Oxidation and Hot Corrosion

Comprehensive Educational Resource for High-Temperature Metal Degradation

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Reactions of Metals in Mixed Environments

Real-world high-temperature environments rarely consist of pure oxygen. Instead, metals and alloys are typically exposed to complex gas mixtures containing various oxidizing and reducing species. These mixed environments can dramatically alter oxidation behavior, often leading to more severe degradation than would occur in pure oxygen. Understanding these complex interactions is crucial for predicting material performance in practical applications such as power generation, petrochemical processing, and aerospace systems.
1 Air–H₂O and Air–CO₂ Atmospheres
The presence of water vapor and carbon dioxide in oxidizing atmospheres significantly modifies the oxidation behavior of metals and alloys. These species act as additional oxidants and can establish redox equilibria that enhance oxygen transport through oxide scales.

Water Vapor Effects

Water vapor accelerates the oxidation of steels through several mechanisms:
Enhanced Oxygen Transport
Water vapor can dissociate to provide additional oxygen according to the equilibrium:
H₂O → H₂ + ½O₂ (ΔG° = 245,993 - 54.84T J/mol)
The H₂/H₂O redox couple can transport oxygen through pores and defects in oxide scales more effectively than molecular oxygen alone. This process involves the cyclic reduction and oxidation of water vapor:
  • At the gas-scale interface: H₂O + 2e⁻ → H₂ + O²⁻
  • At the scale-metal interface: H₂ → 2H⁺ + 2e⁻
  • Overall reaction with iron: Fe + H₂O → FeO + H₂
Scale Property Modifications
Water vapor affects the physical and mechanical properties of oxide scales:
  • Plasticity changes: Water vapor can increase the plasticity of some oxide scales, potentially reducing cracking
  • Adherence effects: Can either improve or worsen scale adherence depending on the specific system
  • Microstructural changes: Alters the porosity and grain structure of growing oxides
Chromia Volatilization
One of the most significant effects of water vapor is the promotion of chromia volatilization through the formation of volatile chromium oxyhydroxide:
Cr₂O₃ + 3H₂O + 3/2O₂ → 2CrO₂(OH)₂(g)
This reaction becomes significant at temperatures above ~1000°C and can lead to rapid loss of protective chromia scales, particularly in flowing gas environments where the volatile species are continuously removed.
Alumina Scale Effects
Water vapor can also affect alumina scales by:
  • Increasing spallation tendency due to enhanced growth stresses
  • Modifying the transport properties of the scale
  • Affecting the formation of metastable alumina phases

Carbon Dioxide Effects

Carbon dioxide can act as an oxidant and establish CO/CO₂ equilibria that affect both oxidation and carburization behavior:
CO₂ → CO + ½O₂ (ΔG° = 282,150 - 86.57T J/mol)
Oxidation Enhancement
Similar to water vapor, CO₂ can enhance oxidation through:
  • Direct reaction with metals: Fe + CO₂ → FeO + CO
  • Establishment of CO/CO₂ redox couples for oxygen transport
  • Modification of local oxygen activities within oxide scales
Carbon Activity and Carburization
CO–CO₂ atmospheres establish a carbon potential that can lead to carburization or decarburization of steels:
2CO ⇌ C + CO₂
The carbon activity is determined by the CO/CO₂ ratio and temperature. High carbon activities can lead to:
  • Internal carburization of alloys
  • Formation of metal carbides
  • Depletion of chromium through carbide formation
  • Reduced oxidation resistance due to chromium depletion
Figure 1.1: Schematic illustration showing the enhanced oxidation of steel in H₂O-containing atmospheres through the H₂/H₂O redox couple mechanism.
2 Metal–Sulfur–Oxygen Systems
Environments containing both sulfur and oxygen species present particularly complex challenges for high-temperature materials. These atmospheres can contain oxidizing species (SO₂, SO₃) or reducing species (H₂S, COS), leading to the formation of oxides, sulfides, or sulfates depending on the local thermodynamic conditions.

