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Background Radiaon
Naturally occurring radiaon is always present, it includes high energy gamma rays and parcles from the sun
and outer space and alpha, beta, and gamma radiaon emied from elements in the earth.
CPM (counts per minute)
The unit of measurement usually used to measure alpha and beta radiaon.
Ion
An atomic parcle, atom, or molecule that has acquired an electrical charge, either posive or negave, by
gaining or losing electrons.
Ionizaon
The process by which neutral atoms of molecules are divided into pairs of oppositely charged parcles known
as ions.
Ionizing Radiaon
Radiaon capable of producing ionizaon by breaking up atoms or molecules into charged parcles called ions.
Radiaon
The emission and propagaon of energy through space or through maer in the form of parcles or waves.
Radionuclide
The naturally occurring or arcially produced radioacve form of an element.
Decay
When an atom emits an alpha or beta parcle or a gamma ray, it becomes a dierent type of atom. Radioacve
substances may go through several stages of decay before they change into a stable, or non-ionizing, form. For
example; U-238 has 14 dierent stages of decay before it stabilizes. An element may have several forms, or
isotopes. A radioacve isotope of an element may be called a radioisotope. However, the more correct term is
radionuclide.
Half-life
Each radionuclide has a characterisc half-life, which is the me required for half of a quanty of the material
to decay.
Chapter 12: Glossary of Common Terms
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