Corrosion

A rusting nail is not "reacting with air" in any vague sense — it is running a fully-formed electrochemical cell on its own surface, complete with an anode, a cathode, an electrolyte, and a measurable driving EMF. One patch of iron oxidises (Fe→Fe2++2e−\text{Fe} \rightarrow \text{Fe}^{2+} + 2e^-), electrons flow through the metal to a nearby patch where dissolved oxygen is reduced, and the two half-reactions never physically separate the way they do in a galvanic cell you build on a bench. This article closes the Electrochemical Systems unit of CY11001 by pointing the same Nernst-equation, standard-reduction-potential, and ΔG=−nFE\Delta G = -nFE machinery you already own at this everyday process — first to explain why iron rusts fastest exactly where you would not expect, then to turn a sacrificial zinc block into a number: how many kilograms of zinc a ship actually eats through in a year of protecting its hull.

The core insight

Corrosion is a short-circuited galvanic cell on a single metal surface, its feasibility and rate follow directly from standard reduction potentials and ΔG=−nFE\Delta G = -nFE, and the same Faraday's-law arithmetic used to size a sacrificial anode predicts how fast it is consumed.

The core idea

Corrosion is an unintentional galvanic cell. On a real metal surface, microscopic differences in composition, strain, or oxygen access make some patches anodic and others cathodic. The metal itself supplies the electron path between them; a thin film of moisture supplies the ionic path — the two conduction routes any galvanic cell needs, except here anode and cathode sit side by side on one piece of metal rather than in separate half-cells.

Anode: Fe(s)→Fe2+(aq)+2e−Cathode: O2(g)+2H2O(l)+4e−→4OH−(aq)\text{Anode: } \text{Fe}(s) \rightarrow \text{Fe}^{2+}(aq) + 2e^- \qquad \text{Cathode: } \text{O}_2(g) + 2\text{H}_2\text{O}(l) + 4e^- \rightarrow 4\text{OH}^-(aq)

where: the anode reaction is the metal loss you actually care about; the cathode reaction merely completes the circuit by consuming the electrons the anode releases. Fe2+\text{Fe}^{2+} and OH−\text{OH}^- subsequently combine and are oxidised further by dissolved oxygen to hydrated Fe2O3⋅xH2O\text{Fe}_2\text{O}_3\cdot x\text{H}_2\text{O}, the rust you see — which deposits away from the anodic site, so it never blocks the ongoing metal loss underneath.

Differential aeration decides who is anode. Oxygen reduction is favoured wherever O2\text{O}_2 is more available, so the well-aerated patch of a surface is pulled toward being the cathode and the oxygen-starved patch is forced into the anodic role — the site of actual dissolution. This is why a steel pipe buried in soil often corrodes fastest in its least-aerated stretch, and why a small nick in an otherwise intact coating corrodes violently: a small anode area feeding electrons to a large cathode area concentrates current density at the nick.

Feasibility is read off potentials, exactly as in any cell. The driving force for the couple is the same cell EMF you already compute for any two half-reactions, and its sign tells you whether corrosion (or protection) is thermodynamically favoured:

Ecell=Ecathode∘−Eanode∘,ΔG=−nFEcellE_{cell} = E^\circ_{cathode} - E^\circ_{anode}, \qquad \Delta G = -nFE_{cell}

where: Ecathode∘E^\circ_{cathode} and Eanode∘E^\circ_{anode} are standard reduction potentials (V) of the two half-reactions, nn is the number of electrons transferred, F=96,500 C mol−1F = 96{,}500\ \text{C mol}^{-1} is the Faraday constant, and ΔG\Delta G (J) is the free-energy change — negative ΔG\Delta G (positive EcellE_{cell}) means the process is spontaneous. Plotting equilibrium potential against pH for a metal's oxide/hydroxide equilibria (a Pourbaix diagram) extends this same Nernst-equation logic to show which EE–pH combinations favour the bare metal, its dissolved ions, or a passive oxide film.

