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Spec Mapping — OCR H432 Module 5.2.3 — Electrochemical cells and cell potential, covering the calculation of standard cell potential from two half-cell potentials via Ecell∘=Ecathode∘−Eanode∘ (where the cathode is the more positive electrode); the construction of overall ionic equations by combining the cathode reduction half-equation with the reversed anode half-equation, balancing electrons by scaling; the prediction of redox feasibility from the sign of Ecell∘ (positive = thermodynamically feasible); the role of the salt bridge in carrying ionic current to balance charge; the bridge between electrochemistry and thermodynamics via ΔG∘=−nFEcell∘ with the Faraday constant F=96485 C mol−1; qualitative use of Le Chatelier on half-cell equilibria to predict the effect of concentration changes on E; the principle and operation of hydrogen–oxygen fuel cells (alkaline KOH and acidic PEM variants) with overall H2+21O2→H2O, Ecell∘≈+1.23 V; awareness of methanol fuel cells as a portable alternative; the distinction between thermodynamic feasibility and kinetic accessibility; and applications to rechargeable Li-ion and lead-acid batteries (refer to the official OCR H432 specification document for exact wording).
Lesson 8 built the vocabulary — the SHE, the standard electrode potential, the IUPAC cell notation, the electrochemical series. This lesson turns vocabulary into arithmetic: how to combine two E∘ values into a single Ecell∘, how to construct the overall ionic equation, how to use Ecell∘ to predict feasibility, and how to bridge to the Gibbs framework of Lesson 7 via ΔG∘=−nFEcell∘. Six worked examples walk through the Daniell cell, magnesium/copper, copper/silver, acidified MnO4−/Fe2+ (the Lesson 10 redox-titration setup), Cl2/Fe2+, and Mg/Ag+. The lesson then applies the framework to hydrogen and methanol fuel cells, the lithium-ion and lead-acid rechargeable batteries, and the qualitative Le-Chatelier effect of concentration changes on cell emf. Lesson 10 closes the module by applying these ideas to quantitative redox titrations.
Key Equations: Ecell∘=Ecathode∘−Eanode∘(with cathode = more positive) ΔG∘=−nFEcell∘ with n = moles of electrons transferred per mole of reaction, F=96485 C mol−1, Ecell∘ in V, ΔG∘ in J mol−1 (divide by 1000 for kJ). Feasibility criterion: Ecell∘>0⇔ΔG∘<0.
By the end of this lesson you should be able to:
When two half-cells are joined through a salt bridge and an external wire, the overall standard cell emf is:
Ecell∘=Ecathode∘−Eanode∘
where:
This is not an arbitrary convention: it falls out of the IUPAC cell-notation rule (Lesson 8) that the cell is written with the more positive electrode on the right. The subtraction is signed — be careful with negative E∘ values, because the minus signs propagate. The cell will always give Ecell∘>0 when the more positive electrode is correctly placed on the right (the cathode position).
Algorithm for any Ecell∘ problem:
graph TD
A[Two half-cells with known E values] --> B[Identify more positive E = CATHODE = reduction]
A --> C[Identify more negative E = ANODE = oxidation - REVERSE the equation]
B --> D["E_cell = E_cathode - E_anode (signed subtraction)"]
C --> D
D --> E{E_cell positive?}
E -->|Yes| F[Reaction THERMODYNAMICALLY feasible as written]
E -->|No| G[Reverse direction feasible]
F --> H[Scale electrons -- add half-equations -- electrons cancel]
H --> I["Apply delta G = -nFE_cell if required (n = electrons per mole of overall reaction)"]
Half-cells: E∘(Cu2+/Cu)=+0.34 V; E∘(Zn2+/Zn)=−0.76 V.
Step 1 — identify cathode/anode. Cu2+/Cu is more positive → cathode. Zn2+/Zn is more negative → anode.
Step 2 — compute Ecell∘.
Ecell∘=Ecathode∘−Eanode∘=(+0.34)−(−0.76)=+1.10V
Step 3 — half-equations.
