Cole equation of state: Difference between revisions
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The '''Cole equation of state''' <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> | ||
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> | ||
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\right]</math> | \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 13:16, 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
In it, is a reference density around which the density varies, is the adiabatic index, and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle 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 Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle B} is large, in the following sense. The fluctuations of the density are related to the speed of sound as
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \frac{\delta \rho}{\rho} = \frac{v^2}{c^2} ,}
where Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle v} is the largest velocity, and is the speed of sound (the ratio Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle v/c} is Mach's number). The speed of sound can be seen to be
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle c^2 = \frac{\gamma B}{\rho_0}. }
Therefore, if Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle B=100 \rho_0 v^2 / \gamma} , 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:
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle p = B \gamma \left[ \frac{\rho-\rho_0}{\rho_0} \right]}
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
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
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle dW= -p dV = dE .}
Taking differences on the EOS,
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle dE = \frac{1}{\gamma-1} [(p+p^*) dV + V dp ] , }
so that the first law can be simplified to
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle - (\gamma p + p^*) dV = V dp.}
This equation can be solved in the standard way, with the result
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle ( p + p^* / \gamma) V^\gamma = 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 .
If the values of the thermodynamic variables are known at some reference state, we may write
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle ( p + p^* / \gamma) V^\gamma = ( p_0 + p^* / \gamma) V_0^\gamma , }
which can be written as
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle p = p_0 + ( p_0 + p^* / \gamma) ( (V_0/V)^\gamma - 1 ) . }
Going back to densities, instead of volumes,
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle p = p_0 + ( p_0 + p^* / \gamma) ( (\rho/\rho_0)^\gamma - 1) . }
Comparing with the Cole EOS, we can readily identify
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle B = p^* / \gamma }
Moreover, the Cole EOS differs slightly, as it should read (as indeed does in e.g. the book by Courant)
with
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle A = p^* / \gamma + p_0 . }
This difference is negligible for liquids but for an ideal gas Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle 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
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle c^2=\frac{dp}{d\rho} }
with the derivative taken along an adiabatic line. This is precisely our case, and we readily obtain
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle c^2= ( p_0 + p^* / \gamma) \gamma /\rho_0 . }
From this expression a value of can be deduced. For water, Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle p^*\approx 23000} bar, from which Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle B\approx 3000} bar. If the speed of sound is used in the EOS one obtains the rather elegant expression
- Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle p = p_0 + ( \rho_0 c^2 / \gamma) ( (\rho/\rho_0)^\gamma - 1) . }
References[edit]
- ↑ Robert H Cole "Underwater explosions", Princeton University Press, Princeton (1948)
- ↑ G. K. Batchelor "An introduction to fluid mechanics", Cambridge University Press (1974) ISBN 0521663962
- ↑ 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)