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## 10.1  Equilibrium

Feynman defined equilibrium to be “when all the fast things have happened but the slow things have not” (reference 28). That statement pokes fun at the arbitrariness of the split between “fast” and “slow” – but at the same time it is 100% correct and insightful. There is an element of arbitrariness in our notion of equilibrium. Note the following contrast:

 Over an ultra-long timescale, a diamond will turn into graphite. Over an ultra-short timescale, you can have non-equilibrium distributions of phonons rattling around inside a diamond crystal, such that it doesn’t make sense to talk about the temperature thereof.

 Usually thermodynamics deals with the intermediate timescale, long after the phonons have become thermalized but long before the diamond turns into graphite. During this intermediate timescale it makes sense to talk about the temperature, as well as other thermodynamic properties such as volume, density, entropy, et cetera.

One should neither assume that equilibrium exists, nor that it doesn’t.

• Diamond has a vast, clear-cut separation between the slow timescale and the fast timescale. Most intro-level textbook thermodynamics deal only with systems that have a clean separation.
• In the real world, one often encounters cases where the separation of timescales is not so clean, and an element of arbitrariness is involved. The laws of thermodynamics can still be applied, but more effort and more care is required. See section 11.3 for a discussion.

The word equilibrium is quite ancient. The word has the same stem as the name of the constellation “Libra” — the scale. The type of scale in question is the two-pan balance shown in figure 10.1, which has been in use for at least 7000 years. Figure 10.1: Equilibrium — Forces in Balance

The notion of equilibrium originated in mechanics, long before thermodynamics came along. The compound word “equilibrium” translates literally as “equal balance” and means just that: everything in balance. In the context of mechanics, it means there are no unbalanced forces, as illustrated in the top half of figure 10.2.

Our definition of equilibrium applies to infinitely large systems, to microscopic systems, and to everything in between. This is important because in finite systems, there will be fluctuations even at equilibrium. See section 10.7 for a discussion of fluctuations and other finite-size effects.

## 10.2  Non-Equilibrium; Timescales

The idea of equilibrium is one of the foundation-stones of thermodynamics ... but any worthwhile theory of thermodynamics must also be able to deal with non-equilibrium situations.

Consider for example the familiar Carnot heat engine: It depends on having two heat reservoirs at two different temperatures. There is a well-known and easily-proved theorem (section 14.4) that says at equilibrium, everything must be at the same temperature. Heat bath #1 may be internally in equilibrium with itself at temperature T1, and heat bath may be internally in equilibrium with itself at temperature T2, but the two baths cannot be in equilibrium with each other.

So we must modify Feynman’s idea. We need to identify a timescale of interest such that all the fast things have happened and the slow things have not. This timescale must be long enough so that certain things we want to be in equilibrium have come into equilibrium, yet short enough so that things we want to be in non-equilibrium remain in non-equilibrium.

Here’s another everyday example where non-equilibrium is important: sound. As you know, in a sound wave there will be some points where the air is compressed an other points, a half-wavelength away, where the air is expanded. For ordinary audible sound, this expansion occurs isentropically not isothermally. It you analyze the physics of sound using the isothermal compressibility instead of the isentropic compressibility, you will get the wrong answer. Among other things, your prediction for the speed of sound will be incorrect. This is an easy mistake to make; Isaac Newton made this mistake the first time he analyzed the physics of sound.

Again we invoke the theorem that says in equilibrium, the whole system must be at the same temperature. Since the sound wave is not isothermal, and cannot even be satisfactorily approximated as isothermal, we conclude that any worthwhile theory of thermodynamics must include non-equilibrium thermodynamics.

For a propagating wave, the time (i.e. period) scales like the distance (i.e. wavelength). In contrast, for diffusion and thermal conductivity, the time scales like distance squared. That means that for ultrasound, at high frequencies, a major contribution to the attenuation of the sound wave is thermal conduction between the high-temperature regions (wave crests) and the low-temperature regions (wave troughs). If you go even farther down this road, toward high thermal conductivity and short wavelength, you can get into a regime where sound is well approximated as isothermal. Both the isothermal limit and the isentropic limit have relatively low attenuation; the intermediate case has relatively high attenuation.

