Biaxial Interference Figure - Sucrose (sugar)
                The crystal in this view has been rotated 45 degrees from
                  its darkest position (extinction Position). The optical
                  axes here are in the first and third quadrant though only the one in the third
                  quadrant is visible here.
              
              
                Transmitted Cross Polarized Light, Conoscopic View
                
Definition/Function:
                Many of the sucrose crystals in granulated sugar are in a position that allows an
                optical axis to nearly an acute bisectorix view. The biaxial
                interference figure changes dramatically as the stage is rotated, unlike the uniaxial
                interference figure. In its extiction position the center
                of the field is dominated by a relatively wide dark band. Rotated off of this position
                normally only one of the two isogyres centered on the
                two optic axis are visible.
                Significance in the Environment:
                The interference figure can be used to determine the crystal group that the particle
                belongs to, uniaxial or biaxial, the optical sign of the
                mineral, and the orientation of the key refractive indices of the mineral. In the case
                of a biaxial crystal the Beta refractive index is
                oriented normal to the line conecting the two optic axes. The grain can be oriented and
                the polarizing filter that aligns with the Beta direction
                can be left in and the Beta refractive index can be measured using different refractive
                index oils. With the crystal class (biaxial), the opitcal
                sign (negative in the case of mica), and the Beta refractive index the mineral can be
                search in any tablular reference for mineral identification.
                Another key property of the biaxial minerals is the angle between the two optical axes,
                the 2V angle. As the angle increases the distance
                between the projection of the optical axes increases in the interference figure.
                Muscovite mica has a large 2V angle but biotite mica has a 2V
                angle of only a few degrees. The optical axes are near the egde of the field of view for
                an objective with a numerical apurature of 0.65 for
                muscovite but are near the center of the field of view for biotite.
                Characteristic Features:
                The biaxial interference figure consists of the two melatopes (projection of the optical
                axes), the isogyres,
                and the isochromes (colored bands).
                References: