Assuming that the polarizers are crossed to produce a dark field, the polariscope is then described as a circular dark-field polariscope. the polariscope is changing from a dark-field configuration to a light-field configuration. Photoelasticity is a nondestructive, whole-field, . the polariscope must be arranged so as to allow light .. izer always looks dark because half the light striking. A polariscope uses polarized light for gem identification. is at right angles to the vibrational direction of the analyzer, the field between them remains dark. Throughout a ° rotation the stone blinks 4 times, light and dark.

Author: Mutaxe Gogor
Country: Liberia
Language: English (Spanish)
Genre: Finance
Published (Last): 18 March 2009
Pages: 304
PDF File Size: 12.36 Mb
ePub File Size: 14.93 Mb
ISBN: 277-8-91969-816-7
Downloads: 60159
Price: Free* [*Free Regsitration Required]
Uploader: JoJot

This image in uniaxial stones will appear different from the image in biaxial stones, each having its own characteristic pattern. This may look very much like the classical bull’s-eye in facetted stones, especially when the optic axis cuts through small facets. Remember that uniaxial minerals have one optic axis while biaxial gemstones have two optical axes. Dichroscope Return to the Table of Contents.

This will create an addition in color on the Newton Color Scale. When one hovers the wedge back and forth over the image, you will see the isochromes moving away and back.

These directions are the optic axes of the gemstone. This means that the wedge can be used as a quarter wave plate aswell as a full wave plate. View the stone under the polariscope from all sides to find where the gemstone does not blink light and dark on lateral rotation.

It should be noted that this image is an ideal one two isogyres seenwhich is rarely the case. All of the above plates can be very expensive since they are usually designed for petrographical microscopes that require special slots in the microscope.

Luckely one can now buy inexpensive around USD These plates are tradionally made from thin sheets of mica with a retardation of approx. Through a series of calculations, it is shown that this retardation is dependent on the thickness and birefringence of the gemstone.



This also depends on the “numerical aperture” of your microscope. With the aid of a few polarizing sheets one can turn the gemological microscope into a polarizing microscope for less than USD Here the interference pattern has the isogyres in the lower right and upper left, but they could be in the lower left and upperright aswell.

The increasing thickness of the wedge provides for a continues range of retardation between, usually, 0 and nm. The small drops act like tiny conoscopes and when applied correctly, you will have an extra hand free the one that usually holds the conoscope.

Polariscope – The Gemology Project

The best aproach is to turn the stone so it will show maximum curvature. When, for instance, a gemstone would create a retardation of nm, the starting spectrum would be on the boundary of the first order and second order and go from magenta to blue to blue-green to yellow to red. As real quartz wedges are very expensive, small and mainly made for use in petrographical microscope this technique was not practised a lot by gemologists.

Retardation plates as those added minerals are known have a known retardation, and the vibrational directions of the slow and fast rays are known. With the quarter wave inserted dqrk Airy Spirals spiral to the right. We concentrate on the areas just around the melatopes, indicated by the white circle around the melatope in the top right isogyre.

Same image as above, but enlarged and the waveplate removed for better view for illustration purposes only. This knowledge can be useful in gemology as one po,ariscope also add another mineral on top of the gemstone to mimic increased thickness and thus create a shift in colors when viewed ad the conoscope. When you do, rotate it to maximum curvature as seen in the images below. Although these images show perfect computer generated interference patterns, one can easily find the optic sign on a partial image.


The first 3 behaviors should pose no problems for the inexperienced user, but the latter ADR can be misinterpreted darj cause one to think the stone is double refractive. All images below are conoscopic images with the conoscope in place. As a result it will not show the typical bull’s-eye but a combination of the left and right Airy Spirals 4 spirals in total under the conoscope.

Many polariscopes for gemological purposes come with a rather large conoscope that can be swivelled like a gemstone holder. We now insert the simulated quartz wedge over the the stone with the conoscope in place from the most concave dafk of the isogyre towards the most convex side and we need to observe how the isochromes behave.

Ideally, a biaxial gemstone will show both isogyres in one image, but alas that is not always the case.

When the biaxial interference figure is laterally turned, the isogyres detach and transform into hyperboles. In the latter case, the fast ray of the cellophane is in the direction of the roll. When the stone is placed between two polarizing filters a polariscopethe two rays combine at the analyzer and either interfere with each other or cancel each other out, depending upon whether the rays are in phase or out of phase.

This technique works best with magnification as the obtained figures are very small. Luckily this is not too difficult. Some quartz especially amethyst is both right-handed as left-handed due to Brazil twinning. When the slow ray of the gemstone and the fast ray of the added mineral align, the shift will be to the left and will create a subtraction in color.