MYP frequently asks you to compare the three types of radiation in a table. Know:
| Radiation | Nature | Charge | Penetration | Ionising ability |
|-----------|--------|--------|-------------|------------------|
| Alpha (α) | Helium nucleus 24He | +2 | Stopped by paper/skin | Highly ionising |
| Beta (β−) | Fast electron −10e | -1 | Stopped by ~3 mm aluminium | Medium |
| Gamma (γ) | EM wave | 0 | Reduced by thick lead/concrete | Low |
Nuclear equations must balance mass number (top) and atomic number (bottom). e.g., 92238U→90234Th+24He.
Always write the full equation, not just the daughter nucleus.
Beta decay: a neutron turns into a proton, so atomic number increases by 1, mass number stays the same.
Gamma emission often accompanies alpha or beta decay – does not change the element.
Half‑life appears in both graphical and numerical form. From a graph showing activity (or count rate) vs time:
Find the time for the activity to halve (e.g., from 800 to 400 counts/s).
Repeat for a second halving to confirm constancy.
Step‑by‑step half‑life problems:
- After 1 half‑life: amount = initial / 2
- After 2 half‑lives: amount = initial / 4, etc.
- Number of half‑lives = total time / half‑life.
Typical question: “A sample has a half‑life of 5 years. How much of a 100 g sample remains after 15 years?” → 15/5 = 3 half‑lives, remaining mass = 100 / 2³ = 12.5 g.
When reading a graph, choose a clear starting point on the curve and show working lines.
The background count rate must sometimes be subtracted before halving.
If asked to ‘explain why a radioactive source is stored in a lead container’, mention penetrating power and ionising risk.
Q1. Which type of radioactive decay emits a helium nucleus?
Q2. Carbon-12 and Carbon-14 are isotopes. What do they have in common?
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