## 10.3  Efficiency; Timescales

Questions of efficiency are central to thermodynamics, and have been since Day One (reference 29).

For example in figure 1.3, if we try to extract energy from the battery very quickly, using a very low impedance motor, there will be a huge amount of power dissipated inside the battery, due to the voltage drop across the internal series resistor R1. On the other hand, if we try to extract energy from the battery very slowly, most of the energy will be dissipated inside the battery via the shunt resistor R2 before we have a chance to extract it. So efficiency requires a timescale that is not too fast and not too slow.

Another example is the familiar internal combustion engine. It has a certain tach at which it works most efficiently. The engine is always nonideal because some of the heat of combustion leaks across the boundary into the cylinder block. Any energy that goes into heating up the cylinder block is unavailable for doing P DV work. This nonideality becomes more serious when the engine is turning over slowly. On the other edge of the same sword, when the engine is turning over all quickly, there are all sorts of losses due to friction in the gas, friction between the mechanical parts, et cetera. These losses increase faster than linearly as the tach goes up.

If you have gas in a cylinder with a piston and compress it slowly, you can (probably) treat the process as reversible. On the other hand, if you move the piston suddenly, it will stir the gas. This can be understood macroscopically in terms of sound radiated into the gas, followed by frictional dissipation of the sound wave (section 11.5.1). It can also be understood microscopically in terms of time-dependent perturbation theory; a sudden movement of the piston causes microstate transitions that would otherwise not have occurred (section 11.5.2).

 Timescales matter.

## 10.4  Spontaneity, Irreversibility, Stability, and Equilibrium

Another of the great achievements of thermodynamics is the ability to understand what processes occur spontaneously (and therefore irreversibly) and what processes are reversible (and therefore non-spontaneous). The topic of spontaneity, reversibility, stability, and thermodynamic equilibrium is discussed in depth in chapter 14.

Any theory of thermodynamics that considers only reversible processes – or which formulates its basic laws and concepts in terms of reversible processes – is severely crippled.

If you want to derive the rules that govern spontaneity and irreversibility, as is done in chapter 14, you need to consider perturbations away from equilibrium. If you assume that the perturbed states are in equilibrium, the derivation is guaranteed to give the wrong answer.

In any reversible process, entropy is a conserved quantity. In the real world, entropy is not a conserved quantity.

If you start with a reversible-only equilibrium-only (ROEO) theory of thermodynamics and try to extend it to cover real-world situations, it causes serious conceptual difficulties. For example, consider an irreversible process that creates entropy from scratch in the interior of a thermally-isolated region. Then imagine trying to model it using ROEO ideas. You could try to replace the created entropy by entropy the flowed in from some fake entropy reservoir, but that would just muddy up the already-muddy definition of heat. Does the entropy from the fake entropy reservoir count as “heat”? The question is unanswerable. The “yes” answer is unphysical since it violates the requirement that the system is thermally isolated. The “no” answer violates the basic conservation laws.

Additional examples of irreversible processes that deserve our attention are discussed in sections 10.3, 11.5.1, 11.5.3, 11.5.5, and 11.6.

Any theory of reversible-only equilibrium-only thermodynamics is dead on arrival.

 ROEO = DoA

## 10.5  Stability

The basic ideas of stability and equilibrium are illustrated in figure 10.2. (A more quantitative discussion of stability, equilibrium, spontaneity, reversibility, etc. can be found in chapter 14.) Figure 10.2: Equilibrium and Stability

We can understand stability as follows: Suppose we have two copies (two instances) of the same system. Suppose the initial condition of instance A is slightly different from the initial condition of instance B. If the subsequent behavior of the two copies remains closely similar, we say the system is stable.

More specifically, we define stability as follows: If the difference in the behavior is proportionate to the difference in initial conditions, we say the system is stable. Otherwise it is unstable. This notion of stability was formalized by Lyapunov in the 1880s, although it was understood in less-formal ways long before then.

