fluorescence

fluorescence

fluorescence (flo͝orĕsˈəns), luminescence in which light of a visible color is emitted from a substance under stimulation or excitation by light or other forms of electromagnetic radiation or by certain other means. The light is given off only while the stimulation continues; in this the phenomenon differs from phosphorescence, in which light continues to be emitted after the excitation by other radiation has ceased. Fluorescence of certain rocks and other substances had been observed for hundreds of years before its nature was understood. Fluoresecence also occurs in some living organisms; some coral, reef fish, jellyfish, and other marine species as well as such terrestrial plants and animals as certain spiders and pitcher plants fluoresce. Probably the first to explain it was the British scientist Sir George G. Stokes, who named the phenomenon after fluorite, a strongly fluorescent mineral. Stokes is credited with the discovery (1852) that fluorescence can be induced in certain substances by stimulation with ultraviolet light. He formulated Stokes's law, which states that the wavelength of the fluorescent light is always greater than that of the exciting radiation, but exceptions to this law have been 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, friction, heat, pressure, and some other excitants. Fluorescent substances, sometimes also known as phosphors, are used in paints and coatings, but their chief use is in fluorescent lighting.

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Fluorescence

Fluorescence is generally defined as a luminescence emission that is caused by the flow of some form of energy into the emitting body, this emission ceasing abruptly when the exciting energy is shut off. In attempts to make this definition more meaningful it is often stated, somewhat arbitrarily, that the decay time, or afterglow, of the emission must be of the order of the natural lifetime for allowed radiative transitions in an atom or a molecule, which is about 10^-8 s for transitions involving visible light. Perhaps a better distinction between fluorescence and its counterpart, phosphorescence, rests not on the magnitude of the decay time per se, but on the criterion that the fluorescence decay is temperature-independent.

In the literature of organic luminescence, the term fluorescence is used exclusively to denote a luminescence which occurs when a molecule makes an allowed optical transition. Luminescence with a longer exponential decay time, corresponding to an optically forbidden transition, is called phosphorescence, and it has a different special distribution from the fluorescence. See Phosphorescence

The decay time of fluorescent materials varies widely, from the order of 5 × 10^-9 s for many organic crystalline materials up to 2 s for the europium-activated strontium silicate phosphor. Fluorescent materials with decay times between 10^-9 and 10^-7 s are used to detect and measure high-energy radiations, such as x-rays and gamma rays, and high-energy particles such as alpha particles, beta particles, and neutrons. These agents produce light flashes (scintillations) in certain crystalline solids, in solutions of many polynuclear aromatic hydrocarbons, or in plastics impregnated with these hydrocarbons. The so-called fluorescent lamps employ the luminescence of gases and solids in combination to produce visible light. See Luminescence

McGraw-Hill Concise Encyclopedia of Physics. © 2002 by The McGraw-Hill Companies, Inc.

fluorescence

(floo-ŏ-ress -ĕns) The transformation of photons of relatively high energy (i.e. high frequencies, especially ultraviolet frequencies) to lower-energy photons through interactions with atoms. It is also the lower-energy radiation that is produced by the process.

Collins Dictionary of Astronomy © Market House Books Ltd, 2006

The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Fluorescence

 

a luminescence that decays in a time τ ~ 10^–8 –10^–9 sec. The division of luminescence into fluorescence and phosphorescence is out of date, since it is an arbitrary distinction based on a qualitative measurement of the duration of luminescence. In terms of the mechanism for converting the excitation energy into visible emission, fluorescence, as a rule, is spontaneous luminescence; hence τ is determined by the lifetime of an atom in an excited state.

Resonance fluorescence, the frequency of which coincides with the frequency of the exciting radiation, is observed in atomic vapors (seeRESONANCE RADIATION). Molecules may fluoresce in highly rarefied vapors; an increase in the vapor pressure or the addition of foreign impurities may quench the fluorescence. Many organic substances, particularly aromatic compounds, fluoresce in liquid and solid solutions as well as in the crystalline state.

The spectra, polarization, and kinetics of fluorescence are associated with the structure and symmetry of molecules and with the nature of molecular interactions and depend, for example, on the concentration of solutions and the type of excitation. Fluorescence may be used, for example, to study crystal structure and excition processes in crystals (seeSPECTROSCOPY, CRYSTAL), the energy levels of molecules, the structure and interaction of molecules, and the processes by which excitation energy is transferred. Fluorescence is used in luminescence analysis, scintillation counters, and mineralogical research.

The decay time of fluorescence is measured by means of fluorometers.

REFERENCES

See references under .

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Fluorescence

 

of minerals, a luminescence that is excited in minerals by light, X rays, or electrons and that decays rapidly (within 10^–2–10^–1 sec) after the excitation ceases. The rapid decay of the luminescence distinguishes fluorescence from phosphorescence and thermoluminescence. The physical phenomenon of the fluorescence of minerals was first observed in fluorite, from which the term “fluorescence” is derived.

Fluorescence is characteristic of dielectric minerals and semiconductors that are transparent to visible light and to near-ultraviolet and infrared radiation. The fluorescence of minerals is associated with impurities or occasionally with intrinsic ions or complexes; such impurities, ions, or complexes form luminescence centers. Fluorescence is sometimes completely or partially quenched by certain isomorphic impurities, such as ions of bivalent iron.

The fluorescence of minerals is used in luminescence analysis to detect such minerals as scheelite, zircon, apatite, and uranites in mining excavations and to analyze microscopic impurities consisting of rare or dispersed elements, such as uranium or rare earths. It is also used for ore dressing by means of the identification of the useful component—for example, diamonds, fluorspar, or scheelite—on the basis of the component’s luminescence.

REFERENCE

Marfunin, A. S. Spektroskopiia, liuminestsentsiia i radiatsionnye tsentry v mineralakh. Moscow, 1975.

B. S. GOROBETS

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.

fluorescence

[flu̇′res·əns]

(atomic physics)

Emission of electromagnetic radiation that is caused by the flow of some form of energy into the emitting body and which ceases abruptly when the excitation ceases.

Emission of electromagnetic radiation that is caused by the flow of some form of energy into the emitting body and whose decay, when the excitation ceases, is temperature-independent.

(nuclear physics)

Gamma radiation scattered by nuclei which are excited to and radiate from an excited state.

(optics)

bloom

McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.

fluorescence

The emission of visible light from a substance (such as a phosphor) as the result of, and during, the absorption of radiation of shorter wavelengths.

McGraw-Hill Dictionary of Architecture and Construction. Copyright © 2003 by McGraw-Hill Companies, Inc.

fluorescence

1. Physics

a. the emission of light or other radiation from atoms or molecules that are bombarded by particles, such as electrons, or by radiation from a separate source. The bombarding radiation produces excited atoms, molecules, or ions and these emit photons as they fall back to the ground state

b. such an emission of photons that ceases as soon as the bombarding radiation is discontinued

c. such an emission of photons for which the average lifetime of the excited atoms and molecules is less than about 10^--8 seconds

2. the radiation emitted as a result of fluorescence

Collins Discovery Encyclopedia, 1st edition © HarperCollins Publishers 2005

fluorescence

The emission of light from a material when subject to photons of another wavelength. A fluorescent object often emits visible light when it receives ultraviolet light. Fluorescence also occurs in nature; for example, fireflies and certain deep sea fish have fluorescent qualities. See fluorescent bulb.

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