Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete...

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Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermody System requires in addition P=P(T,V) equation of state U=U(T,V) and P=P(T,V) complete knowledge of equilibrium propertie However U(T,V) is not a thermodynamic potential We are going to show: U=U(S,V) complete knowledge of equilibrium proper U(S,V): thermodynamic potential

Transcript of Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete...

Page 1: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Thermodynamic Potentials

Why are thermodynamic potentials useful

Consider U=U(T,V)

Complete knowledge of equilibrium properties of a simple thermodynamicSystem requires in addition

P=P(T,V) equation of state

U=U(T,V) and P=P(T,V) complete knowledge of equilibrium properties

However

U(T,V) is not a thermodynamic potential

We are going to show: U=U(S,V) complete knowledge of equilibrium properties

U(S,V): thermodynamic potential

Page 2: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

The thermodynamic potential U=U(S,V)

Consider first law in differential notation WdQddU

inexact differentials

Wd

Qdexpressed by exact differentials

PdVWd

TdSQd

2nd law

PdVTdSdU

Legendre Transformations

PdVTdSdU dU: differential of the function U=U(S,V)natural coordinates

Note: exact refers here to the coordinate differentials dS and dV. T dS and PdV are inexact as we showed previously.

Page 3: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

PdVTdSdU

Legendre transformation Special type of coordinate transformation

Example:

coordinates

Partial derivatives of U(S,V) (vector field components)

Legendre transformation: One (or more) of the natural coordinates becomes a vector field component

while the associated coefficient becomes new coordinate.

PdVTdSdU

Back to our examplebecomes a coordinate

becomes a coefficient in front of dP

Click for graphic example

Page 4: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

VdPTdSPVddU

VdPPVdTdSdU

easy check: PdVVdPPdVVdPVdPPVd

Productrule

VdPTdSPVUd

=:H (enthalpy)

H=H(S,P) is a thermodynamic potential

VdPTdSdH

Enthalpy

Page 5: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Geometrical interpretation of theLegendre transformation

- 1-dimensional example

)xx)(x(Y)x(Y)x(T 000

)x(Yx)x(Y)0(T 000

)Y(xd)xY(ddxYdY

)Y(xd)xYY(d

f:Note: natural variable of f is Y’ Y and X have to be expressed as Y=Y(Y’) and x=x(Y’)

YeY x

mapping between the graph of the function and the family of tangents of the graph

Legendre transformation:

Page 6: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Legendre transformation

from (S,V) to

(T,V): PdVTdSdU PdVSdT)TS(d

PdVSdT)TSU(d

F: Helmholtz free energy

(T,P): PdVSdTdF VdP)PV(dSdT

VdPSdT)PVF(d

G: Gibbs free energy

TSHPVTSUPVFG

Page 7: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

equilibrium thermodynamics and potentials

complete knowledge of equilibrium properties

Consider Helmholtz free energy F=F(T,V)

PdVSdTdF

Differential reads:

VT

FS

and TV

FP

Entropy Equation of state

Response functions from 2nd derivatives

VV T

STC

V

2

2

T

FT

TT V

PVB

2

2

T

FV

V

andPT

TV T

V

V

PB

VT

P

VT

F2

etc.

thermodynamics potential

Page 8: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Maxwell relations

PdVSdTdF differential of the function F=F(T,V)

dF is an exact differential

V

22

T T

P

VT

F

TV

F

V

S

VT T

P

V

S

In general: relations which follow from the exactness of the differentials of thermodynamic potentials are called Maxwell relations

Page 9: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Properties of an ideal gas derived from the Helmholtz free energy

Helmholtz free energy F=U-TS

Reminder:

)V,T(SV

VlnnR

T

Tlnnc)V,T(S rr

rrV

0v nuTnc)V,T(U

r0rr

V TsunV

VlnnRT

T

Tln1Tnc)V,T(F

Equation of state:

TV

F)V,T(P

V

nRT

01 ln lnV rr r T

T Vnc T nRT n u Ts

V T V

T

r

V

V

VlnnRT

Page 10: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Equation of state derived from F

Note: U derived from F

S(T,V)VT

FS

obtained from )V,T(SV

VlnnR

T

Tlnnc)V,T(S rr

rrV

U(T,V) obtained from U=F+TS VT

FTF

0v nuTnc)V,T(U

Heat capacity at constant volume

VV

V ncT

UC

Isothermal bulk modulus

TT V

PVB

PV

nRT

V

nRTV

2

etc.