Thermodynamic Considerations

The stability of different phases in metal-sulfur-oxygen systems is governed by the relative partial pressures of oxygen and sulfur. Phase stability diagrams plotting log pO₂ versus log pS₂ are essential tools for predicting which phases will be stable under given conditions.
Key Equilibria
Several important equilibria govern the behavior of these systems:
½S₂ + O₂ ⇌ SO₂ (ΔG° = -361,700 + 76.68T J/mol)

M + ½O₂ ⇌ MO

M + ½S₂ ⇌ MS
Phase Stability Regions
Typical stability regions in order of increasing oxygen potential:
  • Metal stable: Very low pO₂ and pS₂
  • Sulfide stable: Low pO₂, moderate pS₂
  • Oxide stable: High pO₂, low to moderate pS₂
  • Sulfate stable: Very high pO₂ and pS₂

Duplex Scale Formation

A characteristic feature of metal-sulfur-oxygen systems is the formation of duplex scales consisting of interwoven oxide and sulfide phases. Common examples include:
  • Iron systems: FeO + FeS duplex scales
  • Nickel systems: NiO + Ni₃S₂ duplex scales
  • Cobalt systems: CoO + Co₉S₈ duplex scales
Formation Mechanisms
Duplex scales form through several mechanisms:
  • Simultaneous formation: Both oxide and sulfide phases nucleate and grow simultaneously
  • Sequential formation: One phase forms first, followed by the other due to changing local conditions
  • Decomposition reactions: Intermediate phases decompose to form duplex structures
Transport Properties
Duplex scales typically exhibit poor protective properties because:
  • The interwoven structure creates numerous defects and short-circuit diffusion paths
  • Sulfides generally have higher defect concentrations than oxides
  • Thermal expansion mismatches between phases create cracking
  • The scales are often porous and non-adherent

Sulfur Transport Mechanisms

Sulfur can penetrate oxide scales through two primary mechanisms:
Gas Permeation
SO₂ and other sulfur-containing gas species can transport through pores and cracks in oxide scales. This mechanism is particularly important in:
  • Porous or cracked oxide scales
  • Scales with high defect concentrations
  • Systems with significant thermal cycling
Chemical Diffusion
Sulfur can also diffuse through the crystal structure of oxide scales, though this is generally much slower than gas permeation. The rate depends on:
  • The defect structure of the specific oxide
  • Temperature and sulfur chemical potential
  • The presence of dopants or impurities
Figure 2.1: Phase stability diagram for a metal-sulfur-oxygen system showing the regions where different phases (metal, oxide, sulfide, sulfate) are thermodynamically stable as functions of oxygen and sulfur partial pressures.
3 Conditions for Sulfide Formation
The formation of metal sulfides in mixed oxidizing-sulfidizing environments depends on the local thermodynamic conditions, particularly the sulfur potential relative to the metal activity and temperature.

Thermodynamic Criterion

Sulfides form when the local sulfur potential exceeds the threshold for sulfide stability at the given metal activity. The general condition for sulfide formation is:
μS > μS°(MS) + RT ln(aM)
Where:
  • μS is the local sulfur chemical potential
  • μS°(MS) is the standard chemical potential for sulfide formation
  • aM is the activity of the metal
  • R is the gas constant and T is temperature

Sulfide Formation in SO₂-Containing Gases

In SO₂-containing atmospheres, the condition for sulfide formation can be expressed in terms of gas partial pressures:
pSO₂ > K(T) × pO₂^(1/2) × aM^(-1)
This relationship shows that sulfide formation is favored by:
  • High SO₂ partial pressures
  • Low oxygen partial pressures
  • High metal activities (i.e., at the metal-scale interface)
  • Higher temperatures (through the temperature dependence of K(T))

Nucleation and Growth Patterns

Preferential Nucleation Sites
Sulfides typically nucleate preferentially at:
  • Metal-scale interface: Where metal activity is highest
  • Grain boundaries: High-energy sites with enhanced diffusion
  • Scale defects: Cracks, pores, and other imperfections
  • Phase boundaries: Interfaces between different oxide phases
Growth Morphologies
Sulfide formation can produce various morphologies:
  • Discrete particles: Individual sulfide precipitates within the scale
  • Continuous layers: Sulfide films at specific locations
  • Interwoven structures: Sulfides intimately mixed with oxides
  • Internal precipitation: Sulfides formed within the metal substrate