For a mechanical system, such as in figure 10.2, we can look into the workings of how equilibrium is achieved. In particular,

• Consider the wheel with the weight at the bottom, as shown at the lower left in figure 10.2. Suppose instance A starts out in equilibrium and remains in equilibrium. Instance B starts out at the same position, but is not in equilibrium because of an additional, external, applied force. The applied force gives rise to a displacement, and the displacement gives rise to an internal force that opposes the applied force, eventually canceling the applied force altogether. Such a system has positive static stability.

Note that the equilibrium position in system B is shifted relative to the equilibrium position in system A. Stability does not require the system to return to its original position. It only requires that the response be proportionate to the disturbance.

• Now consider the perfectly balanced wheel. An applied force gives rise to a displacement, and the displacement gives rise to no force whatsoever. Such a system has zero static stability.

If rather than applying a force, we simply move this system to a new position, it will be at equilibrium at the new position. There will be infinitely many equilibrium positions.

• Now consider the wheel with the weight at the top. An applied force gives rise to a displacement. The displacement gives rise to an internal force in the same direction, amplifying the effect of the applied force. We say such a system has negative static stability.

For a non-mechanical system, such as a chemical reaction system, corresponding ideas apply, although you have to work harder to define the notions that correspond to displacement, applied force, restoring force, et cetera.

A system with positive static stability will be stable in the overall sense, unless there is a lot of negative damping or something peculiar like that.

Note that a system can be stable with respect to one kind of disturbance but unstable with respect to another. As a simple example, consider the perfectly balanced wheel, with no damping.

• If system “A” is in equilibrium at rest at position zero, and system “B” is the same except at a different initial position, then the long- term difference in position is proportionate to the disturbance. The system is stable.
• If system “A” is in equilibrium at rest at position zero, and system “B” is the same except with a different initial velocity, then the long-term difference in position is unbounded, completely disproportionate to the disturbance. The system is unstable.

To determine stability, normally you need to consider all the dynamical variables. In the previous example, the long-term velocity difference is bounded, but that doesn’t mean the system is stable, because the long-term position is unbounded.

Properly speaking, a system with zero stability can be called “neutrally unstable”. More loosely speaking, sometimes a system with zero stability is called “neutrally stable”, although that is a misnomer. A so-called “neutrally stable” system is not stable, just as “zero money” is not the same as “money”.

Tangential remark: In chemistry class you may have heard of “Le Châtelier’s principle”. Ever since Le Châtelier’s day there have been two versions of the “principle”, neither of which can be taken seriously, for reasons discussed in section 14.9.

## 10.6  Relationship between Static Stability and Damping

To reiterate: Stability means that two systems that start out with similar initial conditions will follow similar trajectories. Sometimes to avoid confusion, we call this the “overall” stability or the “plain old” stability ... but mostly we just call it the stability.

Meanwhile, static stability arises from a force that depends on position of the system. In contrast, damping refers to a force that depends on the velocity.

The term “dynamic stability” is confusing. Sometimes it refers to damping, and sometimes it refers to the plain old stability, i.e. the overall stability. The ambiguity is semi-understandable and usually harmless, because the only way a system can have positive static stability and negative overall stability is by having negative damping. Figure 10.3: Stability and Damping — Possible Combinations

Static stability can be positive, zero, or negative; damping can also be positive, zero, or negative. A dynamical system can display any combination of these two properties — nine possibilities in all, as shown in figure 10.3. In the top row, the bicycle wheel is dipped in molasses, which provides damping. In the middle row, there is no damping. In the bottom row, you can imagine there is some hypothetical “anti-molasses” that provides negative damping.

The five possibilities in the bottom row and the rightmost column have negative overall stability, as indicated by the pale-red shaded region. The three possibilities nearest the upper-left corner have positive overall stability, as indicated by the pale-blue shaded region. The middle possibility (no static stability and no damping) is stable with respect to some disturbances (such as a change in initial position) but unstable with respect to others (such as a change in initial velocity).

By the way: Damping should be called “damping” not “dampening” — if you start talking about a “dampener” people will think you want to moisten the system.

## 10.7  Finite Size Effects

As we shall discuss, finite size effects can be categorized as follows (although there is considerable overlap among the categories):

• Boundary effects;
• Quantization effects;
• Mean free path effects;
• Transport and dissipation effects; and
• Fluctuations.

