Mg2SiO4

Forsterite · Magnesium orthosilicate

Mg2SiO4 is a stable, insulating magnesium silicate mineral that is essential to both planetary geology and the production of high-performance technical ceramics.

MgOSi
Crystal structure of Mg2SiO4
Ground-state structure · Materials Project
Overview

About Forsterite

Mg2SiO4 is a robust, thermodynamically stable magnesium silicate that serves as a fundamental building block in geological and materials science. As a wide-gap insulator, it exhibits excellent dielectric properties and structural integrity under extreme conditions.

Its significance spans from planetary science, where it constitutes a major portion of the upper mantle, to advanced industrial applications. Due to its high structural stability and resistance to thermal degradation, it is a preferred material for specialized ceramic components and refractory linings.

At a glance

Key Properties

Cross-validated computational properties for Forsterite, aggregated across 4 databases.

Band Gap

2.37–4.75 eV
Range across DFT structures

Energy Above Hull

0.000 eV/atom
Best (lowest) across sources

Stability

On hull (stable)
2 DFT sources

Structures

58
4 databases, 14 space groups
Synthesis

Synthesis Routes

Literature-extracted synthesis procedures targeting Mg2SiO4.

Sol Gel
Procedure available · ceder_sol_gel
Sol Gel
Procedure available · ceder_sol_gel
Sol Gel
Procedure available · ceder_sol_gel
Sol Gel
Procedure available · ceder_sol_gel
Sol Gel
Procedure available · ceder_sol_gel
Sol Gel
Procedure available · ceder_sol_gel
Uses

Applications

Where Forsterite is used.

Refractory ceramicsHigh-temperature electrical insulatorsGeophysical research modelsGemstone industry
Reference

Frequently Asked Questions

Common questions about Forsterite, answered from cross-validated data.

What is Mg2SiO4?

Mg2SiO4 is a stable, insulating magnesium silicate mineral that is essential to both planetary geology and the production of high-performance technical ceramics.

More questions
What is Mg2SiO4 used for?
Forsterite (Mg2SiO4) is used in refractory ceramics, high-temperature electrical insulators, geophysical research models, and gemstone industry.
What is the band gap of Mg2SiO4?
Forsterite (Mg2SiO4) has a DFT-computed band gap of 2.37–4.75 eV across 58 reported structures.
Is Mg2SiO4 a metal, semiconductor, or insulator?
With a wide band gap up to 4.75 eV it is an insulator / wide-band-gap material.
Is Mg2SiO4 thermodynamically stable?
Yes — Forsterite (Mg2SiO4) sits on the convex hull (energy above hull 0 eV/atom), i.e. on hull (stable).
How many polymorphs of Mg2SiO4 are known?
58 structures of Mg2SiO4 are reported across 4 databases, spanning 14 distinct space groups.
How is Mg2SiO4 synthesized?
Literature-reported routes for Mg2SiO4 include sol gel, solid state (10 procedures documented).
What elements does Mg2SiO4 contain?
Forsterite (Mg2SiO4) contains Mg, O, and Si (3 elements).
Where does the data for Mg2SiO4 come from?
Mg2SiO4 data is cross-referenced from latticegraph.
Comparison

How It Compares

As a highly stable and well-characterized compound with extensive structural data, Mg2SiO4 serves as the definitive archetype for magnesium-based silicates. It represents the standard for thermodynamic stability within its chemical family, providing a baseline for understanding the phase behavior and insulating properties of related mineral systems.

Data sources & attribution
  • latticegraph — Lattice Graph Materials Intelligence Platform

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