🧪 Section 1 — Interactive Simulation
💡 Section 2 — The Idea, Step by Step
Picture a fast game of catch where the "ball" is a tiny negative speck called an electron. In every redox (short for reduction–oxidation) reaction, electrons get tossed from one atom to another. The atom that throws electrons away is oxidized; the atom that catches them is reduced. That single hand-off is what rusts a nail, runs the battery in your phone, and lets your body burn food for energy. A handy memory hook: OIL RIG — Oxidation Is Loss, Reduction Is Gain.
Keeping score with oxidation numbers
To track the hand-offs we give every atom an oxidation number — a pretend charge that says how many electrons it "owns." When that number goes up, the atom lost electrons (oxidation); when it goes down, it gained them (reduction). The one rule that balances every redox reaction is simple: electrons lost must equal electrons gained. Drop a strip of zinc into blue copper solution, $\mathrm{Zn + Cu^{2+} \to Zn^{2+} + Cu}$. Zinc climbs $0 \to +2$, handing over $2$ electrons; each copper ion falls $+2 \to 0$, catching those same $2$. Two given, two taken — perfectly matched, so the equation is already balanced.
The grown-up tools
For messier reactions, chemists split things into two half-reactions — one for the loss, one for the gain — balance each for atoms and charge, then scale them so the electrons cancel exactly. Whether the whole thing happens on its own is set by the cell potential:
When permanganate meets iron, $\mathrm{MnO_4^-}$ pulls manganese from $+7 \to +2$, catching $5$ electrons, so it needs five $\mathrm{Fe^{2+}}$ ions, each rising $+2 \to +3$ and releasing one electron. With $E^\circ_{\text{cell}} = 1.51 - 0.77 = +0.74\ \text{V}$, the free-energy change is $\Delta G^\circ = -(5)(96485)(0.74) \approx -357\ \text{kJ/mol}$ — strongly negative, so the reaction races forward. In the sim, the ON sliders set the two oxidation states, n sets how many electrons cross, pH switches acidic versus basic balancing, and the E° sliders feed straight into $E^\circ_{\text{cell}}$.
Try this in the sim above
Pick the Zn + Cu²⁺ preset and count the glowing electrons crossing from zinc to copper — exactly $2$, lost equals gained. Switch to the MnO₄⁻ + Fe²⁺ preset and open the Oxidation States tab to watch manganese plunge $+7 \to +2$ while iron ticks up by one. Finally, drag E°₂ above E°₁: the $E^\circ_{\text{cell}}$ readout flips negative and $\Delta G^\circ$ turns positive — the reaction is now non-spontaneous and would rather run backward.
📐 Section 3 — Equation Derivation
Symbol Definitions
| Symbol | Meaning | Unit |
|---|---|---|
| n | Number of electrons transferred per reaction unit | mol e⁻ / mol rxn |
| F | Faraday constant = 96 485 C·mol⁻¹ | C·mol⁻¹ |
| E° | Standard reduction potential | V |
| ΔG° | Standard Gibbs free energy change | kJ·mol⁻¹ |
| ON | Oxidation number (oxidation state) | integer |
| K | Thermodynamic equilibrium constant | dimensionless |
Step-by-Step: The Ion-Electron (Half-Reaction) Method
Mapping: Simulation Variables → Theory
- ON sliders — set the oxidation states of the two elements, the simulation infers electron transfer ΔON.
- n slider — total electrons transferred per balanced unit (this multiplies the half-reactions).
- pH slider — switches the medium between acidic (H⁺ added) and basic (OH⁻ added) for the balancing display.
- E° sliders — produce E°cell = E°₁ − E°₂ and ΔG° = −nFE°cell visualized in the readouts.
- Latimer mode — shows reduction potentials for sequential oxidation states of the same element (e.g. Mn).
Worked Example: MnO₄⁻ + Fe²⁺ in acidic medium
$\mathrm{Fe^{2+} \to Fe^{3+} + e^-}$ (oxidation, E° = +0.77 V)
$\mathrm{MnO_4^- + 8H^+ + 5e^- \to Mn^{2+} + 4H_2O}$ (reduction, E° = +1.51 V)
Step 2 — Balance e⁻: multiply iron half-reaction by 5:
$5\,\mathrm{Fe^{2+}\to 5\,Fe^{3+}+5e^-}$
Step 3 — Add:
$\mathrm{MnO_4^- + 8H^+ + 5\,Fe^{2+} \to Mn^{2+} + 4H_2O + 5\,Fe^{3+}}$
Step 4 — E°cell and ΔG°:
$E^\circ_{cell}=1.51-0.77=+0.74$ V
$\Delta G^\circ=-(5)(96485)(0.74)=-357\text{ kJ/mol}$
$\log K = nE^\circ/0.0592=5\times0.74/0.0592=62.5\Rightarrow K\approx 10^{62.5}$ — essentially complete.