Step 4 — overall equation (electrons match at 2, so add directly):
Zn(s)+Cu2+(aq)→Zn2+(aq)+Cu(s),Ecell∘=+1.10V
Step 5 — ΔG∘ via ΔG∘=−nFEcell∘ with n=2:
ΔG∘=−2×96485×1.10=−212267J mol−1=−212kJ mol−1
Strongly negative — consistent with the strongly positive Ecell∘ — confirming the Daniell cell reaction is thermodynamically feasible. This is the canonical demonstration of the framework: the cell is built from Zn rod in ZnSO4(aq) and Cu rod in CuSO4(aq), connected by a salt bridge of saturated KNO3, and a voltmeter reads +1.10 V at 298 K with [Zn2+] = [Cu2+] = 1.00 mol dm−3.
graph TD
A[Zn rod in 1.0 mol/dm3 ZnSO4 -- anode -- negative terminal] --> B[Zn loses electrons]
B --> C[External wire carries electrons to Cu electrode]
C --> D[Cu rod in 1.0 mol/dm3 CuSO4 -- cathode -- positive terminal]
D --> E[Cu2+ gains electrons -- Cu deposits on rod]
F[Salt bridge -- saturated KNO3 in agar] --> G[K+ migrates to Cu cell -- NO3- migrates to Zn cell]
G --> H[Charge balance maintained -- no net build-up]
The salt bridge is the unsung hero of the electrochemical cell. Its job is to carry ionic current between the two half-cells to balance the charge that would otherwise build up as electrons leave one half-cell and enter the other. Without it, the cell would polarise within microseconds — the anode compartment would accumulate positive charge from each Zn2+ released, the cathode compartment would accumulate negative charge from each Cu2+ consumed, and the cell emf would collapse.
In a typical salt bridge of saturated KNO3 in agar gel, K+ ions migrate towards the cathode compartment (where positive charge is being consumed) and NO3− ions migrate towards the anode compartment (where positive charge is being released). Both KNO3 ions are electrochemically silent — they are not oxidised or reduced at either electrode in the typical potential range, so they don't contribute to the cell reaction. The choice of KNO3 also avoids the issues of Cl− (which would be oxidised by Cl2/Cl−-active half-cells) or SO42− (which can precipitate Pb2+ or Ba2+ if those are in either compartment).
Critical point: the salt bridge carries ions, not electrons. Electrons flow through the external wire; ions flow through the salt bridge. Saying "the salt bridge completes the circuit" is correct only in the sense that ionic flow closes the electrical loop.
Half-cells: E∘(Cu2+/Cu)=+0.34 V; E∘(Mg2+/Mg)=−2.37 V.
Cu2+/Cu is more positive → cathode. Mg2+/Mg is more negative → anode.
Ecell∘=(+0.34)−(−2.37)=+2.71V
A huge cell emf — over twice the Daniell value — driven by the very negative magnesium half-cell. Half-equations (electrons already balanced at 2):
Overall: Mg(s) + Cu2+(aq) → Mg2+(aq) + Cu(s), Ecell∘=+2.71 V.
ΔG∘ with n=2: ΔG∘=−2×96485×2.71=−523029 J mol−1=−523 kJ mol−1.
This is the chemistry behind magnesium-air primary batteries and sacrificial-anode corrosion protection (a block of Mg attached to a steel ship's hull preferentially oxidises, sparing the iron from rusting).
Half-cells: E∘(Ag+/Ag)=+0.80 V; E∘(Cu2+/Cu)=+0.34 V.
Ag+/Ag is more positive → cathode. Cu2+/Cu is more negative → anode.
Ecell∘=(+0.80)−(+0.34)=+0.46V
Half-equations — note the electron mismatch (Ag+/Ag is 1-electron; Cu2+/Cu is 2-electron) — scale the Ag half-equation by 2:
Overall: Cu(s) + 2Ag+(aq) → Cu2+(aq) + 2Ag(s), Ecell∘=+0.46 V.
ΔG∘=−2×96485×0.46=−88766 J mol−1=−89 kJ mol−1. This is the "silver tree" demonstration (Lesson 8). Note that scaling a half-equation does NOT change E∘ — E∘ is an intensive property, like temperature. We scale the equation, not the potential.
Half-cells: E∘(MnO4−/Mn2+)=+1.51 V (in 1.0 mol dm−3 H+); E∘(Fe3+/Fe2+)=+0.77 V.
MnO4−/Mn2+ is more positive → cathode. Fe3+/Fe2+ is more negative → anode.
Ecell∘=(+1.51)−(+0.77)=+0.74V
Half-equations — MnO4− is 5-electron, Fe3+/Fe2+ is 1-electron — scale Fe by 5:
Overall:
MnO4−(aq)+8H+(aq)+5Fe2+(aq)→Mn2+(aq)+4H2O(l)+5Fe3+(aq)
n=5, so ΔG∘=−5×96485×0.74=−357000 J mol−1=−357 kJ mol−1. Strongly negative — the reaction goes essentially to completion, which is exactly the precondition for using it as the basis of a quantitative titration (Lesson 10). The 1 MnO4− : 5 Fe2+ stoichiometry is set by the electron-balance constraint, and is the foundation of the iron-tablet and iron-ore titration calculations of Lesson 10.
