Harman Patil (Editor)

Entropy (astrophysics)

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In astrophysics, what is referred to as "entropy" is actually the adiabatic constant derived as follows.

Using the first law of thermodynamics for a quasi-static, infinitesimal process for a hydrostatic system

d Q = d U d W .

For an ideal gas in this special case, the internal energy, U, is only a function of the temperature T; therefore the partial derivative of heat capacity with respect to T is identically the same as the full derivative, yielding through some manipulation

d Q = C V d T + P d V .

Further manipulation using the differential version of the ideal gas law, the previous equation, and assuming constant pressure, one finds

d Q = C P d T V d P .

For an adiabatic process d Q = 0 and recalling γ = C P C V , one finds

One can solve this simple differential equation to find

P V γ = constant = K

This equation is known as an expression for the adiabatic constant, K, also called the adiabat. From the ideal gas equation one also knows

P = ρ k B T μ m H ,

where k B is Boltzmann's constant. Substituting this into the above equation along with V = [ g r a m s ] / ρ and γ = 5 / 3 for an ideal monatomic gas one finds

K = k B T μ m H ρ 2 / 3 ,

where μ is the mean molecular weight of the gas or plasma; and m H is the mass of the Hydrogen atom, which is extremely close to the mass of the proton, m p , the quantity more often used in astrophysical theory of galaxy clusters. This is what astrophysicists refer to as "entropy" and has units of [keV cm2]. This quantity relates to the thermodynamic entropy as

S = k B ln Ω + S 0

where Ω , the density of states in statistical theory, takes on the value of K as defined above.

References

Entropy (astrophysics) Wikipedia