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1 THERMODYNAMICS

Lectures on Thermodynamics

1 Thermodynamics

Thermodynamics studies the macroscopic behavior of the many-body systems and describes them in terms of macroscopic parameters characterizing the system which are temperature T , pressure P and volume V . Equation of state is the relation

among these parameters and is written as f (P, T, V ) = 0

The basic assumption is that such an equation always exists. Dierent functions describing thermodynamical systems are divided in two groups:

• functions of state which are complete dierentials and depend only on initial

and nal state. I

df (x) = 0

2 1

df (x) = f (2)− f(1) Examples are thermodynamical potentials (see later).

• functions of process which are not complete dierentials and depend on the path taken between initial and nal state.

I

df (x)̸= 0 Examples are work and heat.

Let us look at the work done during an isothermal T = const. and an isobaric P = const. process. The work is

AT =

V2

V1

n R T

V dV = n R T lnV2 V1 AP =

V2

V1

P dV = P (V2− V1) AT ̸= AP

Thermodynamical potentials are basic functions of state expressed in terms of conjugate coordinates P, V and T, S. Transformation from one coordinate to

another is know as Laplace transform. They are:

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1 THERMODYNAMICS

• Internal energy U(S, V )

dU = dQ− dA = T dS− P dV dU (S, V ) =

(∂U

∂S )

V

dS + (∂U

∂V )

S

dV T =

(∂U

∂S )

V

P =− (∂U

∂V )

S

During an adiabatic ∆Q = 0 process

A|Q =−∆U = Ui− Uf

which means that the work done corresponds to the change of internal energy.

In an isochoric V = const. one nds dUV ≡ dQV = cV dT

cV (∂U

∂T )

V

= (∂S

∂T )

V

(∂U

∂S )

V

cV = T (∂S

∂T )

V

• Enthalpy H(S, P ) is Laplace transform of U(S, V ) in conjugate coordinates V → P

H = U + P V = F + T S + P V dH = T dS + V dP

T = (∂H

∂S )

P

V = (∂H

∂P )

S

During an isobaric P = const. process

Q|P = ∆H|P = Hf − Hi

which means that the exchange of heat corresponds to the change of enthalpy and

dHP ≡ dQP = cPdT cP =

(∂H

∂T )

P

= T (∂S

∂T )

P

Thus, in an isobaric process, enthalpy plays the same role as internal energy in an isochoric process.

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1 THERMODYNAMICS

• Helmoltz free energy F (T, V ) is Laplace transform of U(S, V ) in conjugate coordinates S → T

F = U − T S dF =−S dT − P dV

S =− (∂F

∂T )

V

P =− (∂F

∂V ) ( T

∂S

∂V )

T

=

( 2F

∂T ∂V ) ( T,V

∂P

∂T )

V

=

( 2F

∂T ∂V ) ( T,V

∂P

∂T )

V

= (∂S

∂V )

T

in an reversible isothermal process dF = −P dV so that AT = Fi − Ff

and the work extracted from the system is equal to the loss of free energy. In case of irreversible process one has

AT ≤ Fi− Ff

• Gibbs free energy G(T, P ) is Laplace transform of F (T, V ) in conjugate co- ordinates V → P

G = F + P V dG =−S dT + V dP

S = (∂G

∂T )

P

V = (∂G

∂P )

T

Under constant T and P the Gibbs function satises d G

d t ≤ 0

and is decrising in time reaching its minimum at the thermodynamic equilib- rium.

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1.1 Equation of state of a perfect gas 1 THERMODYNAMICS

1.1 Equation of state of a perfect gas

Perfect or ideal gas is a low pressure approximation of a real gas with the following characteristics:

1. molecules are point-like structures 2. no interaction among particles of gas

Equation of state of a real gas can be obtained combining empirical Boyle-Mariott and Guy-Lisac laws

P V = const. T = const.

P = P0(1 + αP∆t) V = const.

V = V0(1 + αV ∆t) P = const.

αP = αV = 1 273 K P = P0

T0 (T0+ T0αP (T − T0)) = P0 T0T P

T = P0 T0 V T = V0

T0

Let us take a gas from the state P1, V1, T1 to a state P1, V2, T2. Guy-Lisac gives V2 = T2

T1V1

now we take it from P1, V2, T2 ot the nal stateP2, V2, T2. Boyle-Marott gives P1V2 = P2V2

combining together the two results one nds P1V1

T1 = P2V2 T2

leading to the perfect gas law

P · V = N k T (1)

where N is the number of molecules and k = 1, 38 · 10−23J/K is the Boltzman constant. It is much easier to calculate the number of moles than a number of

molecules for a gas so it is convenient to rewrite the gas equation as follows P · V = N k T = n NAk T

R = NAk P · V = n R T

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1.1 Equation of state of a perfect gas 1 THERMODYNAMICS

where n is number of moles, NA= 6, 02· 1023 Avogadro's number and R = NAk = 8, 3· J/K is gas constant.

