Step 1: Relate Retardation, Thickness, and Birefringence
The retardation ($\Gamma$) is defined by the difference in path length between the two rays (O-ray and E-ray) traveling through the mineral, and is calculated as:
$$\Gamma = t \cdot |n_o - n_e|$$
Where:
$\Gamma$ = Retardation (path difference)
$t$ = Thickness of the mineral (thin section)
$n_o$ = Refractive index of the O-ray (Ordinary ray)
$n_e$ = Refractive index of the E-ray (Extraordinary ray)
Step 2: Standardize Units
Convert the given thickness ($t$) from millimeters ($\text{mm}$) and the retardation ($\Gamma$) from nanometers ($\text{nm}$) to the same unit, meters ($\text{m}$), for consistency:
Thickness: $t = 0.03 \text{ mm} = 0.03 \times 10^{-3} \text{ m}$
Retardation: $\Gamma = 5160 \text{ nm} = 5160 \times 10^{-9} \text{ m}$
Step 3: Calculate Birefringence
Rearrange the retardation formula to solve for birefringence ($|n_o - n_e|$):
$$|n_o - n_e| = \frac{\Gamma}{t}$$
Substitute the standardized values:
$$|n_o - n_e| = \frac{5160 \times 10^{-9} \text{ m}}{0.03 \times 10^{-3} \text{ m}}$$
$$|n_o - n_e| = \frac{5160}{0.03} \times 10^{-6} = 172000 \times 10^{-6}$$
$$|n_o - n_e| = 0.172$$
Step 4: Determine $n_o$
The problem states the mineral is uniaxial negative. For a uniaxial negative mineral, the $\text{O-ray}$ has a greater refractive index than the $\text{E-ray}$ ($n_o > n_e$).
Therefore, the birefringence is calculated as:
$$n_o - n_e = 0.172$$
We are given the refractive index of the E-ray: $n_e = 1.486$.
Solve for $n_o$:
$$n_o = n_e + 0.172$$
$$n_o = 1.486 + 0.172$$
$$n_o = 1.658$$
The value of the refractive index of the O-ray is 1.658.
| Group I | Group II |
| P. Sillimanite | 1. First order |
| Q. Quartz | 2. Second order |
| R. Muscovite | 3. Greater than third order |
| S. Calcite | 4. Third order variegated |
| Group I | Group II |
| P. Bababudan Group | 1. Eastern Dharwar |
| Q. Banded Gneissic Complex-I | 2. Western Dharwar |
| R. Bonai Granite | 3. Aravalli |
| S. Kolar Group | 4. Singhbhum |