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Second and Third Laws of Thermodynamics

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(1)

Second and Third Laws

of Thermodynamics

(2)

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

V

d d d d d d nRT d

U C T q w q p V q V

= = + = − = − V

d

rev V

d 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

rev

d d

q C

V

nR

T V

T = T + V

This is an exact differential.

( / )

V

0

T

C T V

 ∂  =

 ∂ 

 

( / )

0

V

nR V T

 ∂  =

 ∂ 

 

dq

rev

T

is the differential of a state function.

ENTROPY

(3)

3.2 The Second Law of Thermodynamics

d

rev

d q

S = T

is a state function.

Entropy

dq

rev

S T

∆ = ∫

dS = 0

∫

d q 0 T

∫

The Clausius theorem leads to

d

d q

ST

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

rev

d q

S = T d d q

ST

(4)

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

rev

q d T = S

2 2

irrev

1 1

d q d 0

TS <

∫ ∫

2 2

irrev

2 1

1 1

d d q

S S S S

∆ = − = ∫ > ∫ T

irrev

d d q

S > T

(5)

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 surroundings

d

universe

d

system

d

rev

0

surr

S S q

= − T = d d

d

system rev rev

surr

q q

S = T = T

An irreversible process in which the system gains heat

dq

irrevfrom the surroundings

d

universe

d

system

d

irrev

0

surr

S S q

= − T > d

d

system irrev

surr

S q

> T

d

system

surr

S q

∆ ≥ ∫ T d

system

d

surr

S q

T

(6)

Heat Transfer

T

α

T

β

dq d d 1 1

d d

a a

q q

S q

T

β

T T

β

T

 

= − =    −   

T

α

> T

β

T

α

= T

β

T

α

< T

β

S > 0

S = 0

S < 0

Spontaneous Equilibrium Impossible

(7)

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

∆ = =

(8)

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

rev

S 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

∆ = ∫ = − ∫ = ∫ = ∫ = = −

(9)

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

(10)

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 1

263

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

∆ = ∆ + = − =

(11)

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

1

S

2

n R

1

ln y

1

n R

2

ln y

2

∆ = ∆ + ∆ = − −

w = 0 and ∆U = 0 at constant T, then q = ∆U – w = 0

Step 2

S 0

∆ =

mix

S S

Step 1

S

Step 2

n R

1

ln y

1

n R

2

ln y

2

∆ = ∆ + ∆ = − −

(12)

Entropy of Mixing Two Ideal Gases

To produce one mole of an ideal mixture

(13)

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

∆ = − − = +

(14)

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

  

is the number of equally probable microscopic arrangement for a system S = k ln

∆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

(15)

S = k

B

ln Ω

(16)

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

=

(17)

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

3

Law

As T → 0 K,

C

P

(T ) → T

3 for most non-metallic crystals

As 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)

(18)

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

∆ =

(19)

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

∆ = =

(20)

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|

(21)

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

V

T 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

C

w q nRT  

= =  

(22)

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 C

A 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 1

2 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

q q 0

TT =

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