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1st Law: Conservation of Energy energy flow boundary = Δ ( E system ) Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal to the energy change of the system NOTE: sign of flow is positive when into the system UNITS: Joules, calories, electron volts …
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1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Jan 13, 2016

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Oswald Boone
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Page 1: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

1st Law: Conservation of Energy

energy flow

boundary

∑ = Δ ( Esystem

)

Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal to the energy change of the system

NOTE: sign of flow is positive when into the system

UNITS: Joules, calories, electron volts …

Page 2: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Types of Work

Electrical

W = – dq

Magnetic

δW= μoV HdM

Surface

W = – dA

Page 3: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Summary so far

Page 4: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Variables and Parameters

System is only described by its macroscopic variables

Variables: Temperature + one variable for every work term that exchanges energy with the system + one variable for every independent component that can leave or enter the system.

Parameters: Quantities that are necessary to describe the system but which do not change as the system undergoes changes.

e.g. for a closed system: ni are parameters for a system at constant volume: V is parameter

Equations of State (Constitutive Relations): equation between the variables of the system. One for each work term or matter flow

Page 5: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Example of Equations of State

pV = nRT: for ideal gas

= E for uniaxial elastic deformation

M = H: paramagnetic material

Page 6: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Properties and State Functions

U = U(variables) e.g. U(T,p) for simple system

Heat capacity

cV =1n

δQdT

⎛ ⎝

⎞ ⎠ V

cp =1n

δQdT

⎛ ⎝

⎞ ⎠ p

Volumetric thermal expansion

Compressibility

αV =1V

dVdT

⎛ ⎝

⎞ ⎠

p

βV = −1V

dVdp

⎛ ⎝ ⎜

⎞ ⎠ ⎟

T

Page 7: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Some Properties Specific to ideal gasses

∂U∂V

⎛ ⎝

⎞ ⎠ T

=0

1) PV = nRT

2) cp - cv = R

3)

ONLY for IDEAL GASSES

Proof that for ideal gas, internal energy only depends on temperature dU =ncvdT

Page 8: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The Enthalpy (H)

H = U + PV

Gives the heat flow for any change of a simple system that occurs under constant pressure

Example: chemical reaction

Page 9: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Example: Raising temperature under constant pressure

dHp =δQp =ncp dT

cp =∂HdT

⎛ ⎝

⎞ ⎠ p

H

TT

m

Δ H

m

C

,p l

C

,p s

Page 10: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Enthalpy of Materials

is always relative

Elements: set to zero in their stable state at 298K and 1 atm pressure

Compounds: tabulated. Are obtained experimentally by measuring the heat of formation of the compounds from the elements under constant pressure.

Page 11: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The Enthalpy (H)

H = U + PV

Gives the heat flow for any change of a simple system that occurs under constant pressure

Example: chemical reaction

Page 12: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Example: Raising temperature under constant pressure

dHp =δQp =ncp dT

cp =∂HdT

⎛ ⎝

⎞ ⎠ p

H

TT

m

Δ H

m

C

,p l

C

,p s

Page 13: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Enthalpy of Materials

is always relative

Elements: set to zero in their stable state at 298K and 1 atm pressure

Compounds: tabulated. Are obtained experimentally by measuring the heat of formation of the compounds from the elements under constant pressure.

Page 14: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Entropy and the Second Law

dS ≥δQT

There exists a Property of systems, called the Entropy (S), for which holds:

How does this solve our problem ?

Page 15: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The Second Law leads to Evolution Laws

System

S

time

equilibrium

Isolated system

Page 16: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Evolution Law for constant Temperature and Pressure

TdS≥dU+pdV

⇒ d(TS) ≥dU+d(pV)

d(U +pV−TS)≤0

dG ≤ 0

G (Gibbs free energy is the relevant potential to determine stability of a material under constant pressure and temperature

Page 17: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Interpretation

For purely mechanical systems: Evolution towards minimal energy.

Why is this not the case for materials ?

Materials at constant pressure and temperature can exchange energy with the environment.

G is the most important quantity in Materials Science

determines structure, phase transformation between them, morphology, mixing, etc.

System

G

time

equilibrium

T,P

Page 18: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Phase Diagrams: One component

Describes stable phase (the one with lowest Gibbs free energy) as function of temperature and pressure.