• Internal energy of perfect gas does not depend on volume (Joule's law) so

dU = (∂U

∂T )

V

dT + (∂U

∂V )

T

dV = cV dT U = U0+ cV T

• Enthalpy

H = U + P V = U0+ cV T + nRT H = cPT + U0

• The entropy of ideal gas is dS(T, V ) = ∂S

∂TdT + ∂S

∂V dV dS(T, V ) = cVdT

T +∂P

∂TdV dS(T, V ) = cV

dT

T +nR V dV S(T, V ) = S0+ cV ln T

T0

+ nR ln V V0

S(T, P ) = S0+ (cP − nR) ln T

T0 + nR ln V

V0 = S0+ cPln T

T0 − nR ln P P0 S(V, P ) = S0+ cP ln V

V0 + cV ln P P0

• Helmoltz free energy

F = U − T S = U0 + cV T − T (

S0+ cV ln T

T0 + nR ln V V0

)

F = cV T (

1− ln T T0

)

− nR lnV

V0 − S0T + U0

• Gibbs free energy

G = U − T S + P V = U0+ cV T − T (

S0+ cPln T

T0 + nR ln P P0

)

+ nRT G = cPT

(

1− ln T T0

)

− nR ln P

P0 − S0T + U0

(6)

1.2 PV diagrams 1 THERMODYNAMICS

1.2 PV diagrams

These diagrams describe work performed A =

P dV A|T =

P dV = nRT

V2

V1

dV /V = nRT lnV2 V1 A|P =

P dV = P (V2− V1) A|V = 0

1.3 TS diagrams

It is usual to dene γ = cP/cV, cV = nR/γ− 1, cP = nRγ/γ− 1 and one can write

S− S0 = (cP − cV) ln V

V0 + cV ln T T0 S− S0 = ln

(V V0

)cP ( P P0

)cV

= ln (V

V0

)nRγ/γ−1( P P0

)nR/γ−1

S− S0 = nR γ− 1ln

(V V0

)γ( P P0

)

P Vγ = const.e−1)S/nR T Vγ−1 = const.e−1)S/nR T Pγ−1/γ = const.e−1)S/nRγ

thus one obtains T, S diagrams describing the exchange of heat as

∆Q =

S2

S1

T (S)dS T (S)|V = const.e(γ−1)S/nR T (S)|P = const.e−1)S/nRγ

1.4 Adiabatic processes

A thermodynamical transformation is called adiabatic if no heat is exchanged during the process dQ = 0. A real transformation taking place very quickly is a good approximation of an adiabatic process. The work is done on the expenses of

internal energy

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1.5 Polytropic equation 1 THERMODYNAMICS

0 = cVdT + P dV dV

V =−cV nR

dT T

0 = d ln (T

T0 ) (V

V0 )γ−1

T Vγ−1 = const.

P Vγ = const.

T P(1−γ)/γ = const.

The work in an adiabatic process is

A = const.

V2

V1

dV /Vγ = const.

1− γV11−γ [

1 (V1

V2

)γ−1]

(2) const. V1γ−1 = P1V1 = nRT1 (3)

A = nRT1 γ− 1

( 1 T2

T1

)

(4)

1.5 Polytropic equation

This is a process during which the heat capacity, dened in general as dQ = c dT , remains constant. From the rst law and ideal gas law one has

c dT = cV dT + P dV P dV + V dP = RdT

P dV + V dP = R P dV c− cV

(c− cP)dV

V = (c− cV)dP P P Vn= const.

n = c− cP

c− cV

c = ncV − cP

n− 1

n is known as polytropic exponent. One can have the following situations

• n = 0 isobaric process c = cP

P = const.

(8)

2 VAN DER WAALS EQUATION FOR REAL GAS

• n = ∞ isochoric process c = cV

V = const.

• n = 1 isothermal process c = ∞

T = const.

n = cP/cV adiabatic process c = 0

dQ = 0

Figure 1: PV graph of a polytropic process while T, S graph is obtained from T = const.e(n−1)S/ncV−cP = const.eS/c

2 Van der Waals equation for real gas

Real gas has interacting molecules of nite size and these facts have to be taken into account. First of all the real volume available to the molecules is less than V

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2 VAN DER WAALS EQUATION FOR REAL GAS

due to the volume of interaction of each molecule b. This volume corresponds to the half (facing incoming molecule) of cross section of two molecules given by

b = 1 2N4π

3 (2R)2 = 16 3 N π R3 so one nds

P (V − b) = nR T

this is known as Clausius equation. Now take into account intermolecular interactions of order 1/r6 (Van der Waals forces) which reduce pressure of gas due to the density of molecules in the last two layers of gas. This net force decreases the

force exerted onto the wall by the particles in the surface layer. The net force on a surface particle, pulling it into the container, is proportional to the number density

