Second and Third Laws
of Thermodynamics
3.1 Entropy is a State Function
The mechanical equations of motion are invariant under time reversal.
The reverse process of a spontaneous process is nonspontaneous.
The first law provide no information regarding spontaneity of a process.
We need to devise a state function to identify a spontaneous process.
Consider that an ideal gas is heated reversibly.
rev rev rev
d
Vd d d d d d nRT d
U C T q w q p V q V
= = + = − = − V
d
rev Vd nRT d
q C T V
= + V
This is an inexact differential. V
0
T
C V
∂ =
∂
( / )
V
nRT V nR
T V
∂ =
∂
Try an integrating factor
1 T
d
revd d
q C
VnR
T V
T = T + V
This is an exact differential.
( / )
V
0
T
C T V
∂ =
∂
( / )
0
V
nR V T
∂ =
∂
dq
revT
is the differential of a state function.ENTROPY
3.2 The Second Law of Thermodynamics
d
revd q
S = T
is a state function.Entropy
dq
revS T
∆ = ∫
dS = 0
∫
d q 0 T ≤
∫
The Clausius theorem leads to
d
d q
S ≥ T
The state function called the entropy S can be calculated from
The change in entropy in any process is given by , where the inequality applies to a spontaneous (irreversible) process and the equality applies to a reversible process.
d
revd q
S = T d d q
S ≥ T
irrev
d d q S > T
1
2
irreversible
1
reversible
2 1
irrev rev
1 2
d d
q q 0
T + T <
∫ ∫
d
revq d T = S
2 2
irrev
1 1
d q d 0
T − S <
∫ ∫
2 2
irrev
2 1
1 1
d d q
S S S S
∆ = − = ∫ > ∫ T
irrev
d d q
S > T
Entropy of a System
universe system surroundings
d S = d S + d S
A reversible process in which the system gains heat
dq
revfrom the surroundingsd
universed
systemd
rev0
surr
S S q
= − T = d d
d
system rev revsurr
q q
S = T = T
An irreversible process in which the system gains heat
dq
irrevfrom the surroundingsd
universed
systemd
irrev0
surr
S S q
= − T > d
d
system irrevsurr
S q
> T
d
system
surr
S q
∆ ≥ ∫ T d
systemd
surr
S q
≥ T
Heat Transfer
T
αT
βdq d d 1 1
d d
a a
q q
S q
T
βT T
βT
= − = −
T
α> T
βT
α= T
βT
α< T
β∆ S > 0
∆ S = 0
∆ S < 0
Spontaneous Equilibrium Impossible
The entropy of expansion of an ideal gas in an isolated system
Example 3.3
An isolated ideal gas at 298K expands into a volume twice as large as its initial volume. Is the expansion of an ideal gas into a larger volume thermodynamically spontaneous in an isolated system?(a) Irreversible expansion of an ideal gas with no heat or work as Joule found no temperature change of a dilute gas allowed to expand in an isolated system.
(b) Reversible isothermal expansion of an ideal gas at 298 with
w = – RT ln 2
. As ∆U = 0, qrev=RT ln 2
1 1
ln 2 5.76 J K mol
S R
− −∆ = =
3.3Entropy Changes in Reversible Processes
phase change, liquid(T,P) →vapour(T,P)
rev
2 1
q H
S S S
T T
∆ = − = = ∆
dq
revS T
∆ = ∫
heating at constant pressure, substance(T1,P) →substance(T2,P)
heating at constant volume, substance(T1,V) →substance(T2,V)
2 2
1 1
rev 2
1
d d ln
T T
V
T T V
q C T
S T C
T T T
∆ = ∫ = ∫ =
(CV constant)2 2
1 1
rev 2
1
d d ln
T T
P
T T P
q C T
S T C
T T T
∆ = ∫ = ∫ =
(CP constant)isothermal expansion, ideal gas(P1, V1, T) →idea gas(P2,V2, T)
2 2
1 1
2 2
1 1
d d 1
d d ln ln
V V
V V
V P
q w P
S V nR V nR nR
T T T V V P
∆ = ∫ = − ∫ = ∫ = ∫ = = −
The Molar Entropy of an Ideal Gas
Example 3.8
Calculate the entropy change of an ideal monatomic gas B in changing from P1, T1to P2, T2.B(T1,P1) → B(T2,P1) → B(T2,P2) B(T1,P1) → B(T2,P1)
2
1
2 2
1 1
d ln ln
T
P P P
T
T T
S C T C nC
T T T
∆ = ∫ = =
B(T2,P1) → B(T2,P2) 2
1
ln P S nR
∆ = − P
5/ 2
2 2
1 1
ln T ln P
S nR
T P
∆ = −
Note
5
p
2
C = R
3.4 Entropy Changes in Irreversible Processes
H2O(l, –10℃)
S H T
∆ = ∆
∆ S
273 liq 263
C d
S T
∆ = ∫ T
H2O(s, –10℃) H2O(s, 0℃) H2O(1, 0℃)
263 ice 273
C d
S T
∆ = ∫ T
The entropy change in an irreversible process should be obtained by calculating ∆S along a reversible path between the initial state and the final state.