WaterCarbon

Page 19: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Temperature Dependence of the Entropy

dS=δQT

dS( )p =δQ( )p

T=

Cp dT( )p

T∂S∂T

⎛ ⎝

⎞ ⎠ p

=Cp

T

S

TTm

Tb

Page 20: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Temperature Dependence of the Entropy

dS=δQT

dS( )p =δQ( )p

T=

Cp dT( )p

T∂S∂T

⎛ ⎝

⎞ ⎠ p

=Cp

T

S

TTm

Tb

Page 21: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

What is a solution ?

SYSTEM with multiple chemical components that is mixed homogeneously at the atomic scale

•Liquid solutions

•Vapor solutions

•Solid Solutions

Page 22: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Composition Variables

MOLE FRACTION:

ATOMIC PERCENT:

CONCENTRATION:

WEIGHT FRACTION:

Xi =ni

ntot

(at%)i =100% Xi

Ci =ni

Vor

Wi

V

wi =Wi

Wtot

Page 23: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Variables to describe Solutions

G=G(T,p,n1,n2, …, nN)

dG=∂G∂T

⎛ ⎝ ⎜

⎞ ⎠ ⎟

p,ni

dT +∂G∂p

⎝ ⎜

⎠ ⎟

T ,ni

dp+∂G∂ni

⎝ ⎜

⎠ ⎟

p,T

dni

dG=−SdT+V dp+μi dni

Partial Molar Quantity

V i =∂V∂ni

⎝ ⎜

⎠ ⎟

T ,p,nj

H i =∂H∂ni

⎝ ⎜

⎠ ⎟

T ,p,n j

S i =∂S∂ni

⎝ ⎜

⎠ ⎟

T ,p,nj

Partial Molar Quantity

μi ≡∂G∂ni

⎝ ⎜

⎠ ⎟

p,T

chemical potential

Page 24: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Partial molar quantities give the contribution of a component to a property of the solution

G =i

∑ μini

V =i

∑ V ini

Page 25: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Properties of Mixing

A,BA

B

Change in reaction:

XA A + XB B -> (XA, XB )

ΔHmix =Hmix −XA H A −XB H B

=Hmix − H A +XB H B −H A( )[ ]

H

HB

HA

XB

Page 26: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Cu-Pd

Ni-Pt

Page 27: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Intercept rule with quantity of mixing

ΔVmix

VB - VB

XBX*BVA - VA

ΔGmix

μB - GB

XBX*B

μA - GA

Page 28: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

General Equilibrium Condition in Solutions

μiα =μi

β =μiγ =...

Chemical potential for a component has to be the same in all phases

For all components i

OPEN SYSTEM

Components have to have the same chemical potential in system as in environment

e.g. vapor pressure

Page 29: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Example: Solubility of Solid in Liquid

pure A liquid

B solid

Gliquid

GlBGlA

XB

GsB

Page 30: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Summary so far

1) Composition variables

2) Partial Molar Quantities

3) Quantities for mixing reaction

4) Relation between 2) and 3): Intercept rule

5) Equilibrium between Solution Phases

Page 31: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Standard State: Formalism for Chemical Potentials in Solutions

μi =μi0 +RT ln(ai )

chemical potential of i in solution

chemical potential of i in a standard state

effect of concentration

Choice of standard state is arbitrary, but often it is taken as pure state in same phase.

Choice affects value of ai

Page 32: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Models for Solution: Ideal Solution

An ideal solution is one in which all components behave Raoultian

ai =xi forall i

A,BA

B

ΔGmix =Gmixture−Gcomponents

xAμA +xBμB xAGA +xBGB

ΔGmix =RT xA lnxA +xB lnxB[ ]

ΔGmix =xA μA0 +RT lnaA( )+xB μB

0 +RT lnaB( ) − xAGA −xBGB

Page 33: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Summary Ideal Solutions

ΔGmix =RT xi lnxii

ΔHmix =0

ΔSmix =−R xi lnxii∑

ΔVmix =0

XB

Page 34: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Solutions: Homogeneous at the atomic level

Random solutionsOrdered solutions

Page 35: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Summary so far

1) Composition variables

2) Partial Molar Quantities

3) Quantities for mixing reaction

4) Relation between 2) and 3): Intercept rule

5) Equilibrium between components in Solution Phases

For practical applications it is important to know relation between chemical potentials and composition

Page 36: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Obtaining activity information: Experimental

e.g. vapor pressure measurement

Pure substance i Mixture with component i in it

vapor pressure pi* vapor pressure pi

Δμi =RT lnpi

pi*

⎝ ⎜

⎠ ⎟

Δμi =RT ln ai( )

pi

pi* = ai

Page 37: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Obtaining activity information: Simple Models

Raoultian behavior

Henry’s behavior

ai =xi

ai =kxi

Usually Raoultian holds for solvent, Henry’s for solute at small enough concentrations.

