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| Chemical Component | Typical Content | Description |
|---|---|---|
| SiO2 | 40% - 50% | Main silicate component |
| Al2O3 | 20% - 38% | Main alumina component |
| K2O | 6% - 11% | Typical mica alkali component |
| Fe2O3 | 0.5% - 6% | Varies by mica type and color |
| MgO | 0.5% - 5% | Varies by mica type |
| CaO | < 2% | Minor component |
| Na2O | < 1.5% | Minor alkali component |
| Loss on Ignition | Varies by grade | Depends on mineral type and processing |
The predominant components of mica are Silicon Dioxide (SiO2), making up 40% to 50%, and Aluminum Oxide (Al2O3), accounting for 20% to 38% of its total composition. Together, they form the core aluminosilicate crystal structure.
Fe2O3 ranges between 0.5% and 6% depending directly on the mineral type and geographical source. Higher iron content typically imparts darker coloration to the mica, such as in phlogopite or biotite, compared to low-iron muscovite.
Potassium Oxide (6% - 11%) serves as the typical interlayer alkali cation that binds the tetrahedral-octahedral-tetrahedral (T-O-T) sheets together, which gives mica its characteristic basal cleavage and high dielectric strength.
Minor components include Magnesium Oxide (MgO, 0.5% - 5%), Calcium Oxide (CaO, < 2%), and Sodium Oxide (Na2O, < 1.5%). These variations occur naturally based on the mineral deposit environment.
Loss on Ignition indicates the release of structural hydroxyl (OH) water and volatile elements when heated at elevated temperatures. The exact percentage depends on the specific mineral grade and refining process.
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