Electrochemistry

Corrosion (Rust)

Iron isn't decaying — it's running a tiny battery

Corrosion is the electrochemical destruction of metal. Iron oxidizes at an anodic site, oxygen reduces at a cathodic site, and the two half-reactions short through the metal itself, with a film of water as the electrolyte. Marine carbon steel loses about 0.1 mm/year; the Golden Gate Bridge is repainted continuously.

  • E°(Fe²⁺/Fe)−0.44 V
  • E°(O₂/H₂O, neutral pH)+0.81 V
  • Rust formulaFe₂O₃·xH₂O
  • Marine steel rate~0.1 mm/yr
  • Arid air rate~0.005 mm/yr
  • US corrosion cost (NACE 2016)$276 B/yr

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How rust really happens

The textbook reaction "iron + oxygen = rust" hides the actual mechanism. Rust is not a direct combination. It's a galvanic cell that lives on every wet iron surface. The cell has four parts running at the same time:

Anode (small patch):     Fe → Fe²⁺ + 2 e⁻              E° = −0.44 V
Cathode (nearby patch):  ½ O₂ + H₂O + 2 e⁻ → 2 OH⁻    E° = +0.40 V (pH 7)
Electrons through:       the bulk metal itself
Ions through:            the water film on top
Net cell EMF:            ~+0.84 V — strongly spontaneous

Once Fe²⁺ ions diffuse outward and meet dissolved O₂, they oxidize again to Fe³⁺ and precipitate as a hydrated oxide:

2 Fe²⁺ + ½ O₂ + 2 H₂O  →  Fe₂O₃·H₂O + 4 H⁺
                          ─────────────
                         the orange flake

The whole thing is just electrochemistry running in parallel with no external wire. Anodes and cathodes can be millimetres apart on the same nail, separated by a microscopic geometry difference (a scratch, a stress concentration, or a drop of water sitting on a paint flaw).

Three things rust needs

Strip any one and corrosion stops:

  1. Iron (or another oxidizable metal). Pure metal in its zero oxidation state is the fuel.
  2. Oxygen. The cathodic reaction needs an oxidant. Buried steel below the water table corrodes much slower because O₂ runs out.
  3. Water. Acts as the electrolyte. Bone-dry iron in a desert vault basically doesn't rust — see ancient artifacts at Luxor.

Add a fourth optional accelerant — chloride ions — and rates jump tenfold. Sea spray, road salt, and coastal humidity all push the curve up. The Pourbaix diagram (potential vs pH) tells you the same story: iron is thermodynamically immune in alkaline anoxic water and aggressively unstable in chloride-rich neutral water.

Forms of corrosion compared

UniformPittingGalvanicCreviceStress-corrosion crackingErosion
GeometryWhole surface, even rateTiny deep holesAt the metal-metal junctionInside narrow gaps and sealsCrack propagation under tensionWhere flow erodes passive film
TriggerGeneral exposureCl⁻ breaks passive film locallyTwo metals in contact + electrolyteO₂ depletion in stagnant pocketTensile stress + corrosive speciesTurbulent fluid scrubs oxide
DetectabilityVery visibleEasy to miss until perforationVisible at junctionHidden under bolts and gasketsOften catastrophic with no warningVisible scoured tracks
RatePredictable, ~mm/yearµm/day local — pit grows in daysFaster than either metal aloneSlow but persistentCrack growth ~mm/hr near failureMaterial-loss like sandblasting
Famous caseSteel ship hullStainless in seawater chlorideStatue of Liberty Cu/Fe armatureAircraft lap joint, Aloha 243Boiler-tube SCC, brass "season cracking"Pump impellers, condenser tubes
Counter-measureCoating, sacrificial anodeMo-alloyed stainless, lower Cl⁻Insulation, similar metalsSeal design, drain pathsStress relief, change alloyLower velocity, harder facing

In practice, real failures combine modes. The Aloha 737 fuselage rip-out in 1988 was crevice corrosion that primed a fatigue crack — pure SCC in a salt-air environment that normal NDT had missed.