C = N/V

The number of particles in the surface layers is, again by assuming homogeneity, also proportional to the density. In total, the force on the walls is decreased by a factor proportional to the square of the density, and the pressure (force per unit

surface) is decreased by

a C2 = a (N

V )2

Thus, modied equation is [

P + a (N

V )2]

(V − b) = nR T

if we introduce abbreviations as a = a NA2, b = b NA/N the equation can be written as

R T = (

P + a V2

)

(V − b) P = R T

V − b a V2

which is Van der Waals equation for one mole. For large volume V → ∞ it becomes the equation of perfect gas. VDW equation is cubic equation having an inexion

point characterized by critical values of Tc, Pc, Vc. Critical values correspond to

(10)

2 VAN DER WAALS EQUATION FOR REAL GAS

coinciding roots of the cubic equation V1 = V2 = V3 that can be found as follows.

0 = (V − Vc)3

0 = V3− 3V2Vc+ 3V Vc2− Vc3 0 = V3

(R T P + b

)

V2+ V a P ab

P 3Vc= R Tc

Pc + b 3Vc2 = a

Pc Vc3 = ab Pc

Tc= 8 a 27 b R Pc= a

27 b2 Vc= 3 b

VDW equation can be written in reduced form which is independent of type of gas involved. Introduce notation t = T/Tc, p = P/Pc, v = V /Vc to nd

p = 8 t

3 v− 1 3 v2

Figure 2: PV graph of Van der Waals gas

(11)

3 STATICS AND DYNAMICS OF A RIGID BODY

3 Statics and dynamics of a rigid body

Rigid body is dened as a collection of particles (atoms and molecules) that maintain xed position with respect to each other. Therefore, a rigid body moves as

a whole, rigid object. To every rigid body we associate a point called centre of mass, where we can consider concentrated the total mass of the object. In other words, the extended object can be replaced by its centre of mass. The motion of a

rigid body can thus be split into a motion of its centre of mass and a motion around an axis passing through its centre of mass. The centre of mass is dened as

⃗rCM =

nmn⃗rn Mtot

⃗rCM = 1 M

⃗r ρ dV

Example: The position of centre of mass of a circular section of angle φ0.

⃗rCM = 1 M

⃗r ρ dV

⃗rCM = ρ M

R 0

r2dr

φ0

0

(

cos φ⃗i + sin φ⃗j )

⃗rCM = ρ R3 3 M

(

sin φ0⃗i + (1− cos φ0) ⃗j )

M = ρ

R

0

r dr

φ0

0

dφ = ρR2 2 φ0

⃗rCM = 2 R 0

(

sin φ0⃗i + (1− cos φ0) ⃗j )

We can consider translation and rotation of a rigid body. Physical quantities characterizing translation are linear momentum ⃗p = m⃗v and force ⃗F = d ⃗p/d t.

Rotation is characterized by angular momentum ⃗L = ⃗r × ⃗p and by the momentum of force or twisting force known as torque (Latin torquere=to twist) M⃗ ≡ ⃗r × ⃗F = d⃗L/d t. The table below put in relation various quantities describing

translation and rotation

Translation Rotation

m-mass I-moment of inertia

p = m⃗v-linear momentum L = I⃗⃗ ω-angular momentum F = d⃗⃗ p/dt-force M = d⃗⃗ L/dt-torque EK = m v2/2-kinetic energy EK = Iω2/2-kinetic energy

One can see that the quantities describing rotation do not depend only on mass but also on the distance from the axis of rotation.

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3 STATICS AND DYNAMICS OF A RIGID BODY

The moment of inertia of a rigid body is dened as

I = lim

n→∞

n i=1

∆ mi⃗r2i =

⃗r2ρ d V

where ρ is the volume density of the substance. The angular momentum is Examples:

1. The moment of inertia of a circular section of angle φ0. I =

r2ρ dV I = ρ

R 0

r3dr

φ0

0

dφ = ρφ0R4 4 M = ρπ R2

Mφ = ρ R2φ0 2 = φ0

M Iφ0 = φ0

4πM R2

2. The moment of inertia of a circular ring of width R2− R1. I = IR2 − IR1 = 1

2

(M2R22− M1R21)

M1 = ρπ R21 M2 = ρπ R22

M = M2− M1 = M1

R21

(R22− R12

)

I = 1 2ρπ(

R42− R41

)

I = 1 2M(

R22+ R21)

3. Moment of inertia of a cylinder of radius R and hight h around an axis z passing through its centre

Iz = ρ

r2dV = ρ

R

0

r3dr

0

h/2

−h/2

dz Iz = ρπ

2R4h M = ρπ R2h

Iz = 1 2M R2

(13)

