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Classical statistical mechanics

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#物理#热力学

Classical statistical mechanics

· 更新于 2026年10月10日· 约 32 分钟· 6303 字

点击跳转到中文版(Chinese ver.)

Thermodynamics does not develop methods for the computations of thermodynamic parameters. Thermodynamics does not look fundamental and systematic, and all the important laws seem isolated from each other. Kinetic theory of molecules offers certain understanding, but not sufficiently general.

Postulates

Statistical mechanics:

  • the equilibrium state
  • non-equilibrium states

Statistical mechanics in this course is mainly concerned with the equilibrium state.

  • Calculate macroscopic parameters from microstructures and interactions.
  • Derive thermodynamics, e.g. define and calculate temperature, internal energy, entropy; prove the important laws in thermodynamics.
  • Statistical mechanics generally goes beyond thermodynamics, e.g. compute correlation functions.

The system: a classical system isolated in the sense that the energy is conserved or nearly conserved, is composed of a large number NN of elements, typically

N≃1023\begin{align} N \simeq 10^{23} \end{align}

The thermodynamic limit:

N→∞,V→∞\begin{align} N \rightarrow \infty, \quad V \rightarrow \infty \end{align}

but

VN→v(a non-zero constant)\begin{align} \frac{V}{N} \rightarrow v \quad (\text{a non-zero constant}) \end{align}

Here VV is measured in a microscopic unit, e.g.

V≃1023molecular volumes\begin{align} V \simeq 10^{23} \quad \text{molecular volumes} \end{align}

In other words, extremely dilute or dense systems are excluded in the thermodynamic limit.

The thermodynamic properties of the system may be tackled from three levels.

Fundamental level

Solve the microscopic equations of motion, such as Newton, Hamiltonian and Heisenberg equations.

Difficulties

  • too many degrees of freedom
  • microscopic initial conditions and boundary conditions
  • irregular disturbance from environments

Here the time tt and space coordinate qiq_i are microscopic.

Even if the fundamental equations could be solved, we still have to compute the macroscopic physical parameters from the microscopic solutions, based on certain statistical theories. Therefore, statistical mechanics does provide ‘fundamental’ methods for dealing with many-body systems.

Quasi-fundamental level

Do not trace the motion of each molecule, and consider only the probability distribution ρ(pi,qi,t)\rho(p_i, q_i, t) with

ρ(pi,qi,t)∏id3pid3qi\begin{align} \rho(p_i, q_i, t) \prod_i \dd^3 p_i \dd^3 q_i \end{align}

being the probability of the system lying within a volume ∏id3pid3qi\prod_i \dd^3 p_i \dd^3 q_i of the coordinate qiq_i and momentum pip_i.

Equations of motion:

  • Liouville’s equation
  • Boltzmann equation

These equations can be solved only in some simple cases, such as dilute gases. The time tt and space coordinate qiq_i are mesoscopic. Otherwise there is no meaning for the probability distribution.

Statistical mechanics

Do not solve any equations of motion, but assume a form of ρ(pi,qi,t)\rho(p_i, q_i, t) in the equilibrium state, i.e. ρ(pi,qi,∞)≡ρ(p,q)\rho(p_i, q_i, \infty) \equiv \rho(p,q).

  • It can be tested by experiments.
  • It can be derived from equations of motion in some special cases.

More strictly, this is the so-called ensemble theory. The equilibrium state is in the macroscopic sense, i.e. the time scale is macroscopic. For non-equilibrium states, one usually assumes certain effective equations of motion. The time scale is usually mesoscopic.

Γ\Gamma space: the phase space spanned by (p,q)(p,q); each point in Γ\Gamma space represents a microscopic state of the system.

An ensemble: A collection of systems, identical in composition and macroscopic conditions, existing in (different or the same) microscopic states, without interactions with each other. A system in the ensemble can be represented by a point in Γ\Gamma space, and these systems obey the probability distribution ρ(p,q)\rho(p,q), i.e.

ρ(p,q)dpdq≡ρ(pi,qi)∏idpidqi\begin{align} \rho(p,q)\dd p \dd q \equiv \rho(p_i,q_i) \prod_i \dd p_i \dd q_i \end{align}

is the number of systems at the volume element dpdq\dd p \dd q.

In simple words, an ensemble is a set of microscopic states of the system with the probability distribution ρ(p,q)\rho(p,q), and it is introduced to replace the dynamic evolution of the microscopic states. Physically, such a description is reasonable just because a macroscopic state may correspond to many microscopic states. Naturally, ρ(p,q)\rho(p,q) should depend on the macroscopic environment of the system. The basic assumption in statistical mechanics starts from an isolated system.

Postulate of equal a priori probability

When an isolated system is in thermodynamic equilibrium, its microscopic state is equally likely to be any state satisfying the macroscopic conditions, i.e.

ρ(p,q)={const,E<H(p,q)<E+Δ,0,otherwise.\begin{align} \rho(p,q) = \begin{cases} \text{const}, & E < H(p,q) < E + \Delta,\\ 0, & \text{otherwise}. \end{cases} \end{align}

where EE is the energy, Δ≪E\Delta \ll E, HH is the Hamiltonian, and the ensemble described by this distribution is the so-called microcanonical ensemble.

Here it is important that the Hamiltonian is assumed to be known, which contains the microstructure and interactions of the system.

  • Why is Δ\Delta introduced? Theoretically, it is convenient. Practically, isolation is not strict.
  • Why is ρ(p,q)\rho(p,q) a constant for all microscopic states with energy around EE? Energy is assumed to be the most important quantity for the microscopic motion. If ρ(p,q)\rho(p,q) is not a constant, another quantity should be specified.

One may understand the postulate from ergodicity, which assumes that the system experiences all the microscopic states in an infinitesimal macroscopic time. If there is ergodicity, it is natural that the real path of a system should be a simple loop in Γ\Gamma space. Therefore, the postulate holds.

If the path does not form a loop in an infinitesimal macroscopic time, the macroscopic state is not in equilibrium. If there are two loops, it is not ergodic. In fact, ergodicity is not strict. For example, if the walls of a cubic container are completely smooth, molecules of an ideal gas with parallel velocities will not change their velocities. But ergodicity may be assumed because of:

  • the measure of non-ergodic states is negligibly small;
  • the irregular disturbance from environments.

On the other hand, we may introduce the probability distribution P(f)P(f) for the observable f(p,q)f(p,q). The average of f(p,q)f(p,q) can be computed by ∫df fP(f)\int \dd f\, f P(f). Obviously, P(f)P(f) is different from ρ(p,q)\rho(p,q).

As shown in Fig. 2.1, P(f)P(f) is usually assumed to have a single sharp peak. We define the most probable value f0f_0 of f(p,q)f(p,q) by the maximum probability P(f)P(f).

The ensemble average ⟨f⟩\langle f \rangle and the most probable value f0f_0 are nearly the same under the condition of Eq. (2.1.1), and should become identical in the thermodynamic limit. Otherwise, statistical mechanics should be questioned. But it does not mean that statistical mechanics is necessarily invalid; one should carefully study.