Duplex Scale Development

The formation of duplex oxide-sulfide scales often follows a characteristic sequence:
  1. Initial oxide formation: Protective oxide scale forms initially
  2. Sulfur penetration: Sulfur species penetrate through scale defects
  3. Local sulfide nucleation: Sulfides form at the metal-scale interface
  4. Scale disruption: Sulfide formation disrupts the protective oxide
  5. Duplex structure: Continued growth produces interwoven oxide-sulfide structure
This process often becomes self-accelerating because the duplex structure provides easier pathways for continued sulfur penetration.
Critical Point: Once sulfide formation begins, it often becomes self-sustaining and can rapidly destroy the protective nature of oxide scales. This is why even small amounts of sulfur in high-temperature environments can have disproportionately large effects on material degradation rates.
4 Attack of Alloys in Complex Atmospheres
The behavior of alloys in complex atmospheres is significantly more complicated than that of pure metals. Alloys typically contain a base metal (A) and one or more alloying elements (B), with the alloying elements often chosen specifically to form protective oxide scales. However, complex atmospheres can penetrate and destabilize these protective scales through various mechanisms.

Protective Scale Formation and Breakdown

In simple oxidizing environments, protective alloys form scales according to reactions such as:
pB + ½O₂ → BpO (protective oxide formation)

qB + ½S₂ → BqS (sulfide formation - usually non-protective)
Competition Between Oxide and Sulfide Formation
The protective alloying element B (typically Cr or Al) can react with either oxygen or sulfur. The relative rates and thermodynamic driving forces determine which reaction dominates:
  • Sufficient B content + favorable conditions: Protective BpO scale forms
  • Insufficient B or unfavorable conditions: Non-protective BqS forms or internal attack occurs
  • Mixed conditions: Both phases may form, leading to duplex structures
Internal Attack Phenomena
When the alloying element B is insufficient to form a continuous protective scale, internal oxidation or sulfidation can occur:
  • Internal oxidation: Discrete oxide particles (BpO) precipitate within the alloy
  • Internal sulfidation: Discrete sulfide particles (BqS) precipitate within the alloy
  • Mixed internal attack: Both oxides and sulfides form internally

Specific Effects of Complex Atmosphere Components

Water Vapor Effects on Alloys
Water vapor affects alloy behavior through several mechanisms:
  • Chromium loss via volatilization: Accelerated loss of Cr through CrO₂(OH)₂ formation
  • Enhanced oxygen transport: Faster oxidation kinetics through H₂/H₂O couples
  • Scale adherence changes: Modified mechanical properties of protective scales
  • Selective attack: Preferential attack of certain alloy phases or grain boundaries
CO/CO₂ Effects on Alloys
Carbon-containing atmospheres create additional complications for alloy behavior:
  • Carburization: Carbon uptake leads to carbide formation, depleting Cr from solid solution
  • Chromium depletion: Cr₂₃C₆ and other carbides tie up protective chromium
  • Microstructural changes: Carbide precipitation alters alloy properties and diffusion paths
  • Scale-metal interface effects: Carbon can affect the adherence and growth of protective scales
  • Dual atmosphere effects: Simultaneous oxidation and carburization can create complex degradation patterns
SO₂/H₂S Effects on Alloys
Sulfur-containing species create some of the most severe challenges for protective alloys:
  • Sulfidation of protective elements: Cr₂S₃, Al₂S₃ formation depletes protective elements
  • Duplex scale formation: Mixed oxide-sulfide scales with poor protective properties
  • Internal sulfidation: Sulfide precipitation within the alloy substrate
  • Cr₂O₃ breakdown: Even established chromia scales can be attacked by sulfur
  • Al₂O₃ degradation: Alumina scales, while more resistant, can also be compromised
Chlorine/HCl Effects on Alloys
Chlorine-containing species create unique attack mechanisms:
  • Volatile chloride formation: CrCl₃, AlCl₃ formation leads to active oxidation cycles
  • Scale penetration: Cl₂ can penetrate oxide scales more easily than O₂
  • Pitting and localized attack: Chlorides often cause localized rather than uniform attack
  • Synergistic effects: Chlorine enhances the effects of other aggressive species

