Radioactivity: counts, count rate and background
Turn counts into a rate, then subtract the background — and expect ±√N scatter.
In Unit 5 you meet radioactivity; in Unit 6 you must handle its measurements correctly. A Geiger–Müller (GM) tube connected to a scaler (which totals counts) or a ratemeter (which shows a rate directly) detects ionising radiation.
From counts to count rate. A scaler records the total number of counts in a fixed time. The count rate is quoted in s⁻¹ (counts per second) or counts per minute. Always divide by the time and state the unit — a bare count is not a rate.
Subtracting the background. Ionising radiation is always present (cosmic rays, rocks, building materials, food). This background is detected even with no source. So you must:
- Record the background count rate with no source present.
- Subtract it from every measured rate: Omitting this step is a systematic error that inflates the source's apparent activity.
Counts are statistical. Radioactive decay is a random process, so successive counts of the same source are not identical. For a count the natural spread is about . So 512, 498, 505 and 507 counts are all consistent (spread of order ) — these are not anomalies. Counting for longer (larger ) reduces the relative scatter, since .
- Count rate = counts ÷ time; state the unit (s⁻¹ or per minute).
- Corrected rate = measured rate − background rate; always measure the background.
- Counts scatter by about ±√N (random decay) — small differences are not anomalies.
- Count for longer (larger N) to reduce the relative statistical scatter.
See the full worked example for practical skills ii - implementation and measurement →