Thermodynamics: Defining Pressure

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The discussion centers on the relationship between pressure, temperature, and entropy in thermodynamics, specifically the equation P = T (∂S/∂V)U,N. It highlights that pressure is well-defined only in systems at thermal equilibrium, as non-equilibrium systems exhibit varying pressures. The derivation of this relationship stems from the first law of thermodynamics, leading to the equation TdS = dU + PdV, which clarifies how pressure relates to heat flow and volume change when energy and particle number are constant. The conversation also touches on the complexities of extending this understanding to non-equilibrium thermodynamics and the behavior of systems over time. Understanding these principles is crucial for grasping the dynamics of energy exchange and system behavior in thermodynamic contexts.
matsciguy
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I'm trying to understand the relation:

P=T (∂S/∂V)U,N.

I understand the definition of temperature as:

1/T =(∂S/∂U)V,N.

The relation for pressure has a similar derivation, but how can T be thrown in there? In my textbook, the author derives the relation for two systems in thermal equilibrium. Are we supposed to only compare the pressures of systems in thermal equilibrium? I'm clearly a little confused -- any help would be appreciated.
 
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Pressure as a single value is only well defined for a system in equilibrium, because if the system were not in equilibrium then the pressure would generally vary throughout the system. So unless you are studying non-equilibrium thermodynamics you will only compare pressures of systems in equilibrium
 
matsciguy said:
I'm trying to understand the relation:

P=T (∂S/∂V)U,N.

I understand the definition of temperature as:

1/T =(∂S/∂U)V,N.

The relation for pressure has a similar derivation, but how can T be thrown in there? In my textbook, the author derives the relation for two systems in thermal equilibrium. Are we supposed to only compare the pressures of systems in thermal equilibrium? I'm clearly a little confused -- any help would be appreciated.

As far as fluids and other such things, you consider them as a collection of many subsystems, each of which have a well defined pressure. in the continuous limit, you get a continuous variation of pressure.

As was said before, to consider the behavior of such systems in time, we need to look at non equilibrium thermodynamics, namely kinetics and transport theory in general. That will teach you about diffusion and the forces that drive the system as a whole toward equilibrium. You may want to look into the Boltzmann transport equation in particular.
 
Thank you.

Perhaps I'm thinking about this wrong. But:

Say we have two systems that can exchange energy only. Their respective volumes are held constant, as well as number of particles, and total energy between them.

The definition of temperature gives us a basis for seeing which way energy will flow in this system, knowing entropy of the total system to increase. Compare the derivatives for different distributions of energy.

I'm having a hard time extending this intuition to pressure, given the extra T. (Or likewise, chemical potential.) I'm not sure what systems could have constant energy and number of particles and exchange volume only. Nonetheless, the situation seems akin to multiplying (∂S/∂V)U,N by P, in which case I'm not sure about its comparative value.
 
Alternatively you can define pressure as the change in energy of the system with respect to volume.
 
matsciguy said:
I'm trying to understand the relation:

P=T (∂S/∂V)U,N.

I understand the definition of temperature as:

1/T =(∂S/∂U)V,N.

The relation for pressure has a similar derivation, but how can T be thrown in there? In my textbook, the author derives the relation for two systems in thermal equilibrium. Are we supposed to only compare the pressures of systems in thermal equilibrium? I'm clearly a little confused -- any help would be appreciated.
It follows from the first law, which leads to the fundamental equation of thermodynamics: TdS = dU + PdV

If you start with TdS = dU + PdV, and keep U and N constant (dU = 0), then:

T\left(\frac{\partial S}{\partial V}\right)_{U, N} = P\left(\frac{\partial V}{\partial V}\right)_{U, N} = P

This means that pressure is the rate of heat flow with respect to change in volume in a reversible process where U and N are held constant. For an ideal gas, of course, holding U constant means T is constant. So this is simply saying that the work done in a quasi-static isothermal process is equal to the heat flow.

AM
 
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