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Radioactivity

Background Radiation.

Radioactive nuclei (the source of radioactivity) are all around us.
They are found naturally in the air, the ground and the sea.
Everything living (and food) is also radioactive.
Radiation also comes from space.
Some comes from the Sun,
some comes from all directions as gamma ray bursts.

All of this radioactivity is called the background radiation.
The level of this radiation (called the background count) is low.
If you switch on a Geiger counter it will detect this background radiation
and give a reading for the level.

The reading is not constant but keeps going up and down.
This is because radioactive decay is a random process
(remember this phrase, it will be useful in the exams).
A random process means that you don't know when the decay will happen.
On average, the background count might be 0·4 Bq.
At any one time, the background count might be 0, 1, 2 or 3 Bq.
To get an accurate reading for the background count
(or other radioactive source)
you need to calculate the average value of a large number of readings
which have been taken over a long period of time.
The background count is different in different parts of the country.
It is affected by the release of radioactive radon from rocks (granite).

When a Bq value for a radioactive material is given,
the background count is subtracted first.
Otherwise the value would represent the radioactive source
plus the background count.
This is particularly important if the source is a weak emitter of radioactivity,
where the background count might be a significant amount of the total reading.

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