


Study with the several resources on Docsity
Earn points by helping other students or get them with a premium plan
Prepare for your exams
Study with the several resources on Docsity
Earn points to download
Earn points by helping other students or get them with a premium plan
Community
Ask the community for help and clear up your study doubts
Discover the best universities in your country according to Docsity users
Free resources
Download our free guides on studying techniques, anxiety management strategies, and thesis advice from Docsity tutors
Constant volume, Distinguishable indistinguishable subsystems, Calculation of average energy and pressure are key points
Typology: Lecture notes
1 / 4
This page cannot be seen from the preview
Don't miss anything!
A brief summary of material from McQuarrie & Simon, Chapters 17 and 18, on the partition function and its use in the calculation of some equilibrium properties. You have already seen this material in Chem 389. The concepts outlined here will be applied in Chem 390 to a number of important problems.
For a system in equilibrium at (absolute) temperature T , the probability of finding the system in the quantum state with energy Ej is proportional to the Boltzmann factor
pj ∝ e−Ej^ /kBT^ ≡ e−βEj^ (1)
where kB is Boltzmann’s constant, and we have defined the useful combination β ≡ 1 /kBT. Each pj is (and has to be ) > 0. As the probability of finding the system in any state j is 1, we must have ∑
j
pj = 1, (2)
A suitable normalization factor is then 1/Q, where Q is the partition function
Q ≡
j
e−Ej^ /kBT^ , (3)
so that the properly normalized probabilities pj are [McQ&S, eq. (17.13)]
pj = e−βEj Q
e−βEj ∑ j e −βEj.^ (4)
For a system of N particles (for example, a gas of particles in a container of volume V ), the energies Ej are the eigenvalues of the Schr¨odinger equation
HˆΨj = Ej Ψj. (5)
The system energies Ej will naturally be functions of how many particles there are (N ) and how big the box is (V ), so Ej = Ej (N, V ), and the full dependence of Q and the pj s is
Q(N, V, T ) =
j
e−Ej^ (N,V^ )/kBT^ (6a)
pj (N, V, T ) =
e−βEj^ (N,V^ ) Q(N, V, T )
(6b)
or
Q(N, V, β) =
j
e−βEj^ (N,V^ )^ (7a)
pj (N, V, β) =
e−βEj^ (N,V^ ) Q(N, V, β)
(7b)
where it is important to note that we can use either the temperature T or β = 1/kBT as an independent variable in addition to N and V. The average energy of the system 〈E〉, which we equate with the observed energy U , is calculated by evaluating the sum of each energy Ej multiplied by the corresponding probability pj
j
Ej pj =
j
Ej (N, V )e−βEj^ (N,V^ )^ (8)
which is (McQ&S, equations (17.20) and (17.21))
∂ln Q ∂β
N,V
= kBT 2
∂ln Q ∂T
N,V
We therefore have the first essential route from the quantum levels Ej to an equilibrium bulk property
{Ej } =⇒ Q(N, V, T ) =⇒ U (N, V, T ). (10)
Once we have (in principle) the average energy as a function of T , N and V , we can calculate the rate at which 〈E〉 changes as we change T at constant N and V : this is the (constant volume) heat capacity CV (eq. (17.25))
CV =
N,V
N,V
For a macroscopic system in level j, energy Ej , the associated level pressure Pj is directly related to the rate at which the energy Ej (N, V ) changes as the volume of the system varies:
Pj (N, V ) = −
∂Ej ∂V
N
The equilibrium pressure p at temperature T is obtained by averaging the level pressures Pj over the probabilities pj
p ≡ 〈P〉 =
j
pj Pj (13a)
j
pj
∂Ej ∂V
N
(13b)
j
∂Ej ∂V
N
e−βEj^. (13c)
We therefore have (17.32)
p =
β
∂ln Q ∂V
N,T
= kBT
∂ln Q ∂V
N,T
and a second essential route from the quantum levels Ej to an equilibrium bulk property
{Ej } =⇒ Q(N, V, T ) =⇒ p(N, V, T ). (15)
In principle we can calculate the equation of state, p = p(N, V, T ) from the {Ej }.
q1D(V, T ) =
mkBT 2 πℏ^2
For a particle of mass m in a 3D volume V at temperature T ,
qtrans(V, T ) =
mkBT 2 πℏ^2
V McQ&S, eq. (18.20) (23)
EJ = BJ(J + 1), J = 0, 1 ,... (24)
B = ℏ^2 / 2 I. The rotational partition function is
qrot =
J=0, 1 ,...
(2J + 1)e−ΘrotJ(J+1)/T^ McQ&S, eq. (18.33) (25)
where Θrot = B/kB. For T Θrot we can replace the sum over rotational quantum number J by an integral,
⇒ qrot =
Θrot
2 IkBT ℏ^2 McQ&S, eq. (18.34). (26)
In general qrot =
σΘrot
where σ is the symmetry number, σ = 1 for a heteronuclear diatomic, σ = 2 for a homonuclear.
qvib =
n=0, 1 ,...
e−ℏω(n+
1 2 )/kBT^ (28a)
e−βℏω/^2 1 − e−βℏω^
McQ&S, eq. (18.23) (28b)
e−Θvib/^2 T 1 − e−Θvib/T^
McQ&S, eq. (18.24). (28c)
with Θvib = ℏω/kB. For T Θvib, qvib =
Θvib