Model radioactive release with clear unit controls. Choose atoms or activity, then set elapsed time. See energy, power, and remaining nuclei instantly here now.
Enter half-life, elapsed time, and energy per decay. Choose atoms or activity for the starting amount. Results appear above this form after submission.
Decay constant: λ = ln(2) / T½, where T½ is the half-life in seconds.
Exponential decay: N(t) = N0 · e−λt.
Number of decays: ΔN = N0 − N(t).
Total energy released: E = ΔN · Edecay · BR.
Activity: A(t) = λ · N(t). Instantaneous power is P(t) = A(t) · Edecay · BR.
These sample values demonstrate typical outputs. Results vary by isotope and energy channel.
| Mode | Half-life | Elapsed time | Start amount | Energy per decay | Total energy (approx.) | Avg power (approx.) |
|---|---|---|---|---|---|---|
| Atoms | 30 day | 10 day | 2.00e20 atoms | 0.66 MeV | ~1.24 MJ | ~1.44 W |
| Activity | 8 day | 24 h | 5.0 MBq | 1.00 MeV | ~0.48 kJ | ~5.6 mW |
| Atoms | 1.0 h | 30 min | 1.00e18 atoms | 2.00 MeV | ~2.2 kJ | ~1.2 W |
Radioactive sources release energy as particles and photons. Estimating this energy supports shielding design, detector planning, thermal loading checks, and safe storage decisions. For many sealed sources, heating is small, but high-activity inventories can create measurable power.
Half-life describes how quickly the number of unstable nuclei decreases. The calculator converts your half-life into seconds, then uses the decay constant λ = ln(2)/T½. This keeps unit handling consistent across seconds, minutes, hours, days, and years.
Activity is the decay rate, measured in becquerels (Bq), where 1 Bq equals 1 decay per second. If you start from activity, the tool computes N0 using N0 = A0/λ. For reference, 1 curie equals 3.7×1010 Bq.
Nuclear energies are often provided in eV, keV, or MeV. The calculator converts to joules using 1 eV = 1.602176634×10−19 J. Enter a Q-value, dominant gamma energy, or another channel energy that matches your study goal.
Some nuclides decay through multiple pathways. If the energy you entered applies only to a fraction of decays, set the branching ratio (BR) between 0 and 1. Total energy becomes E = ΔN·Edecay·BR, which can prevent large overestimates.
Total energy sums all decays from time 0 to time t. Average power divides that energy by elapsed time. The instantaneous power uses activity at time t: P(t) = A(t)·Edecay·BR. This is useful when heat output changes significantly during the interval.
A few watts can warm a small capsule, while milliwatts are typically negligible. Compare results to the thermal capacity of the package and ambient cooling conditions. If you export CSV, you can trend energy and power across multiple time points.
Use consistent energy definitions and verify whether neutrino energy is included. Measured dose rates do not directly equal released energy without transport modeling. Always follow local radiation safety rules and approved handling procedures when working with real sources.
It reports remaining nuclei, activity at time t, decays in the interval, total released energy, average power over the interval, and power at time t. You can export results as CSV or PDF.
Use atoms when you know the inventory from chemistry or production data. Use activity when you have a measured source value. Both paths use the same decay constant and time conversion.
Enter the energy channel you want to track, such as a gamma line or total Q-value. If your dataset lists several lines, use the branching ratio to weight the chosen line appropriately.
Dose rate depends on radiation type, geometry, shielding, distance, and energy absorption. Power here is the released nuclear energy rate, not the absorbed dose in a person or detector.
Run the calculator with different elapsed times and export CSV each time, or copy values into a spreadsheet for time-series plots. Keep half-life, energy per decay, and branching ratio consistent.
The tool returns initial conditions. Total energy becomes zero over the interval, average power is zero, and instantaneous power reflects the initial activity and chosen energy per decay.
No. It models a single radionuclide with exponential decay. For chains or ingrowth, you need Bateman equations or a dedicated decay-chain tool, especially when daughter half-lives are comparable.
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.