Question: in what case may Eq. (2.1.1) be not valid?

Answer: strongly correlated systems, for example, with long-range interactions, or around continuous phase transitions.

Microcanonical ensemble

To establish statistical mechanics, it is first important to define all the macroscopic physical parameters through the microscopic degrees of freedom, i.e. f(p,q)f(p,q), especially for those typical thermodynamic observables. The average of the Hamiltonian HH is naturally defined as the internal energy. So, it is crucial how to define the entropy and temperature.

Let us denote the volume in Γ\Gamma space of the microcanonical ensemble by

Γ(E)≡∫E<H(p,q)<E+Δdpdq\begin{align} \Gamma(E) \equiv \int_{E < H(p,q) < E + \Delta} \dd p \dd q \end{align}

Γ(E)\Gamma(E) is understood to depend on N,VN, V and also Δ\Delta. For example, the volume is shown for H(p,q)=p2+q2H(p,q) = p^2 + q^2 in Fig. 2.2.

TikZ 源码
\begin{tikzpicture}[>=stealth, thick, font=\small]
\draw[->] (-2.8,0) -- (2.8,0) node[below] {$q$};
\draw[->] (0,-2.8) -- (0,2.8) node[left] {$p$};
\draw[thick] (0,0) circle (1.2);
\draw[thick] (0,0) circle (1.6);
\fill[gray!30] (0,0) circle (1.6);
\fill[white] (0,0) circle (1.2);
\node at (0,0) {$E$};
\node at (1.4,1.4) {$E+\Delta$};
\end{tikzpicture}

Please note that Γ(E)\Gamma(E) is the volume, not simply the number of states in Γ\Gamma space. To define the “number”, one should introduce the unit volume.

From experiments, the entropy is closely related to the number of microscopic states. The entropy is thus defined by

S(E,V)≡klog⁡Γ(E)\begin{align} S(E,V) \equiv k \log \Gamma(E) \end{align}

where kk is a universal constant eventually shown to be the Boltzmann constant. Such a definition is closely related to the fact that the entropy must be extensive.

To justify the definition of SS, we should show:

(a) SS is extensive.
(b) SS satisfies the properties of the entropy as required by the second law of thermodynamics.

Proof:

(a) Let the system be divided into two subsystems:

1: N1,V1,H1N_1, V_1, H_1
2: N2,V2,H2N_2, V_2, H_2

with fixed N1,N2,V1N_1, N_2, V_1 and V2V_2, which satisfy

N=N1+N2V=V1+V2H(p,q)=H1(p1,q1)+H2(p2,q2)\begin{align} N &= N_1 + N_2\\ V &= V_1 + V_2\\ H(p,q) &= H_1(p_1,q_1) + H_2(p_2,q_2) \end{align}

Here (p1,q1)(p_1,q_1) are the coordinates of particles in system 1, and (p2,q2)(p_2,q_2) are the coordinates of particles in system 2. Especially it is assumed that the interaction between two subsystems is negligibly small, although it must exist to allow the exchange of energy between two subsystems. For example, if the intermolecular potential is finite-range, and the surface-to-volume ratio of each subsystem is negligibly small.

If we define

S1(E1,V1)=klog⁡Γ1(E1,Δ)S2(E2,V2)=klog⁡Γ2(E2,Δ)S(E,V)=klog⁡Γ(E,2Δ)\begin{align} S_1(E_1,V_1) &= k \log \Gamma_1(E_1,\Delta)\\ S_2(E_2,V_2) &= k \log \Gamma_2(E_2,\Delta)\\ S(E,V) &= k \log \Gamma(E,2\Delta) \end{align}

we should show in the thermodynamic limit

S(E,V)=S1(E1,V1)+S2(E2,V2)\begin{align} S(E,V) = S_1(E_1,V_1) + S_2(E_2,V_2) \end{align}

If E=E1+E2E = E_1 + E_2 is a given decomposition of the energy, i.e. H1H_1 fluctuates around E1E_1 and H2H_2 around E2E_2, the volume in Γ\Gamma space of the whole system is

Γ(E)=∫E1<H1<E1+Δ, E2<H2<E2+Δdp1dp2dq1dq2=∫E1<H1<E1+Δdp1dq1∫E2<H2<E2+Δdp2dq2=Γ1(E1)Γ2(E2)\begin{align} \Gamma(E) &= \int_{E_1 < H_1 < E_1+\Delta,\ E_2 < H_2 < E_2+\Delta} \dd p_1 \dd p_2 \dd q_1 \dd q_2\\ &= \int_{E_1 < H_1 < E_1+\Delta} \dd p_1 \dd q_1 \int_{E_2 < H_2 < E_2+\Delta} \dd p_2 \dd q_2\\ &= \Gamma_1(E_1)\Gamma_2(E_2) \end{align}

In other words, the extensive property of SS has been proven if the two subsystems are simply added up.

The key point is that the possible decomposition of the energy E=E1+E2E = E_1 + E_2 is not unique when the system is divided into two subsystems. In other words, both E1E_1 and E2E_2 may fluctuate from zero to EE although constrained by the energy conservation E1+E2=EE_1 + E_2 = E.

Let us divide EE into E/ΔE/\Delta intervals with Ei=iΔE_i = i\Delta, i=0,1,…,E/Δi=0,1,\dots,E/\Delta, then

Γ(E)=∑i=0E/ΔΓ1(Ei)Γ2(E−Ei)\begin{align} \Gamma(E) = \sum_{i=0}^{E/\Delta} \Gamma_1(E_i)\Gamma_2(E-E_i) \end{align}

We will show or have to show that only one term in the sum is dominating. This is the only possibility to set up the extensiveness of the entropy.

Let us assume that there uniquely exists a decomposition of energy Eˉ1+Eˉ2=E\bar{E}_1 + \bar{E}_2 = E with the largest term Γ1(Eˉ1)Γ2(Eˉ2)\Gamma_1(\bar{E}_1)\Gamma_2(\bar{E}_2). Then

Γ1(Eˉ1)Γ2(Eˉ2)≤Γ(E)≤EΔΓ1(Eˉ1)Γ2(Eˉ2)\begin{align} \Gamma_1(\bar{E}_1)\Gamma_2(\bar{E}_2) \le \Gamma(E) \le \frac{E}{\Delta}\Gamma_1(\bar{E}_1)\Gamma_2(\bar{E}_2) \end{align}

or

S1(Eˉ1,V1)+S2(Eˉ2,V2)≤S(E,V)≤S1(Eˉ1,V1)+S2(Eˉ2,V2)+klog⁡EΔ\begin{align} S_1(\bar{E}_1,V_1) + S_2(\bar{E}_2,V_2) &\le S(E,V)\\ &\le S_1(\bar{E}_1,V_1) + S_2(\bar{E}_2,V_2) + k \log \frac{E}{\Delta} \end{align}

In the thermodynamic limit, we expect or assume

log⁡Γ1∝N1,log⁡Γ2∝N2\begin{align} \log \Gamma_1 \propto N_1,\quad \log \Gamma_2 \propto N_2 \end{align}

and

E∝N1+N2=N\begin{align} E \propto N_1 + N_2 = N \end{align}

In addition, both N1N_1 and N2N_2 should be of order NN, otherwise it may not be meaningful. Then

S(E,V)=S1(Eˉ1)+S2(Eˉ2)+O(log⁡N)\begin{align} S(E,V) = S_1(\bar{E}_1) + S_2(\bar{E}_2) + O(\log N) \end{align}

In thermodynamic equilibrium, the system is homogeneous, therefore

N∝V\begin{align} N \propto V \end{align}

Thus SS is extensive up to the order of NN, i.e. when omitting the terms of order O(log⁡N)O(\log N).

