Is dn = dS = 0 when two phases are equilibrium?

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Discussion Overview

The discussion revolves around the conditions of phase equilibrium in thermodynamics, specifically whether differentials of state variables (such as entropy, particle number, and volume) are zero when two phases are in equilibrium. Participants explore the implications of these conditions on thermodynamic equilibrium and the definitions involved.

Discussion Character

  • Debate/contested
  • Conceptual clarification
  • Technical explanation

Main Points Raised

  • One participant suggests that at phase equilibrium, all differentials (dS, dn, dV) should be zero, which leads to contradictions in deriving conditions for thermal, mechanical, and diffusive equilibrium.
  • Another participant argues that if macroscopic state variables are not constant, the system cannot be considered in equilibrium, citing examples like changing color in a solution.
  • A different viewpoint is presented, stating that a mixture of ice and water can be in equilibrium even as ice melts, challenging the notion that all state variables must remain constant.
  • Some participants discuss the relationship between phase equilibrium and thermodynamic equilibrium, with one stating that phase equilibrium is a special case of thermodynamic equilibrium.
  • There is a debate about the definitions of equilibrium, with one participant asserting that equilibrium is defined by maximum entropy under certain conditions, while others point out that this may depend on the system's constraints (e.g., constant temperature, pressure).
  • Another participant mentions that in equilibrium thermodynamics, only thermodynamic equilibrium states are considered, suggesting that phase equilibria are a subset of thermodynamic equilibria.
  • One participant proposes that the definitions of phase and thermodynamic equilibrium are somewhat circular and that there are more phase equilibria than thermodynamic equilibria.
  • Further discussion includes the conditions under which total internal energy, volume, and particle number remain constant in an isolated system, leading to the conclusion that temperature and other state variables must equalize at equilibrium.

Areas of Agreement / Disagreement

Participants express differing views on the relationship between phase equilibrium and thermodynamic equilibrium, with no consensus reached on whether all differentials must be zero at equilibrium. The discussion remains unresolved regarding the definitions and implications of equilibrium in thermodynamics.

Contextual Notes

Participants highlight that the definitions of equilibrium may depend on specific system conditions, such as whether the system is isolated or subject to external work. There are also unresolved questions about the implications of these definitions on the behavior of systems at equilibrium.

Philethan
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Hello, every one! I'm studying the Section 9.2 - Phase Equilibrium of "Classical and Statistical Thermodynamics" written by Carter.

In equation (9.21) and (9.22)

He said:

dS_{A}=\frac{1}{T_{A}}(dU_{A}+P_{A}dV_{A}-\mu _{A}dn_{A})-----(9.21)

dS_{B}=\frac{1}{T_{B}}(dU_{B}+P_{B}dV_{B}-\mu _{B}dn_{B})-----(9.22)

I think dS and differentials of all other state variables should be zero! That is, dSA=dSB=dnA=dnB=dVA=dVB=...=0

Is it correct? If it's correct, then I cannot get the following conclusions which needs to assume those increments dUA,dVA,dnA,... could be arbitrary.

TA = TB (thermal equilibrium)
PA = PB (mechanical equilibrium)
μA = μB (diffusive equilibrium)

Thanks in advance!
 
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No, why should these differential be constant?
 
DrDu said:
No, why should these differential be constant?
It's due to the definition of equilibrium. In other words, if those macroscopic state variables are not constant, then it's not at equilibrium.
For example, if the color of the solution is changing, then it's not at equilibrium.

I don't know why I was wrong..
 
But e.g. you can have a mixture of ice and water and even if some of the ice is melting (i.e. both the amount of ice and water is changing), the two are in equilibrium.
 
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Really? Even if some of the ice is melting, the two are still in equilibrium?
So... What's the definition of equilibrium? It seems that the exact definition of equilibrium is "the system is at equilibrium if and only if its entropy is a maximum".

Is that correct?

Thank you very much :)
 
I think DD is straying somewhat. A phase equilibrium is not enough for a thermodynamic equilibrium: matter and energy can still flow macroscopically.
So I'm siding with PhE post #5.
However, physics isn't a democratic thingy, so if someone knows better, I'm eager to be put right !
 
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BvU said:
I think DD is straying somewhat. A phase equilibrium is not enough for a thermodynamic equilibrium: matter and energy can still flow macroscopically.
I'd rather say that phase equilibrium is a special case of thermodynamic equilibrium.
 
Philethan said:
Really? Even if some of the ice is melting, the two are still in equilibrium?
At equilibrium, the system is insensitive to changes in particle number of the two phases.

So... What's the definition of equilibrium? It seems that the exact definition of equilibrium is "the system is at equilibrium if and only if its entropy is a maximum".

Is that correct?

Thank you very much :)
This depends on the system. Is it thermally isolated or constant temperature, constant volume or constant pressure. E.g. at constant temperature and pressure, free enthalpy has to be maximal, not entropy. Which case is your book considering?
 
We aren't making progress here if I rather say that thermodynamic equilibrium is a special case of phase equilibrium, namely phase equilibrium plus constant P, U, G, A, H, S etc... :smile:
 
  • #10
I don't know what you have in mind, but in equilibrium thermodynamics (I suppose we are talking about this) we are considering only thermodynamic equilibrium states. E.g. considering the state diagram of water as a function of p and T, there is one line where both phases are in equilibrium. In this sense, phase equilibria are a subset of thermodynamic equilibria.
 
  • #11
DrDu said:
in equilibrium thermodynamics (I suppose we are talking about this) we are considering only thermodynamic equilibrium states
Somewhat circular, to me that seems.

The 'subset' issue is a matter of language, it seems to me. I think we agree: phase equilibrium isn't thermodynamic equilibrium, but thermodynamic equilibrium is phase equilibrium.

(The "fruit isn't orange but orange is fruit" comes to mind. For me that makes oranges a subset of fruit. Not the other way around).

Yet another approach: there are a lot more phase equilibria than thermodynamic equilibria. A TE is a PE with some extra restrictions. So TE is a subset of PE.

DrDu said:
considering the state diagram of water as a function of p and T, there is one line where both phases are in equilibrium
If a system is moving back and forth over this line where both phases are in equilibrium, I can not consider that system to be in thermodynamic equilibrium: T changes. [edit] woops, V changes.
 
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  • #12
Philethan said:
It seems that the exact definition of equilibrium is "the system is at equilibrium if and only if its entropy is a maximum".
This is true if the system is isolated and there is also no work done on the overall system. Then it is clear that ##dU_B=-dU_A##, ##dV_B=-dV_A## and ##dn_B=-dn_A## as total internal energy, volume and particle number of the two phases taken together is constant. As total S is maximal, we can write ##0=\partial S/\partial U_A=1/T_A-1/T_B##, so that ##T_A=T_B##. Analogous equations hold for p and ##
mu##.
 
  • #13
DrDu said:
This is true if the system is isolated and there is also no work done on the overall system. Then it is clear that ##dU_B=-dU_A##, ##dV_B=-dV_A## and ##dn_B=-dn_A## as total internal energy, volume and particle number of the two phases taken together is constant. As total S is maximal, we can write ##0=\partial S/\partial U_A=1/T_A-1/T_B##, so that ##T_A=T_B##. Analogous equations hold for p and ##
mu##.
Yes. I think this is more like what the original question was getting at. The idea is to look at the combined system in a situation where the combination is isolated.
 
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