Page 11: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

System

Heat Reservoir R

Systems in Contact with Reservoirs

Entropy statement of 2nd law: entropy always increased in an adiabatically isolated system

What can we say about evolution of systems which are not adiabatically isolated

T=const.

adiabatic wall

changes from initial state with

oooo PVTSUG

to final state with

ffff PVTSUG

VPSTUGGG 0f

remain constant

Consider system at constant temperature and pressure

Page 12: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

VPSTUG From Entropy change of :T

GVPUS

Entropy change

Aim: Find the total entropy change Rtot SSS and apply 2nd law

of the reservoir:RS

L

RR T

QdS

LRQd

T

1

T

QR

Heat QR that, e.g., leaves the reservoir flows into the system Q = -QR

Rtot SSS T

Q

T

GVPU R

With 1st law:VPQWQU

T

Q

T

GQ R

totST

G

Heat reservoir: T=const.

Page 13: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Entropy statement of 2nd law: 0Stot

0T

G

for an adiabatically isolated system

0G

Gibbs free energy never increases in a process at fixed pressurein a system in contact with a heat reservoir.

Gibbs free energy will decrease if it can, since in doing so it causes the total entropy to increase.

(T=const, P=const.)

System with V=const. in contact with a heat reservoir Special case, very important for problems in solid state physics

STUF T

FUS

T

FQ Rtot SSS

T

QRT

F 0F (T=const, V=const.)

Q = -QR

T

FQ

Page 14: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Summary: Thermodynamic potentials for PVT systems

T=const,P=constT=const,V=constIsobaric process

1st law:Properties

Maxwell

relations

Vector field components

dG=-SdT+VdPdF=-SdT-PdVdH=TdS+VdPdU=TdS-PdVdifferential

Gibbs free energy

G(T,P)

G=U –TS+PV

Helmholtz free energy

F(T,V)

F=U -TS

Enthalpy

H(S,P)

H=U+PV

Internal energy

U(S,V)Potential

VS

UT

SV

UP,

PS

HT

SP

HV,

VT

FS

TV

FP,

PT

GS

TP

GV,

VS S

P

V

T

VT T

P

V

S

ST T

V

P

S

WQU QH 0F 0G

PS S

V

P

T

Page 15: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Open Systems and Chemical Potentials

Open system Particle exchange with the surrounding allowed

Heat Reservoir RT=const.

Thermodynamic potentials depend on variable particle number N

Example: U=U(S,V,N)

Particle reservoir

Page 16: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

U( S, V, N) = 2 U(S,V,N)2 2 2

In general: )N,V,S(U)N,V,S(U

)N(

)N(

U)V(

)V(

U)S(

)S(

U

V,SN,SN,V

)N,V,S(U

S V N

holds and in particular for =1

)N,V,S(UNN

UV

V

US

S

U

V,SN,SN,V

(homogeneous function of first order)

Page 17: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

)N,V,S(UNN

UV

V

US

S

U

V,SN,SN,V

keep N constant as in closed systems

TS

U

N,V

,S N

UP

V

:N

U

V,SChemical potential

NPVTS)N,V,S(U

dNN

UdV

V

UdS

S

UdU

V,SN,SN,V

dNPdVTdSdU

Page 18: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Intuitive meaning of the chemical potential μ

First law: WdQddU with TdSQd

WdTdSdU

mechanical work PdV work μdN required to change # of particles by dN

+

How do the other potentials change when particle exchange is allowed

Helmholtz free energy F=U-TS

SdTTdSdU)TS(ddUdF

dNPdVTdSdU

dNPdVSdTdF

Page 19: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Gibbs free energy G=U -TS+PV

VdPPdVdF )PV(ddFdG

dNPdVSdTdF

dNVdPSdTdG

P,TV,TV,S N

G

N

F

N

U

Properties of μ

With and NPVTSU PVTSUG

N

G both extensive )P,T( intensive (independent of N)

F

Page 20: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Equilibrium Conditions

Adiabatically isolatingrigid wall

System1:T1,P1, 1

System2:T2,P2, 2

Qd

From

differentials of entropy changes

dNPdVTdSdU

11

11

1

1

1

11 dN

TdV

T

P

T

dUdS

22

22

2

2

2

22 dN

TdV

T

P

T

dUdS

Page 21: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

Total entropy change 1 2S S S 0

2nd law

In equilibrium 1 2dS dS dS 0

With conservation of

-total internal energy 1 2U U const. 1 2dU dU

-total volume 1 2V V const. 1 2dV dV

-total # of particles 1 2N N const. 1 2dN dN

1 2 1 21 1 1

1 2 1 2 1 2

1 1 P PdS dU dV dN 0

T T T T T T

Page 22: Thermodynamic Potentials Why are thermodynamic potentials useful Consider U=U(T,V) Complete knowledge of equilibrium properties of a simple thermodynamic.

1 2 1 21 1 1

1 2 1 2 1 2

1 1 P PdS dU dV dN 0

T T T T T T

small changes dU1, dV1, dN1

0 0 0

Equilibrium conditions

T1 = T2 , P1 = P2 ,1 = 2

Remark: )P,T(T1 = T2 , P1 = P2and 1 = 2

1 = 2 no new information for system in a single phase

but

Important information if system separated into several phases (see next chapter)