In summary, the extensive property of SS is based on that a single decomposition E=Eˉ1+Eˉ2E = \bar{E}_1 + \bar{E}_2 of the energy is dominating when the system is divided into two subsystems, with fixed N1,N2N_1, N_2 and V1,V2V_1, V_2. The existence of such a dominating decomposition will be discussed below.

E∝N1+N2=NE \propto N_1 + N_2 = N is simply the extensive property of EE. However, log⁡Γ1∝N1∝V1\log \Gamma_1 \propto N_1 \propto V_1 indicates already that S1S_1 is extensive. Therefore, the derivation with E=Eˉ1+Eˉ2E = \bar{E}_1 + \bar{E}_2 sounds only to prove that if S1S_1 and S2S_2 are extensive then SS is also extensive.

Finally, we may notice that there is still another small parameter Δ\Delta. However, this is a macroscopic parameter, and not necessarily infinitesimal in the microscopic sense. At least, one should not mix this small parameter with the thermodynamic limit.

Understanding:

Alternatively, we may consider Eˉ1\bar{E}_1 and Eˉ2\bar{E}_2 are the averaged energy of the two subsystems. In the thermodynamic limit, the fluctuation δ\delta of E1E_1 around Eˉ1\bar{E}_1 should be much smaller than Eˉ1\bar{E}_1. Let us take δ<Δ\delta < \Delta, then only Γ1(Eˉ1)Γ2(Eˉ2)\Gamma_1(\bar{E}_1)\Gamma_2(\bar{E}_2) is dominating:

Γ(E)=∑i=1E/ΔΓ1(Ei)Γ2(E−Ei)\begin{align} \Gamma(E) = \sum_{i=1}^{E/\Delta} \Gamma_1(E_i)\Gamma_2(E-E_i) \end{align}

Therefore

S(E,V)=S1(Eˉ1,V1)+S2(Eˉ2,V2)\begin{align} S(E,V) = S_1(\bar{E}_1,V_1) + S_2(\bar{E}_2,V_2) \end{align}

with E=Eˉ1+Eˉ2E = \bar{E}_1 + \bar{E}_2.

This also explains why we can add two systems up in equilibrium, and divide a system into two parts in equilibrium.

In fact, following the discussions below Eq. (2.1.1), it is natural that the decomposition of energy with the largest term Γ1(E1)Γ2(E2)\Gamma_1(E_1)\Gamma_2(E_2) should be identical to the decomposition of the average energy, since the former corresponds to the most probable values of energy for the two subsystems.

Question: why is it only “an understanding”?

Answer: Γ1(Ei)Γ2(E−Ei)\Gamma_1(E_i)\Gamma_2(E-E_i) is just P(E1=Ei)P(E_1 = E_i), the probability that E1E_1 takes the value EiE_i. When we assume δ<Δ\delta < \Delta, it indicates already that all other terms are negligible.

In fact, Γ1(E1)Γ2(E−E1)\Gamma_1(E_1)\Gamma_2(E-E_1) is usually a very sharp function of E1E_1, and such an understanding is reasonable. For example, suppose Γ1(E1)=E1N1\Gamma_1(E_1) = E_1^{N_1}, Γ2(E−E1)=(E−E1)N2\Gamma_2(E-E_1) = (E-E_1)^{N_2} and N1=N2N_1 = N_2, then

Γ1(E1)Γ2(E−E1)=[E1(E−E1)]N1\begin{align} \Gamma_1(E_1)\Gamma_2(E-E_1) = [E_1(E-E_1)]^{N_1} \end{align}

This function has a maximum at E1=E/2E_1 = E/2, and it is very sharp for a large N1N_1.

Reading materials: Why

Γ(E)=∑i=1E/ΔΓ1(Ei)Γ2(E−Ei)?\begin{align} \Gamma(E) = \sum_{i=1}^{E/\Delta} \Gamma_1(E_i)\Gamma_2(E-E_i)? \end{align}

e.g. N=2N=2:

H=12mp2+12ω2q2H1=12ω2q2,H2=12mp2\begin{align} H &= \frac{1}{2m}p^2 + \frac{1}{2}\omega^2 q^2\\ H_1 &= \frac{1}{2}\omega^2 q^2,\quad H_2 = \frac{1}{2m}p^2 \end{align} Γ(E)=∫E<H<E+2ΔdqdpΓ1(E1)=∫E1<H1<E1+ΔdqΓ2(E−E1)=∫E−E1<H2<E−E1+Δdp\begin{align} \Gamma(E) &= \int_{E < H < E+2\Delta} \dd q \dd p\\ \Gamma_1(E_1) &= \int_{E_1 < H_1 < E_1+\Delta} \dd q\\ \Gamma_2(E-E_1) &= \int_{E-E_1 < H_2 < E-E_1+\Delta} \dd p \end{align}

Γ(E)\Gamma(E) is just the area of a circular ring. Γ1(E1)Γ2(E−E1)\Gamma_1(E_1)\Gamma_2(E-E_1) is an element of the circular ring at q=E1q = \sqrt{E_1}. If E1E_1 is fixed, one may write

Γ(E)=Γ1(E1)Γ2(E−E1)\begin{align} \Gamma(E) = \Gamma_1(E_1)\Gamma_2(E-E_1) \end{align}

If not, one needs to integrate over E1E_1:

Γ(E)=∑i=1E/ΔΓ1(Ei)Γ2(E−Ei)\begin{align} \Gamma(E) = \sum_{i=1}^{E/\Delta} \Gamma_1(E_i)\Gamma_2(E-E_i) \end{align}

since E1E_1 takes values from 0 to EE, corresponding to different states.

End reading materials.