Critical Concentration Effects

The concentration of protective alloying elements determines the mode of attack in complex atmospheres:
Above Critical Concentration
When the protective element concentration exceeds the critical value:
  • Continuous protective scale can form initially
  • However, complex atmosphere components can still penetrate over time
  • Gradual degradation occurs through scale breakdown mechanisms
  • Eventually, the protective element may be depleted locally
Below Critical Concentration
When the protective element concentration is insufficient:
  • Internal oxidation/sulfidation occurs from the beginning
  • No continuous protective scale forms
  • Rapid degradation through internal attack mechanisms
  • Base metal oxidation dominates the overall kinetics
Alloy System Protective Element Critical Concentration (wt%) Complex Atmosphere Sensitivity
Fe-Cr Chromium 12-15 High (especially to S, Cl)
Ni-Cr Chromium 15-20 Moderate to High
Fe-Al Aluminum 4-6 Low to Moderate
Ni-Al Aluminum 3-5 Low
Co-Cr Chromium 20-25 High
5 Practical Observations and Case Studies
Real-world experience with high-temperature alloys in complex atmospheres has revealed several important practical considerations that complement the fundamental understanding of these systems.

Limitations of Pre-oxidation

Pre-oxidation treatments, where alloys are deliberately oxidized in clean environments to establish protective scales before service, have limited effectiveness in complex atmospheres:
Why Pre-oxidation Fails
  • Scale permeability: Even the best pre-formed scales have defects that allow penetration
  • Thermal cycling damage: Service conditions often involve thermal cycling that cracks pre-formed scales
  • Chemical breakdown: Aggressive species can chemically attack even well-formed protective scales
  • Scale evolution: Scales continue to evolve during service, often losing their protective character
Temporary Protection
While pre-oxidation may not provide long-term protection, it can:
  • Extend the incubation period before rapid attack begins
  • Provide some protection during startup and shutdown cycles
  • Reduce the initial rate of attack in mildly aggressive environments

Semi-protective Sulfide Scales

In some rare cases, sulfide scales can exhibit semi-protective behavior, though this is exceptional rather than typical:
FeCr₂S₄ Scales in Syngas Environments
Fe-Ni-Cr alloys in certain syngas (synthesis gas) environments can form FeCr₂S₄ spinel sulfide scales that show:
  • Lower transport rates than typical sulfide scales
  • Better adherence than most sulfide scales
  • Some degree of self-healing capability
  • However, still much less protective than good oxide scales
Conditions for Semi-protective Behavior
Semi-protective sulfide behavior requires very specific conditions:
  • Precise control of pO₂/pS₂ ratios
  • Specific alloy compositions
  • Stable temperature and gas composition
  • Absence of thermal cycling

Industrial Case Studies

Power Generation Environments
Coal-fired power plants:
  • Complex atmospheres containing SO₂, H₂O, CO₂, and ash deposits
  • Superheater tubes experience both gas-side and deposit-induced corrosion
  • Chromia-forming alloys show limited lifetimes due to chromium volatilization
  • Alumina-forming alloys perform better but are more expensive
Petrochemical Processing
Hydroprocessing environments:
  • High-pressure H₂S/H₂ atmospheres with trace contaminants
  • Sulfidation is the dominant degradation mechanism
  • Even small amounts of oxygen can dramatically change behavior
  • Alloy selection requires careful consideration of all trace species
Gas Turbine Engines
Marine and industrial gas turbines:
  • Salt-laden air creates complex Cl/S/O atmospheres
  • Hot corrosion becomes the life-limiting factor
  • Coatings are essential for acceptable component lifetimes
  • Regular washing is required to remove salt deposits
Waste Incineration
Municipal waste incinerators:
  • Extremely complex atmospheres with Cl, S, Pb, Zn, and other species
  • Rapid degradation of conventional high-temperature alloys
  • Specialized alloys and coatings required
  • Frequent maintenance and component replacement necessary

