Electrochemistry
Randles-Sevcik Equation: Peak Current vs Scan Rate in Voltammetry
Double the scan rate of a cyclic voltammogram and the peak current rises by exactly 41% (a factor of the square root of 2), not by 100%. That single, counter-intuitive scaling is the fingerprint of the Randles-Sevcik equation — the relationship that ties the peak current of a redox wave to the square root of how fast you sweep the electrode potential.
Formally, the equation predicts the peak current (ip) of a reversible, diffusion-controlled electron transfer at a planar electrode during linear-sweep or cyclic voltammetry. At 25 °C it reads ip = (2.69 × 10⁵) · n^(3/2) · A · D^(1/2) · C · v^(1/2), and its square-root dependence on scan rate v is the workhorse diagnostic for deciding whether a species is freely diffusing in solution or stuck to the electrode surface.
- TypeElectroanalytical relation (CV/LSV)
- Introduced1948, by J. E. B. Randles and A. Ševčík (independently)
- Key equationip = (2.69×10⁵) n^(3/2) A D^(1/2) C v^(1/2) at 25 °C
- Core scalingip ∝ v^(1/2) (diffusion) vs ip ∝ v (adsorbed)
- Applies toReversible, diffusion-controlled electron transfer, planar electrode
- Measured byCyclic / linear-sweep voltammetry with a potentiostat
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What the Randles-Sevcik equation is and where it applies
The Randles-Sevcik equation quantifies the height of the current peak seen when you sweep an electrode's potential linearly through a redox couple's formal potential. As the potential passes E°′, the electroactive species is oxidized or reduced at the surface; the current rises, peaks, then falls as the near-electrode region becomes depleted and diffusion can no longer keep pace with the sweep.
It applies specifically to a reversible (Nernstian), diffusion-controlled electron transfer at a planar electrode, with the redox species freely dissolved in a well-supported electrolyte. Key assumptions:
- Fast, reversible electron transfer (kinetics never limit the current).
- Semi-infinite linear diffusion — no convection, negligible migration (excess supporting electrolyte), no ohmic drop.
- A flat electrode large compared with the diffusion layer, so edge/spherical effects are ignored.
Where it matters: measuring diffusion coefficients, determining the number of electrons n, quantifying analyte concentration, characterizing new redox mediators, battery and fuel-cell materials, and screening electrocatalysts. It is arguably the single most-cited equation in practical electrochemistry.
Deriving it step by step from Fick's second law
The derivation starts with mass transport. The flux of the electroactive species obeys Fick's second law: ∂C/∂t = D · ∂²C/∂x², with C the concentration, x the distance from the electrode, and D the diffusion coefficient.
- Boundary condition at the surface: because the couple is reversible, the surface concentrations of oxidized and reduced forms track the applied potential through the Nernst equation, E = E°′ + (RT/nF) ln([O]s/[R]s). As E is ramped, the potential-dependent factor is θ = exp[(nF/RT)(E − E°′)].
- Sweep: the potential is E(t) = Ei − v·t, so time and potential are interchangeable through the scan rate v.
- Solution: substituting the moving boundary into the diffusion equation gives an integral (a convolution / Abel-type integral) that has no closed form. Randles and Ševčík solved it numerically.
The result: the current is i = nFAC(πDσ)^(1/2)·χ(σt), where σ = nFv/RT and χ is a tabulated dimensionless function. Its maximum value is χmax = 0.4463. Collecting terms gives the general form ip = 0.4463 · nFAC · (nFvD/RT)^(1/2). Plugging in F, R, and T = 298 K bundles the constants into the familiar 2.69 × 10⁵.
Key quantities and a worked example
Track the units carefully — the equation is written for CGS-flavored electrochemistry, not pure SI:
- ip in amperes; n dimensionless; A in cm²; D in cm²/s; C in mol/cm³ (so 1 mM = 1×10⁻⁶ mol/cm³); v in V/s.
