High-Temperature Oxidation of Metals — Mechanisms, Pilling-Bedworth Ratio, Wagner Theory, and Protective Coatings
When metals are exposed to oxygen at elevated temperatures, they react to form oxide scales. Whether those scales protect the underlying metal for decades or accelerate its destruction in hours depends on a precise set of physical and chemical conditions — the volume relationship between oxide and parent metal, the ionic defect structure of the oxide, the rate of mass transport through it, and the adhesion between the scale and the alloy surface under cyclic thermal loading. High-temperature oxidation is the dominant degradation mode for gas turbine hot-section components, industrial furnace hardware, boiler tubes, automotive exhaust systems, and nuclear fuel cladding. This article provides a graduate-engineer-level treatment of the complete discipline: oxidation kinetics and rate law derivations, the Pilling-Bedworth ratio and its limitations, Wagner’s ionic transport theory, selective oxidation thermodynamics, the reactive element effect, chromia and alumina former alloy systems, hot corrosion and sulfidation mechanisms, and the complete thermal barrier coating system that extends turbine component life beyond what any metallic alloy can achieve alone — with a built-in oxidation rate calculator.
Key Takeaways
- Three rate laws govern oxide growth: parabolic (Δm² = kpt, diffusion-limited, protective), linear (Δm = klt, interface-limited, destructive), and logarithmic (low-temperature thin-film growth). The Arrhenius activation energy Q extracted from parabolic kp data identifies the rate-limiting diffusing species.
- The Pilling-Bedworth ratio PBR = (MoxρM)/(nMMρox) predicts oxide scale protectiveness: PBR < 1 → porous (non-protective); PBR 1–2 → compressive, adherent (protective); PBR > 2 → excessive compressive stress → spallation.
- Wagner theory derives kp from the ionic conductivity of the oxide and the oxygen chemical potential gradient; it predicts that aliovalent doping reduces cation vacancy concentration and lowers kp — the mechanistic basis for chromium and aluminium additions to alloys.
- Reactive elements (Y, Ce, La, Hf, Zr) at 0.01–0.3 wt% segregate to oxide grain boundaries, switch transport from outward cation diffusion to inward oxygen diffusion, and improve scale adhesion 5–20× during thermal cycling. All MCrAlY coatings rely on this effect.
- Hot corrosion Types I (850–950 °C) and II (650–750 °C) proceed by molten Na2SO4-based salt fluxing and dissolution of protective Cr2O3 and Al2O3 scales at rates orders of magnitude faster than normal oxidation.
- TBC life is limited by TGO (thermally grown oxide) thickness: when the α-Al2O3 TGO reaches 5–8 μm, thermal expansion mismatch on cooling drives interface crack propagation and top-coat spallation. CMAS attack at T > 1240 °C further destabilises YSZ by dissolving the yttria stabiliser.
Oxidation Rate Calculator
Parabolic rate law | Pilling-Bedworth ratio | Arrhenius kp temperature correction
Given kp at a known temperature T1, calculate kp at a new temperature T2 using the Arrhenius relationship.
Typical Q values: Fe in air 160 kJ/mol; Ni-20Cr (Cr₂O₃) 200 kJ/mol; FeCrAl (Al₂O₃) 310 kJ/mol; SiO₂ 120 kJ/mol
Oxidation Kinetics — Rate Law Derivation
The rate at which an oxide scale grows on a metal surface is determined by which step in the overall reaction sequence is slowest — the rate-limiting step. Identifying the rate law from experimental mass gain data immediately reveals the mechanism and whether the scale is protective.
