The table below shows calculated activities for selected fission products and actinides in irradiated fuel (based on Pickering CANDU fuel irradiated to 7.5 MWd/kg U). Use this to check your understanding of the approximations.
| Isotope | Half-Life | Yield (%) | Activity at Discharge (Bq/kg U) | Activity at 1 yr (Bq/kg U) | Activity at 10 yr (Bq/kg U) | Notes |
|---|---|---|---|---|---|---|
| Kr | 10.76 y | 0.29 | Noble gas; moderate half-life | |||
| Sr | 28.8 y | 5.8 | Long-lived; bone-seeker | |||
| Zr | 64.0 d | 6.5 | ~0 | Short-lived; decays to Nb | ||
| Nb | 35.0 d | --- | ~0 | Daughter of Zr | ||
| I | 8.02 d | 2.9 | ~0 | ~0 | Very short-lived; thyroid hazard | |
| Cs | 2.06 y | --- | Produced by neutron capture on Cs | |||
| Cs | 30.17 y | 6.2 | Long-lived; dominant gamma source | |||
| Ce | 284.9 d | 5.5 | Moderate half-life | |||
| Pu | 24,110 y | --- | Alpha emitter; very long-lived | |||
| Am | 432.2 y | --- | Grows in from Pu decay |
Key observations from this table:
- Short-lived isotopes (I, Zr) dominate the activity at discharge but decay rapidly --- they are essentially gone after 1 year of cooling.
- Medium-lived isotopes (Ce, Cs) decay significantly over 1—10 years but are still present.
- Long-lived isotopes (Sr, Cs) barely decrease over 1 year and remain significant even after 10 years. These dominate the intermediate-term hazard.
- Actinides (Pu, Am) are essentially unchanged over 10 years and dominate the very long-term hazard.
- Am increases after discharge because it is continuously produced by the beta decay of Pu ( = 14.3 y).
Common Mistakes --- Worked Example 3
Mistake How to Avoid It Assuming all activities decrease after shutdown Remember: Am increases because its parent Pu continues to decay Ignoring the difference between fission product and actinide half-lives Fission products: days to ~30 years. Actinides: thousands to millions of years Confusing activity at discharge with activity after cooling Always state the cooling time when quoting an activity value