Revision notes · Atomic structure
Atoms and nuclear radiation
Radioactive decay and nuclear radiation4.4.2.1
Activity is the rate at which a radioactive source decays, measured in becquerels (Bq) — 1 Bq is one decay per second. Count-rate is the number of decays detected per second by a detector (such as a Geiger-Müller tube), which is usually lower than the true activity because a detector doesn't pick up every decay.
| Radiation | What it is | Ionising power | Penetration (range in air) |
|---|---|---|---|
| Alpha (α) | 2 protons + 2 neutrons (a helium nucleus) | Strongly ionising | Weakly penetrating — absorbed by a few cm of air or a sheet of paper |
| Beta (β) | A fast-moving electron ejected from the nucleus | Moderately ionising | Moderately penetrating — travels ~1 m in air, absorbed by a few mm of aluminium |
| Gamma (γ) | Electromagnetic radiation from the nucleus | Weakly ionising | Strongly penetrating — absorbed only by many cm of lead or metres of concrete |
Some unstable nuclei also decay by directly emitting a neutron.
Nuclear equations4.4.2.2
A nuclear equation shows the mass number and atomic number of the nucleus before and after a decay, and must balance on both sides: total mass number and total atomic number are conserved.
| Decay | Effect on the nucleus | Example |
|---|---|---|
| Alpha (α) | Mass number decreases by 4, atomic number decreases by 2 — an alpha particle (⁴₂He) is emitted | ²²⁶₈₈Ra → ²²²₈₆Rn + ⁴₂He |
| Beta (β) | Mass number unchanged, atomic number increases by 1 — a neutron turns into a proton and an electron (⁰₋₁e) is emitted | ¹⁴₆C → ¹⁴₇N + ⁰₋₁e |
| Gamma (γ) | No change to mass number or atomic number — the nucleus loses energy only | no change to the nucleus's composition |
Half-lives and the random nature of radioactive decay4.4.2.3
Radioactive decay is random at the level of an individual nucleus, but with a very large number of nuclei the overall activity follows a predictable pattern — this is why half-life is a useful, reliable measure even though decay itself is unpredictable.
- 1Example: a sample starts with an activity of 80 Bq.
- 2After one half-life, the activity has halved to 40 Bq.
- 3After a second half-life, it has halved again to 20 Bq.
- 4If this drop from 80 Bq to 20 Bq took 10 minutes (two half-lives), the half-life is 10 ÷ 2 = 5 minutes.
This trade-off is why americium-241 (half-life 432 years, an alpha emitter) is used in household smoke alarms: its weakly-penetrating alpha radiation ionises the air inside a small chamber, allowing a tiny electric current to flow. Smoke entering the chamber absorbs the alpha radiation, reducing the ionisation and the current — this drop triggers the alarm. Its long half-life means the source doesn't need replacing for decades, and its low activity keeps continuous exposure safe.
Radioactive contamination4.4.2.4
| Contamination | Irradiation | |
|---|---|---|
| What happens | Unwanted radioactive atoms get onto or into an object or person | Exposure to radiation from a source outside the body, without the source touching it |
| Does the object/person become radioactive? | Yes — the contaminating material itself keeps emitting radiation | No — once removed from the source, exposure stops |
| Duration of hazard | Long-lasting, until the contaminating material is removed or decays away | Only while exposed to the source |
Because radiation hazards affect public health and safety, findings from research into radiation risks must go through peer review before publication — this lets other scientists check the methods and conclusions are sound before the results influence safety guidance.
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