5.2 Radioactivity
5.2.1 Detection of radioactivity
Core Content
1. What is background radiation?
Background radiation is the low level of radiation that is always present in our surroundings. It comes from natural and artificial sources.
2. Main sources of background radiation:
Natural Radiation Sources (85%):
- (a) Radon gas (in the air):
A radioactive gas released from rocks underground. It mixes with the air and contributes to about half of the natural background radiation. - (b) Rocks and buildings:
Some rocks contain radioactive materials. These are used in construction, exposing us to small amounts of radiation. - (c) Food and drink:
Plants absorb radioactive materials from the soil, and animals eat these plants. So food and drink contain tiny amounts of radiation. - (d) Cosmic rays (from space):
High-energy radiation from the Sun and outer space. More exposure occurs at higher altitudes (e.g., mountains or flying in airplanes).
Artificial Radiation Sources (15%)
- Medical use (X-rays, cancer treatment) – 14%
- Other sources (nuclear industry, past weapon tests, flying) – 1%

Figure 1: Pie chart showing radiation sources. Total natural radiation = 50% + 14% + 11% + 10% = 85%. Total artificial radiation = 14% + 1% = 15%
3. Measuring radiation
Radiation is measured using a Geiger-Müller (GM) tube connected to a counter.
- The GM tube detects the radiation.
- The counter shows the count rate – how often radiation is detected.
4. Count rate units:
- Count rate is measured in:
counts per second (count/s) or
counts per minute (count/min)
Supplement Content
5. Corrected count rate
When measuring radiation from a radioactive source, we must first measure and subtract the background radiation.
How to correct the count rate:
- Measure the background radiation using the GM tube without the source present.
- Calculate the background count rate:
Background count rate = Total counts / Time (s or min) - Measure the total count rate with the source present.
- Subtract the background count rate to get the corrected count rate.