To determine the correct range for the absolute refractive index of minerals, let's analyze the optical properties of minerals:
1. Definition of Absolute Refractive Index:
The absolute refractive index (n) of a mineral is defined as:
n = (speed of light in vacuum or air) / (speed of light in the mineral)
2. Typical Ranges for Minerals:
Most rock-forming minerals have refractive indices between:
The vast majority fall in the 1.3 to 2.0 range.
3. Why Other Ranges Are Incorrect:
- 1-1.2: Too low (only gases approach n=1)
- 2-3: Too high (only rare minerals exceed 2.0)
- 3-4.5: Impossible for natural minerals
4. Common Examples:
- Quartz: 1.544-1.553
- Calcite: 1.486-1.658
- Olivine: 1.63-1.87
Final Answer:
The correct range is 1.3 and 2.