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Metallurgical Thermodynamics Syllabus

April 02, 2025

GATE MT - Metallurgical Thermodynamics

Metallurgical Thermodynamics

Complete Guide for GATE Metallurgy (MT) - Section 2 (TestUrSelf)

2.1 Laws of Thermodynamics

First Law of Thermodynamics

Energy Conservation

The first law states that energy cannot be created or destroyed, only converted from one form to another.
ΔU = q + w

Where:

  • ΔU = change in internal energy of the system
  • q = heat transferred to the system
  • w = work done on the system

Enthalpy

H = U + PV
ΔH = ΔU + PΔV (at constant pressure)

Heat Capacity

Type Definition Relation
Constant Volume (CV) (∂U/∂T)V CV = (∂q/∂T)V
Constant Pressure (CP) (∂H/∂T)P CP = (∂q/∂T)P

Applications to Metallurgical Systems

Heat effects in metallurgical processes:

ΔH = ΣHproducts - ΣHreactants

Kirchhoff's Law for temperature dependence:

(∂(ΔH)/∂T)P = ΔCP
ΔH(T2) = ΔH(T1) + ∫ΔCPdT
Example: Heat of Formation

For the reaction: Fe + ½O2 → FeO

ΔH298 = -267 kJ/mol

Calculate ΔH at 500K given ΔCP = 10 J/mol·K

Solution: ΔH500 = -267,000 + 10×(500-298) = -265 kJ/mol

Second Law of Thermodynamics

Entropy

The second law introduces the concept of entropy as a measure of disorder and establishes the direction of spontaneous processes.
dS ≥ δq/T (Clausius Inequality)

For reversible processes:

dS = δqrev/T

Carnot Cycle Efficiency

η = 1 - Tcold/Thot

Entropy Changes

Process Entropy Change
Isothermal expansion ΔS = nRln(V2/V1)
Isochoric heating ΔS = nCVln(T2/T1)
Isobaric heating ΔS = nCPln(T2/T1)
Phase transition ΔS = ΔHtransition/Ttransition

Key Points

  • Entropy always increases for irreversible processes
  • The universe tends toward maximum entropy
  • Entropy is a state function

Thermodynamic Potentials

Gibbs and Helmholtz Free Energy

Potential Definition Natural Variables
Gibbs Free Energy (G) G = H - TS T, P, n
Helmholtz Free Energy (A) A = U - TS T, V, n

Chemical Potential

μi = (∂G/∂ni)T,P,nj≠i

For a pure substance: μ = Gm (molar Gibbs free energy)

Maxwell's Relations

Relation Derived From
(∂T/∂V)S = -(∂P/∂S)V dU = TdS - PdV
(∂T/∂P)S = (∂V/∂S)P dH = TdS + VdP
(∂S/∂V)T = (∂P/∂T)V dA = -SdT - PdV
(∂S/∂P)T = -(∂V/∂T)P dG = -SdT + VdP
Example Application

Using (∂S/∂P)T = -(∂V/∂T)P to find entropy change with pressure:

For an ideal gas: (∂V/∂T)P = nR/P

Thus: (∂S/∂P)T = -nR/P

ΔS = -nRln(P2/P1) for isothermal pressure change

2.2 Solutions and Phase Equilibria

Ideal and Regular Solutions

Raoult's Law

Pi = xiPi0

Where Pi0 is the vapor pressure of pure component i

Activity and Activity Coefficient

μi = μi0 + RTln(ai)
ai = γixi

Where γi is the activity coefficient (γi = 1 for ideal solutions)

Excess Properties

Solution Type GE Behavior
Ideal 0 ΔHmix = 0, ΔVmix = 0
Regular Ωx1x2 ΔHmix ≠ 0, ΔSmix = ideal
Athermal -TΔSE ΔHmix = 0, ΔSmix ≠ ideal

Henry's Law

Pi = KHxi (for dilute solutions)

Where KH is Henry's constant

Phase Diagrams

Gibbs Phase Rule

F = C - P + 2

Where:

  • F = degrees of freedom
  • C = number of components
  • P = number of phases

Lever Rule

Wα/Wβ = (Cβ - C0)/(C0 - Cα)

Where Wα and Wβ are weight fractions of phases α and β

Common Binary Phase Diagrams

Type Features Example System
Isomorphous Complete solid solubility Cu-Ni
Eutectic Eutectic point, limited solubility Pb-Sn
Peritectic Peritectic reaction: L + α → β Fe-C (δ-ferrite region)
Monotectic Liquid immiscibility gap Cu-Pb