In other words, E=Eˉ1+Eˉ2E = \bar{E}_1 + \bar{E}_2 maximizes the function Γ1(E1)Γ2(E2)\Gamma_1(E_1)\Gamma_2(E_2), i.e. also log⁡[Γ1(E1)Γ2(E2)]\log[\Gamma_1(E_1)\Gamma_2(E_2)] with the restriction δE=δE1+δE2=0\delta E = \delta E_1 + \delta E_2 = 0, therefore,

δlog⁡[Γ1(E1)Γ2(E2)]=0,δE1+δE2=0\begin{align} \delta \log [\Gamma_1(E_1)\Gamma_2(E_2)] = 0,\quad \delta E_1 + \delta E_2 = 0 \end{align}

This leads to

∂∂E1log⁡Γ1(E1)∣E1=Eˉ1=∂∂E2log⁡Γ2(E2)∣E2=Eˉ2\begin{align} \left.\frac{\partial}{\partial E_1}\log \Gamma_1(E_1)\right|_{E_1=\bar{E}_1} = \left.\frac{\partial}{\partial E_2}\log \Gamma_2(E_2)\right|_{E_2=\bar{E}_2} \end{align}

or

∂S1(E1)∂E1∣E1=Eˉ1=∂S2(E2)∂E2∣E2=Eˉ2\begin{align} \left.\frac{\partial S_1(E_1)}{\partial E_1}\right|_{E_1=\bar{E}_1} = \left.\frac{\partial S_2(E_2)}{\partial E_2}\right|_{E_2=\bar{E}_2} \end{align}

We define the temperature of any system by

∂S(E,V)∂E=1T\begin{align} \frac{\partial S(E,V)}{\partial E} = \frac{1}{T} \end{align}

Then

∂S1∂E1=∂S2∂E2\begin{align} \frac{\partial S_1}{\partial E_1} = \frac{\partial S_2}{\partial E_2} \end{align}

it is simply the zeroth law:

T1=T2\begin{align} T_1 = T_2 \end{align}

TT defined in this way is an intensive parameter, and ∂S/∂E=1/T\partial S/\partial E = 1/T is also one of the Maxwell relations in thermodynamics. Therefore, if SS is correctly defined, TT should also be correct.

Thermodynamics

Let us define

Σ(E)=∫H(p,q)<Edpdq\begin{align} \Sigma(E) = \int_{H(p,q) < E} \dd p \dd q \end{align}

Then

ω(E)=∂Σ(E)∂E\begin{align} \omega(E) = \frac{\partial \Sigma(E)}{\partial E} \end{align}

Then

Γ(E)=ω(E)ΔΓ(E)=Σ(E+Δ)−Σ(E)\begin{align} \Gamma(E) &= \omega(E)\Delta\\ \Gamma(E) &= \Sigma(E+\Delta) - \Sigma(E) \end{align}

It can be proved that up to an additive constant of order O(log⁡N)O(\log N), the following definitions are equivalent:

S=klog⁡Γ(E)S=klog⁡ω(E)S=klog⁡Σ(E)\begin{align} S &= k \log \Gamma(E)\\ S &= k \log \omega(E)\\ S &= k \log \Sigma(E) \end{align}

Question: why?

For example, suppose Σ(E)∝EN\Sigma(E) \propto E^N, then Γ(E)∝NEN−1\Gamma(E) \propto N E^{N-1}. Or, more generally, Γ(E)<Σ(E)<Γ(E)⋅E/Δ\Gamma(E) < \Sigma(E) < \Gamma(E) \cdot E/\Delta. The behaviors of log⁡Σ(E)\log \Sigma(E) and log⁡Γ(E)\log \Gamma(E) look similar, up to order O(log⁡N)O(\log N).

From the definition itself, SS is a state function.

With the definition

S(E,V)=klog⁡Σ(E)\begin{align} S(E,V) = k \log \Sigma(E) \end{align}

it is easy to show that SS never decreases, i.e. the second law for a thermally isolated system in thermodynamics.

Proof: Consider a system described by the parameters N,E,VN, E, V. By the definition of an isolated system, NN and EE cannot change, VV cannot decrease. Therefore, the second law here is simply stated as that SS is a non-decreasing function of VV. This is obvious, for Σ(E)\Sigma(E) is a non-decreasing function of VV by its definition.

Hint: an isolated gas can expand only, although it is somewhat less clear for liquid and solid.

For reversible thermodynamic transformations, the entropy should satisfy the fundamental equation of the second law. Assuming that the system is changed slowly by coupling the system to external environments, then it is a quasi-static process:

dS(E,V)=(∂S∂E)VdE+(∂S∂V)EdV=1TdE+(∂S∂V)EdV\begin{align} \dd S(E,V) &= \left(\frac{\partial S}{\partial E}\right)_V \dd E + \left(\frac{\partial S}{\partial V}\right)_E \dd V\\ &= \frac{1}{T}\dd E + \left(\frac{\partial S}{\partial V}\right)_E \dd V \end{align}

Here one again assumes that there are only two independent parameters.

Define the pressure of the system to be

P≡T(∂S∂V)E\begin{align} P \equiv T\left(\frac{\partial S}{\partial V}\right)_E \end{align}

then

dS=1T(dE+PdV)\begin{align} \dd S = \frac{1}{T}(\dd E + P \dd V) \end{align}

or

dE=TdS−PdV\begin{align} \dd E = T \dd S - P \dd V \end{align}

Keeping in mind that EE is the internal energy, this looks like the first law.

Question: Is it reasonable to define

P≡T(∂S∂V)E\begin{align} P \equiv T\left(\frac{\partial S}{\partial V}\right)_E \end{align}

Hints:

  1. PP is intensive.
  2. Exercise: prove that PP defined above satisfies
P=−(∂E∂V)S\begin{align} P = -\left(\frac{\partial E}{\partial V}\right)_S \end{align}

Up to here, the definition of PP indeed is reasonable. The definition of TT is also correct if SS is really entropy.

Finally, dQ=TdS\dd Q = T \dd S is the heat absorbed by the system by assuming the first law; thus SS should be the entropy. In fact, one may show that SS exhibits all the properties of the entropy analyzed in thermodynamics. Here it is important that the first law is still an assumption in statistical mechanics!

If it is possible to compute S(E,V)S(E,V), and to obtain the internal energy as E=E(S,V)E = E(S,V), i.e. the characteristic function, one may derive all the thermodynamic quantities just by differentiation. But this can be done only in very simple cases.

Equipartition theorem

The Hamiltonian of the system is written as

H=H(p,q)=H(pj,qj),j=1,…,3N\begin{align} H = H(p,q) = H(p_j,q_j),\qquad j = 1,\dots,3N \end{align}

e.g. for an ideal gas,

H=12m∑pi2\begin{align} H = \frac{1}{2m}\sum p_i^2 \end{align}

or a set of harmonic oscillators,

H=12m∑pi2+12ω2∑qi2\begin{align} H = \frac{1}{2m}\sum p_i^2 + \frac{1}{2}\omega^2 \sum q_i^2 \end{align}

We will derive an equipartition theorem for a general Hamiltonian, and then apply it to a simple one.

