Using Homogenuous Functions to Understand Thermodynamics

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Homogeneous functions of degree r can be applied in thermodynamics to express relationships such as dU=TdS-pdV+μdN, leading to U=TS-pV+μN when U is a homogeneous function of degree 1. This assumption holds true for macroscopic quantities of substances, where doubling the amount also doubles the energy, volume, and entropy. Exceptions arise with very small quantities, such as individual molecules, where energy does not simply double. Additionally, the assumption fails in scenarios with significant long-range interactions, like in astrophysical contexts. The discussion highlights the practical applicability of homogeneous functions in thermodynamic analysis.
Petar Mali
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If I have homogenuous function f(x,y,z,...) of degree r than:
x\frac{\partial f}{\partial x}+y\frac{\partial f}{\partial y}+...=rf

In thermodynamics:
dU=TdS-pdV+\mu dN

If I said U is homogenuous function of degree 1 I will get

U=TS-pV+\mu N

When can I use this assumption?
 
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You can almost always use this assumption. It amounts to the assumption that when you have some substance, and you double the amount of it, and so its volume and entropy, you also double the energy. This will be true for macroscopic amounts of a substance.

The only exceptions occur for very small amounts of a substance. If you have one molecule, and then you add one more, the energy is not just doubled. Same goes for going from two molecules to four. It will start working when there is enough of the substance that the effects of the surface are negligible and you basically have a totally homogeneous material.
 
You also have to assume that there are no long range interactions between the molecules. So e.g., in astrophysical problems where gravity is important you cannot make this assumption.
 
Thanks!
 
Hi!
You know..? This is exacly what I need for my thesis.
In which mathematic books can I find that theorem?
 
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