Nernst Equation
Cell potential away from standard, E = E° − (RT/nF)·ln Q, with K, ΔG, the temperature-corrected 0.0592 V slope, and single-ion membrane potentials.
The actual potential and its shift from standard, the reaction quotient from listed concentrations, K = exp(nFE°/RT), ΔG and ΔG°, whether the reaction runs, and the mV-per-decade slope at your temperature.
Example: A 1.10 V cell with n = 2 at Q = 10 delivers 1.0704 V — a 29.6 mV drop, since the slope is 59.16 mV per decade at 25 °C; ΔG is −207 kJ/mol and K is 1.5 × 10³⁷. A 4 / 140 mM ion ratio gives −91.3 mV.
Concentration moves
the voltage.
Where the equation comes from, what the 0.0592 really is, and the single-ion case.
The equation
A cell's potential falls as its reactants are used up: E = E° − (RT ÷ nF)·ln Q, with Q the reaction quotient, n the electrons transferred and F Faraday's constant. In base-10 form the factor 2.303RT ÷ F is the famous 0.0592 V per decade — but only at 25 °C. At 60 °C it is 0.0661, and the page recomputes it for the temperature you give rather than repeating the textbook number. Every tenfold change in Q moves the potential by that slope divided by n.
Q, K and ΔG
The quotient is products over reactants, each raised to its stoichiometric coefficient, with pure solids, pure liquids and the solvent left out at unit activity; gases use partial pressures in bar. Concentrations stand in for activities, which is good to a few percent in dilute solution and poor above about 0.1 M. At equilibrium E = 0 and Q = K, which gives K = exp(nFE° ÷ RT) from the standard potential alone. The free energy follows as ΔG = −nFE: negative means the reaction as written runs, and its magnitude is the electrical work the cell can do.
Membranes and ion-selective electrodes
The same equation with one ion crossing a membrane gives E = (RT ÷ zF)·ln(c_out ÷ c_in), the voltage at which an ion's electrical and chemical driving forces balance — about −91 mV for a 4 / 140 mM potassium ratio at body temperature, and the basis of every pH and ion-selective electrode. A real membrane potential is a weighted mixture of several ions (Goldman–Hodgkin–Katz) and is not computed here. Standard potentials come from your own table; none is stored, and they shift with temperature themselves in ways this equation does not model. Nothing leaves the browser; the same four anonymous usage counts as the rest of the site apply.
SOURCES
- E = E° − (RT/nF)·ln Q; 2.303RT/F = 59.16 mV per decade at 25 °C, recomputed at your temperature; K = exp(nFE°/RT); ΔG = −nFE; R = 8.314 462 618 J/(mol·K), F = 96 485.332 12 C/mol (SI 2019 exact)
Last reviewed 22 September 2026. How results are checked: How we verify.