Parabolic Rate Law — Derivation
For a dense, adherent, continuous scale, the only path for the reaction to proceed is transport of ions or electrons through the scale. The flux of ions through the scale is inversely proportional to the scale thickness x (the diffusion path length), giving a growth rate that decreases as the scale thickens — the signature of diffusion-controlled kinetics:
Parabolic rate law derivation:
Scale growth rate: dx/dt = k' / x (growth rate inversely proportional to thickness)
Separating variables and integrating:
x·dx = k'·dt
∫₀ˣ x·dx = ∫₀ᵗ k'·dt
x² / 2 = k'·t
x² = 2k'·t = K_p·t (K_p = parabolic rate constant for thickness)
In practice, oxidation measured by MASS GAIN per unit area (Δm, mg/cm²):
Δm² = k_p · t [k_p in mg²/cm⁴·s or g²/cm⁴·s]
Instantaneous oxidation rate (differentiating):
d(Δm)/dt = k_p / (2·Δm) → rate decreases as scale thickens
Arrhenius temperature dependence of k_p:
k_p = A · exp(−Q / RT)
A = pre-exponential factor (material and gas-composition dependent)
Q = apparent activation energy (kJ/mol) — identifies rate-limiting step:
Q ≈ 120–160 kJ/mol → O²⁻ diffusion (inward; anion transport)
Q ≈ 200–250 kJ/mol → cation diffusion (M²⁺ outward; cation transport)
Q ≈ 300–350 kJ/mol → grain boundary diffusion in Al₂O₃
Converting mass gain to oxide thickness (using oxide density ρ_ox):
Scale thickness x (µm) = Δm (mg/cm²) × M_ox / (n × M_O × ρ_ox × 10)
where n = number of O atoms per oxide formula unit
For Al₂O₃: M_ox=102, M_O=16, ρ_ox=3.99 g/cm³, n=3:
x = Δm × 102 / (3 × 16 × 3.99 × 10) = Δm × 0.534 [µm per mg/cm²]
Linear Rate Law
When the scale provides no diffusion barrier — either because it is porous, cracks on growth, is volatile, or melts — the metal surface is always directly exposed to the oxidising gas and the interface reaction controls the rate. The growth rate is constant (independent of scale thickness) and the degradation is continuous and destructive:
Linear rate law:
d(Δm)/dt = k_l (constant) → Δm = k_l · t
Conditions producing linear kinetics:
(a) Porous scale: FeO (wüstite) above 570°C — pores allow rapid gas access
(b) Volatile oxide: MoO₃ (bp 795°C) — oxide evaporates as fast as it forms
(c) Liquid oxide: V₂O₅ (mp 675°C), liquid at service temperature → runs off
(d) Mechanically unstable: scale with PBR >> 2 spalls continuously
(e) Very thin non-adherent scale: no barrier to diffusion
Examples of linear oxidation rate constants at 700°C:
Fe (wüstite layer regime): k_l ≈ 0.5 mg/cm²·h
Mo (volatile MoO₃): k_l ≈ 2.0 mg/cm²·h (accelerates with temp)
W (volatile WO₃ at >750°C): k_l ≈ rapid and catastrophic
Nb (loose Nb₂O₅): k_l ≈ 0.8 mg/cm²·h
Engineering consequence: LINEAR oxidation means unlimited metal loss.
A steel component corroding at 0.5 mg/cm²·h at 700°C consumes:
~0.3 mm of section thickness per 1000 hours of operation.
This is why unprotected carbon steel cannot be used above ~570°C.
The Pilling-Bedworth Ratio
The Pilling-Bedworth (PB) ratio, introduced by N.B. Pilling and R.E. Bedworth in 1923, provides a first-order criterion for whether an oxide scale will be protective by comparing the volume of oxide produced with the volume of metal consumed in its formation.
Pilling-Bedworth Ratio definition:
PBR = (Molar volume of oxide) / (n × Molar volume of metal consumed)
= (M_ox / ρ_ox) / (n × M_M / ρ_M)
= (M_ox × ρ_M) / (n × M_M × ρ_ox)
M_ox = molar mass of oxide (g/mol)
M_M = atomic mass of metal (g/mol)
ρ_ox = density of oxide (g/cm³)
ρ_M = density of metal (g/cm³)
n = number of metal atoms per oxide formula unit
Worked example — Aluminium / Al₂O₃:
M_ox = 101.96 g/mol; ρ_ox = 3.99 g/cm³ (corundum)
M_M = 26.98 g/mol; ρ_M = 2.70 g/cm³
n = 2 (two Al atoms per Al₂O₃ formula unit)
PBR = (101.96 × 2.70) / (2 × 26.98 × 3.99) = 275.3 / 215.4 = 1.28 ✓ protective
Interpretation:
PBR < 1: Oxide volume < metal volume consumed → porous scale → non-protective
Examples: MgO (0.81), Li₂O (0.59), Na₂O (0.57)
PBR 1–2: Oxide in compressive stress → continuous, adherent scale → protective
Examples: Al₂O₃ (1.28), NiO (1.65), Cr₂O₃ (2.07, borderline)
PBR > 2: Excessive compressive growth stress → buckling, cracking, spallation
Examples: WO₃ (3.35), Nb₂O₅ (2.68), VO₂ (3.19)
PBR for iron oxide system (three layers at > 570°C):
FeO: PBR = (71.85 × 7.87) / (1 × 55.85 × 5.74) = 1.77 (porous despite PBR!)
