Fe2SiO4 (fayalite) is an iron silicate ceramic belonging to the olivine family of mineral phases. It forms naturally as a constituent in iron-rich rocks and is of primary interest in high-temperature materials science and metallurgical slag systems, where it contributes to melt behavior and refractory performance. The material is notable for its thermal stability and presence in ironmaking byproducts, making it relevant to process optimization rather than as a primary structural ceramic in most engineering applications.
Compliance & Regulations
| Property | Value | Unit | Conditions | Source | |
|---|---|---|---|---|---|
Density(ρ) | 4.438 | kg/m³ | — |
| Property | Value | Unit | Conditions | Source | |
|---|---|---|---|---|---|
Band Gap(Eg) | 0.000 | eV | — | ||
Seebeck Coefficient(S) | -15.07 | µV/K | — |
| Property | Value | Unit | Conditions | Source | |
|---|---|---|---|---|---|
Energy Above Hull(ΔEhull) | 0.1528 | eV/atom | — | ||
Formation Energy(ΔHf)2 entries | -2.178 | eV/atom | — | ||
| ↳ | -1.781 | eV/atom | — |