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| Chemical Component | Typical Content | Description |
|---|---|---|
| SiO2 | 35% - 45% | Main silicate component |
| Al2O3 | 10% - 18% | Aluminosilicate component |
| Fe2O3 + FeO | 12% - 28% | Contributes dark color |
| MgO | 8% - 18% | Typical biotite component |
| K2O | 6% - 10% | Interlayer potassium component |
| CaO | 0.5% - 3% | Minor component |
| TiO2 | 0.5% - 3% | Trace or minor component |
| Loss on Ignition | 1% - 5% | Depends on ore source |
Silicon Dioxide (SiO2) is the dominant constituent, ranging between 35% and 45%, providing the fundamental structural framework as the main silicate component.
The coloration is primarily attributed to the significant concentration of Iron Oxides (Fe2O3 + FeO), which make up 12% to 28% of the total composition.
Potassium Oxide (K2O) accounts for 6% to 10% and serves as the interlayer potassium component within the layered aluminosilicate mineral structure.
Calcium Oxide (CaO) and Titanium Dioxide (TiO2) constitute the minor and trace components, each typically occurring in quantities between 0.5% and 3%.
The Loss on Ignition (1% - 5%) reflects the percentage of volatile substances released during high-temperature heating, which varies depending on the specific ore source.
With a concentration ranging from 8% to 18%, Magnesium Oxide (MgO) represents a quintessential biotite component, contributing to its chemical stability and structural classification.
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