Techniques of Optical Crystallography (Optical Mineralogy)
Identification of crystalline materials with the polarized light microscope is of importance for those working in forensics, soil science, pharmaceuticals, environmental analyses, pigment analysis, and earth sciences. This class introduces the student to a range of methods used for the identification of crystalline materials. A number of techniques are employed or demonstrated, including immersion methods, crystal rotation methods and the use of rotating compensators. Optical properties of both isotropic and anisotropic comminuted mineral samples are used as examples throughout the course.
— Daniel E. Kile
- Crystal systems and symmetry; review of Miller indices
- Properties of light and polarized light; dispersion
- Refraction and Snell’s law; velocity vs. refraction; relief
- Isotropic and anisotropic substances, and the relation of crystal symmetry to optical properties; calcite experiment
- Anisotropic optics: Extinction, retardation, phase interference phenomena, birefringence, and extinction
- The optical indicatrix; isotropic and anisotropic (uniaxial/biaxial)
- The petrographic microscope: components, and adjustment for orthoscopic and conoscopic observation
- Properties observable with the petrographic microscope: twinning, pleochroism, cleavage, birefringence, sign of elongation, extinction angles; relation to crystal symmetry, anomalous interference colors, interference figures
- Formation of interference figures: optic axis, off-center optic axis, Bxa, Bxo, optic normal (flash), random figures; use of angle of entry and exit of hyperbola (AEEH) to diagnose centered figures
- Recognition of interference figures and application to interpretation of crystal orientation in uniaxial and biaxial minerals: optic sign; determination using both a waveplate and a quartz wedge, optic angle (2V) and relation to indices of refraction in biaxial minerals, optic axis dispersion; crossed axial plane dispersion
- Refractometry: identification of crystalline materials using calibrated index liquids and the colored Becke line; cause of Becke line colors
- Properties of the more important rock-forming and accessory minerals in thin section: Silica-group minerals; polymorphs of SiO2, feldspar minerals; K-spar and plagioclase groups, amphibole- and pyroxene-group minerals, phyllosilicates, carbonates, accessory minerals
Principles, theory, and practice of optical crystallography using polarized light microscopy (PLM) applied to particle and materials characterization and identification.
Everyone with the need for problem solving using optical crystallography and polarized light microscopy, including:
- Materials scientists
- Detailed course manual
- Olympus BX51 microscope with polarized light capabilities for each student
Students are expected to successfully complete a variety of tasks in the form of hands-on exercises, laboratory exercises, identifications of unknowns, and quizzes. In addition, the students are required to have 100% attendance during the course, participate in class, complete a student evaluation form and pre- and post-course assessment forms.
The student is notified at the end of the course whether or not they have successfully completed the requirements of the course based on:
- 100% Attendance
- Class participation
- Completion of all course material
- Completed and signed student evaluation form
Upon successfully meeting these requirements, a student is awarded a certificate of completion and CEU credits, if available. Those who have not successfully passed the course requirements do not receive a certificate or CEU credits.