Page 38: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Intercept rule

Page 39: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

General Equilibrium Condition in Solutions

μiα =μi

β =μiγ =...

Chemical potential for a component has to be the same in all phases

For all components i

OPEN SYSTEM

Components have to have the same chemical potential in system as in environment

e.g. vapor pressure

Page 40: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Raoultian case and Real case

Page 41: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Review•At constant T and P, a closed system strives to minimize its Gibbs free energy: G = H - TS

•Mixing quantities are defined as the difference between the quantity of the mixture and that of the constituents. All graphical constructions derived for the quantity of a mixture can be used for a mixing quantity with appropriate adjustment of standard (reference) states.

G AG B

X B0 1

G

X B0 1

Δ Gmix

μA

- GA

μB

- GB

Page 42: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Review (continued)

Some simple models for solutions can be me made: Ideal solution, regular solution.Many real solution are much more complex than these !

ΔGmix= ΔHmix – TΔSmix

= ω xB(1−xB) + RT xA lnxA +xB lnxB[ ]

Regular Solution

Page 43: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The Chord Rule

What is the free energy of an inhomogeneous systems ( a system that contains multiple distinct phases) ?

CHORD RULE: The molar free energy of a two-phase system as function of composition of the total system, is given by the chord connecting the molar free energy points of the two constituent phases

Page 44: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The Chord Rule graphically

A B

With pure components Components are solutions

overall composition is XB*

XB

overall composition is XB*

G

0 1XB

XB*

G

0 1XB

XB*

XB

Page 45: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Regular Solution Model

ΔGmix= ωxB(1−xB) + RT (1−xB)ln(1−xB) +xB lnxB[ ]

0 XB 1< 0

Page 46: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Regular Solution Model

ΔGmix= ωxB(1−xB) + RT (1−xB)ln(1−xB) +xB lnxB[ ]

0 XB 1

> 0

Page 47: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Effect of concave portions of G

0 XB* 1

Page 48: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Single-Phase and Two-phase regions

0 XB* 1XB

XB

Single-phase

Single-phaseTwo-phase

Page 49: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Two-phase coexistence

When ΔGmix has concave parts (i.e. when the second derivative is negative) the coexistence of two solid solutions with different compositions will have lower energy.

The composition of the coexisting phases is given by the Common Tangent construction

The chemical potential for a species is identical in both phases when they coexist.

Page 50: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Common tangent does not need to be horizontal

0 XB* 1

Page 51: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Temperature Dependence of Two-phase region

0XB

1

ΔHmix

0XB

1

ΔHmix

0XB

1

ΔHmix

Low temperature Intermediate temperature High temperature

Page 52: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Phase Diagram of Regular Solution Model with > 0

0 XB 1

T

Page 53: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Example: Cr-W

Page 54: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Miscibility gap does not have to be symmetric

Page 55: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Lens-Type Diagram

Liquid

Solid

L+S

XB

0 1

Page 56: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Free energy curves for liquid and solid

0

XB

1

G

0

XB

1

G

0

XB

1

G

T > TBM > TA

M TBM > T > TA

M

TBM > TA

M > T

Page 57: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

How much of each phase ? - The Lever Rule

Since the composition of each phase is fixed by the common tangent, the fraction of each phase can be determined from requiring that the system has the given overall composition

XB* = fαXB

α +fβ XBβ

1= fα +fβ-> solve for f and f

fα =XB

β −XB*

XBβ −XB

α fβ =XB

* −XBα

XBβ −XB

α

The result is known as the Lever Rule

Page 58: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Lever Rule

x x

x

x x

x

f

f

Page 59: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

In a two-phase region chemical potential is constant

0 XB 1

0 XB 1

G

μ

Page 60: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Comparison between Eutectic and Peritectic

L

L

Eutectic Peritectic

Cooling: L -> Heating: -> L +

Page 61: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Nucleation 

(1) The structure of the liquid Many small closed packed solid clusters are present in the liquid. These clusters would form and disperse very quickly. The number of spherical clusters of radius r is given by 

 nr : average number of spherical clusters with radius r.

n0: total number of atoms in the system.

