Background radiation is the natural ionising radiation that surrounds us at all times. Think of it as the invisible hum of a city that you can’t see but can feel. It comes from sources such as the Earth’s crust, the atmosphere, and even the food we eat.
We can compare it to the “ambient noise” in a quiet room. Just as a calm room has a low level of background chatter, the Earth has a low level of background radiation that is always present.
Scientists use devices called Geiger–Müller counters and scintillation detectors to measure background radiation. These instruments count the number of ionising events that happen in a given time.
For example, a typical background level in a city is about 50–70 CPM. If your detector reads 200 CPM, something extra is contributing to the radiation.
Knowing the background level helps scientists:
| Location | Background CPM |
|---|---|
| Urban area | 50–70 |
| Mountainous region | 70–90 |
| Underground lab | 5–10 |