Let xix_i be either pip_i or qiq_i:

⟨xi∂H∂xj⟩=1Γ(E)∫E<H<E+Δdpdq xi∂H∂xj=ΔΓ(E)1Δ(∫H<E+Δdpdq−∫H<Edpdq)xi∂H∂xj=ΔΓ(E)∂∂E∫H<Edpdq xi∂H∂xj\begin{align} \left\langle x_i \frac{\partial H}{\partial x_j} \right\rangle &= \frac{1}{\Gamma(E)} \int_{E < H < E+\Delta} \dd p \dd q\, x_i \frac{\partial H}{\partial x_j}\\ &= \frac{\Delta}{\Gamma(E)} \frac{1}{\Delta} \left( \int_{H < E+\Delta} \dd p \dd q - \int_{H < E} \dd p \dd q \right) x_i \frac{\partial H}{\partial x_j}\\ &= \frac{\Delta}{\Gamma(E)} \frac{\partial}{\partial E} \int_{H < E} \dd p \dd q\, x_i \frac{\partial H}{\partial x_j} \end{align}

The second equality is based on the definition of the integration.

∫H<Edpdq xi∂H∂xj=∫H<Edpdq xi∂∂xj(H−E)=∫H<Edpdq ∂∂xj[xi(H−E)]−δij∫H<Edpdq (H−E)\begin{align} \int_{H<E} \dd p \dd q\, x_i \frac{\partial H}{\partial x_j} &= \int_{H<E} \dd p \dd q\, x_i \frac{\partial}{\partial x_j}(H-E)\\ &= \int_{H<E} \dd p \dd q\, \frac{\partial}{\partial x_j}[x_i(H-E)] - \delta_{ij} \int_{H<E} \dd p \dd q\, (H-E) \end{align}

The second equality is obtained through integration by parts. The first term in the last line reduces to a surface integral over the boundary of the region defined by H<EH<E, i.e.

the first term=∫H=Edpdq xi(H−E)=0\begin{align} \text{the first term} = \int_{H=E} \dd p \dd q\, x_i (H-E) = 0 \end{align}

Question: how to describe this more convincingly?

Hint: suppose the volume H<EH<E is enclosed by the surface H=EH=E, and the surface consists of the upper and lower sheets, i.e. xj=F2(xi,… )x_j = F_2(x_i,\dots) and xj=F1(xi,… )x_j = F_1(x_i,\dots).

⟨xi∂H∂xj⟩=δijω(E)∂∂E∫H<Edpdq (E−H)=δijω(E)(∫H<Edpdq+1Δ∫E<H<E+Δdpdq (E−H))\begin{align} \left\langle x_i \frac{\partial H}{\partial x_j} \right\rangle &= \frac{\delta_{ij}}{\omega(E)} \frac{\partial}{\partial E} \int_{H<E} \dd p \dd q\, (E-H)\\ &= \frac{\delta_{ij}}{\omega(E)} \left( \int_{H<E} \dd p \dd q + \frac{1}{\Delta} \int_{E < H < E+\Delta} \dd p \dd q\, (E-H) \right) \end{align}

(the second term is negligible, at least when compared to the first term)

=δijω(E)Σ(E)=δij(∂log⁡Σ(E)∂E)−1=δijk(∂S∂E)−1=δijkT\begin{align} &= \frac{\delta_{ij}}{\omega(E)} \Sigma(E) = \delta_{ij} \left( \frac{\partial \log \Sigma(E)}{\partial E} \right)^{-1}\\ &= \delta_{ij} k \left( \frac{\partial S}{\partial E} \right)^{-1} = \delta_{ij} k T \end{align}

If i=ji=j,

⟨xi∂H∂xi⟩=kT\begin{align} \left\langle x_i \frac{\partial H}{\partial x_i} \right\rangle = kT \end{align}

If

H=∑iAiPi2+∑iBiQi2\begin{align} H = \sum_i A_i P_i^2 + \sum_i B_i Q_i^2 \end{align}

where Pi,QiP_i, Q_i are canonical conjugate variables, then one may easily show

∑i(Pi∂H∂Pi+Qi∂H∂Qi)=2H\begin{align} \sum_i \left( P_i \frac{\partial H}{\partial P_i} + Q_i \frac{\partial H}{\partial Q_i} \right) = 2H \end{align}

Denote the number of degrees of freedom by ff and take the ensemble average of the above equation,

⟨H⟩=12fkT\begin{align} \langle H \rangle = \frac{1}{2} f k T \end{align}

Exercise: Prove the equipartition theorem for

H=12mp2+12ω2q2\begin{align} H = \frac{1}{2m}p^2 + \frac{1}{2}\omega^2 q^2 \end{align}

by explicitly calculating the ensemble average.

Classical ideal gas

The Hamiltonian of an ideal gas:

H=12m∑i=1Npi2\begin{align} H = \frac{1}{2m}\sum_{i=1}^N p_i^2 \end{align}

Then one may compute

Σ(E)=∫H<Ed3p1…d3pNd3q1…d3qN=VN∫H<Ed3p1…d3pN\begin{align} \Sigma(E) &= \int_{H<E} \dd^3 p_1 \dots \dd^3 p_N \dd^3 q_1 \dots \dd^3 q_N\\ &= V^N \int_{H<E} \dd^3 p_1 \dots \dd^3 p_N \end{align}

Let

R=2mE\begin{align} R = \sqrt{2mE} \end{align} Σ(E)=VNΩ3N(R)\begin{align} \Sigma(E) = V^N \Omega_{3N}(R) \end{align}

Ωn(R)\Omega_n(R) is the volume of an nn-sphere of radius RR:

Ωn(R)=CnRnCn=2πn/2Γ(n/2+1)\begin{align} \Omega_n(R) &= C_n R^n\\ C_n &= \frac{2\pi^{n/2}}{\Gamma(n/2+1)} \end{align}

Γ(z)\Gamma(z) is the gamma function:

log⁡Cn→n→∞n2log⁡π−n2log⁡n2+n2\begin{align} \log C_n \xrightarrow[n\to\infty]{} \frac{n}{2}\log \pi - \frac{n}{2}\log \frac{n}{2} + \frac{n}{2} \end{align}

hence

Σ(E)=C3N[V(2mE)3/2]N\begin{align} \Sigma(E) = C_{3N} \left[ V (2mE)^{3/2} \right]^N \end{align} S(E,V)=klog⁡Σ(E)≃Nklog⁡[V(4πmE3N)3/2]+32Nk\begin{align} S(E,V) &= k \log \Sigma(E)\\ &\simeq Nk \log \left[ V \left( \frac{4\pi m E}{3N} \right)^{3/2} \right] + \frac{3}{2} Nk \end{align} U(S,V)≡E=3N4πmV2/3exp⁡(2S3Nk−1)\begin{align} U(S,V) \equiv E = \frac{3N}{4\pi m V^{2/3}} \exp\left( \frac{2S}{3Nk} - 1 \right) \end{align} T=(∂U∂S)V=2U3Nk,U=32NkT\begin{align} T = \left( \frac{\partial U}{\partial S} \right)_V = \frac{2U}{3Nk},\quad U = \frac{3}{2} NkT \end{align} CV=32Nk\begin{align} C_V = \frac{3}{2} Nk \end{align} P=−(∂U∂V)S=NkTV\begin{align} P = -\left( \frac{\partial U}{\partial V} \right)_S = \frac{NkT}{V} \end{align}

From the above calculation, Ωn(R)∝Rn\Omega_n(R) \propto R^n is essential, and CnC_n is not much relevant.

