Leave a steel nail in damp air and within days it turns crumbly and orange; a gold ring stays shiny for centuries. Why the difference? Iron is "eager" to give away its electrons, and oxygen is "eager" to grab them. All that's missing is something to carry charge between them — and a thin film of water does exactly that. The moment water connects the two, iron quietly builds a tiny battery on its own surface, and that battery slowly eats the metal.
A battery has two electrodes, and so does a corroding surface. At an anode the metal dissolves and leaves its electrons behind: $\mathrm{Fe \to Fe^{2+} + 2e^-}$. At a cathode dissolved oxygen mops those electrons up: $\mathrm{O_2 + 2H_2O + 4e^- \to 4OH^-}$. The electrons travel through the solid metal from anode to cathode, while ions drift through the water — a complete circuit, just like a real cell. The push that drives it is the cell voltage,
A positive voltage means the reaction runs all by itself — iron in moist air is thermodynamically doomed. How fast metal vanishes is set by the corrosion current. A handy rule of thumb for iron is that $1\ \mu\mathrm{A/cm^2}$ of corrosion current eats about $0.012$ mm of metal per year, so a typical seawater rate near $30\ \mu\mathrm{A/cm^2}$ thins a hull by roughly $0.35$ mm every year.
Voltage tells you whether iron corrodes; Faraday's law tells you how much. The mass lost is $\Delta m = ItM/nF$, where $n = 2$ electrons leave each iron atom and $F = 96485$ C/mol. Two knobs change almost everything: oxygen, which feeds the cathode, and chloride, which punctures iron's thin protective oxide — which is why de-icing salt and seawater are so brutal. Warming the water speeds the chemistry exponentially through an Arrhenius factor.
First, switch to Sacrificial Anode (Zn) and watch the iron's mass-loss curve flatten — the zinc volunteers to corrode in iron's place. Next, in Iron Rusting, drag the $[\mathrm{Cl^-}]$ slider from $0$ up toward seawater ($0.5$ M) and watch the corrosion rate climb. Finally, raise the pH into the $9\text{–}13$ range and see the rate collapse as iron passivates — then push past $13$ and watch "caustic corrosion" return.
Corrosion is fundamentally an electrochemical process — a short-circuited galvanic cell formed on the metal surface itself. Anodic and cathodic regions are connected by the metal (electron path) and the electrolyte (ion path).
| Symbol | Meaning | SI Unit |
|---|---|---|
| $E^\circ_{cell}$ | Standard cell potential | V |
| $\Delta G^\circ$ | Standard Gibbs free energy | J/mol or kJ/mol |
| $n$ | Electrons transferred per Fe atom | (2 for Fe → Fe²⁺) |
| $F$ | Faraday constant | 96 485 C/mol |
| $i_{corr}$ | Corrosion current density | A/m² |
| $\beta_a, \beta_c$ | Tafel slopes (anodic, cathodic) | V/decade |
| $M$ | Molar mass of Fe (55.85) | g/mol |
| $\rho$ | Density of Fe (7.87) | g/cm³ |
| Slider | Symbol | Used in |
|---|---|---|
| [O₂] | $[O_2]$ | cathodic limiting current |
| pH | $[H^+]$ | shifts cathode reaction (acid → H₂ evolution) |
| [Cl⁻] | chloride | pitting factor in $i_{corr}$ |
| Temperature | $T$ | Arrhenius factor |
| Anode area | $A$ | total mass loss |
References:
[Atkins & de Paula — Physical Chemistry, 11th Ed., Ch. 16.7 "Corrosion"]
[Housecroft & Sharpe — Inorganic Chemistry, 5th Ed., Ch. 8.10 "Electrolysis and Corrosion"]
[Jones — Principles and Prevention of Corrosion, 2nd Ed., Ch. 3]
Best resource: LibreTexts Chemistry — "Corrosion" (chem.libretexts.org/Bookshelves/Analytical_Chemistry/Supplemental_Modules/Electrochemistry/Corrosion); Khan Academy — Galvanic Cells & Corrosion.
Misconceptions reference: Schmidt et al., "Students' alternative conceptions about corrosion," J. Chem. Educ. 2007, 84(10), 1620; Taber — Chemical Misconceptions: Prevention, Diagnosis and Cure (RSC, 2002), Ch. 5 "Electrochemistry."