Fluorescence of certain rocks and other substances had been observed for many years before its nature was understood. The British scientist George Stokes coined the term when he discovered, in 1852, that the mineral fluorite (fluorspar) emitted red light when it was illuminated by ultraviolet radiation. He formulated what became known as Stokes's law, which states that the wavelength of the fluorescent light is always greater than that of the exciting radiation (though exceptions to this law were subsequently found). Later it was discovered that certain organic and inorganic substances can be made to fluoresce by activation not only with ultraviolet light but also with visible light, infrared radiation, X-rays, radio waves, cathode rays (streams of electrons), friction, and pressure.
Fluorescence is now explained in terms of electrons inside certain molecules, having been raised to allowed higher energy levels, falling in two or more steps to their original states with the emission of light at specific wavelengths.
Related categories OPTICS AND OPTICAL PHENOMENA
ATOMIC AND NUCLEAR PHYSICS
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