1
1 1
273 ( 6004 J mol )
1 1263
1 1(75.3 J K mol ) ln (36.8 J K mol ) ln 20.54 J K mol
263 273 K 273
S
− − − − − − −
∆ = + − + = −
1 1 1 1 1 1
(263 K) (75.3 J K mol )(10 K) 6004 J mol (36.8 J K mol )(10 K) 5619 J mol
H
− − − − − −∆ = − − = −
1
1 1
reservoir
(263 ) 5619 J mol
21.37 J K mol
263 263 K
H K
S
− − −
∆ = −∆ = =
1 1
universe reservoir 1 1
(21.73 20.54) J K mol 0.83 J K mol
S S
S ∆
− − − −∆ = ∆ + = − =
3.5 Entropy of Mixing Ideal Gases
P, T, V2 n1+n2
P, T, V1
P, T, V2
P, T, V P, T, V
n1 n2
1 2
V = + V V
1 1
1 1 1 1 1
1 2
ln V ln n ln
S n R n R n R y
V n n
∆ = − = − = −
+
2 2
2 2 2 2 2
1 2
ln V ln n ln
S n R n R n R y
V n n
∆ = − = − = −
+
Step1
S S
1S
2n R
1ln y
1n R
2ln y
2∆ = ∆ + ∆ = − −
w = 0 and ∆U = 0 at constant T, then q = ∆U – w = 0
Step 2
S 0
∆ =
mix
S S
Step 1S
Step 2n R
1ln y
1n R
2ln y
2∆ = ∆ + ∆ = − −
Entropy of Mixing Two Ideal Gases
To produce one mole of an ideal mixture
The Gibbs Paradox
Example 3.11
When two equal volumes of the same gas are mixed, what is the change in entropy?1 2
mix 1 2 1 2
1 2
ln V ln V ln V ln V
S n R n R n R n R
V V V V
∆ = − − = +
3.6 Entropy and Statistical Probability
The equilibrium state of an isolated system is that in which entropy has its maximum value.
From a microscopic point of view, it would be the state with the maximum statistical probability.
What is the statistical probability that all of the molecules will be in the original chamber?
1 2
N
Ω is the number of equally probable microscopic arrangement for a system S = k ln Ω
∆S = S
2– S
1= k ln(Ω
2/Ω
1)
The ratio Ω2/Ω1is equal to the ratio of the probabilities P2/P1. For one mole of gas molecules, P2= 1 and
6.022 1023
1
1 P 2
×=
A
1 1
A
ln 1 / 1 ln 2 ln 2 (8.314 J K ) ln 2 = 5.76 J K 2
N
S k kN R
− −∆ = = = =
The Boltzmann constant kB = 1.68 X10–23J·K–1 kB NA= R = 8.314 J·K–1·mol–1
S = k
Bln Ω
3.7 Calorimetric Determination of Entropy
m b
m b
fus vap
0 0
m b
(s) (l) (g)
d d d
T P T P T P
T T T
H H
C C C
S S T T T
T T T T T
∆ ∆
− = ∫
+
+ ∫
+
+ ∫
Entropy of SO2(g) at 298.15 K relative to its entropy at 0 K T/K Method of Calculation
0 – 15 Debye function 1.26
15 – 197.64 Graphical, solid 84.18
197.64 Fusion, 7402/197.64 37.45
197.64 – 263.08 Graphical, liquid 24.94
263.08 Vaporization, 24937/263.08 94.79
263.08 – 298.15 From CPof gas 5.23
247.85
1 1
/J K mol
S − −
∆
298.15 0
S
− S
=
Cryogenic Temperatures and Debye Function
Liquid nitrogen b.p. 77K at 1 bar
Liquid helium b.p. 4.2 K at 1 bar
Liquid helium down to 0.3 K at low pressures
Adiabatic demagnetization of a paramagnetic salt like gadolinium sulfate reaches 0.001 K
Adiabatic demagnetization of nuclear spins reaches 10–6K
The Debye T
3Law
As T → 0 K,
C
P(T ) → T
3 for most non-metallic crystalsAs T → 0 K,
C
P(T) → aT + bT
3 for metallic crystals (a and b are constants) This T3law is valid from 0 K to about 15 K (the Debye temperature)The change in entropy approaches zero as the temperature was reduced.
