Nernst Equation Calculator

Calculate cell potential at non-standard conditions with E = E° − (RT/nF)ln(Q).
Inputs: standard potential, electrons, reaction quotient, and temperature.

Cell Potential

The Nernst equation tells you the actual voltage of an electrochemical cell at non-standard conditions, accounting for concentration, pressure, and temperature differences from the standard state. It’s the bridge between the textbook E° values listed in tables and the real voltage you’d measure with a multimeter on a working cell.

The full equation: E = E° − (RT / nF) × ln(Q)

The handy 25 °C form (most common in practice): E = E° − (0.05916 / n) × log₁₀(Q)

The constant 0.05916 V at 298 K is (RT/F) × ln(10). It’s worth memorizing if you do any electrochemistry by hand.

What each variable means

Symbol Meaning Unit
E Cell potential at the actual conditions V
Standard cell potential (from tables) V
R Gas constant, 8.314 J/(mol·K)
T Temperature (absolute) K
n Moles of electrons transferred per reaction unit (dimensionless)
F Faraday’s constant, 96,485 C/mol
Q Reaction quotient, [products]/[reactants] in current state (dimensionless)

Computing Q for common cases

For a half-reaction like Cu²⁺ + 2e⁻ → Cu(s), the cell-wide quotient depends on which half-cells you’re using. For the full Daniell cell Zn(s) + Cu²⁺ → Zn²⁺ + Cu(s):

Q = [Zn²⁺] / [Cu²⁺]

(Solids and pure liquids don’t appear in Q; gas activities use partial pressures in atm.)

For a redox titration or a concentration cell, Q is just the ratio of the more-concentrated species to the less-concentrated one, raised to whatever powers the balanced equation requires.

Worked example: Zn/Cu cell during discharge

A standard zinc-copper cell has E° = 1.10 V and transfers n = 2 electrons. As it discharges, [Zn²⁺] builds up and [Cu²⁺] drops. If [Zn²⁺] = 1.0 M and [Cu²⁺] = 0.01 M at 25 °C:

Q = 1.0 / 0.01 = 100 E = 1.10 − (0.05916/2) × log₁₀(100) = 1.10 − 0.0296 × 2 = 1.041 V

The cell voltage drops 60 mV from the textbook value because the products have built up. Continued discharge drives Q higher and E lower until E = 0, at which point the cell is dead (equilibrium reached).

At equilibrium, E = 0

When the cell can do no more work, E = 0 and Q = K (the equilibrium constant). Rearranging: log₁₀(K) = nE° / 0.05916 (at 25 °C)

For the Zn/Cu cell: log K = 2 × 1.10 / 0.05916 ≈ 37.2, so K ≈ 10³⁷. Huge — which is why the cell drives so far to completion before reaching equilibrium.

Practical applications

  • Battery voltage prediction. Lithium-ion cells start near their nominal E° but drop steadily as Li⁺ shuttles between electrodes; the discharge curve is essentially the Nernst equation running backwards in real time.
  • Corrosion analysis. The Nernst equation tells you whether a metal will spontaneously oxidize in a given environment. Iron in seawater (high Cl⁻, low O₂) corrodes faster than iron in dry air because Q shifts the effective potential.
  • pH electrodes. A glass pH probe is fundamentally a Nernst-equation device. The 0.05916 V per decade slope at 25 °C is what gives you ~59 mV per pH unit — the calibration spec on every pH meter.
  • Biological membrane potentials. The Nernst equation predicts the equilibrium voltage across a cell membrane for a single ion species. The Goldman-Hodgkin-Katz equation extends it to multiple ions for real neuron physiology.
  • Concentration cells. When two half-cells are chemically identical but at different concentrations, E° = 0 and the entire voltage comes from the (RT/nF)ln(Q) term. Used in oxygen sensors, glucose meters, and reference electrodes.

Why the temperature term matters

Most textbook problems are at 25 °C, but real batteries operate from −40 °C (cold-weather automotive) to 80 °C (data-center cells). The (RT/nF) coefficient changes from 0.0257 V at 298 K to 0.0240 V at 280 K to 0.0301 V at 350 K — about 17% across that range. Same Q, different voltage, depending on temperature.

Common pitfalls

  • Forgetting that n is electrons per reaction unit, not per mole of product. The reaction 2H⁺ + 2e⁻ → H₂ has n = 2, not n = 1.
  • Mixing log₁₀ and ln. The full formula uses ln; the 0.05916 shortcut uses log₁₀. Off by a factor of 2.303 if confused.
  • Using activities vs concentrations. At very high ionic strength (>1 M), the calculator’s Q based on concentrations alone is wrong by 10% or more; rigorous work needs activity coefficients.
  • Plugging in temperature in Celsius. R requires Kelvin. 25 °C is 298.15 K, not 25.

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This calculator runs entirely in your browser, so the numbers you enter stay on your device. The math behind it is written by hand and tested against worked examples and standard references before the page goes live.

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