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| Radioluminescence ： ウィキペディア英語版 |
Radioluminescence
Radioluminescence is the phenomenon by which light is produced in a material by bombardment with ionizing radiation such as beta particles. Radioluminescence is used as a low level light source for night illumination of instruments or signage or other applications where light must be produced for long periods without external energy sources. Radioluminescent paint used to be used for clock hands and instrument dials, enabling them to be read in the dark. Radioluminescence is also sometimes seen around high-power radiation sources, such as nuclear reactors and radioisotopes.
==Mechanism==
Radioluminescence occurs when an incoming radiation particle collides with an atom or molecule, exciting an orbital electron to a higher energy level. The particle usually comes from the radioactive decay of an atom of a radioisotope, an isotope of an element which is radioactive. The electron then returns to its ground energy level by emitting the extra energy as a photon of light. The emitted photon is often in the ultraviolet energy range or higher and so invisible to the human eye. Therefore, in radioluminescent light sources, the radioactive substance is mixed with a phosphor, a chemical that releases light of a particular color when struck by the particle.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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