Becke Lines and Index of Refraction in a Uniaxial Crystal

Goal: To find the indices of refraction, ω and ε, of an unknown uniaxial mineral using oils with known indices of refraction by using the Becke Line method.

Materials:

Procedure:

Results: I had mineral grain sample UA. Five oils were tried. The first one, with an index of refraction equal to 1.502, had Becke line movement into the grain, so I tried a few more oils with higher indices of refraction. The oils with indices of refraction equal to 1.504, 1.550, and 1.578 all resulted in the Becke line going into the grain. The next oil had an index of refraction equal to 1.580 and I did not see a Becke line, so 1.580 is the value of ω.

Table 1 - Oils used in order to find ω
no Becke line
1.502 Into grain
1.504 Into grain
1.550 Into grain
1.578 Into grain
1.580 No Becke line

Then, while still in the oil with an index of refraction equal to 1.580, I found a grain that went extinct four times with a 360° stage rotation and made sure it was not oriented along the ω axis. The Becke line moved into the oil meaning that the mineral grain is optically negative and that the value of ε must be less than the value of ω.

I used six oils in order to find the value of ε. They all resulted in the Becke line going into the oil, so I kept trying oils with lower indices of refraction. I finally tried the oil with an index of refraction equal to 1.540 and no Becke line appeared, so that is my value for ε.

Table 2 - Oils used in order to find ε
no Becke line
1.578 Into oil
1.576 Into oil
1.570 Into oil
1.566 Into oil
1.560 Into oil
1.540 No Becke line

Conclusion: Becke lines appear because of refraction at the lens-like edge of a grain. If the grain has an index of refraction lower than the oil, the grain will act like a diverging lens and the Becke line will go into the oil. If the grain has an index of refraction higher than the oil, the grain will act like a converging lens and the Becke line will move into the grain. If the grain and the oil have the same index of refraction, then the light will not be refracted and a Becke line will not appear. If the mineral is anisotropic, there will be more than one index of refraction depending on the vibration direction of light in the crystal.

The UA mineral grain sample and the oil with an index of refraction equal to 1.580 did not create a Becke line along the ω axis, so ω is equal to 1.580. I observed that grains in the ω oil that were oriented along the ε axis had their Becke lines move into the oil, so the mineral is optically negative. The oil which produced no Becke line along the ε axis had an index of refraction equal to 1.540. Using these values for ω and ε, I determined that the sample is Mizzonite.

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