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Nicol Prism

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Nicol prism

A Nicol prism is a type of polarizer, an optical device made from calcite crystal used to produce
and analyse plane polarized light. It is made in such a way that it eliminates one of the rays by
total internal reflection, i.e. the ordinary ray is eliminated and only the extraordinary ray is
transmitted through the prism. It was the first type of polarizing prism, invented in 1828 by
William Nicol (1770–1851) of Edinburgh. It consists of a rhombohedral crystal of Iceland spar (a
variety of calcite) that has been cut at an angle of 68° with respect to the crystal axis, cut again
diagonally, and then rejoined as shown, using a layer of transparent Canada balsam as a glue.[1]

Schematic representation of the propagation of light in a Nicol prism showing the splitting of unpolarized light into
ordinary and extraordinary polarized rays

Unpolarized light ray enters through the left face of the crystal, as shown in the diagram, and is
split into two orthogonally polarized, differently directed rays by the birefringence property of
calcite. The ordinary ray, or o-ray, experiences a refractive index of no = 1.658 in the calcite and
undergoes a total internal reflection at the calcite–glue interface because of its angle of
incidence at the glue layer (refractive index n = 1.550) exceeds the critical angle for the interface.
It passes out the top side of the upper half of the prism with some refraction, as shown. The
extraordinary ray, or e-ray, experiences a lower refractive index (ne = 1.486) in the calcite crystal
and is not totally reflected at the interface because it strikes the interface at a sub-critical angle.
The e-ray merely undergoes a slight refraction, or bending, as it passes through the interface into
the lower half of the prism. It finally leaves the prism as a ray of plane-polarized light, undergoing
another refraction, as it exits the far right side of the prism. The two exiting rays have
polarizations orthogonal (at right angles) to each other, but the lower, or e-ray, is the more
commonly used for further experimentation because it is again traveling in the original
horizontal direction, assuming that the calcite prism angles have been properly cut. The
direction of the upper ray, or o-ray, is quite different from its original direction because it alone
suffers total internal reflection at the glue interface, as well as a final refraction on exit from the
upper side of the prism.

Nicol prisms were once widely used in mineralogical microscopy and polarimetry, and the term
"using crossed Nicols" (abbreviated as XN) is still used to refer to the observing of a sample
placed between orthogonally oriented polarizers. In most instruments, however, Nicol prisms
have been replaced by other types of polarizers such as Polaroid sheets and Glan–Thompson
prisms.

See also

Glan–Foucault prism

Glan–Thompson prism

Nomarski prism

Rochon prism

Sénarmont prism

Wollaston prism

References

1. Greenslade, Thomas B., Jr. "Nicol Prism" (http://physics.kenyon.edu/EarlyApparatus/Polarized_Light/Nic


ol_Prism/Nicol_Prism.html) . Kenyon College. Retrieved 23 January 2014.
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