Fe₃O₄: PBR = (231.5 × 7.87) / (3 × 55.85 × 5.16) = 2.10
Fe₂O₃: PBR = (159.7 × 7.87) / (2 × 55.85 × 5.24) = 2.14
→ Iron scale is destructive NOT because of PBR but because FeO is porous
(stoichiometric defects: excess Fe vacancies make FeO a leaky lattice)
Wagner Theory of Ionic Transport Through Oxide Scales
While the Pilling-Bedworth ratio is a useful first estimate, the quantitative prediction of oxidation rate requires a theory of ionic transport through the scale. Carl Wagner (1933) provided this by treating the growing oxide as a solid electrolyte and applying the Nernst-Planck equation for ionic flux under combined concentration and electrical potential gradients.
Defect Chemistry and Point Defects in Oxides
The ionic transport rate through an oxide depends critically on its defect chemistry — specifically on the concentration and mobility of the point defects (vacancies, interstitials) that are the carriers of ionic flux. Two major oxide types exist:
Oxide defect types (Kröger-Vink notation):
p-TYPE oxides (metal-deficient; metal vacancies dominant):
Example: NiO, Cr₂O₃, FeO, CoO
Defect reaction: Ni(s) + ½O₂(g) → Ni_Ni + V''_Ni + O_O
(cation vacancy V''_Ni forms; acceptor)
In p-type oxides:
· Cation vacancies are majority defects
· Cations diffuse OUTWARD (from metal to oxide surface) via vacancy hopping
· Scale grows at the oxide-gas interface (new oxide forms at outer surface)
· Increasing pO₂ → more vacancies → faster oxidation
· Doping with higher-valent cations (e.g., Cr³⁺ in NiO) reduces V''_Ni
→ REDUCES k_p → basis for chromium alloying in nickel
n-TYPE oxides (oxygen-deficient; oxygen vacancies or interstitial cations):
Example: ZnO, TiO₂ (low pO₂), Al₂O₃ (debated; likely mixed)
Defect reaction: O_O → ½O₂(g) + V··_O + 2e'
(oxygen vacancy V··_O forms; donor)
In n-type oxides:
· Anion vacancies or interstitial cations are dominant
· Oxygen diffuses INWARD (via vacancy hopping)
· Scale grows at the metal-oxide interface
· Reducing pO₂ → more oxygen vacancies → faster oxidation (opposite to p-type!)
· Doping with lower-valent cations increases V··_O → increases oxidation rate
Wagner's parabolic rate constant:
k_p = (RT / F²) × ∫[μ'_O₂ to μ''_O₂] (σ_M · σ_e) / (σ_M + σ_e) d(μ_O₂)
σ_M = ionic (metal cation or oxide anion) conductivity
σ_e = electronic conductivity
Integration from metal-oxide interface (low μ_O₂) to oxide-gas interface (high μ_O₂)
For most engineering oxides, σ_e >> σ_M (good electronic conductors):
k_p ≈ (RT/F²) × ∫ σ_M d(μ_O₂)
This shows: k_p ∝ concentration of mobile ionic species (defects)
→ Doping to REDUCE defect concentration → REDUCES k_p → design principle
Selective Oxidation — Thermodynamics of Protective Scale Formation
When a binary or multicomponent alloy is oxidised, not all constituent elements oxidise at the same rate. The element with the most negative standard free energy of oxide formation — the most thermodynamically stable oxide — tends to oxidise preferentially, depleting the alloy surface in that element and building up a concentration gradient that drives further diffusion to the surface. This selective oxidation process is the thermodynamic basis for designing corrosion-resistant alloys.
Richardson-Ellingham Diagram
Ellingham diagram: ΔG° vs T for oxide formation reactions (per mole O₂):
More negative ΔG° at a given T → oxide is more stable → forms preferentially
Selected values at 1000°C (1273 K) in kJ/mol O₂:
SiO₂: ΔG° ≈ −670 kJ/mol O₂ (most stable practical oxide)
Al₂O₃: ΔG° ≈ −840 kJ/mol O₂ (extremely stable; thermodynamically favoured)
Cr₂O₃: ΔG° ≈ −630 kJ/mol O₂ (stable; selective oxidation above 15% Cr)
FeO: ΔG° ≈ −400 kJ/mol O₂
NiO: ΔG° ≈ −350 kJ/mol O₂
CoO: ΔG° ≈ −370 kJ/mol O₂
WO₃: ΔG° ≈ −450 kJ/mol O₂ (moderately stable but volatile above 800°C)
MoO₃: ΔG° ≈ −440 kJ/mol O₂ (volatile; MoO₃ sublimes at 795°C)
Selective oxidation condition (binary A-B alloy where oxide B_xO is more stable):
For selective formation of B_xO that covers the alloy surface:
The activity of B at the alloy surface must be sufficient to maintain the
equilibrium oxygen partial pressure at the metal-oxide interface:
pO₂,int = exp(ΔG°_B_xO / RT) / a_B^x
If pO₂,int < pO₂,bulk → B oxidises selectively
If B diffusion in the alloy cannot supply the surface fast enough →
internal oxidation of B (precipitates within the alloy rather than continuous surface scale)
Critical aluminium content for external Al₂O₃ scale formation:
In Ni-Al alloys (diffusion coefficient D_Al in Ni ≈ 3×10⁻¹⁴ m²/s at 1000°C):
N*_Al ≈ √(π·N_O · D_O / (3·D_Al)) ≈ 4–7 at% Al for external scale
→ MCrAlY bond coats require 10–12% Al to ensure reliable α-Al₂O₃ formation
Reactive Element Effect — How Y, Ce, Hf Improve Scale Adhesion
The reactive element effect (REE) is one of the most practically important phenomena in high-temperature oxidation. Small additions of reactive elements (RE) — yttrium (Y, typically 0.1–0.3 wt%), cerium (Ce), hafnium (Hf), lanthanum (La), or zirconium (Zr) at 0.01–0.1 wt% — dramatically improve the oxidation resistance of chromia-forming and alumina-forming alloys and coatings.
Mechanisms of the REE
Multiple mechanisms operate simultaneously:
- Grain boundary segregation: RE atoms have large ionic radii and low solubility in the oxide lattice. They segregate to oxide grain boundaries during scale growth, where they block the outward diffusion of metal cations. This switches the dominant transport mechanism from outward cation diffusion (which leaves Kirkendall voids at the metal-oxide interface) to inward oxygen anion diffusion (which grows scale at the metal-oxide interface with good contact). The switch produces a scale that remains adherent rather than lifting off on the support of growing oxide grains.
- Reduction of interfacial void formation: Conventional Al2O3-forming alloys develop voids at the metal-oxide interface because the outward flux of Al3+ is not compensated by an inward flux of material — a vacancy condensation (Kirkendall effect). RE additions suppress cation outflux, reducing vacancy supersaturation and void formation.
- Oxide pegging and chemical bonding: RE oxide nodules (Y2O3, HfO2) nucleate at alloy grain boundaries and grow into the scale as oxide pegs, mechanically anchoring the scale to the metal. Additionally, RE-O bonds are thermodynamically more stable than Al-O bonds, helping maintain interfacial integrity during thermal cycling.
