Inhibited reflection in uniaxial crystals

When an ordinary or extraordinary ray that propagates through a birefringent crystal is reflected it gives rise to two reflected rays whose directions may be calculated with formulas similar to Snell's law for refraction. When the reflection angle is greater than the incidence angle there is a...

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Autores principales: Simon, M.C., Echarri, R.M.
Formato: JOUR
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_01469592_v14_n5_p257_Simon
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spelling todo:paper_01469592_v14_n5_p257_Simon2023-10-03T15:00:16Z Inhibited reflection in uniaxial crystals Simon, M.C. Echarri, R.M. When an ordinary or extraordinary ray that propagates through a birefringent crystal is reflected it gives rise to two reflected rays whose directions may be calculated with formulas similar to Snell's law for refraction. When the reflection angle is greater than the incidence angle there is a critical angle for which the reflected ray is grazing, and for values of the incidence angle greater than this critical value the reflected ray no longer exists. We call this phenomenon inhibited reflection. We show how the critical angles may be calculated, and an experiment that visualizes the phenomenon shows good agreement with theory. © 1989 Optical Society of America. Fil:Simon, M.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Echarri, R.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_01469592_v14_n5_p257_Simon
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
description When an ordinary or extraordinary ray that propagates through a birefringent crystal is reflected it gives rise to two reflected rays whose directions may be calculated with formulas similar to Snell's law for refraction. When the reflection angle is greater than the incidence angle there is a critical angle for which the reflected ray is grazing, and for values of the incidence angle greater than this critical value the reflected ray no longer exists. We call this phenomenon inhibited reflection. We show how the critical angles may be calculated, and an experiment that visualizes the phenomenon shows good agreement with theory. © 1989 Optical Society of America.
format JOUR
author Simon, M.C.
Echarri, R.M.
spellingShingle Simon, M.C.
Echarri, R.M.
Inhibited reflection in uniaxial crystals
author_facet Simon, M.C.
Echarri, R.M.
author_sort Simon, M.C.
title Inhibited reflection in uniaxial crystals
title_short Inhibited reflection in uniaxial crystals
title_full Inhibited reflection in uniaxial crystals
title_fullStr Inhibited reflection in uniaxial crystals
title_full_unstemmed Inhibited reflection in uniaxial crystals
title_sort inhibited reflection in uniaxial crystals
url http://hdl.handle.net/20.500.12110/paper_01469592_v14_n5_p257_Simon
work_keys_str_mv AT simonmc inhibitedreflectioninuniaxialcrystals
AT echarrirm inhibitedreflectioninuniaxialcrystals
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