The given formula is:
\[ \text{KAl}_3\text{Si}_3\text{O}_{10}(\text{F}_{0.5}\text{OH}_x) \]
This represents a mineral where the sum of **fluorine (F−)** and **hydroxyl (OH−)** groups should balance the structural requirement.
The total content of **fluorine (F−)** and **hydroxyl (OH−)** ions must equal 2. Therefore, we have the equation:
\[ \text{F}^{0.5} + \text{OH}^x = 2 \]
Substituting **F− = 0.5**, we get:
\[ 0.5 + \text{OH}^x = 2 \]
Solving for **x**:
\[ \text{OH}^x = 2 - 0.5 = 1.5 \]
Thus, the value of **x** is: 1.5.
| 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 |