Free Energy vs Composition

(∂G/∂xB)α = (∂G/∂xB)β (common tangent rule)
Gmix = RT(xAlnxA + xBlnxB) (ideal solution)

Thermodynamic Diagrams

Equilibrium Constant

ΔG° = -RTlnK
K = exp(-ΔG°/RT)

Ellingham Diagrams

ΔG° = A + BT

Key features:

  • Slope = -ΔS°
  • Y-intercept = ΔH°
  • Phase change points show slope changes
Reaction ΔG° (J/mol) Equation
4/3Al + O2 → 2/3Al2O3 -1,120,000 + 214T
2C + O2 → 2CO -223,000 - 175T
2Fe + O2 → 2FeO -529,000 + 125T

Phase Stability Diagrams

Showing stable phases as functions of thermodynamic variables (T, P, composition)

Example: Fe-O System

Stable phases at different oxygen partial pressures and temperatures:

  • Low pO2: Metallic Fe
  • Intermediate pO2: FeO (wüstite)
  • High pO2: Fe2O3 (hematite)

2.3 Defects and Interfaces

Point Defects

Vacancies

nv/N = exp(-ΔGf/kT)

Where:

  • nv = number of vacancies
  • N = number of lattice sites
  • ΔGf = Gibbs free energy of formation

Schottky Defects

[VM][VX] = KS = exp(-ΔGS/kT)

For NaCl: [VNa] = [VCl] = exp(-ΔGS/2kT)

Frenkel Defects

[VM][Mi] = KF = exp(-ΔGF/kT)

Where Mi is interstitial metal ion

Defect Type Example Materials Formation Energy (eV)
Vacancy Metals (Cu, Fe) 0.5-2.0
Schottky NaCl, MgO 2.0-4.0
Frenkel AgCl, ZrO2 1.5-3.0

Surfaces and Interfaces

Surface Energy

γ = (∂G/∂A)T,P,ni

Typical values:

  • Metals: 1-3 J/m2
  • Oxides: 0.5-1.5 J/m2
  • Water: 0.072 J/m2 at 20°C

Gibbs Adsorption Equation

dγ = -ΣΓii

For binary systems:

Γ2 = -(∂γ/∂μ2)T

Segregation Phenomena

Xisurface/Xibulk = exp(-ΔGseg/RT)

Where ΔGseg is segregation free energy

Interface Type Energy (J/m2) Characteristics
Grain boundary 0.5-1.0 Depends on misorientation angle
Phase boundary 0.2-0.8 Depends on lattice mismatch
Solid-liquid 0.1-0.5 Important in wetting phenomena

2.4 Electrochemistry

Single Electrode Potential

Standard electrode potential measured against SHE (Standard Hydrogen Electrode)

Electrode Reaction E° (V vs SHE)
Li+ + e- → Li -3.04
Al3+ + 3e- → Al -1.66
Fe2+ + 2e- → Fe -0.44
Cu2+ + 2e- → Cu +0.34
Ag+ + e- → Ag +0.80

Electrochemical Cells

Ecell = Ecathode - Eanode
ΔG = -nFEcell

Where:

  • n = number of electrons transferred
  • F = Faraday's constant (96,485 C/mol)
Cell Type Example E° (V)
Galvanic Zn|Zn2+||Cu2+|Cu +1.10
Concentration Cu|Cu2+(0.1M)||Cu2+(1M)|Cu ≈0.03

Nernst Equation

E = E° - (RT/nF)ln(Q)

At 298K:

E = E° - (0.0591/n)log(Q)
Example: Zn/Zn2+ Electrode

For Zn2+ + 2e- → Zn, E° = -0.76V

At [Zn2+] = 0.01M:

E = -0.76 - (0.0591/2)log(1/0.01) = -0.76 - 0.0591 = -0.82V

Potential-pH Diagrams

Pourbaix Diagrams

Showing stable phases as functions of potential (E) and pH

Key Lines

Hydrogen evolution reaction (HER):

2H+ + 2e- → H2; E = -0.0591pH

Oxygen evolution reaction (OER):

O2 + 4H+ + 4e- → 2H2O; E = 1.23 - 0.0591pH
Region Fe Species Condition
Immunity Fe Low potential
Corrosion Fe2+, Fe3+ Intermediate potential, acidic pH
Passivation Fe2O3, Fe3O4 High potential, neutral/alkaline pH