Conoscopic light microscopy

Conoscopic light microscopy is performed as a complement to the orthoscopic light method to characterize birefringent materials on thin slides with parallel faces, because knowing the neutral axis orientations and path difference numerical values between both related polarized rays would not be sufficient to identify materials without any uncertainty. This method consists in illuminating a uniform region of the specimen with a cone-shaped polarized light (so-called conoscopy) and then in observing through an analyzer the interferences said to be “in convergent light” which are formed at infinity or at the focus of the objective [ Born 1999[1]]. For practical purposes, the cone-shaped light beam should be made by Köhler illumination with a very open aperture diaphragm; the field diaphragm should be closed enough to limit the illumination to the chosen region in the middle of the field. The interferences figure in convergent light will appear on the image focus of the objective of the microscope. Observing the interferences figure through the eyepiece of the microscope requires adding a convergent objective, called “Bertrand lens”, to the body of the microscope, which will project the interferences figure at infinity (Figure 4). It is important to highlight that this method does not give an image of the preparation but a complex figure (Figure 5cd) which will permit the characterization of birefringent properties of the specimen's uniform region which had been chosen with orthoscopic illumination.

Rappel

On microscopes without removable BERTRAND lens, it is often possible to make that observation using an auxiliar viewfinder (in order to adjust phase contrast) which would be inserted in place of the eyepiece, but then you could not use the camera exit or the microscope.

Complément

The figures c and d are typical of a biaxial crystal, a property that we could not determine on the images a and b with orthoscopic light. (On the figures c and d, the center of the image corresponds to a light beam which is the normal to the preparation and the edges correspond to a beam inclined by \(\arcsin (0.75)\) \(\approx 49^{\circ}\) in the air where \(0.75\) is the numerical aperture of the \(40 \times\) objective.

Remarque

Because birefringent crystals optic axes can be oriented in any direction to the microscope axis, it could be useful to work with theodolite stages which allow adjusting in any directions the normal to the preparation which has to be inserted between two half-spheres of glass. See, for instance, the reference [ Roblin 99[2]] or the article http://www.zeiss.com/C1256D18002CC306/0/F2BA0A81B5929487C1256D59003351AA/$file/46-0014_e.pdf and geology units and experiments about rock identification with polarized light microscopes to learn more about the topic.