- The constant 2.69 × 10⁵ carries units of C·mol⁻¹·V⁻¹ᐟ² and is temperature-specific (25 °C). The general 0.4463 form is temperature-independent.
Worked example: the classic ferricyanide couple, [Fe(CN)6]³⁻/⁴⁻, with n = 1, D ≈ 7.6 × 10⁻⁶ cm²/s, C = 1.0 mM = 1×10⁻⁶ mol/cm³, at a 3 mm-diameter disk (A ≈ 0.071 cm²), swept at v = 0.1 V/s.
- ip = 2.69×10⁵ × 1^(3/2) × 0.071 × (7.6×10⁻⁶)^(1/2) × 1×10⁻⁶ × (0.1)^(1/2)
- = 2.69×10⁵ × 0.071 × 2.76×10⁻³ × 1×10⁻⁶ × 0.316 ≈ 1.7 × 10⁻⁵ A ≈ 17 µA.
Raising v to 0.4 V/s (4×) doubles ip to ~34 µA — the square-root law made concrete.
How it is measured and used in the lab
In practice you run cyclic voltammetry with a three-electrode cell (working, reference, counter) driven by a potentiostat, and record ip at a series of scan rates.
- Randles-Sevcik plot: plot ip against v^(1/2). A straight line through the origin confirms diffusion control; the slope equals 2.69×10⁵·n^(3/2)·A·D^(1/2)·C.
- Extracting D: if n, A, and C are known, solve the slope for the diffusion coefficient — the most common analytical use.
- Counting electrons: with D and C known, the slope gives n^(3/2), pinning down how many electrons the step transfers.
- Quantifying concentration: ip is linear in C, so calibrated CV becomes a sensor readout.
Practical cautions: subtract capacitive (double-layer) charging current, which itself scales linearly with v and can swamp small faradaic peaks at high scan rates; add ample supporting electrolyte to kill migration; compensate for uncompensated resistance (iR drop), which artificially widens ΔEp and depresses ip at fast sweeps. Always verify reversibility first: ΔEp ≈ 59/n mV and a return-to-forward peak ratio near 1.
How it relates to neighboring concepts
The Randles-Sevcik equation sits inside a family of transport-and-kinetics relations, and knowing its cousins prevents misuse:
- Cottrell equation: governs a potential step (chronoamperometry), giving i = nFAC·D^(1/2)/(π^(1/2) t^(1/2)) — same D, same planar diffusion, but time-decay rather than a scanned peak.
- Nernst equation: supplies the surface boundary condition; the 0.4463 peak factor only exists because the couple is Nernstian.
- Butler-Volmer / Nicholson analysis: take over when electron transfer is slow (quasi-reversible or irreversible), replacing 0.4463 with 0.496·(αnα)^(1/2) and letting peak potential drift with v.
- Levich equation: the rotating-disk analog where forced convection, not diffusion alone, sets a steady limiting current proportional to ω^(1/2).
- Surface (Laviron) behavior: for adsorbed species ip ∝ v, not v^(1/2) — the litmus test that distinguishes solution-phase from surface-confined redox.
Exceptions, limits, and lasting significance
Because the equation encodes so many assumptions, its deviations are as diagnostically useful as the law itself.
- Non-planar diffusion: at ultramicroelectrodes (radius ≤ ~25 µm) radial diffusion dominates and the CV becomes a sigmoidal steady-state wave with no peak — Randles-Sevcik simply does not apply.
- Slow kinetics: quasi-reversible/irreversible couples show ΔEp > 59/n mV that grows with v, and ip falls below the reversible prediction; use the irreversible form ip = 2.99×10⁵·n(αnα)^(1/2)·A·D^(1/2)·C·v^(1/2).
- Coupled chemistry (EC, ECE): following reactions distort ip/v^(1/2), which is exactly how mechanisms are unraveled.