Gibbs paradox

Consider the mixture of two ideal gases at the same temperature and the same density, with volumes V1V_1 and V2V_2, and particle numbers N1N_1 and N2N_2 respectively. Initially, two gases are separated by a partition wall, then the wall is removed and two gases mix.

If two gases are different, the entropy increases, since both gases expand. If two gases are identical, nothing is changed in thermodynamics, but the entropy seems increasing in statistical mechanics as described above, since both gases still expand.

To solve this problem, one may introduce a Gibbs factor in the computation of Σ(E)\Sigma(E), i.e.

Σ(E)=1N!∫H(p,q)<EdNpdNq\begin{align} \Sigma(E) = \frac{1}{N!} \int_{H(p,q)<E} \dd^N p \dd^N q \end{align}

With this correction factor, and log⁡N!≈Nlog⁡N−N\log N! \approx N \log N - N, one obtains

S(E,V)=Nklog⁡[VN(4πmE3N)3/2]+52Nk\begin{align} S(E,V) = Nk \log \left[ \frac{V}{N} \left( \frac{4\pi m E}{3N} \right)^{3/2} \right] + \frac{5}{2} Nk \end{align}

Thus the entropy remains unchanged after the mixture of two identical gases. In other words, S∼Nklog⁡VS \sim Nk \log V is unreasonable, since VV is extensive. The Gibbs factor corrects it to S∼Nklog⁡(V/N)S \sim Nk \log(V/N). The Gibbs factor is needed whenever there exists an exchange of particles in different volumes.

In fact, it seems that the factor one needs is NNN^N rather than N!N!. Why does one not directly introduce NNN^N? In quantum mechanics, an exchange of two identical particles does not yield a new quantum state, and N!N! is the total number of such exchanges for NN particles.

Alternatively, when VV is decomposed into V1V_1 and V2V_2,

1N!∫VdNq=1N!∑N1=0NN!N1!(N−N1)!∫V1dN1q∫V2dN−N1q\begin{align} \frac{1}{N!}\int_V \dd^N q = \frac{1}{N!}\sum_{N_1=0}^N \frac{N!}{N_1!(N-N_1)!} \int_{V_1} \dd^{N_1} q \int_{V_2} \dd^{N-N_1} q \end{align}

In the thermodynamic limit, however, only one term dominates the sum, which ensures the same density for both V1V_1 and V2V_2, i.e. N1/V1=N2/V2N_1/V_1 = N_2/V_2. Therefore,

1N!∫VdNq≈1N1!N2!∫V1dN1q∫V2dN2q\begin{align} \frac{1}{N!}\int_V \dd^N q \approx \frac{1}{N_1! N_2!} \int_{V_1} \dd^{N_1} q \int_{V_2} \dd^{N_2} q \end{align}

The factorial number looks intrinsic here.

Maxwell-Boltzmann distribution

There are NN identical molecules in volume VV,

H(p,q)=E\begin{align} H(p,q) = E \end{align}

The system may be described by a microcanonical ensemble. If the molecules are quasi-independent,

H=∑ih(pi,qi)\begin{align} H = \sum_i h(p_i,q_i) \end{align}

where h(pi,qi)h(p_i,q_i) represents the Hamiltonian of each molecule. There could be a number of atoms in a molecule, but the interactions between two molecules are negligible. For example, the simplest case is

H=12m∑ipi2\begin{align} H = \frac{1}{2m}\sum_i p_i^2 \end{align}

μ\mu space: the phase space spanned by a single-molecule coordinate (p,q)(p,q).

A microscopic state of a single molecule can be represented by a point in μ\mu space. A microscopic state of the system is described by a set of such points.

Since the energy of a molecule is bounded by EE, the points are confined to a finite region of μ\mu space. We divide the region into KK elements of volume ω=d3pd3q\omega = \dd^3 p \dd^3 q, and denote the number of molecules in the ll-th element by nln_l, then

∑l=1Knl=N,∑l=1Kϵlnl=E.\begin{align} \sum_{l=1}^K n_l = N,\qquad \sum_{l=1}^K \epsilon_l n_l = E. \end{align}

Here the molecules are assumed to be quasi-independent, ϵl\epsilon_l is the energy level of a single particle.

It is important to note that a microscopic state of the system may be described by a set of occupation numbers {nl}\{n_l\}, but a set of {nl}\{n_l\} corresponds to not only one microscopic state, e.g. interchange of two molecules in different elements may lead to new states. That is, a given set of {nl}\{n_l\} corresponds to a volume in Γ\Gamma space, which is called the volume occupied by {nl}\{n_l\}.

To describe a macroscopic state, we need to average over the microcanonical ensemble, i.e. all possible microscopic states. In other words, we should first obtain {⟨nl⟩}\{\langle n_l \rangle\}, then calculate all macroscopic quantities from this distribution. Here ⟨… ⟩\langle \dots \rangle represents the ensemble average.

However, it is difficult to perform this ensemble average.

We thus assume that the equilibrium state in the thermodynamic limit is described by the most probable distribution of {nl}\{n_l\}, which occupies the largest volume in Γ\Gamma space.

Why may such an assumption hold?

  • This is somewhat similar to the case when we calculate Γ(E)≃Γ1(Eˉ1)Γ2(Eˉ2)\Gamma(E) \simeq \Gamma_1(\bar{E}_1)\Gamma_2(\bar{E}_2) by dividing the system into two subsystems.
  • For a fixed ll, if the relative fluctuation
(⟨nl2⟩−⟨nl⟩2)/⟨nl⟩2\begin{align} (\langle n_l^2 \rangle - \langle n_l \rangle^2) / \langle n_l \rangle^2 \end{align}

is still not small enough, we increase the total number NN to reduce it. Finally, ⟨nl⟩\langle n_l \rangle should be equal to the most probable nˉl\bar{n}_l.

The procedure:

(a) Calculate the volume of {nl}\{n_l\}.
(b) Maximize it to obtain the most probable {nˉl}\{\bar{n}_l\}.

The volume of {nl}\{n_l\}:

Ω({nl})∝N!∏l=1Knl!∏k=1Kgknk\begin{align} \Omega(\{n_l\}) \propto \frac{N!}{\prod_{l=1}^K n_l!} \prod_{k=1}^K g_k^{n_k} \end{align}

where gkg_k is introduced for convenience, and may finally be put to 1. For example, the derivative over gkg_k yields nkn_k. Alternatively, gkg_k may be understood as the volume of the kk-th element in μ\mu space.

Understanding: There are N!N! ways of distributing NN distinguishable molecules to NN positions. However, NN positions form KK groups with the distribution {nl}\{n_l\}. Inside a group, there are nl!n_l! ways of distributing nln_l molecules, which do not lead to new states in Γ\Gamma space. In other words, we consider that molecules in the same element are in the same state, since their contributions to the physical quantity f(p,q)f(p,q) are the same.