S
(rhombic) =S
(monoclinic)Molar entropies of monoclinic and rhombic sulfur from absolute zero to the transition temperature 368.5 K
p
0 0T
d
T
C
S S T
− = ∫ T
Assuming
S
0= 0
368.5 368.5
tr
1 1
(monoclinic) (rhombic) 1.09 J K mol
S S S
− −
∆ = −
=
1 tr
H 401 J mol
−∆ =
1
1 1
tr tr
tr
401 J mol
1.09 J K mol 368.5 K
S H T
− − −
∆ = ∆ = =
In 1905, Nernst concluded that as temperature approaches 0 K, ∆rS for all reactions approaches zero.
0 r
lim 0
T
S
→
∆ =
3.8 The Third Law of Thermodynamics
In 1913, Max Planck stated.
The entropy of each pure element or substance in a perfect crystalline form is zero at absolute zero.
Corollary to Clausius’ statement of the second law.
It is impossible to reduce the temperature of a system to 0 K in a finite number of steps.
Residual entropies
N2O
H2O
NNO NNO NNO NNO NNO NNO NNO ONN NNO NNO ONN NNO
1 1
mix
1 1 1 1
ln ln 5.76 J K mol
2 2 2 2
S R
− −∆ = − + =
1 1
residual
ln 3 3.37 J K mol
S R 2
− −∆ = =
3.9 Carnot Heat Engines
Heat reservoir at high temperature T1
Heat reservoir at low temperature T2
Surroundings Engine
working fluid
|q
1|
|q
2|
|w|
PV diagram for the working fluid in a Carnot engine. Heat |q1| is absorbed in the isothermal expansion at T1, and heat |q2| is evolved in the isothermal compression at T2. The other two steps are adiabatic.
A – B Reversible isothermal expansion at T1. Absorbs heat |q1| and does work |w1|
B – C Reversible adiabatic expansion. Temperature drops to T2and does work |w2|
C – D Reversible isothermal compression at T2. Discards heat |q2| and absorbs work |w3|
D – A Reversible adiabatic compression. Temperature rises to T1and absorbs work |w4|
Carnot Heat Engines
C – D Reversible isothermal compression at T2. Discards heat |q2| and absorbs work |w3|
B – C Reversible adiabatic expansion. Temperature drops to T2.
A – B Reversible isothermal expansion at T1. Absorbs heat |q1| and does work |w1|
1
B B
1 1 1 1
A A
d d d d d d
d d d
ln
q U P V C
VT P V P V q w nRT V
V
V w q nRT dV nRT
V V
= + = + =
= =
= = =
∫
1 1
1 B 2 C
T V
γ−= T V
γ−ln V
Cw q nRT
= =
Carnot Heat Engines
A – B isothermal expansion ∆U1= q1+ w1
B – C adiabatic expansion ∆U2= w2
C – D isothermal compression ∆U3= q2+ w3
D – A adiabatic compression ∆U4= w4
1 1
1 B 2 C
T V
γ−= T V
γ−1 1
1 A 2 D
T V
γ−= T V
γ−1 1 1 B 2 C
1 1
1 A 2 D
T V T V
T V T V
γ γ
γ γ
−
−
−
=
− B CA D
V V
V = V
C
2 2
D
ln V q nRT
V
=
B
1 1
A
ln V q nRT
V
=
1 1 AB 12 C 2
2
D
ln
ln nRT V
q V T
q V T
nRT V
= =
cy cy cy
cy 1 2
cy 1 2 3 4
cy cy 1 2
cy 1 2
0
| | | | | |
U q w
q q q
w w w w w
w q q q
w q q
∆ = + =
= +
= + + +
− = = +
= −
cy 1 2 2
1 1 1
| | 1 | |
w q q q
q q q
ε = − = + = −
2 2
1 1
q T q = T
2 1
1 T ε = − T
1 2
1 2