Chlorophane

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Chlorophane
Fluorite, var. Chlorophane.jpg
General
CategoryHalide mineral
Formula
(repeating unit)
CaF2
Strunz classification3.AB.25
Crystal systemIsometric
Crystal classHexoctahedral (m3m)
H–M symbol: (4/m 3 2/m)
(cF12)
Space groupFm3m (No. 225)
Unit cella = 5.4626 Å; Z = 4
Identification
ColorWhite, reddish pink or red (fluorescence/ phosphorescence in emerald green)
Crystal habitWell-formed coarse sized crystals; also nodular, botryoidal, rarely columnar or fibrous; granular, massive
TwinningCommon on {111}, interpenetrant, flattened
CleavageOctahedral, perfect on {111}, parting on {011}
FractureSubconchoidal to uneven
TenacityBrittle
Mohs scale hardness4 (defining mineral)
LusterVitreous
StreakWhite
Specific gravity3.175–3.184; to 3.56 if high in rare-earth elements
Optical propertiesIsotropic; weak anomalous anisotropism
Refractive index1.433–1.448
Fusibility3
Solubilityslightly water soluble and in hot hydrochloric acid

Chlorophane, also sometimes known as pyroemerald, cobra stone, and pyrosmaragd, is a rare variety of the mineral fluorite with the unusual combined properties of thermoluminescence, thermophosphoresence, triboluminescence, and fluorescence: it will emit light in the visible spectrum when exposed to ultraviolet light, when heated, and when rubbed; if heated, it will continue to emit light for a period of time after a heat source is withdrawn. The small amount of heat generated by being held in the hand has been reported as enough to induce luminiscence, though this may be the result of experimental error.[1] Although chemically very similar to fluorite, chlorophane has several impurities including magnesium, aluminum, manganese, and traces of iron and sodium (none of which occur in fluorite). As of 2013 it was still not known which if any of these impurities imparts to chlorophane the luminescent properties that distinguish it from fluorite.[2] Some samples of chlorophane, particularly those exposed to high temperatures, will only luminesce once or will do so with only weakened intensity over time.[3] A very bright luminescence can be achieved at between 200 °C (392 °F) and 300 °C (572 °F),[4] and mineralogists once believed that it would glow indefinitely at temperatures of just 30 °C (86 °F), meaning that when exposed on the ground in warmer climates, the mineral would glow year-round.[5] This effect, which was reported many times without having been observed, was eventually attributed in part to a combination of both heat and light acting on the mineral.

The unusual properties of chlorophane have been attributed to samarium, terbium, dysprosium, gadolinium, ytterbium, and yttrium; none of these rare earth elements, however, has been consistently found in all chlorophane specimens.[2][6]

References[edit]

  1. ^ Suzanne Bettonville (2013). Rock Roles: Facts, Properties, and Lore of Gemstones. Lulu.com. p. 36. ISBN 978-1-257-03762-9.
  2. ^ a b Jack DeMent (16 April 2013). Handbook of Fluorescent Gems and Minerals - An Exposition and Catalog of the Fluorescent and Phosphorescent Gems and Minerals, Including the Use of Ultraviolet Light in the Earth Sciences. Read Books Limited. p. 64. ISBN 978-1-4733-8276-3.
  3. ^ Charles Palache; Harry Berman; Clifford Frondel (1951). The System of Mineralogy: Of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892. Halides, nitrates, borates, carbonates, sulfates, phosphates, arsenates, tungstates, molybdates, etc. Wiley. p. 29.
  4. ^ The Engineer. Morgan-Grampian (Publishers). 1881. p. 28.
  5. ^ Gustave Le Bon (1908). ... The Evolution of Forces. K. Paul, Trench, Trübner & Company, Limited. p. 249.
  6. ^ The Chemical News and Journal of Physical Science. Griffin, Bohn and Company. 1906. p. 290.