Quantitative effect of Y on Al₂O₃ growth rate:
k_p (FeCrAl, no RE) at 1000°C: ~1 × 10⁻¹⁶ g²/cm⁴·s
k_p (FeCrAl + 0.1%Y) at 1000°C: ~2 × 10⁻¹⁷ g²/cm⁴·s (5× reduction)
k_p (MCrAlY, optimised) at 1000°C: ~3–8 × 10⁻¹⁸ g²/cm⁴·s (10–30× reduction)
Practical consequence at 1000°C over 10,000 hours:
Without RE: Δm ≈ √(1×10⁻¹⁶ × 3.6×10⁷) = 0.60 mg/cm² → TGO ~0.32 µm
With 0.1%Y: Δm ≈ √(3×10⁻¹⁷ × 3.6×10⁷) = 0.10 mg/cm² → TGO ~0.053 µm
The Y-containing alloy reaches the critical TGO thickness (5–8 µm)
approximately 10–30× more slowly → component life extended by same factor
Optimal RE concentration:
Too little (<0.02 wt% Y): insufficient grain boundary saturation — limited benefit
Optimal (0.05–0.2 wt% Y): maximum benefit; fine, adherent scale
Too much (>0.5 wt% Y): Y₂O₃ particles form continuous phase → embrittlement;
"overdoping" can INCREASE oxidation rate (fast diffusion
through Y-rich grain boundary phase)
Chromia-Forming and Alumina-Forming Alloy Systems
Chromia-Forming Alloys — Mechanism and Limits
Adding 15–25 wt% Cr to iron or nickel base alloys causes selective oxidation of chromium in preference to the base metal, establishing a continuous Cr2O3 scale at the alloy surface. The thermodynamic driving force is the more negative Gibbs free energy of Cr2O3 formation (ΔG° ≈ −630 kJ/mol O2 at 1000 °C) compared to FeO (−400) or NiO (−350). The parabolic rate constant for Cr2O3 at 900 °C is approximately 10−14 g²/cm&sup4;·s, reducing iron’s oxidation rate by approximately 10,000×.
The practical temperature ceiling for chromia-forming alloys is approximately 1050 °C in air. Above this temperature, Cr2O3 reacts further with oxygen to form volatile CrO3:
Chromia volatility above 1050°C:
2Cr₂O₃(s) + 3O₂(g) → 4CrO₃(g) ΔG° becomes negative above ~1060°C at 0.21 bar O₂
K_eq = pCrO₃^4 / (pO₂^3) → increases sharply with temperature
CrO₃ vapour pressure at pO₂ = 0.21 bar:
At 900°C: p(CrO₃) ≈ 10⁻⁶ bar → negligible loss
At 1050°C: p(CrO₃) ≈ 10⁻⁴ bar → begins to matter in flowing gas
At 1200°C: p(CrO₃) ≈ 10⁻² bar → catastrophic volatility; linear kinetics
Consequence: all gas turbine hot-section components (>1050°C) must use
alumina-forming alloys or MCrAlY coatings — NOT chromia formers.
Chromia formers (310SS, Alloy 600, Hastelloy X) are limited to
furnace hardware, boiler superheater tubes, and exhaust systems
operating below 1050°C.
Wet oxidation (steam environments):
CrOOH(g) = H₂O + CrO₂ → effective Cr loss accelerated in high steam atmospheres
This is why 9Cr creep-resistant steels require protection by thin Al₂O₃-forming
overlay coatings in advanced ultra-supercritical (A-USC) steam turbines above 700°C.