For a large nln_l,

log⁡nl!≃nl(log⁡nl−1)\begin{align} \log n_l! \simeq n_l (\log n_l - 1) \end{align}

(i.e. nl!≃nlnln_l! \simeq n_l^{n_l})

log⁡Ω({nl})=N(log⁡N−1)−∑l=1Knl(log⁡nl−1)+∑l=1Knllog⁡gl+const\begin{align} \log \Omega(\{n_l\}) &= N(\log N - 1) - \sum_{l=1}^K n_l(\log n_l - 1) + \sum_{l=1}^K n_l \log g_l + \text{const} \end{align}

Now we vary {nl}\{n_l\} under the conditions ∑l=1Knl=N\sum_{l=1}^K n_l = N and ∑l=1Kϵlnl=E\sum_{l=1}^K \epsilon_l n_l = E, to find the most probable {nl}\{n_l\}. We introduce the Lagrange multipliers α\alpha and β\beta, and calculate

δ[log⁡Ω({nl})]−δ(α∑l=1Knl+β∑l=1Kϵlnl)=0\begin{align} \delta \left[ \log \Omega(\{n_l\}) \right] - \delta \left( \alpha \sum_{l=1}^K n_l + \beta \sum_{l=1}^K \epsilon_l n_l \right) = 0 \end{align}

Now we consider all nln_l are independent of each other.

∑l=1K[−(log⁡nl)+log⁡gl−α−βϵl]δnl=0\begin{align} \sum_{l=1}^K \left[ -(\log n_l) + \log g_l - \alpha - \beta \epsilon_l \right] \delta n_l = 0 \end{align} ∴log⁡nˉl=log⁡gl−α−βϵlnˉl=gle−α−βϵl\begin{align} \therefore \log \bar{n}_l &= \log g_l - \alpha - \beta \epsilon_l\\ \bar{n}_l &= g_l e^{-\alpha - \beta \epsilon_l} \end{align}

Finally, α\alpha and β\beta can be determined by the conservation of the total particles and the total energy.

To prove that {nˉl}\{\bar{n}_l\} maximizes Ω({nl})\Omega(\{n_l\}), we can simply calculate the second variation:

−∑l=1K1nl(δnl)2<0\begin{align} -\sum_{l=1}^K \frac{1}{n_l}(\delta n_l)^2 < 0 \end{align}

Note that nˉl\bar{n}_l is only a function of ϵl=ϵ(p,q)\epsilon_l = \epsilon(p,q), and does not generally depend on (p,q)(p,q). This is an important feature of the equilibrium state. The molecules tend to gather in the lower energy states.

Boltzmann statistical theory

We put gl=1g_l = 1.

N=∑lnˉl=∑le−α−βϵlE=∑lϵlnˉl=∑lϵle−α−βϵl\begin{align} N &= \sum_l \bar{n}_l = \sum_l e^{-\alpha - \beta \epsilon_l}\\ E &= \sum_l \epsilon_l \bar{n}_l = \sum_l \epsilon_l e^{-\alpha - \beta \epsilon_l} \end{align}

Let us assume

ϵl=ϵ(p,q,y)\begin{align} \epsilon_l = \epsilon(p,q,y) \end{align}

The original subscript ll just labels pp and qq, and y={yk}y = \{y_k\} represent macroscopic external parameters such as the external fields.

Define the partition function of a single particle:

Z(β,y)=∑le−βϵl=∫l≤Edpdq e−βϵ(p,q,y)\begin{align} Z(\beta,y) = \sum_l e^{-\beta \epsilon_l} = \int_{l \le E} \dd p \dd q\, e^{-\beta \epsilon(p,q,y)} \end{align}

then

N=e−αZ(β,y)orα=log⁡Z(β,y)NE=−N∂log⁡Z(β,y)∂β\begin{align} N &= e^{-\alpha} Z(\beta,y)\quad \text{or}\quad \alpha = \log \frac{Z(\beta,y)}{N}\\ E &= -N \frac{\partial \log Z(\beta,y)}{\partial \beta} \end{align}

Suppose the system is changed very slowly.

dE=∑lnˉldϵl+∑lϵldnˉl\begin{align} \dd E = \sum_l \bar{n}_l \dd \epsilon_l + \sum_l \epsilon_l \dd \bar{n}_l \end{align}

Here we assume that the upper and lower bounds of the summation are fixed. The first term represents the macroscopic interaction with the external environment.

∑lnˉldϵl=∑l,knˉl∂ϵl∂ykdyk=∑k(∑lnˉl∂ϵl∂yk)dyk\begin{align} \sum_l \bar{n}_l \dd \epsilon_l &= \sum_{l,k} \bar{n}_l \frac{\partial \epsilon_l}{\partial y_k} \dd y_k\\ &= \sum_k \left( \sum_l \bar{n}_l \frac{\partial \epsilon_l}{\partial y_k} \right) \dd y_k \end{align}

Question: why not differentiate over pp and qq?

Answer: pp and qq are integrating variables.

Here

Yk≡−∑lnˉl∂ϵl∂yk=Nβ∂log⁡Z(β,y)∂yk\begin{align} Y_k \equiv -\sum_l \bar{n}_l \frac{\partial \epsilon_l}{\partial y_k} = \frac{N}{\beta} \frac{\partial \log Z(\beta,y)}{\partial y_k} \end{align}

are the forces acting on the environment by the system. Therefore, the term −∑lnˉldϵl-\sum_l \bar{n}_l \dd \epsilon_l just represents the work done by the system.

Proof: since

e−α=NZ(β,y)\begin{align} e^{-\alpha} = \frac{N}{Z(\beta,y)} \end{align}

therefore

Nβ∂log⁡Z(β,y)∂yk=NβZ(β,y)∂Z(β,y)∂yk=e−αβ∂∂yk∑le−βϵl=−∑le−α−βϵl∂ϵl∂yk=−∑lnˉl∂ϵl∂yk\begin{align} \frac{N}{\beta} \frac{\partial \log Z(\beta,y)}{\partial y_k} &= \frac{N}{\beta Z(\beta,y)} \frac{\partial Z(\beta,y)}{\partial y_k}\\ &= \frac{e^{-\alpha}}{\beta} \frac{\partial}{\partial y_k} \sum_l e^{-\beta \epsilon_l}\\ &= -\sum_l e^{-\alpha - \beta \epsilon_l} \frac{\partial \epsilon_l}{\partial y_k}\\ &= -\sum_l \bar{n}_l \frac{\partial \epsilon_l}{\partial y_k} \end{align}

Note that for yk=Vy_k = V, one should rescale qq such that the bounds of the summation or integration over qq are not dependent on VV. Or, the dependence of the bounds on VV should be taken into account.

Then the force is just the pressure:

P=Nβ∂log⁡Z(β,V)∂V\begin{align} P = \frac{N}{\beta} \frac{\partial \log Z(\beta,V)}{\partial V} \end{align}

Question: how to prove it?

Hint: in the integration

∫−∞∞d3p∫Vd3q e−βϵ(p,q),\begin{align} \int_{-\infty}^{\infty} \dd^3 p \int^V \dd^3 q\, e^{-\beta \epsilon(p,q)}, \end{align}

one may perform the transformation

q→qV1/3,p→pV−1/3.\begin{align} q \rightarrow q V^{1/3},\quad p \rightarrow p V^{-1/3}. \end{align}

The parameter VV is then transformed into ϵ(p,q)\epsilon(p,q). For a free particle, for example, ϵ(p,q)=p2/2m\epsilon(p,q) = p^2/2m is transformed into ϵ(p,q)V−2/3\epsilon(p,q)V^{-2/3}.

If dϵl=0\dd \epsilon_l = 0, one identifies the heat by the first law:

dQ=∑lϵldnˉl\begin{align} \dd Q = \sum_l \epsilon_l \dd \bar{n}_l \end{align}

which induces the change of the particle distribution. Again, one notes that α\alpha is a function of β\beta and yky_k, and the differentiation here acts only on β\beta and yky_k, not on pp and qq. Direct computation of dQ\dd Q may be complicated, but in general

dQ=∑lϵldnˉl=dE+∑kYkdyk=−Nd(∂log⁡Z(β,y)∂β)+Nβ∑k∂log⁡Z(β,y)∂ykdyk\begin{align} \dd Q &= \sum_l \epsilon_l \dd \bar{n}_l = \dd E + \sum_k Y_k \dd y_k\\ &= -N \dd \left( \frac{\partial \log Z(\beta,y)}{\partial \beta} \right) + \frac{N}{\beta} \sum_k \frac{\partial \log Z(\beta,y)}{\partial y_k} \dd y_k \end{align}

Since

dlog⁡Z(β,y)=∂log⁡Z(β,y)∂βdβ+∑k∂log⁡Z(β,y)∂ykdyk\begin{align} \dd \log Z(\beta,y) = \frac{\partial \log Z(\beta,y)}{\partial \beta} \dd \beta + \sum_k \frac{\partial \log Z(\beta,y)}{\partial y_k} \dd y_k \end{align}

hence

dQ=Nβd(log⁡Z(β,y)−β∂log⁡Z(β,y)∂β)\begin{align} \dd Q = \frac{N}{\beta} \dd \left( \log Z(\beta,y) - \beta \frac{\partial \log Z(\beta,y)}{\partial \beta} \right) \end{align}

Define the temperature by

β=1kT\begin{align} \beta = \frac{1}{kT} \end{align}

and the entropy by

dS=Nkd(log⁡Z(β,y)−β∂log⁡Z(β,y)∂β)S=Nk(log⁡Z(β,y)−β∂log⁡Z(β,y)∂β)+const\begin{align} \dd S &= Nk \dd \left( \log Z(\beta,y) - \beta \frac{\partial \log Z(\beta,y)}{\partial \beta} \right)\\ S &= Nk \left( \log Z(\beta,y) - \beta \frac{\partial \log Z(\beta,y)}{\partial \beta} \right) + \text{const} \end{align}

Then, dQ=TdS\dd Q = T \dd S, i.e. assuming the first law, we may prove the second law.

Exercise: Perform the calculations for an ideal gas with

H=12m∑ipi2\begin{align} H = \frac{1}{2m}\sum_i p_i^2 \end{align}

Hint: Since ϵl≪E∝N\epsilon_l \ll E \propto N, we neglect the bound of EE in calculating

Z(β,y)=∑le−βϵl\begin{align} Z(\beta,y) = \sum_l e^{-\beta \epsilon_l} \end{align}

Question: What is the relation between the Boltzmann theory and the microcanonical theory?

Answer: Since

Γ(E)=1N!∑{nl}Ω({nl})≈1N!Ω({nˉl})\begin{align} \Gamma(E) = \frac{1}{N!} \sum_{\{n_l\}} \Omega(\{n_l\}) \approx \frac{1}{N!} \Omega(\{\bar{n}_l\}) \end{align}

and n!≈nnn! \approx n^n,

log⁡Ω({nˉl})=∑lnˉllog⁡nˉl=∑l(α+βϵl)e−α−βϵl=α∑le−α−βϵl+β∑lϵle−α−βϵl=Nlog⁡Z(β,y)N−Nβ∂log⁡Z(β,y)∂β\begin{align} \log \Omega(\{\bar{n}_l\}) &= \sum_l \bar{n}_l \log \bar{n}_l\\ &= \sum_l (\alpha + \beta \epsilon_l) e^{-\alpha - \beta \epsilon_l}\\ &= \alpha \sum_l e^{-\alpha - \beta \epsilon_l} + \beta \sum_l \epsilon_l e^{-\alpha - \beta \epsilon_l}\\ &= N \log \frac{Z(\beta,y)}{N} - N \beta \frac{\partial \log Z(\beta,y)}{\partial \beta} \end{align} ∴S=Nk(log⁡Z(β,y)N−β∂log⁡Z(β,y)∂β)\begin{align} \therefore S = Nk \left( \log \frac{Z(\beta,y)}{N} - \beta \frac{\partial \log Z(\beta,y)}{\partial \beta} \right) \end{align}

The difference comes from the Gibbs factor.

Fix yy,

dS=Nk∂log⁡Z(β,y)∂βdβ−Nk∂log⁡Z(β,y)∂βdβ+kβdE=kβdE\begin{align} \dd S &= Nk \frac{\partial \log Z(\beta,y)}{\partial \beta} \dd \beta - Nk \frac{\partial \log Z(\beta,y)}{\partial \beta} \dd \beta + k \beta \dd E\\ &= k \beta \dd E \end{align} ∴1T=(∂S∂E)y=kβ\begin{align} \therefore \frac{1}{T} = \left( \frac{\partial S}{\partial E} \right)_y = k \beta \end{align}

Summary

Ergodicity

→\rightarrow Postulate of equal a priori probability for the microcanonical ensemble

A special case: the most probable distribution of quasi-independent particles.

→T,S,P\rightarrow T, S, P and thermodynamics.

The drawback is that the calculation of observables is clumsy because of the restriction of the energy.

Exercise

  • Assuming
P≡T(∂S∂V)E,(∂S∂E)V=1T,\begin{align} P \equiv T\left(\frac{\partial S}{\partial V}\right)_E,\quad \left(\frac{\partial S}{\partial E}\right)_V = \frac{1}{T}, \end{align}

prove

P=−(∂E∂V)S.\begin{align} P = -\left(\frac{\partial E}{\partial V}\right)_S. \end{align}
  • Prove the equipartition theorem for
H=12mp2+12ω2q2\begin{align} H = \frac{1}{2m}p^2 + \frac{1}{2}\omega^2 q^2 \end{align}

by explicitly calculating the ensemble average.

  • Perform the calculations of the Boltzmann statistical theory for an ideal gas with
H=12m∑ipi2\begin{align} H = \frac{1}{2m}\sum_i p_i^2 \end{align}
  • Exercises 6.1 and 6.3 in the textbook.

Discussion:

  • Negative temperature

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