Worked example: marine vs urban exposure

ISO 9223 classifies atmospheres by how fast they eat carbon steel:

  • C1 (controlled indoor): < 1.3 µm/year. A bank vault.
  • C2 (rural arid): 1.3–25 µm/year. Sahara, high desert.
  • C3 (urban, low-humidity): 25–50 µm/year. Madrid, Denver.
  • C4 (industrial or coastal): 50–80 µm/year. Pittsburgh in 1960; Lisbon today.
  • C5 (severe coastal/industrial): 80–200 µm/year. Aberdeen, Mumbai monsoon shore.
  • CX (offshore / splash zone): 200–700 µm/year. North Sea oil-platform splash zones.

So a 6 mm steel plate left unpainted at the splash zone of an offshore rig perforates in roughly 6000 / 500 = 12 years. The same plate inside a heated office is still useful in 4000 years — barring scratches.

Prevention strategies

  • Barrier coatings. Paint, epoxy, polymer wrap. The cheapest line of defense, but breaks down at edges and pinholes — every car body has them.
  • Galvanizing. Hot-dip the steel in molten zinc. Zinc is anodic to iron (E° = −0.76 V), so even at a scratch the zinc oxidizes preferentially and protects the bare iron underneath. Standard galvanized steel: 50–80 µm Zn, ~50-year life in C3.
  • Sacrificial anodes. Bolt slabs of zinc, magnesium, or aluminum to the protected structure. Ship hulls carry 50–100 kg of zinc per metre of waterline. Replaced every 1–3 years.
  • Impressed-current cathodic protection (ICCP). A DC power supply pushes the structure to a more negative potential than its corrosion potential. Used on long pipelines, harbour piers, and even reinforced-concrete bridge decks.
  • Alloying. Stainless steel (≥10.5% Cr) forms a self-healing Cr₂O₃ passive layer 1–2 nm thick. 316L adds 2–3% Mo to resist chloride pitting.
  • Inhibitors. Add a chemical (chromate, phosphate, organic film-formers) that adsorbs onto the surface and slows the anodic or cathodic step. Engine coolants are inhibitor cocktails.
  • Environmental control. Lower humidity, deoxygenate (boilers run at <5 ppb O₂ via hydrazine), shift pH alkaline.

Real-world case studies

  • Golden Gate Bridge. Salt fog plus 100% humidity ate the original lead-and-linseed paint in 30 years. Since 1965, a permanent crew of ~30 painters has been continuously stripping and repainting with epoxy zinc primer + intermediate + topcoat ("International Orange"). They never finish — when they reach one end they start over at the other.
  • Statue of Liberty (1980s restoration). Galvanic corrosion between the copper skin and the iron armature behind it — the asbestos shellac insulation had failed. The iron was replaced with stainless 316L, with PTFE spacers between metals.
  • Trans-Alaska Pipeline. 800 miles of buried steel, protected by ~10 000 sacrificial Mg anodes plus impressed-current rectifier stations every 30 km. Wall loss after 45 years: under a millimetre on average.
  • Boston "Big Dig" rebar. Chloride ingress from de-icing salt drove pitting in unprotected reinforcing bar; epoxy-coated rebar and ICCP retrofits cost the project several hundred million extra.
  • Silver Bridge collapse, 1967. Stress-corrosion cracking in a single eyebar pin link. 46 dead. The disaster created the modern US bridge inspection program.
  • Sunken WWII battleships. Hulls below ~30 m and below the seabed lose only ~25 µm/year because dissolved O₂ runs out. This is why "low-background steel" — pre-1945 wreck plate — is salvaged for radiation-sensitive instruments.

