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Activation Energy Calculator

If a rate constant rises from 0.001 at 300 K to 0.01 at 350 K, the two-point Arrhenius calculation gives 40.204 kJ/mol. Enter two paired measurements below, or use Advanced mode for a graph slope. Keep the rate constants in the same units and for the same reaction and rate law.

Input
Illustrative measurements and plot conventions; no reaction-specific material data is assumed.
Molar energy units. Thermochemical kcal uses exactly 4184 J.

Molar energy units. Thermochemical kcal uses exactly 4184 J.

First absolute temperature. K / °C in the header converts your measurements.
K

First absolute temperature. K / °C in the header converts your measurements.

Rate constant at T1. Scientific notation such as 1e-3 is accepted; use the same rate units as k2.

Rate constant at T1. Scientific notation such as 1e-3 is accepted; use the same rate units as k2.

Second temperature, different from T1. Keep the rate constant paired with its own temperature.
K

Second temperature, different from T1. Keep the rate constant paired with its own temperature.

Rate constant at T2. Rate sliders are logarithmic; type precise values directly.

Rate constant at T2. Rate sliders are logarithmic; type precise values directly.

Use the same reaction and rate-constant units for both measurements.

Assumes constant Arrhenius parameters over the interval.

Visual
Arrhenius relationship in reciprocal Kelvin and natural log rate ratio
Output
Apparent activation energy
40.204 kJ/mol

From two paired rate constants · no uncertainty estimate

Six significant digits shown; this does not establish experimental precision or a mechanistic energy barrier.

From two rate constants to activation energy

The Arrhenius equation defined by IUPAC is

k=Aexp⁡ ⁣(−EaRT).k=A\exp\!\left(-\frac{E_a}{RT}\right).

Here T is absolute temperature, R is the molar gas constant, and A is the pre-exponential factor. Assuming A and apparent activation energy are constant over the interval, subtracting the logarithmic equations for two measurements cancels A:

Ea=R ln⁡(k2/k1)1/T1−1/T2.E_a = R\,\frac{\ln(k_2/k_1)}{1/T_1-1/T_2}.

Use Kelvin in the reciprocal terms. The header buttons convert Celsius to Kelvin with the exact relation T(K) = t(°C) + 273.15, as specified in the NIST SI guide. The example's temperatures are 26.85 °C and 76.85 °C. Putting those Celsius numbers directly into the formula would describe different absolute temperatures and give the wrong energy.

For the illustrative pair above, the rate ratio is 10 and

1300−1350=12100 K−1,Ea=2100Rln⁡(10)≈40.204 kJ mol−1.\frac{1}{300}-\frac{1}{350}=\frac{1}{2100}\ \mathrm{K^{-1}},\qquad E_a=2100R\ln(10)\approx40.204\ \mathrm{kJ\,mol^{-1}}.

The calculator uses R = 8.31446261815324 J mol⁻¹ K⁻¹, derived from the exact Avogadro and Boltzmann constants in the NIST fundamental constants listing. Divide J/mol by 1000 for kJ/mol. Thermochemical kcal/mol uses 4184 J per kcal; it is distinct from other historical calorie definitions.

Swapping both complete temperature/rate pairs leaves the answer unchanged. Swapping only the rates reverses the sign. Mixing a rate constant in minutes with one in seconds changes the ratio and invalidates the comparison; use matching units first.

Match both axes when using an Arrhenius slope

OpenStax's Arrhenius linearization writes the relationship as

ln⁡k=−EaR1T+ln⁡A.\ln k=-\frac{E_a}{R}\frac{1}{T}+\ln A.

Therefore a slope m from ln(k) against 1/T gives Eₐ = −mR. A graph using common logarithms or 1000/T has a different numerical slope:

Vertical axis Horizontal axis Activation energy in J/mol
ln(k) 1/T −mR
log10(k) 1/T −mR ln(10)
ln(k) 1000/T −1000mR
log10(k) 1000/T −1000mR ln(10)

For example, m = −2.5 from log10(k) versus 1000/T gives

Ea=2500Rln⁡(10)≈47.8619 kJ mol−1.E_a=2500R\ln(10)\approx47.8619\ \mathrm{kJ\,mol^{-1}}.

Reading that same number as a natural-log slope against 1/T would omit both conversion factors. Select the axes exactly as they appear on the graph. A slope alone gives energy but does not determine the intercept or absolute rate constants.

The calculator's paired-data diagram uses ln(k/k1) versus 1/T. This shifts the vertical origin without changing the slope and makes the logarithm dimensionless. Slope-only diagrams also use natural-log/reciprocal-Kelvin coordinates, with an explicitly arbitrary vertical offset. Their extra result reports the equivalent natural-log slope in Kelvin.

Read zero, negative and sensitive results

Equal positive rate constants at different temperatures give zero apparent activation energy for that pair. Equal temperatures cannot determine a slope, even if the rate constants also match; the calculator asks for distinct temperatures.

A negative result means the fitted rate constant decreases as temperature rises for the entered pair. It does not, by itself, establish a negative elementary reaction barrier. Check the pairing, units and whether one Arrhenius relationship describes the measurements. IUPAC defines activation energy as an empirical temperature-dependence parameter; this two-point estimate is not a direct measurement of a transition-state energy difference.

When temperatures are very close, small measurement changes can strongly affect the answer. This tool flags pairs less than 1 K apart as a sensitivity prompt, rather than assigning an uncertainty that the supplied data cannot establish. Two points always define a line, so they cannot reveal curvature or a changing reaction mechanism. Additional measurements and an appropriate regression are needed to assess that behavior.

Rates accept scientific notation from 1e-100 to 1e100, with up to 15 significant decimal digits. Temperatures and plot slopes accept up to six decimal places. The six-significant-digit result is a display choice, not a claim about experimental precision. The model does not calculate vacancy-formation energies or supply reaction-specific material data.

Calculation Methodology Documented

Read the formula definitions, supported input ranges, and limitations before using this estimate.

Review Methodology
Debjeet Bhowmick
Author Debjeet Bhowmick AWS Certified Solutions Architect • Cloud & DevOps Consultant

AWS Certified Solutions Architect Professional and Senior Cloud & DevOps Consultant with over 14 years of hands-on expertise architecting resilient cloud infrastructure across AWS, GCP, and Azure. Specializes in infrastructure as code, continuous delivery automation, and telemetry across Terraform, Ansible, Docker, Kubernetes, ELK, Python, and SQL. Creator of OrangeCalc, delivering client-side high-precision computational tools.