Standard potentials assume 1 M solutions. Real cells drift away from that as they run, and their voltage changes. Combining ΔG = −nFE with ΔG = ΔG° + RT ln Q gives the correction.
Key idea
Why it works
Worked examples
Worked example: A cell running down
- $$\mathrm{Zn(s)} + \mathrm{Cu^{2+}(aq)} \to \mathrm{Zn^{2+}(aq)} + \mathrm{Cu(s)}$$: $Q = \dfrac{[\mathrm{Zn^{2+}}]}{[\mathrm{Cu^{2+}}]} = \dfrac{1.0}{0.010} = 100$ (the metals are left out).
- $$E = 1.10 - \dfrac{0.0592}{2}\log 100 = 1.10 - (0.0296)(2) = 1.04\ \text{V}$$
Answer: $1.04\ \text{V}$.
Worked example: A concentration cell
- $E^\circ = 0$: the two half-reactions are the same. The dilute side is the anode (copper dissolves there, raising its concentration); the concentrated side is the cathode.
- Overall: $$\mathrm{Cu^{2+}(1.0\ M)} \to \mathrm{Cu^{2+}(0.0010\ M)}$$ so $Q = \dfrac{0.0010}{1.0} = 1.0 \times 10^{-3}$.
- $$E = 0 - \dfrac{0.0592}{2}\log(1.0 \times 10^{-3}) = (0.0296)(3) = 0.089\ \text{V}$$
Answer: $0.089\ \text{V}$.
The correction is small but not negligible: every factor of 10 in $Q$ changes $E$ by $0.0592/n$ volts. For a two-electron cell, that is 30 mV per factor of 10.
Common mistake
A pH meter uses the same law. Its glass electrode responds to $[\mathrm{H_3O^+}]$, and at 25 °C its voltage changes by about $0.0592\ \text{V}$ (59 mV) for each unit of pH, the Nernst slope for one electron per proton. That is why meters are calibrated with buffers of known pH, and why they correct for temperature.