Variants and edge cases

  • Microbiologically influenced corrosion (MIC). Sulfate-reducing bacteria in anaerobic biofilms generate H₂S that pits steel from underneath. Notorious in oilfield piping and ship ballast tanks.
  • Hydrogen embrittlement. Atomic H produced at the cathode diffuses into high-strength steel, accumulates at grain boundaries, and embrittles it. Bolts that crack months after installation are the classic case.
  • Filiform corrosion. Hairline rust threads creeping under paint, driven by humidity gradients. Cosmetic on cars, structurally serious on aluminum aircraft skins.
  • Cold-worked iron resists. Cold-rolling raises dislocation density and surface stress, but oddly it can shift corrosion potential to be slightly more noble in some media. Engineers don't trust this; it's a curiosity.
  • "Self-healing" rust on weathering steel. COR-TEN forms a tight, adherent rust patina (rich in Cr, Cu, P) that slows further attack. Used for sculpture and exposed-frame buildings; depends on alternating wet-dry to seal.

Common pitfalls and misconceptions

  • "Stainless can't rust." 304 stainless pits readily in seawater. The chromium oxide film breaks down where Cl⁻ ions concentrate; specify 316L or duplex steel for marine use.
  • "More paint is better." Thick, brittle coats crack first; thin elastic ones flex with the substrate. Modern coating systems specify dry-film thickness in tens of microns per layer, not millimetres.
  • "Galvanic series tells me everything." Position in the seawater galvanic series sets which metal becomes anodic, but rate depends on area ratio. A small steel rivet in a large copper plate corrodes catastrophically; reverse the ratio and the steel barely moves.
  • "Rust is purely chemical." It's electrochemical. Without electron and ion paths, the reaction stops. That's why a shielded patch of iron sealed under perfect lacquer in a vacuum doesn't rust.
  • "Sealing the surface is enough." If water gets in through any crack, the anode is now trapped under the coating with no oxygen — perfect crevice geometry. Coatings must drain, or flooding will accelerate, not stop, attack.

Frequently asked questions

Why does iron rust but gold doesn't?

It comes down to standard reduction potentials. Fe²⁺/Fe sits at −0.44 V, well below the H⁺/H₂O₂ and O₂/H₂O cathode reactions, so iron is thermodynamically unstable in moist air. Au³⁺/Au sits at +1.50 V, above almost every available oxidant — there's no driving force to oxidize gold under ordinary conditions.

Why is rust orange but the iron underneath is grey?

The reddish-brown colour comes from hydrated iron(III) oxide — Fe₂O₃·xH₂O — formed when Fe²⁺ ions diffuse outward and react with dissolved oxygen. Fresh metallic iron is grey because the Fermi-level electron sea reflects most visible light. The colour difference is a chemistry change at the surface, not a coating change.

Why doesn't aluminum rust the same way iron does?

Both metals oxidize, but aluminum's oxide is special. Al₂O₃ is dense, hard, sticks tightly to the surface, and forms a 2–4 nm passivation layer in seconds. Iron oxide is porous and flakes off, exposing fresh metal. So aluminum "rusts" once and stops; iron rusts forever.

What's the difference between rust and tarnish?

Rust is specifically iron(III) oxide-hydroxide. Tarnish is the analogous surface oxide or sulfide on other metals — Ag₂S on silver, Cu₂O/CuS on copper. The mechanism is the same (electrochemical oxidation), but tarnish layers are usually thin and self-limiting; rust grows indefinitely.

How does cathodic protection actually work?

You force the protected structure to be the cathode of a galvanic couple. Either bolt on a more reactive "sacrificial" anode (zinc, magnesium, or aluminum) that oxidizes in the steel's place, or supply external current from a power supply ("impressed current"). Pipelines, ship hulls, and bridge piers all use both.

Why is salt water so much harsher than fresh water?

Three reasons. Salt is an electrolyte — it raises the conductivity of the surface water film by ~10 000×, so anodic and cathodic sites can be far apart and still close the circuit. Chloride ions disrupt the passive oxide layer that protects iron in fresh water. And salt water holds more dissolved oxygen at the splash zone. Marine carbon steel loses ~0.1–0.2 mm/year vs ~0.005 mm/year in arid air.