Thermodynamic equation of differentials (and how to work with them)

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SUMMARY

The discussion centers on the thermodynamic identity expressed in differential form as dU = TdS - PdV + \mu dN, where U is internal energy, T is temperature, S is entropy, P is pressure, V is volume, \mu is chemical potential, and N is the number of particles. The participant explores the implications of this identity for a monoatomic ideal gas at height z above sea level, leading to the conclusion that the chemical potential \mu(z) includes an additional term mgz due to gravitational potential energy. The participant expresses confusion regarding the manipulation of these equations and the treatment of gravitational energy in relation to internal energy and the Sackur-Tetrode equation.

PREREQUISITES
  • Understanding of thermodynamic identities and their differential forms
  • Familiarity with the Sackur-Tetrode equation for entropy
  • Knowledge of the ideal gas law and its implications
  • Basic principles of statistical mechanics, particularly the equipartition theorem
NEXT STEPS
  • Study the derivation and applications of the Sackur-Tetrode equation in detail
  • Learn about the implications of gravitational potential energy on thermodynamic properties
  • Explore the mathematical techniques for manipulating thermodynamic identities
  • Investigate the relationship between chemical potential and entropy in various systems
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Physicists, thermodynamics students, and researchers interested in the mathematical foundations of thermodynamic equations and their applications to ideal gases in varying gravitational fields.

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Disclaimer: I am not a mathematician, I am a physicist.

The thermodynamic identity is usually expressed in the following differential form

$$
dU = TdS - PdV + \mu dN,
$$

where U , T, S, P, V, \mu and N are the internal energy, temperature, entropy, pressure, volume, chemical potential and number of particles of the system respectively. If I am not mistaken, I can act with a vector, say \frac{\partial}{\partial N}, to yield

$$
\frac{\partial U}{\partial N} = T \frac{\partial S}{\partial N} - P \frac{\partial V}{\partial N} + \mu \implies \mu = \frac{\partial U}{\partial N} - T \frac{\partial S}{\partial N} + P \frac{\partial V}{\partial N}.
$$

Consider the following question:

Consider a monoatomic ideal gas that lives at height z above sea level, so each molecule has potential energy mgz in addition to its kinetic energy. Show that the chemical potential \mu is the same as if the gas were at sea level, plus am additional term mgz:

$$
\mu(z) = -k_b T \text{ln}\left[\frac{V}{N}\left(\frac{2\pi m k_bT}{h^2}\right)^{3/2}\right] + mgz.
$$My attempt was knowing that:

The "ideal monoatomic gas" implies U = \frac{3}{2}k_bT (by equipartition theorem) and the validity of Sackur-Tetrode equation:

$$
S=k_bN\ln \left[{\frac {V}{N}}\left({\frac {4\pi m}{3h^{2}}}{\frac {U}{N}}\right)^{3/2}\right]+{\frac {5}{2}},
$$

together with the assumption that V \neq V(N). If one uses the above formula for \mu and takes the partial derivatives I yield

$$
\mu(z) = -k_b T \text{ln}\left[\frac{V}{N}\left(\frac{2\pi m k_bT}{h^2}\right)^{3/2}-\frac{3}{2}\right] + mgz,
$$

which is almost correct except for that -\frac{3}{2}, although it still exhibits the problems described below.

I came to the conclusion that I don't know how to manipulate these equations in differential form, am I allowed to do the above "act with \frac{\partial}{\partial N}" business? The solution provided by the book is to say, hey hold U and V fixed so that the thermodynamic identity now reads

$$
0 = TdS - 0 + \mu dN \implies \mu = T \left(\frac{\partial S}{\partial N}\right)_{V,U \text{ fixed}}
$$

but U = U(N), in particular U = \frac{3}{2} k_b N T I could litterally make all the Ns in S disappear by substituting N = \frac{2 U}{3 k_b T} and claim that

$$
\mu = T \left(\frac{\partial S}{\partial N}\right)_{V,U \text{ fixed}} = 0,
$$

which is ridiculous. I'm really lost with the mathematics behind this type of calculations... Which would be the correct way to proceed?
 
Science news on Phys.org
Here gravity or gravitational energy is considered for chemical potential. It is not considered for internal energy and Sackur-Tetrode equation. Why don't you treat them in a same way ?
 

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