Figure
Iron surface acting as a short circuited galvanic cell with an anodic pit losing electrons and a cathodic region reducing oxygen
One metal, two roles: local anode and local cathode iron — electron path (metal) thin electrolyte film — ion path anode (pit) Fe to Fe2+ + 2e- cathode (aerated) O2 + 2H2O + 4e- to 4OH- electrons flow through metal ions complete the circuit in the film Same electron and ion paths as a bench galvanic cell, just not physically separated
Derivation Asacrificial-anode consumption rate from EcellE_{cell} and Faraday's law

Engineers protecting a steel hull do not just want to know that zinc is thermodynamically willing to corrode instead of iron — they need a number: how many kilograms of zinc a given protective current consumes in a given time, so the blocks can be sized and scheduled for replacement, and this derivation chains the cell-potential feasibility check straight into that quantity using only the Faraday relation already used for electroplating and electrolysis problems.

Step 1. Confirm feasibility from standard reduction potentials. With E∘(Fe2+/Fe)=−0.44 VE^\circ(\text{Fe}^{2+}/\text{Fe}) = -0.44\ \text{V} and E∘(Zn2+/Zn)=−0.76 VE^\circ(\text{Zn}^{2+}/\text{Zn}) = -0.76\ \text{V}, zinc is more easily oxidised, so when hull and zinc are electrically connected through seawater, zinc takes the anodic role and the hull is forced cathodic (only O2\text{O}_2 reduction occurs there, no net Fe\text{Fe} loss). The driving EMF is Ecell=Ecathode∘−Eanode∘=(−0.44)−(−0.76)=0.32 VE_{cell} = E^\circ_{cathode} - E^\circ_{anode} = (-0.44) - (-0.76) = 0.32\ \text{V}, and ΔG=−nFEcell<0\Delta G = -nFE_{cell} < 0 confirms the couple is spontaneous in this direction.

Step 2. Recognise that the protective current is an electrolysis-style charge flow. The zinc anode reaction Zn→Zn2++2e−\text{Zn} \rightarrow \text{Zn}^{2+} + 2e^- passes n=2n = 2 mol of electrons per mole of zinc dissolved. A steady protective current II sustained for time tt delivers a total charge Q=ItQ = It, exactly as in any Faradaic process.

Step 3. Convert charge to moles of zinc consumed using Faraday's law. Q=nF×(moles of Zn)Q = nF \times (\text{moles of Zn}), so moles of Zn\text{Zn} consumed =QnF=ItnF= \dfrac{Q}{nF} = \dfrac{It}{nF}, with F=96,500 C mol−1F = 96{,}500\ \text{C mol}^{-1}.

Step 4. Convert moles to mass using the molar mass MM of zinc. Mass consumed m=ItMnFm = \dfrac{ItM}{nF} — the general sacrificial-anode consumption formula, with II in amperes, tt in seconds, MM in g/mol, and mm in grams. Result: m=I t Mn Fm = \dfrac{I\,t\,M}{n\,F}, where II is the protective current, tt the protection time, MM the anode metal's molar mass, nn its ionic charge, and FF the Faraday constant — the same equation resurfaces in the worked example below with real numbers.

Worked example

Problem. The ship's hull from the sacrificial-anode setup above (Ecell=0.32 VE_{cell} = 0.32\ \text{V}, Zn→Zn2++2e−\text{Zn} \rightarrow \text{Zn}^{2+} + 2e^-) draws a steady protective current of 2.0 A2.0\ \text{A} through its zinc blocks. Find (a) the free-energy change per mole of zinc oxidised, and (b) the mass of zinc consumed over one year of continuous protection (1 yr=3.156×107 s1\ \text{yr} = 3.156\times10^{7}\ \text{s}, MZn=65.4 g/molM_{\text{Zn}} = 65.4\ \text{g/mol}, F=96,500 C mol−1F = 96{,}500\ \text{C mol}^{-1}).

Step 1 — Free energy per mole. With n=2n = 2, ΔG=−nFEcell=−(2)(96,500)(0.32)=−61,760 J/mol≈−61.8 kJ/mol\Delta G = -nFE_{cell} = -(2)(96{,}500)(0.32) = -61{,}760\ \text{J/mol} \approx -61.8\ \text{kJ/mol}. The negative sign confirms the zinc-sacrifices-itself reaction is spontaneous, consistent with Step 1 of the derivation.

