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 N of elements, typically
N≃1023
The thermodynamic limit:
N→∞,V→∞
but
NV→v(a non-zero constant)
Here V is measured in a microscopic unit, e.g.
V≃1023molecular volumes
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 t and space coordinate qi 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) with
ρ(pi,qi,t)i∏d3pid3qi
being the probability of the system lying within a volume ∏id3pid3qi of the coordinate qi and momentum pi.
Equations of motion:
Liouville’s equation
Boltzmann equation
These equations can be solved only in some simple cases, such as dilute gases. The time t and space coordinate qi 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) in the equilibrium state, i.e. ρ(pi,qi,∞)≡ρ(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 space: the phase space spanned by (p,q); each point in Γ 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 space, and these systems obey the probability distribution ρ(p,q), i.e.
ρ(p,q)dpdq≡ρ(pi,qi)i∏dpidqi
is the number of systems at the volume element dpdq.
In simple words, an ensemble is a set of microscopic states of the system with the probability distribution ρ(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) 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,0,E<H(p,q)<E+Δ,otherwise.
where E is the energy, Δ≪E, H 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 introduced? Theoretically, it is convenient. Practically, isolation is not strict.
Why is ρ(p,q) a constant for all microscopic states with energy around E? Energy is assumed to be the most important quantity for the microscopic motion. If ρ(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 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) for the observable f(p,q). The average of f(p,q) can be computed by ∫dffP(f). Obviously, P(f) is different from ρ(p,q).
As shown in Fig. 2.1, P(f) is usually assumed to have a single sharp peak. We define the most probable value f0 of f(p,q) by the maximum probability P(f).
The ensemble average ⟨f⟩ and the most probable value f0 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), especially for those typical thermodynamic observables. The average of the Hamiltonian H 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 space of the microcanonical ensemble by
Γ(E)≡∫E<H(p,q)<E+Δdpdq
Γ(E) is understood to depend on N,V and also Δ. For example, the volume is shown for H(p,q)=p2+q2 in Fig. 2.2.
Please note that Γ(E) is the volume, not simply the number of states in Γ 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)≡klogΓ(E)
where k 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 S, we should show:
(a) S is extensive.
(b) S satisfies the properties of the entropy as required by the second law of thermodynamics.
Proof:
(a) Let the system be divided into two subsystems:
Here (p1,q1) are the coordinates of particles in system 1, and (p2,q2) 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.
In other words, the extensive property of S has been proven if the two subsystems are simply added up.
The key point is that the possible decomposition of the energy E=E1+E2 is not unique when the system is divided into two subsystems. In other words, both E1 and E2 may fluctuate from zero to E although constrained by the energy conservation E1+E2=E.
Let us divide E into E/Δ intervals with Ei=iΔ, i=0,1,…,E/Δ, then
Γ(E)=i=0∑E/ΔΓ1(Ei)Γ2(E−Ei)
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 with the largest term Γ1(Eˉ1)Γ2(Eˉ2). Then
In addition, both N1 and N2 should be of order N, otherwise it may not be meaningful. Then
S(E,V)=S1(Eˉ1)+S2(Eˉ2)+O(logN)
In thermodynamic equilibrium, the system is homogeneous, therefore
N∝V
Thus S is extensive up to the order of N, i.e. when omitting the terms of order O(logN).
In summary, the extensive property of S is based on that a single decomposition E=Eˉ1+Eˉ2 of the energy is dominating when the system is divided into two subsystems, with fixed N1,N2 and V1,V2. The existence of such a dominating decomposition will be discussed below.
E∝N1+N2=N is simply the extensive property of E. However, logΓ1∝N1∝V1 indicates already that S1 is extensive. Therefore, the derivation with E=Eˉ1+Eˉ2 sounds only to prove that if S1 and S2 are extensive then S is also extensive.
Finally, we may notice that there is still another small parameter Δ. 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 and Eˉ2 are the averaged energy of the two subsystems. In the thermodynamic limit, the fluctuation δ of E1 around Eˉ1 should be much smaller than Eˉ1. Let us take δ<Δ, then only Γ1(Eˉ1)Γ2(Eˉ2) is dominating:
Γ(E)=i=1∑E/ΔΓ1(Ei)Γ2(E−Ei)
Therefore
S(E,V)=S1(Eˉ1,V1)+S2(Eˉ2,V2)
with E=Eˉ1+Eˉ2.
