In discussing calcite, we pointed out that its large birefringence arises from the fact that the carbonate
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In discussing calcite, we pointed out that its large birefringence arises from the fact that the carbonate groups lie in parallel planes (normal to the optic axis). Show in a sketch and explain why the polarization of the group will be less when vector E is perpendicular to the CO3 plane than when vector E is parallel to it. What does this mean with respect to v⊥ and v||, that is, the wave’s speeds when vector E is linearly polarized perpendicular or parallel to the optic axis?
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