Long-term Degradation Patterns

Long-term exposure to complex atmospheres reveals several characteristic degradation patterns:
Incubation-Acceleration Pattern
Many systems show a characteristic two-stage behavior:
  1. Incubation period: Slow attack while protective scales remain intact
  2. Acceleration period: Rapid attack once protective scales break down
The duration of the incubation period depends on:
  • Alloy composition and microstructure
  • Severity of the complex atmosphere
  • Temperature and thermal cycling
  • Mechanical stresses and vibration
Localized vs. General Attack
Complex atmospheres often produce localized rather than uniform attack:
  • Pitting: Deep, localized penetration
  • Intergranular attack: Preferential attack along grain boundaries
  • Selective phase attack: Preferential attack of specific microstructural features
  • Crevice corrosion: Enhanced attack in confined geometries
Key Engineering Insight: The transition from protective to non-protective behavior in complex atmospheres is often sudden and catastrophic. This makes it essential to design for the post-breakdown condition rather than relying on the maintenance of protective scales throughout the component lifetime.

Design and Mitigation Strategies

Understanding the mechanisms of attack in complex atmospheres enables the development of effective strategies for material selection, system design, and operational procedures to minimize degradation.

Material Selection Principles

Hierarchy of Resistance
For complex atmosphere applications, materials can be ranked in approximate order of resistance:
  1. Alumina-forming alloys: Best overall resistance to complex atmospheres
  2. High-chromium alloys (>25% Cr): Good resistance with proper design
  3. Coated systems: Can provide excellent protection if properly maintained
  4. Standard chromia-forming alloys: Limited resistance in severe environments
  5. Low-alloy steels: Suitable only for mild conditions or with coatings
Composition Optimization
Key compositional strategies include:
  • Maximize protective element content: Higher Cr or Al levels provide better resistance
  • Add reactive elements: Y, Hf, Zr improve scale adherence and properties
  • Minimize detrimental elements: Reduce Mo, W, V content where possible
  • Control minor elements: Manage S, P, and other impurities

Protective Coatings

Coating Types and Applications
  • Diffusion aluminide coatings: Form protective Al₂O₃ scales
  • MCrAlY overlay coatings: Provide both oxidation and hot corrosion resistance
  • Thermal barrier coatings: Reduce substrate temperature and provide some chemical protection
  • Slurry coatings: Cost-effective protection for less critical applications

System Design Considerations

  • Temperature management: Minimize peak temperatures where possible
  • Atmosphere control: Remove or neutralize aggressive species when feasible
  • Thermal cycling minimization: Reduce startup/shutdown frequency
  • Maintenance accessibility: Design for inspection and coating renewal

Summary and Conclusions

The behavior of metals and alloys in mixed high-temperature environments is significantly more complex and generally more severe than in simple oxidizing atmospheres. The presence of water vapor, carbon dioxide, sulfur species, and chlorine can dramatically alter oxidation mechanisms and accelerate material degradation through various synergistic effects.

Critical Factors

  • Thermodynamic complexity: Multiple competing reactions and phase equilibria
  • Transport enhancement: Additional pathways for aggressive species to reach the metal
  • Scale destabilization: Breakdown of normally protective oxide scales
  • Synergistic effects: Combined effects often exceed the sum of individual contributions
  • Time-dependent evolution: Changing conditions and degradation patterns over time

Design Recommendations

  • Higher alloy contents: Increased levels of protective elements to account for enhanced consumption
  • Alternative protection strategies: Coatings, environmental control, or alternative materials
  • Comprehensive testing: Laboratory testing in simulated service atmospheres
  • Conservative safety factors: Account for the accelerating nature of degradation
  • Monitoring systems: Early detection of protective scale breakdown
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