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) 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) is just P(E1=Ei), the probability that E1 takes the value Ei. When we assume δ<Δ, it indicates already that all other terms are negligible.
In fact, Γ1(E1)Γ2(E−E1) is usually a very sharp function of E1, and such an understanding is reasonable. For example, suppose Γ1(E1)=E1N1, Γ2(E−E1)=(E−E1)N2 and N1=N2, then
Γ1(E1)Γ2(E−E1)=[E1(E−E1)]N1
This function has a maximum at E1=E/2, and it is very sharp for a large N1.
T defined in this way is an intensive parameter, and ∂S/∂E=1/T is also one of the Maxwell relations in thermodynamics. Therefore, if S is correctly defined, T should also be correct.
Thermodynamics
Let us define
Σ(E)=∫H(p,q)<Edpdq
Then
ω(E)=∂E∂Σ(E)
Then
Γ(E)Γ(E)=ω(E)Δ=Σ(E+Δ)−Σ(E)
It can be proved that up to an additive constant of order O(logN), the following definitions are equivalent:
SSS=klogΓ(E)=klogω(E)=klogΣ(E)
Question: why?
For example, suppose Σ(E)∝EN, then Γ(E)∝NEN−1. Or, more generally, Γ(E)<Σ(E)<Γ(E)⋅E/Δ. The behaviors of logΣ(E) and logΓ(E) look similar, up to order O(logN).
From the definition itself, S is a state function.
With the definition
S(E,V)=klogΣ(E)
it is easy to show that S never decreases, i.e. the second law for a thermally isolated system in thermodynamics.
Proof: Consider a system described by the parameters N,E,V. By the definition of an isolated system, N and E cannot change, V cannot decrease. Therefore, the second law here is simply stated as that S is a non-decreasing function of V. This is obvious, for Σ(E) is a non-decreasing function of V 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:
Here one again assumes that there are only two independent parameters.
Define the pressure of the system to be
P≡T(∂V∂S)E
then
dS=T1(dE+PdV)
or
dE=TdS−PdV
Keeping in mind that E is the internal energy, this looks like the first law.
Question: Is it reasonable to define
P≡T(∂V∂S)E
Hints:
P is intensive.
Exercise: prove that P defined above satisfies
P=−(∂V∂E)S
Up to here, the definition of P indeed is reasonable. The definition of T is also correct if S is really entropy.
Finally, dQ=TdS is the heat absorbed by the system by assuming the first law; thus S should be the entropy. In fact, one may show that S 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), and to obtain the internal energy as 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
e.g. for an ideal gas,
H=2m1∑pi2
or a set of harmonic oscillators,
H=2m1∑pi2+21ω2∑qi2
We will derive an equipartition theorem for a general Hamiltonian, and then apply it to a simple one.
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<E, i.e.
the first term=∫H=Edpdqxi(H−E)=0
Question: how to describe this more convincingly?
Hint: suppose the volume H<E is enclosed by the surface H=E, and the surface consists of the upper and lower sheets, i.e. xj=F2(xi,…) and xj=F1(xi,…).
From the above calculation, Ωn(R)∝Rn is essential, and Cn is not much relevant.
Gibbs paradox
Consider the mixture of two ideal gases at the same temperature and the same density, with volumes V1 and V2, and particle numbers N1 and N2 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), i.e.
Σ(E)=N!1∫H(p,q)<EdNpdNq
With this correction factor, and logN!≈NlogN−N, one obtains
S(E,V)=Nklog[NV(3N4πmE)3/2]+25Nk
Thus the entropy remains unchanged after the mixture of two identical gases. In other words, S∼NklogV is unreasonable, since V is extensive. The Gibbs factor corrects it to S∼Nklog(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 NN rather than N!. Why does one not directly introduce NN? In quantum mechanics, an exchange of two identical particles does not yield a new quantum state, and N! is the total number of such exchanges for N particles.
Alternatively, when V is decomposed into V1 and V2,
In the thermodynamic limit, however, only one term dominates the sum, which ensures the same density for both V1 and V2, i.e. N1/V1=N2/V2. Therefore,
N!1∫VdNq≈N1!N2!1∫V1dN1q∫V2dN2q
The factorial number looks intrinsic here.
