double refraction in calcite crystal pdf

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[ (camera) -236.987 (lens\054) -239.002 (such) -235.988 (as) -237.017 (a) -236.005 (calcite) -237.014 (crystal\054) -239.004 (to) -237.009 (o) 14.9828 (v) 14.9828 (erlap) -236 (tw) 10.0081 (o) -237.014 (shifted) ] TJ /Annots [ ] >> /R113 140 0 R /Group 17 0 R

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/a0 << /R279 242 0 R [ (we) -433.997 (r) 37.0196 (e) 15.0128 (visit) -433.983 (double\055r) 37 (efr) 14.9865 (action) -433.001 (ima) 10.013 (ging) -433.984 (using) -434.016 (a) -434.001 (bir) 36.9914 (efr) 14.9877 (active) ] TJ This process, first reported by Erasmus Bartholinus in 1669, is called double refraction. [ (Calcite) -249.979 (crystal) ] TJ T*

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/R341 266 0 R T* /R315 377 0 R (b) and (c) estimated depth map and restored color image from the input. 1 0 0 -1 0 792 cm /R217 281 0 R /Type /Page Phenomenon of double refraction was explained by Huygens’ for which he extended his principle of secondary wavelets and made the following assumptions. /Parent 1 0 R endstream 96.422 5.812 m

When a beam of unpolarized light enters a birefringent crystal at normal incidence (but not along the optic axis), two light beams emerge.

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Calcite has rhombohedral cleavage which means it breaks into blocks with parallelogram - shaped faces. /R198 276 0 R �,[�i��+U}��^��6U�����;n��h�%��!ۿ�=6�PbaB� K DJȔ���Q�Q���N��� �� T�1 �\�$��K)H�WZ��n�"x�$BiHql|J$��D2-����ׇ�lT���l��-J����A�� o. /R127 156 0 R /R138 176 0 R /R311 381 0 R

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If a clear rhombic cleavage block is placed over a point and observed from the top, two images of the point are seen through the calcite crystal. 1 0 0 1 0 0 cm T*

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>> BT Our algorithm provides both sparse depth and clear RGB image within 34ms. [ (e) 15.0128 (ver) 110.999 (\054) -251.995 (e) 19.9924 (xi) 0.98329 (sting) -252.006 (double\055r) 37 (efr) 14.9865 (action) -250.992 (methods) -250.99 (ar) 36.9865 (e) -250.983 (or) 36.9865 (der) 10.0057 (s) -251.012 (of) -251.985 (ma) 10.0057 (g\055) ] TJ /Rotate 0 /R64 112 0 R 95.863 15.016 l f

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Therefore, the phenomenon of

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Light passing through a calcite crystal is split into two rays by refraction.

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/R208 307 0 R Geometry of Calcite Crystal • Double refraction is an optical property in which a single ray of unpolarised light when passes through a uniaxial crystal gets split into two refracted rays, each propagating in a different direction.

Rotate the crystal. The convention is to make the incident beam with arbitrary; this determines the size of the sections of the wave surfaces. /R225 363 0 R

The best-known birefringent crystal is the mineral calcite (Iceland spar), the colorless, transparent rhombohedral salt calcium carbonate, .The optical axis coincides with the three-fold axes of the equilateral groups, along which the ions are also situated. 15 0 obj /Parent 1 0 R /Parent 1 0 R /R303 368 0 R /R233 343 0 R

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<>/Font<>/XObject<>/ProcSet[/PDF/Text/ImageB/ImageC/ImageI] >>/MediaBox[ 0 0 595.32 841.92] /Contents 4 0 R/Group<>/Tabs/S/StructParents 0>> -11.9547 -11.9551 Td 68.543 0 Td /Resources << [ (guity) -206.995 (and) -208 (runtime) -206.995 (restrictions) -208.009 (of) -206.985 (double\055refraction) -207.985 (methods\056) ] TJ /R249 226 0 R

[ (ing) 14.995 (\056) -289.988 (Instead) -191.986 (of) -191.015 (learning) -190.991 (depth) -191.009 (fr) 44.9864 (om) -191.02 (single\055ima) 9.99588 (g) 10.0032 (e) -190.993 (depth) -191.99 (cues\054) ] TJ Lecture Notes - Optics 3: Double Refraction, Polarized Light • Experiment: observations with optical calcite. 5 0 obj Get permission to re-use this article. [ (to) -330.011 (the) -330.996 (bir) 36.9926 (efr) 14.9871 (active) -330.017 (medium\056) -550.985 (Doing) -329.999 (so) -330.993 (mak) 10 (es) -329.982 (it) -330.009 (possible) -331.006 (to) ] TJ /R259 386 0 R �Z��b�z@�N�ʼ���q���i��o��e5��%l�mh�l��M��ʦ!���>��#�9?

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/R89 69 0 R /R368 224 0 R Calcite is 'birefringent' or 'double refracting'. 23.2641 0 Td

/R52 131 0 R >> Physics Education, Volume 7, Number 7.

birefringence; any direction not perpendicular to the optic axis is called . [ (to) -279 (obtain) -278.988 (depth\054) -286.991 (which) -278.998 (prohibits) -279.007 (their) -279.002 (use) -279.007 (in) -280.022 (dynamic) ] TJ /R317 379 0 R 4.73203 -4.33789 Td

(KAIST) Tj Double refraction When light enters the optical axis of anisotropic crystals, it behaves in a manner similar to the interaction with isotropic crystals, and passes through at a single velocity.

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