Cyclic Voltammetry Current Calculator

Predict cyclic peak current quickly and clearly in seconds. Tune electrode, diffusion, and scan settings. Save clean outputs for reports and review work today.

Calculator Input

cm²
K
Used for irreversible mode.
Used for irreversible mode.
nmol/cm²
Used for surface-confined mode.
µF/cm²
µA

Example Data Table

Case n Area cm² Concentration mM D cm²/s Scan rate mV/s Expected use
Ferricyanide check 1 0.071 1.00 7.60e-6 100 Reversible diffusion test
Slow electron transfer 1 0.125 0.50 5.20e-6 50 Irreversible estimate
Modified electrode 1 0.196 1.00 6.00e-6 25 Surface process review

Formula Used

Reversible Diffusion Current

The calculator uses the temperature-aware Randles-Sevcik form:

Ip = 0.4463 n F A C √(n F D v / R T)

Irreversible Diffusion Current

For a totally irreversible peak, it uses:

Ip = 0.4958 n F A C √(α nα F D v / R T)

Surface-Confined Current

For an adsorbed reversible species, it uses:

Ip = n² F² A Γ v / 4 R T

Capacitive Current

Double-layer current is added as:

Ic = Cdl A v

Here, Ip is peak current. F is Faraday constant. R is gas constant. A is electrode area. C is bulk concentration. D is diffusion coefficient. v is scan rate. T is absolute temperature. Γ is surface coverage.

How to Use This Calculator

Select the current model that matches your experiment. Use reversible diffusion for a fast and Nernstian redox couple. Use irreversible diffusion when electron transfer is slow. Use surface confined for adsorbed films or modified electrodes.

Enter the electron number, electrode area, concentration, diffusion coefficient, scan rate, and temperature. Choose units carefully. Add transfer data for the irreversible model. Add surface coverage for the surface model. Include double-layer capacitance and baseline current when you want a closer measured current estimate.

Press the calculate button. The result appears above the form. Review the Faradaic current, capacitive current, total current, and current density. Download CSV for spreadsheets. Download PDF for lab notes or reports.

About Cyclic Voltammetry Current Calculation

Why Peak Current Matters

Cyclic voltammetry is a practical method for studying redox behavior. It shows how current changes as potential is swept forward and backward. The peak current is often the first value checked. It helps estimate concentration, diffusion, electrode area, and reaction control.

Diffusion Controlled Response

In a reversible diffusion controlled system, the peak current rises with the square root of scan rate. This relation is useful. It can test whether mass transport is mainly linear diffusion. A straight line in a current versus square root scan rate plot supports diffusion control.

Role of Electrode Area

Electrode area has a direct effect. A larger area gives a larger current when other values stay fixed. Real electrodes may behave differently from their polished geometric area. Surface roughness, coatings, and fouling can change the active area. This is why calibration remains important.

Concentration and Diffusion Effects

Concentration also has a direct effect on current. Higher analyte concentration gives a larger Faradaic signal. Diffusion coefficient affects how quickly species reach the electrode. Small molecules usually diffuse faster than large molecules. Viscosity, solvent, electrolyte, and temperature can shift diffusion values.

Scan Rate Choice

Scan rate controls the experiment time scale. Slow scans allow more time for mass transfer. Fast scans raise current but can increase capacitive background. Very fast scans may also reveal kinetic limits. This calculator includes a capacitive current estimate to separate charging effects from redox current.

Temperature and Kinetics

Temperature appears in the full peak current equations. Many quick estimates use the 25 Celsius coefficient. This tool uses absolute temperature, so it can support warmer or colder experiments. Irreversible mode also uses transfer coefficient and rate step electrons, which help represent sluggish charge transfer.

Using Results Carefully

Treat calculated current as an estimate. Real voltammograms may include uncompensated resistance, adsorption, convection, electrode contamination, and reference drift. Use the value to design experiments and compare trends. Confirm final conclusions with measured data, blanks, standards, and repeated scans under controlled conditions.

FAQs

What does this calculator estimate?

It estimates cyclic voltammetry peak current, capacitive current, total current, and current density using selected electrochemical models and user supplied experimental values.

Which model should I choose?

Choose reversible diffusion for fast electron transfer. Choose irreversible diffusion for slow charge transfer. Choose surface confined when the redox species is adsorbed on the electrode.

Why does scan rate affect current?

Scan rate changes the experiment time scale. Diffusion peak current commonly follows the square root of scan rate, while capacitive current rises linearly.

What units should concentration use?

You may enter mM, µM, M, or mol/cm³. The calculator converts the value internally to mol/cm³ for the equations.

What is double-layer capacitance?

Double-layer capacitance represents electrode charging at the interface. It creates background current, especially at high scan rates or large electrode areas.

Can this replace measured voltammograms?

No. It gives a model estimate. Real experiments may include resistance, noise, fouling, convection, adsorption, and instrument limits.

Why is temperature entered in Kelvin?

Electrochemical equations use absolute temperature. Entering Kelvin keeps the gas constant term consistent and avoids Celsius conversion mistakes.

What does current density show?

Current density divides total current by electrode area. It helps compare electrodes of different sizes under similar experimental conditions.

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Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.