Maxwell-Boltzmann distribution
There are N identical molecules in volume V,
H(p,q)=E
The system may be described by a microcanonical ensemble. If the molecules are quasi-independent,
H=i∑h(pi,qi)
where h(pi,qi) 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=2m1i∑pi2
μ space: the phase space spanned by a single-molecule coordinate (p,q).
A microscopic state of a single molecule can be represented by a point in μ space. A microscopic state of the system is described by a set of such points.
Since the energy of a molecule is bounded by E, the points are confined to a finite region of μ space. We divide the region into K elements of volume ω=d3pd3q, and denote the number of molecules in the l-th element by nl, then
l=1∑Knl=N,l=1∑Kϵlnl=E.
Here the molecules are assumed to be quasi-independent, ϵl 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}, but a set of {nl} 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} corresponds to a volume in Γ space, which is called the volume occupied by {nl}.
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⟩}, then calculate all macroscopic quantities from this distribution. Here ⟨…⟩ 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}, which occupies the largest volume in Γ space.
Why may such an assumption hold?
This is somewhat similar to the case when we calculate Γ(E)≃Γ1(Eˉ1)Γ2(Eˉ2) by dividing the system into two subsystems.
For a fixed l, if the relative fluctuation
(⟨nl2⟩−⟨nl⟩2)/⟨nl⟩2
is still not small enough, we increase the total number N to reduce it. Finally, ⟨nl⟩ should be equal to the most probable nˉl.
The procedure:
(a) Calculate the volume of {nl}.
(b) Maximize it to obtain the most probable {nˉl}.
The volume of {nl}:
Ω({nl})∝∏l=1Knl!N!k=1∏Kgknk
where gk is introduced for convenience, and may finally be put to 1. For example, the derivative over gk yields nk. Alternatively, gk may be understood as the volume of the k-th element in μ space.
Understanding: There are N! ways of distributing N distinguishable molecules to N positions. However, N positions form K groups with the distribution {nl}. Inside a group, there are nl! ways of distributing nl molecules, which do not lead to new states in Γ 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) are the same.
Now we vary {nl} under the conditions ∑l=1Knl=N and ∑l=1Kϵlnl=E, to find the most probable {nl}. We introduce the Lagrange multipliers α and β, and calculate
δ[logΩ({nl})]−δ(αl=1∑Knl+βl=1∑Kϵlnl)=0
Now we consider all nl are independent of each other.
Finally, α and β can be determined by the conservation of the total particles and the total energy.
To prove that {nˉl} maximizes Ω({nl}), we can simply calculate the second variation:
−l=1∑Knl1(δnl)2<0
Note that nˉl is only a function of ϵl=ϵ(p,q), and does not generally depend on (p,q). This is an important feature of the equilibrium state. The molecules tend to gather in the lower energy states.
The original subscript l just labels p and q, and y={yk} represent macroscopic external parameters such as the external fields.
Define the partition function of a single particle:
Z(β,y)=l∑e−βϵl=∫l≤Edpdqe−βϵ(p,q,y)
then
NE=e−αZ(β,y)orα=logNZ(β,y)=−N∂β∂logZ(β,y)
Suppose the system is changed very slowly.
dE=l∑nˉldϵl+l∑ϵldnˉl
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.
Note that for yk=V, one should rescale q such that the bounds of the summation or integration over q are not dependent on V. Or, the dependence of the bounds on V should be taken into account.
Then the force is just the pressure:
P=βN∂V∂logZ(β,V)
Question: how to prove it?
Hint: in the integration
∫−∞∞d3p∫Vd3qe−βϵ(p,q),
one may perform the transformation
q→qV1/3,p→pV−1/3.
The parameter V is then transformed into ϵ(p,q). For a free particle, for example, ϵ(p,q)=p2/2m is transformed into ϵ(p,q)V−2/3.
If dϵl=0, one identifies the heat by the first law:
dQ=l∑ϵldnˉl
which induces the change of the particle distribution. Again, one notes that α is a function of β and yk, and the differentiation here acts only on β and yk, not on p and q. Direct computation of dQ may be complicated, but in general
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