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Birefringence
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{{short description|Refractive property of materials}} [[File:Crystal on graph paper.jpg|right|thumb|A [[calcite]] crystal laid upon a graph paper with blue lines showing the double refraction]] [[File:Positively birefringent material.svg|right|thumb|In this example, optic axis along the surface is shown perpendicular to plane of incidence. Incoming light in the {{mvar|s}} polarization (which means perpendicular to plane of incidence – and so in this example becomes "parallel polarisation" to optic axis, thus is called extraordinary ray) sees a greater [[refractive index]] than light in the {{mvar|p}} polarization (which becomes ordinary ray because "perpendicular polarisation" to optic axis) and so {{mvar|s}} polarization ray is undergoing greater [[Snell's law|refraction]] on entering and exiting the crystal.]] '''Birefringence''', also called '''double refraction''', is the [[optical properties|optical property]] of a material having a [[refractive index]] that depends on the [[polarization (waves)|polarization]] and propagation direction of [[light]].<ref>{{cite web |url=https://olympus-lifescience.com/en/microscope-resource/primer/lightandcolor/birefringence |title=Olympus Microscopy Resource Center |publisher=Olympus Life Science Inc. |last1=Abramowitz |first1=Mortimer |last2=Davidson |first2=Michael W. |access-date=2021-07-21 }}</ref> These optically [[anisotropic]] materials are described as '''birefringent''' or '''birefractive'''. The birefringence is often quantified as the maximum difference between refractive indices exhibited by the material. [[Crystal]]s with non-cubic [[crystal structure]]s are often birefringent, as are [[plastic]]s under [[mechanical stress]]. Birefringence is responsible for the [[optical phenomenon|phenomenon]] of '''double refraction''' whereby a [[ray (optics)|ray]] of light, when incident upon a birefringent material, is split by polarization into two rays taking slightly different paths. This effect was first described by Danish scientist [[Rasmus Bartholin]] in 1669, who observed it<ref>See: * Erasmus Bartholin, [https://books.google.com/books?id=F7RAAAAAcAAJ&pg=PP11 ''Experimenta crystalli islandici disdiaclastici quibus mira & infolita refractio detegitur''] [Experiments on birefringent Icelandic crystal through which is detected a remarkable and unique refraction] (Copenhagen, Denmark: Daniel Paulli, 1669). * Erasmus Bartholin (January 16, 1671) [https://books.google.com/books?id=Zl5FAAAAcAAJ&pg=PA2141 "An account of sundry experiments made and communicated by that learn'd mathematician, Dr. Erasmus Bartholin, upon a chrystal-like body, sent to him out of Island,"] ''Philosophical Transactions of the Royal Society of London'', '''5''' : 2041–2048 (pdf pp 282–289).</ref> in [[Iceland spar]] ([[calcite]]) crystals which have one of the strongest birefringences. In the 19th century [[Augustin-Jean Fresnel]] described the phenomenon in terms of polarization, understanding light as a wave with field components in transverse polarization (perpendicular to the direction of the wave vector).<ref name=fresnel-1821a>A. Fresnel, "Note sur le calcul des teintes que la polarisation développe dans les lames cristallisées" et seq., ''Annales de Chimie et de Physique'', Ser. 2, vol. 17, pp. 102–111 (May 1821), 167–96 (June 1821), 312–15 ("Postscript", July 1821); reprinted (with added section nos.) in Fresnel, 1866–70, vol. 1, pp. 609–648; translated as "On the calculation of the tints that polarization develops in crystalline plates, & postscript", {{Zenodo|4058004}} (Creative Commons), 2021; §14.</ref><ref name=fresnel-1822-25>A. Fresnel, "Extrait d'un Mémoire sur la double réfraction", ''Annales de Chimie et de Physique'', Ser. 2, vol. 28, pp. 263–279 (March 1825); reprinted as "Extrait du second Mémoire sur la double réfraction" in Fresnel, 1866–70, vol. 2, pp. 465–478; translated as "Extract of a [second] memoir on double refraction", {{Zenodo|5442206}}, 2021 (open access).</ref>
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