We shall see that:

1. In microscopic systems, finite-size effects dominate.
2. In moderately-large systems, finite-size effects lead to smallish correction terms.
3. In infinite systems, finite-size effects are negligible.

Let’s start with an example: The usual elementary analysis of sound in air considers only adiabatic changes in pressure and density. Such an analysis leads to a wave equation that is non-dissipative. In reality, we know that there is some dissipation. Physically the dissipation is related to transport of energy from place to place by thermal conduction. The amount of transport depends on wavelength, and is negligible in the hydrodynamic limit, which in this case means the limit of very long wavelengths.

We can come to the same conclusion by looking at things another way. The usual elementary analysis treats the air in the continuum limit, imagining that the gas consists of an infinite number density of particles each having infinitesimal size and infinitesimal mean free path. That’s tantamount to having no particles at all; the air is approximated as a continuous fluid. In such a fluid, sound would travel without dissipation.

So we have a macroscopic view of the situation (in terms of nonzero conductivity) and a microscopic view of the situation (in terms of quantized atoms with a nonzero mean free path). These two views of the situation are equivalent, because thermal conductivity is proportional to mean free path (for any given heat capacity and given temperature).

In any case, we can quantify the situation by considering the ratio of the wavelength Λ to the mean free path λ. Indeed we can think in terms of a Taylor series in powers of λ/Λ.

• The zeroth-order term is all that survives in the hydrodynamic limit (or the continuum limit). This is the only term that is considered in the usual elementary analysis.
• The first-order terms allow us to understand additional details of the situation, such as the fact that the sound wave undergoes some damping.

Let us now discuss fluctuations.

As an example, in a system at equilibrium, the pressure as measured by a very large piston will be essentially constant. Meanwhile, the pressure as measured by a very small piston will fluctuate. These pressure fluctuations are closely related to the celebrated Brownian motion.

Fluctuations are the rule, whenever you look closely enough and/or look at a small enough subsystem. There will be temperature fluctuations, density fluctuations, entropy fluctuations, et cetera.

We remark in passing that the dissipation of sound waves is intimately connected to the fluctuations in pressure. They are connected by the fluctuation / dissipation theorem, which is a corollary of the second law of thermodynamics.

There is magnificent discussion of fluctuations in Feynman volume I chapter 46 (“Ratchet and Pawl”). See reference 8.

As another example, consider shot noise. That is: in a small-sized electronic circuit, there will be fluctuations in the current, because the current is not carried by a continuous fluid but rather by electrons which have a quantized charge.

Let us now discuss boundary terms.

If you change the volume of a sample of compressible liquid, there is a well-known P dV contribution to the energy, where P is the pressure and V is the volume. There is also a τ dA contribution, where τ is the surface tension and A is the area.

A simple scaling argument proves that for very large systems, the P dV term dominates, whereas for very small systems the τ dA term dominates. For moderately large systems, we can start with the P dV term and then consider the τ dA term as a smallish correction term.

## 10.8  Words to Live By

1. Temperature is not energy.
2. Rate is not equilibrium.
3. Entropy is not energy.
4. «Heat» is not the same as «heat».

In more detail:

1. Temperature and energy follow completely different scaling laws: one them is intensive, while the other is extensive. As a familiar example, the sparks that fly from a grinding wheel have a very high temperature, but very little energy.

Just because a reaction proceeds faster at high temperature does not mean it is exothermic. As a familiar example, the combustion of coal is famously exothermic, yet it proceeds much faster at elevated temperature.

2. As a familiar example, catalysis can change the rate of reaction by many orders of magnitude, but it never changes the equilibrium point.

Temperature is not the same as catalysis, insofar as sometimes it changes the equilibrium point. However, you can’t infer the equilibrium point or the energy balance just by casual obseration of the temperature.

3. Equilibrium is determined more directly by entropy than by energy. Therefore the fact that you can dehydrate something at temperatures above 100 C in a dessicator and rehydrate it by adding a huge excess of water below 100 C tells you practically nothing about the enthalpies of formation.
4. The nice thing about defining «heat» is that there are so many definitions to choose from. When people say let’s «heat» the sample, they might be talking about temperature. When they say the sample gives off «heat>, they might be talking about energy.

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