- Adsorption: a peak scaling linearly with v flags surface confinement or thin-layer behavior.
Its lasting significance: introduced in 1948 by John E. B. Randles in England and, independently, Augustin Ševčík in Czechoslovakia, it turned voltammetry from a qualitative curiosity into a quantitative analytical method. Nearly eight decades on, it remains the first equation any electrochemist reaches for to interrogate a new redox system.
| System | Peak current expression (25 °C) | Scan-rate dependence | Peak-to-peak signature |
|---|---|---|---|
| Reversible (Nernstian), diffusion | ip = 2.69×10⁵ · n^(3/2) A D^(1/2) C v^(1/2) | ip ∝ v^(1/2) | ΔEp = 59/n mV, ip,a/ip,c = 1, Ep independent of v |
| Irreversible, diffusion | ip = 2.99×10⁵ · n(αnα)^(1/2) A D^(1/2) C v^(1/2) | ip ∝ v^(1/2) | No reverse peak; Ep shifts ~30/(αnα) mV per decade of v |
| Quasi-reversible, diffusion | Between the two limits (Nicholson analysis) | ≈ v^(1/2), curvature at high v | ΔEp grows with v; use ψ vs v to extract k0 |
| Surface-confined / adsorbed | ip = (n²F²/4RT) A Γ v | ip ∝ v (linear) | ΔEp ≈ 0, symmetric peak, thin-layer shape |
Frequently asked questions
Why does peak current scale with the square root of scan rate?
Because the current is limited by diffusion of the analyte to the electrode. A faster sweep depletes the surface more quickly, so the diffusion layer is thinner and the concentration gradient steeper, giving more current. But the amount of extra current only grows as the square root of scan rate because the diffusion-layer thickness itself scales with (Dt)^(1/2), and t is inversely tied to v. Hence ip ∝ v^(1/2).
What is the 2.69 × 10⁵ constant and where does it come from?
It is the bundle of physical constants (Faraday constant F, gas constant R) evaluated at 298 K, multiplied by the dimensionless peak factor 0.4463 from the numerical solution of the diffusion problem. Its units are C·mol⁻¹·V⁻¹ᐟ². Because it fixes T = 25 °C, use the temperature-independent general form, ip = 0.4463·nFAC·(nFvD/RT)^(1/2), at any other temperature.
What units must I use to get the right answer?
Use the mixed CGS-style units the constant assumes: electrode area A in cm², diffusion coefficient D in cm²/s, concentration C in mol/cm³ (so a 1 mM solution is 1×10⁻⁶ mol/cm³), scan rate v in V/s, and you get ip in amperes. Forgetting to convert mM to mol/cm³ is the single most common error, producing answers 1000× too large.
How do I tell if my system is diffusion-controlled or surface-adsorbed?
Run CV at several scan rates and plot peak current against v and against v^(1/2). A straight line through the origin versus v^(1/2) means diffusion control (Randles-Sevcik applies). A straight line versus v instead means the species is adsorbed or surface-confined, where ip = (n²F²/4RT)·A·Γ·v governs the response.
How does the equation change for an irreversible reaction?
When electron transfer is slow, the peak factor changes from 0.4463 to 0.496 and the transfer coefficient enters: ip = 2.99×10⁵·n(αnα)^(1/2)·A·D^(1/2)·C·v^(1/2), where α is the transfer coefficient and nα the electrons in the rate-determining step. There is no return peak, and the peak potential shifts to more extreme values as scan rate increases — about 30/(αnα) mV per decade of v.
Can I get the diffusion coefficient from a Randles-Sevcik plot?
Yes — that is its most common use. The slope of ip versus v^(1/2) equals 2.69×10⁵·n^(3/2)·A·D^(1/2)·C. If you know n, the electrode area A, and the concentration C, solve for D. Verify reversibility first (ΔEp ≈ 59/n mV, peak ratio near 1); otherwise the reversible slope over-estimates D.