ΔGr: excess free energy associated with the cluster.

 

n nG

kTrr= −⎛

⎝⎞⎠0 xp

Δ

Page 62: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

(2) The driving force for nucleation

 The free energies of the liquid and solid at a temperature T are given by GL = HL- TSL and GS = HS- TSS

 GL and GS are the free energies of the liquid and solid respectively.

HL and HS are the enthalpy of the liquid and solid respectively.

SL and SS are the entropy of the liquid and solid respectively.

 At temperature T, we have ΔGV = GL- GS = HL-HS-T(SL-SS) =ΔH-TΔS,

 ΔGV: volume free energy.

where ΔH and ΔS are approximately independent of temperature.

Page 63: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

For a spherical solid of radius r, 

Δ ΔG r G rV SL= − +4

343 2π π γ

For a given ΔT, the solid reach a critical radio r*, whend G

dr

( )Δ=0

rG

SL

V

* =2γΔ

ΔΔ

GG

SL

V

∗ =16

3

3

2

πγ

( )

ΔΔ

G LT

TV mm

=

rT

L TSL m

m

* =2 1γ

Δ( )22m

3SL

T

1

L3

Tm16G

Δ

πγ=Δ ∗

)(

We get

If

and

then,

and

When r < r, the solid is not stable, and when r > r, the solid is stable.

Page 64: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The effect of temperature on the size of critical nucleation and the actual shape of a nucleus.

Page 65: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

(4) Heterogeneous nucleation If a solid cap is formed on a mould, the interfacial tensions balance in the plane of the mould wall, or

γSL, γSM and γML: the surface tensions of the solid/liquid, solid/mould and mould/liquid interfaces

respectively.

γ γ γ θML SM SL= + coscosθ γ γγ=−ML SM

SL

The excess free energy for formation of a solid spherical cap on a mould is ΔGhet = -VSΔGV + ASLγSL + ASMγSM - ASMγML

 Where VS: the volume of the spherical cap.

ASL and ASM: the areas of the solid/liquid and

solid/mould interfaces. It can be easily shown that,   where

Δ ΔG r G r fhet V SL= − + ×( ) ( )43 43 2π π γ θ

f ( )( cos cos )θ θ θ

=− +2 3

43

Page 66: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

(c) Nucleation rate and nucleation time as a function of temperature

The overall nucleation rate, I, is influenced both by the rate of cluster formation and by the rate of atom transport to the nucleus, which are both influenced in term by temperature. TTT diagram gives time required for nucleation, which is inversely proportional to the nucleation rate.

Page 67: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

600620640660680700720740760780800820840860

100 1000 10000

Actual examples of TTT diagram

Page 68: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Nucleation in Solid

Interface structure

Page 69: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Coherency loss

24

3

μ

γ= st

critr

Page 70: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Homogeneous Nucleation

(a) Homogeneous nucleation

SV GVAGVG ΔΔΔ +γ+−=

 

The free energy change associated with the nucleation process will have the following three contributions.

1 . At temperatures where the phase is stable, the creation of a volume V of will cause a volume free energy reduction of VΔGv.  

2. Assuming for the moment that the / interfacial energy is isotropic the creation of an area A of interface will give a free energy increase of Aγ.

3. In general the transformed volume will not fit perfectly into the space originally occupied by the matrix and this gives rise to a misfit strain energy ΔGv, per unit volume of . (It was shown in Chapter 3 that, for both coherent and incoherent inclusions, ΔGv, is proportional to the volume of the inclusion.) Summing all of these gives the total free energy change as

Page 71: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

If we assume the nucleus is spherical with a radius r, we have

γp+−p−= 23 43

4rGGrG SV )( ΔΔΔ

)(*

SV GGr

ΔΔ −γ

=2

2

3

3

16

)( SV GGG

ΔΔΔ

pγ=∗

Similarly we have

Page 72: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Nucleation at Grain Boundary

The excess free energy associated with the embryo at a grain boundary will be given by

ΔG = -VΔGv + Aγ - Aγ

Where V is the volume of the embryo, A is the area of / interface of energy created, and

A the area of / grain boundary of energy destroyed during the process.

