Experiments with quartz hexagon

Double parhelia


Quartz hexagon quartz hexagon

During August 1993 and January 1999, I performed experiments with a polished slice from a hexagonal quartz crystal (approx 3cm in diameter and 8mm thick) to show, by analogy, the formation of the mock suns (parhelia or sundogs). Water ice is birefringent with only a small difference in refractive index between the O- and E-rays. Quartz, however, has a birefringence of +0.009 which is sufficient to produce double parhelia whose different positions can be seen easily by rotating a polaroid when viewing them on a screen.


Quartz crystal drawing quartz crystal lightpaths

This shows a sketch of the light path through the quartz hexagon. With a white light source the projected spectrum is desaturated in the middle due to the birefringence. A polaroid oriented perpendicular or parallel to the dispersion direction isolates each of the spectra in turn.


Quartz spectra quartz double spectra

Illumination of the crystal with white light produces this double spectrum which can be split with a polaroid.


Laser illumination quartz double spectra

Illumination with a laser produces a double spot (actually a double line in this picture because of optical imperfections in the polishing of the crystal). This composite picture shows the doubled image with and without a polaroid.


Is it possible to see this effect in a real mock sun produced by ice hexagons?


Last update: 4 April 1999
rfosbury@eso.org

Go to Bob Fosbury's homepage