3 STATICS AND DYNAMICS OF A RIGID BODY

4. Moment of inertia of a cylinder of radius R and hight h around an axis x passing through the centre of its height h

Ix = ρ∫ (

z2 + y2)

dV = ρ

R

0

r dr

0

h/2

−h/2

(r2sin2φ + z2) dz

Ix = ρ

R

0

r dr

h/2

−h/2

d z(

r2π + 2π z2)

Ix = ρ

h/2

−h/2

d z (π

4R4+ π z2R2 )

= ρπ 4R2h

(

R2+ h2 3

)

M = ρπ R2h Ix = 1

4M (

R2+ h2 3

)

To show the advantage of choosing a proper basis for calculation let us calculate the area of a circle in Cartesian and polar coordinates.

R2 = x2+ y2circle in Cartesian coordinates A =

dx dy =

R/2

−R/2

dx

R2−x2/2

R2−x2/2

dy = 2

R/2

−R/2

√R2− x2dx

A =|x = R sin α| = 2 R

π/2

−π/2

sin2α dα = R2 (

α + sin 2α 2

)

|π/2−π/2 A = π R2

R = const. circle in polar coordinates A =

R 0

r dr

0

dφ = π R2

General form of moment of inertia following from the denition of angular momentum is

L = m ⃗⃗ r× ⃗vt= m ⃗r× (⃗ω × ⃗r) = m

3 i=1

(x2i ⃗ω− (⃗ω · ⃗r) ⃗xi

)

L = m⃗ [

ω(

x2+ y2+ z2)

− (ωx· x + ωyy + ωzz) ⃗xi] L = m⃗

[ ωx

(y2+ z2)

⃗i + ωy

(x2+ z2)

⃗j + ωx

(y2+ x2)

⃗k

− (ωyy + ωzz) x⃗i− (ωxx + ωzz) y ⃗j− (ωyy + ωxx) z ⃗k ]

Lx = m(

y2 + z2)

ωx− m x y ωy− m x z ωz = Ixxωx− Ixyωy− Ixzωz Ly = m(

x2+ z2)

ωy − m y x ωx− m y z ωz = Iyyωy− Iyxωx− Iyzωz Lz = m(

y2 + x2)

ωz − m z y ωy− m z x ωx = Izzωz− Izyωy− Izxωx

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3 STATICS AND DYNAMICS OF A RIGID BODY

One can see that the moments of inertia are components of a second-rank tensor (matrix)

Ixx Ixy Ixz Iyx Iyy Iyz Izx Izy Izz

Fortunately, it is always possible to choose three axis in a way that the mixed momenta are zero. These axis are known as principal axis and coincide with axis

of symmetry of the rigid body. The torque is

M =⃗ d⃗L

d t =∑

i

Iii (i

d t⃗ei+d⃗ei d tωi

)

d⃗ei

d t = ⃗ω× ⃗ei

M = I⃗ · ⃗α + ⃗ω × ⃗L → Euler equations

in the principal axis system one has Mx = Ixω˙x+ (Iz− Iy) ωyωz My = Iyω˙y+ (Ix− Iz) ωzωx Mz = Izω˙z+ (Iy − Ix) ωxωy

To dene equilibrium conditions for translation and rotation one requires F⃗tot ≡ ⃗F1+ ⃗F2+· · · + ⃗Fn = 0

M⃗tot ≡ ⃗M1+ ⃗M2+· · · + ⃗Mn = 0

The above condition lead also to the conservation of linear and angular momentum, which, together with conservation of energy represent fundamental

conservation laws of physics F⃗tot = 0 ⇒ ⃗ptot = const..

M⃗tot = 0 ⇒ ⃗Ltot = const..

Torque can be written in terms of of the components of force ⃗F and its arm ⃗r in the Cartesian coordinate system as

M = ⃗⃗ r× ⃗F Mx = y Fz− z Fy

My = z Fx− x Fz

Mz = x Fy− y Fx

(15)

3 STATICS AND DYNAMICS OF A RIGID BODY

Assume that we have two forces ⃗F1, ⃗F2, in the y, z plane, producing two torques M⃗1, ⃗M2 around a centre of rotation O having an arm ⃗r. The resulting (total) torque

is M⃗R = ⃗M1+ ⃗M2

Mx,R = y Fz,1− z Fy,1+ y Fz,2− z Fy,2

Mx,R = y (Fz,1+ Fz,2)− z (Fy,1+ Fy,2) Mx,R = y FR,z− z FR,y = Mx,1+ Mx,2

this simple property of vectors goes under the name of Varignon theorem in civil engineering. The proof is based on equivalence of areas which simply means that the geometrical meaning of a cross-product is an area formed by the two vectors in

the product.

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