Polytropic process

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A polytropic process is a thermodynamic process that a system undergoes that obeys the relation

pVn = K,

where p is pressure, V is volume, n is any real number, and K is a constant. Since this is a definition, it is absolutely general. The rest refers exclusively to ideal gases, where the processes are usually categorized more specifically depending on the index n:

Note that 1 \le \gamma \le 2, since \gamma=\frac{c_p}{c_V}=\frac{c_V+R}{c_V}=1+\frac{R}{c_V}


Any number between two of this values means that the polytropic curve will lay between the corresponding curves.

The equation is valid assuming that

  • the process is quasistatic, and
  • the values of the heat capacities (cp and cV) are almost constant (Actually, they depend on the temperature, but are linear within small changes).

[edit] Polytropic fluids

Polytropic fluids are idealized fluid models that are used often in astrophysics. A polytropic fluid is a type of barotropic fluid for which the equation of state is written as

P = Kρ(1 + 1 / n)

where P is the pressure, K is a constant, ρ is the density, and n is a quantity called the polytropic index.

This is also commonly written in the form

P = Kργ

Note that γ need not be the adiabatic index (or ratio of specific heats), and in fact often it is not. This is sometimes a cause for confusion.

In the case of an isentropic ideal gas, γ is the ratio of specific heats, or adiabatic index:

\gamma =  \frac{c_P}{ c_V}

An isothermal ideal gas is also a polytropic gas. Here, the polytropic γ differs from the adiabatic index γ, and in particular it is equal to one: γ = 1.

In order to discriminate between the two gammas, the polytropic gamma is sometimes capitalized, Γ.

To confuse matters further, some authors refer to Γ as the polytropic index, rather than n. Note that

n = \frac{1}{\Gamma - 1}.

A solution to the Lane-Emden equation using a polytropic fluid is known as a polytrope.

[edit] See also

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