Alumina-Forming Alloys — Why Al2O3 Is Superior
| Property | Cr2O3 | α-Al2O3 | SiO2 |
|---|---|---|---|
| kp at 1000 °C (g²/cm&sup4;·s) | ~10−14 | ~10−16 | ~10−15 |
| ΔG° of formation at 1000 °C (kJ/mol O2) | −630 | −840 | −670 |
| Maximum useful temperature in air | ~1050 °C (CrO3 volatility) | ~1350 °C (α-Al2O3 stable) | ~1650 °C (cristobalite) |
| Required alloy content for external scale | 15–20 wt% Cr | 4–10 wt% Al (+ Cr or RE to assist) | 8–15 wt% Si |
| Scale stability in SO2/H2S (sulfidising) | Poor (Cr2S3 forms) | Good (α-Al2O3 not sulfidised readily) | Good |
| Scale stability in water vapour | Volatile CrOOH in steam above ~700 °C | Stable in water vapour to 1300 °C | Stable but slow volatility of Si(OH)4 |
| Mechanical properties (embrittlement risk) | Cr addition reduces toughness slightly | Al addition must be balanced with γ′ forming elements; too much Al embrittles | Si above ~5 wt% embrittles most alloys significantly |
| Key alloy systems | 304SS, 310SS, Alloy 600, Hastelloy X | FeCrAl (Kanthal), MCrAlY, NiAl, bond coats | Si-Mo cast iron, refractory SiC-based ceramics |
Hot Corrosion — Salt-Induced Accelerated Oxidation
Hot corrosion is a form of high-temperature degradation fundamentally different from normal oxidation: it involves dissolution of the protective oxide scale by a molten salt deposit rather than its growth by ionic diffusion. Hot corrosion is the primary life-limiting mechanism for gas turbine hot-section components in industrial and marine environments where sodium chloride (from sea air) or sulfur-containing fuels produce sodium sulphate deposits.
Type I Hot Corrosion (850–950 °C)
Type I hot corrosion (Na₂SO₄-induced, ~900°C):
Source of deposit:
NaCl (sea salt, airborne) + SO₃ (from fuel combustion) → Na₂SO₄ (mp 884°C)
At component surface ~900°C: Na₂SO₄ is LIQUID → forms continuous melt film
Two-stage mechanism:
Stage 1 — Initiation:
Na₂SO₄ melt contacts protective Cr₂O₃ or Al₂O₃ scale
Basic fluxing: Cr₂O₃ + Na₂SO₄ → Na₂CrO₄ + SO₃ (gas)
Al₂O₃ + Na₂SO₄ → NaAlO₂ + SO₃
The protective oxide dissolves into the melt as chromate/aluminate ions
→ scale is destroyed; metal surface re-exposed
Stage 2 — Propagation (autocatalytic):
CrO₄²⁻ in the Na₂SO₄ melt migrates outward → precipitates as Cr₂O₃ at melt surface
S²⁻ released inward → reacts with metal → sulfide layer at metal surface
Metal sulfides oxidise at the sulfide-melt interface → regenerate SO₃
SO₃ dissolves back into melt → self-sustaining cycle
Kinetics:
Initiation period: 10–100 hours (depends on salt flux rate, temperature)
Propagation: CATASTROPHICALLY FAST — similar to linear kinetics
Component life reduced from thousands of hours to tens of hours
Critical threshold:
Salt deposition rate > ~0.1 µg/cm²·h → Type I initiates
Temperature must be above Na₂SO₄ melting point (884°C) and below ~1000°C
(above 1000°C: Na₂SO₄ vapour pressure too high for stable melt deposit)
Affected alloys (in order of decreasing Type I susceptibility):
Highly susceptible: Co-base alloys (Stellite, MAR-M509)
Moderately susceptible: Ni-base alloys without MCrAlY coating (IN738, IN792)
Resistant: alloys with >35% Cr (but Cr level incompatible with high strength)
Best resistance: MCrAlY coatings (Al₂O₃ scale resists basic fluxing better than Cr₂O₃)
Type II Hot Corrosion (650–750 °C)
Type II hot corrosion occurs at temperatures well below the Na2SO4 melting point where a deposit of pure sodium sulphate would be solid. It is triggered by the formation of low-melting eutectic mixtures of Na2SO4 with metal sulphates produced at the component surface:
Type II hot corrosion (mixed sulphate eutectic, 650–750°C):
At 650–750°C, pure Na₂SO₄ is solid (mp 884°C) → no liquid deposit → no Type I
However: SO₃ from combustion gas reacts with Ni and Co in the alloy:
Ni + SO₃ → NiSO₄ (mp 848°C — solid alone)
Co + SO₃ → CoSO₄ (mp 735°C — solid alone)
Eutectic formation:
Na₂SO₄ – NiSO₄ eutectic: mp = 671°C → LIQUID at 700°C service temperature!