Step 2 — Total charge passed in one year. Q=It=(2.0 A)(3.156×107 s)=6.312×107 CQ = It = (2.0\ \text{A})(3.156\times10^{7}\ \text{s}) = 6.312\times10^{7}\ \text{C}.

Step 3 — Moles of zinc consumed. Using n=2n = 2 for Zn2+\text{Zn}^{2+}: moles =QnF=6.312×107(2)(96,500)=6.312×1071.93×105≈327 mol= \dfrac{Q}{nF} = \dfrac{6.312\times10^{7}}{(2)(96{,}500)} = \dfrac{6.312\times10^{7}}{1.93\times10^{5}} \approx 327\ \text{mol}.

Step 4 — Mass consumed. m=(327 mol)(65.4 g/mol)≈21,400 gm = (327\ \text{mol})(65.4\ \text{g/mol}) \approx 21{,}400\ \text{g}, so about 21.4 kg of zinc is consumed per year at this protective current — the figure a ship's maintenance schedule is built around.

Competitive stretch

If the current instead varied with season (say 3.0 A3.0\ \text{A} for four winter months and 1.5 A1.5\ \text{A} for eight remaining months), the same formula applies separately to each interval and the masses add, since QQ (and hence moles consumed) is simply additive over time — a reminder that m=ItM/(nF)m = ItM/(nF) assumes constant II only within each segment you apply it to.

Common traps

  • Assuming more oxygen always means more corrosion at that spot — differential aeration makes the oxygen-poor region the anode, the actual site of metal loss, while the oxygen-rich region merely hosts the cathodic reaction.
  • Confusing cathodic protection with a physical coating — cathodic protection works by forcing the metal to be thermodynamically the cathode (EcellE_{cell} and ΔG\Delta G shift), not by blocking the electrolyte path the way paint or galvanising does.
  • Forgetting the small-anode/large-cathode effect — a tiny exposed anodic area (a scratch in a coating) feeding a large cathodic area concentrates current density there, corroding the scratch far faster than uniform bare metal would.
  • Dropping nn or using the wrong ionic charge in m=ItM/(nF)m = ItM/(nF) — zinc dissolves as Zn2+\text{Zn}^{2+} (n=2n=2), and using n=1n=1 would double the predicted mass, understating how much anode metal a given current actually consumes.

Ask the tutor: if the jump from cell EMF to anode consumption mass in the derivation feels like a leap, ask the AI tutor to swap in a magnesium anode and a different current so you can rebuild m=ItM/(nF)m = ItM/(nF) from scratch yourself.

Why does rust form away from the pit where the metal is actually being eaten, instead of sealing it

Because the anodic and cathodic half-reactions happen in different places. Fe2+\text{Fe}^{2+} ions produced at the anode diffuse through the electrolyte film before meeting the OH−\text{OH}^- produced at the distant cathode; the resulting Fe2O3⋅xH2O\text{Fe}_2\text{O}_3\cdot x\text{H}_2\text{O} precipitates in between, not over the pit. Since the actively dissolving anode stays exposed, corrosion continues underneath even as visible rust builds up nearby — which is also why rust itself offers little practical protection.

Does a sacrificial anode ever run out, and what happens then

Yes — the derivation's m=ItM/(nF)m = ItM/(nF) shows the anode mass consumed grows linearly with time at a given protective current, so a real installation is sized with a service-life margin and inspected on a schedule. Once the zinc (or magnesium) block is consumed, the electrical connection to a fresh anodic metal is broken, the driving EMF disappears, and the originally protected structure becomes the most easily oxidised metal in the circuit again — so replacement, not permanence, is the design assumption.

If inhibitors do not change the thermodynamics, how do they slow corrosion at all

An inhibitor adsorbs onto the anodic or cathodic sites and raises the activation energy of the rate-limiting step, which is a kinetic effect, not a thermodynamic one. EcellE_{cell} and ΔG\Delta G for the underlying Fe/O2\text{Fe}/\text{O}_2 couple are unchanged — corrosion is still spontaneous — but the rate at which that spontaneous process proceeds drops sharply, similar to how a catalyst changes rate without changing ΔG\Delta G for a reaction.

Before this

Where this leads