISBN  0521663962</ref>
can be written, when atmospheric pressure is negligible, has the form
can be written, when atmospheric pressure is negligible, has the form



Revision as of 15:11, 5 September 2011

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.

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