Half-cells: E∘(Cl2/Cl−)=+1.36 V; E∘(Fe3+/Fe2+)=+0.77 V.
Ecell∘=1.36−0.77=+0.59V
Half-equations (both 2-electron when Cl2 is balanced; Fe scaled by 2):
Overall: Cl2(g) + 2Fe2+(aq) → 2Cl−(aq) + 2Fe3+(aq), Ecell∘=+0.59 V.
ΔG∘=−2×96485×0.59=−114000 J mol−1=−114 kJ mol−1. Negative — chlorine water can oxidise iron(II) salts to iron(III), the chemistry behind chlorine bleaching of iron-stained fabrics and a school demonstration of feasibility via Ecell∘.
Can Cu(s) reduce Zn2+(aq) to Zn(s)? Proposed reaction: Cu(s) + Zn2+(aq) → Cu2+(aq) + Zn(s).
For this to be feasible as written, Cu would have to be the anode (oxidised) and Zn2+/Zn the cathode. So Ecell∘ for the proposed direction is:
Ecell∘=E∘(Zn2+/Zn)−E∘(Cu2+/Cu)=−0.76−0.34=−1.10V
Negative — NOT feasible. The reverse direction (the Daniell cell, Worked Example 1) is feasible with Ecell∘=+1.10 V.
This worked example shows the diagnostic step: if you propose a direction and get a negative Ecell∘, then the proposed direction is infeasible and the reverse is what spontaneously occurs.
Lesson 7 introduced ΔG∘=ΔH∘−TΔS∘ as the criterion of feasibility (ΔG∘<0). For electrochemical cells the same criterion appears in a different dress:
ΔG∘=−nFEcell∘
where:
F has units of coulombs per mole; Ecell∘ in V is equivalently J C−1 (joules per coulomb of charge). So nFEcell∘ has units of joules per mole — the same units as ΔG∘. The minus sign ensures that positive Ecell∘ (feasible) gives negative ΔG∘ (feasible).
Equivalences:
| Ecell∘ | ΔG∘ | Reaction status |
|---|---|---|
| >0 | <0 | Feasible as written |
| =0 | =0 | At equilibrium (K=1) |
| <0 | >0 | Infeasible as written; reverse is feasible |
These two criteria are exactly equivalent. Electrochemistry simply expresses Lesson 7's Gibbs criterion in volts rather than in kJ mol−1.
The E∘ values assume [solute] = 1.00 mol dm−3, p(gas) = 100 kPa, T=298 K. When conditions deviate, E (the actual electrode potential) shifts from E∘. Treating each half-equation as an equilibrium and applying Le Chatelier: increasing [oxidised species] (LHS) shifts equilibrium right and makes E more positive; decreasing [oxidised species] makes E more negative; increasing [reduced species] makes E more negative. For H+-dependent half-cells (e.g. MnO4− + 8H+ + 5e−), increasing [H+] shifts the reduction right, raising E and making MnO4− a stronger oxidising agent. Increasing temperature also shifts E via the half-cell Keq. The Nernst equation E=E∘−(RT/nF)lnQ makes these qualitative arguments quantitative (undergraduate footnote); at A-Level, qualitative Le-Chatelier reasoning suffices.
A fuel cell is an electrochemical cell in which the reactants are fed continuously from external tanks and the products are removed, giving a steady output of electrical power. Unlike a battery, a fuel cell does not "run down" — it keeps generating power as long as H2 (fuel) and O2 (oxidant) are supplied. The hydrogen–oxygen fuel cell is the workhorse of low-emission transport and space-mission power generation (the Apollo command module ran on alkaline H2/O2 cells supplied by Pratt & Whitney).
Alkaline hydrogen–oxygen fuel cell (electrolyte: aqueous KOH, ~6 mol dm−3):
Acidic PEM (proton-exchange membrane) hydrogen–oxygen fuel cell (electrolyte: solid acidic polymer membrane, typically Nafion — used in fuel-cell vehicles):
Both versions have the same net chemistry — water from hydrogen and oxygen, with all the redox energy released as electrical work rather than heat. The choice of electrolyte (alkaline vs acidic) affects operating temperature, longevity, and electrolyte handling but not the thermodynamics.
graph TD
A[H2 fuel tank] --> B[Anode: H2 oxidised to H+ or H2O]
B --> C[Electrons flow through external circuit -- ELECTRICAL WORK]
D[O2 from air] --> E[Cathode: O2 reduced to OH- or H2O]
C --> E
F[Electrolyte -- acidic PEM or alkaline KOH] --> G[H+ or OH- migration completes circuit]
E --> H[Water exhaust]
B --> H
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