Na₂SO₄ – CoSO₄ eutectic: mp = 565°C → liquid even at cooler components
Type II mechanism:
· High-SO₃ partial pressure environment required (pSO₃ > 10⁻³ bar)
· Mixed eutectic salt melt dissolves protective Cr₂O₃ by acidic fluxing:
Cr₂O₃ + 3SO₃ → 2CrO·SO₄ (chromyl sulphate — highly corrosive)
· Pitting morphology characteristic of Type II: discrete pits rather than
uniform attack (unlike Type I which is more uniform)
Affected components:
· Low-pressure turbine blades (cooler than HPT blades → Type II temperature range)
· Industrial gas turbines burning heavy fuel oil (high SO₃ content)
· Marine turbines in high-NaCl environments
Prevention:
· Fuel desulphurisation (reduce SO₃ partial pressure)
· MCrAlY coatings (Al₂O₃ scale is more resistant to acidic than basic fluxing)
· Platinum-aluminide coatings (Pt modifies Al activity; better salt resistance)
· High-Co content alloys are MORE susceptible to Type II (CoSO₄ eutectic)
Sulfidation in Mixed Oxidising-Sulfidising Atmospheres
Many industrial environments — coal combustion, petroleum refining, chemical reactors, biomass gasification — contain both oxygen and sulphur-containing gases (H2S, SO2, COS). In these mixed atmospheres, competitive formation of oxides and sulphides occurs, and in certain pO2-pS2 conditions, catastrophically fast corrosion results. The Cr2S3 and FeS phases that form in sulfidising conditions are far more defective and ion-conducting than their oxide counterparts, and many sulphide-oxide or sulphide-metal eutectic systems melt at temperatures well below service conditions, producing liquid at the metal surface that completely destroys corrosion protection.
Sulfidation kinetics comparison at 700°C:
Parabolic rate constant k_p for sulphide formation:
FeS on iron: k_p ≈ 10⁻⁸ g²/cm⁴·s (10⁶× faster than Cr₂O₃ oxidation!)
Ni₃S₂ on Ni: k_p ≈ 10⁻⁷ g²/cm⁴·s (catastrophic)
Cr₂S₃ on Cr: k_p ≈ 10⁻¹² g²/cm⁴·s (still 100× faster than Cr₂O₃ oxidation)
Critical eutectic melting points:
Ni – Ni₃S₂: 637°C → liquid in many refinery service conditions!
Fe – FeS: 988°C → liquid in furnace environments
Co – Co₄S₃: 880°C → liquid in hot turbine hot corrosion + sulfidation
Stability diagram (log pS₂ vs log pO₂) at 700°C:
Region A (high pO₂, low pS₂): protective oxide stable
Region B (low pO₂, high pS₂): sulphide stable → catastrophic attack
Region C (intermediate): mixed oxide + sulphide → complex behaviour
Alloy selection for mixed environments:
Best resistance: alloys with high Cr (>25%) + high Si (>1.5%)
FeCrAl alloys: Al₂O₃ more resistant to sulfidation than Cr₂O₃
Ni-base superalloys: avoid — Ni₃S₂ eutectic is too low
Cobalt alloys: moderate — Co₄S₃ eutectic higher than Ni₃S₂
Ferritic 310 stainless (25Cr-20Ni): reasonable in refinery service to 650°C
Interference Colours on Steel — The Thermal Tint Scale
The familiar blue-gold-purple colours that appear on heated stainless steel and titanium welds are thin-film interference colours produced when white light reflects from both the outer surface of the transparent oxide film and the metal surface beneath. The phase difference between the two reflected beams depends on film thickness and produces constructive interference at specific wavelengths. The colour changes predictably with oxide thickness and therefore with peak temperature, making it a useful qualitative temperature indicator:
~250–290 °C
~30–40 nm oxide
~290–340 °C
~50–70 nm
~340–370 °C
~70–90 nm
~370–400 °C
~90–110 nm
~400–440 °C
~110–140 nm
~440–480 °C
~140–180 nm
>480 °C
Scale too thick
Colours on carbon and stainless steel at tempering temperatures. Titanium shows similar colours but shifted: silver = excellent (EBW vacuum condition), pale gold = acceptable (<450 °C), blue = reject (>550 °C, O2 contamination).