γγ

=ϑ2

cos

Page 73: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Fick I

It would be reasonable to take the flux across a given plane o be proportional to the concentration gradient across the plane:

⎥⎦

⎤⎢⎣

⎡∂∂

−=x

cDJ

J: the flux, [quantity/m2s]

D: diffusion coefficient, [m2/s]

⎥⎦

⎤⎢⎣

⎡∂∂x

cConcentration gradient, [quantity /m-4]

Here, quantity can be atoms, moles, kg etc.

Page 74: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Fick II:

2

2

x

CD

t

C

∂=

Page 75: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

1. Thin Film (Point Source) Solution

M( )x

X

1D

X

2Dy

M( ) x per unit y

X

3D

M( ) x per unit area

c(x,t) =M

4πDtexp−

x2

4Dt

⎝ ⎜

⎠ ⎟

assume boundaries at infinity c(x,0) =Mδ(x)

c(∞,t)=c(−∞,t)=0

Solution to Fick II

Page 76: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

c(x,t) =M

4πDtexp−

x2

4Dt

⎝ ⎜

⎠ ⎟

Page 77: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Measurement of diffusion coeffiecient

c(x,t) =M

4πDtexp−

x2

4Dt

⎝ ⎜

⎠ ⎟

Dt4

xtconsc

2−= tanln

If c versus x is known experimentally, a plot of ln(c) versus x2 can then be used to determine D.

x

Page 78: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Error functions

exp(−x2)

exp(−u2)0

x

∫ du =erf(x)

)()(

)()(

)(

)(

zerfzerf

xerf1xerfc

1erf

00erf

−=−−=

=∞=

Page 79: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

The final solution should be:

⎥⎦

⎤⎢⎣

⎡⎟⎠

⎞⎜⎝

⎛+=

Dt2

xerf1

2

ctxc

'),(

( )

⎥⎥⎦

⎢⎢⎣

⎡ −−

p= ∫∞ d

Dt4

x

Dt2

ctxc 0

2exp

'),(

Page 80: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

⎥⎦

⎤⎢⎣

⎡⎟⎟⎠

⎞⎜⎜⎝

⎛+=

Dt2

xerf1Ctxc s),(

When x=0, the composition is always kept at c=c’/2

⎥⎦

⎤⎢⎣

⎡⎟⎠

⎞⎜⎝

⎛+=

Dt2

xerf1

2

ctxc

'),(

erf(-z)=-erf(z)

⎥⎦

⎤⎢⎣

⎡⎟⎠

⎞⎜⎝

⎛−=

Dt2

xerf1Ctxc s),(

Page 81: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Diffusion Mechanis

Interstitial mechanism Self Diffusion with Vacancy

Ring Mechanism Interstitialcy

These are the two most common mechanisms

Page 82: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

A Random Jump Process

  

1B1 n6

1J Γ=

2n

6

1J B2 Γ=

)( 21B21B nn6

1JJJ −Γ=−=

⎟⎠

⎞⎜⎝

⎛∂∂

−=−x

C2C1C B

BB )()(

x

C

6

1J B2

BB ∂∂

⎟⎠

⎞⎜⎝

⎛ Γ−=

Page 83: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Diffusion by Vacancy mechanism

⎟⎠

⎞⎜⎝

⎛ Δ−υ=Γ

RT

GXz m

vB exp

⎟⎠

⎞⎜⎝

⎛−=RT

GX v

v exp

2BA 6

1D Γ=

⎟⎠

⎞⎜⎝

⎛ Δ+Δ−⎟

⎞⎜⎝

⎛ Δ+Δυ=

RT

HH

R

SSz

6

1D vmvm2

A expexp

⎟⎠

⎞⎜⎝

⎛−=RT

QDD 0A exp

⎟⎠

⎞⎜⎝

⎛ Δ+Δυ=

R

SSz

6

1D vm2

0 exp

Page 84: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Effeect of temperature on diffusion

⎟⎠

⎞⎜⎝

⎛−=RT

QDD 0A exp

Page 85: 1st Law: Conservation of Energy Energy is conserved. Hence we can make an energy balance for a system: Sum of the inflows – sum of the outflows is equal.

Effect of defect on diffusion