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Next: Implications Up: Lecture_17_web Previous: Equilibrium Thermodynamics

Unconstrained Equilibrium

Consider a an isolated system, in this case:

\bgroup\color{blue}$ dU = 0$\egroup and \bgroup\color{blue}$ dV = 0$\egroup

If we consider a system that can only perform \bgroup\color{blue}$ PV$\egroup-work on its surroundings, we can write for any quasi-static (constantly in equilibrium).

$\displaystyle \input{equations/11-3A}$ (17-1)

Therefore, at equilibrium the entropy must be a maximum or a minimum ( \bgroup\color{blue}$ dS =
0$\egroup) (This is the equation of a tangent plane)

Figure 17-2: The surface of $ S$ as a function of $ U$ and $ V$
\begin{figure}\resizebox{6in}{!}
{\epsfig{file=figures/S-surf.eps}}
\end{figure}


Since entropy must always increase as a system approaches equilibrium, it must be a maximum at equilibrium. (In other words, it must be at the summit of a hill with \bgroup\color{blue}$ U$\egroup given as north and \bgroup\color{blue}$ V$\egroup given as west.)

How to express this maximal relationship?

Let \bgroup\color{blue}$ \ensuremath{\delta}S$\egroup represent any possible variation (change internal temperature, distribution, heat flow, etc.) to the entropy. Then, if the supposed variation also has \bgroup\color{blue}$ \ensuremath{\delta}U = \ensuremath{\delta}V = 0$\egroup,


$\displaystyle \input{equations/gibbs-eq-1}$ (17-2)

implies \bgroup\color{blue}$ S$\egroup is a maximum and is thus the equilibrium state.

This introduces the concept of a virtual change:


Equation 17-2 is equivalent to

$\displaystyle \input{equations/gibbs-eq-2}$ (17-3)

(See if you can figure out why--hint: \bgroup\color{blue}$ ({\partial U}/{\partial S})_V = T >0$\egroup

Implies \bgroup\color{blue}$ U$\egroup is a minimum at constant \bgroup\color{blue}$ S$\egroup and \bgroup\color{blue}$ V$\egroup--and that is what we expect from mechanics.

Figure 17-3: Ball rolling on a surface.
\begin{figure}\resizebox{6in}{!}
{\epsfig{file=figures/ball.eps}}
\end{figure}



next up previous
Next: Implications Up: Lecture_17_web Previous: Equilibrium Thermodynamics
W. Craig Carter 2002-10-17