MgCoSiO4

MgCoSiO4 is a metastable semiconducting silicate compound containing magnesium and cobalt.

CoMgOSi
Crystal structure of MgCoSiO4 (orthorhombic, Pnma (No. 62))
Ground-state structure · Materials Project
Overview

About MgCoSiO4

MgCoSiO4 is a complex silicate material characterized by its semiconducting electronic nature. As a metastable compound, it represents a unique structural configuration that offers intriguing possibilities for materials scientists investigating transition metal-doped silicate frameworks.

Its existence across multiple reported structures highlights its significance in solid-state chemistry. The integration of magnesium and cobalt within the silicate lattice makes it a subject of interest for those studying the influence of cation substitution on electronic and structural stability.

At a glance

Key Properties

Cross-validated computational properties for MgCoSiO4, aggregated across 3 databases.

Band Gap

2.70–2.82 eV
Range across DFT structures · ground state: wide gap

Energy Above Hull

0.000 eV/atom
Best (lowest) across sources

Stability

Stable
3 DFT sources

Structures

6
3 databases, 1 space group
Validation

Cross-Source DFT Agreement

How well independent DFT databases agree on the thermodynamics of MgCoSiO4. Tight agreement means computed properties can be trusted without re-running calculations.

Agreement Score

0.54 / 1.00
Trust tier: low

Hull Spread

0.116 eV
EAH spread across sources

Sources Compared

3
jarvis, materials_project, oqmd

Space Group Consensus

All match
Crystallography

Reported Structures

Lowest-energy structures reported for MgCoSiO4, ranked by energy above hull.

Space GroupCrystal SystemBand Gap (eV)E above hull (eV/atom)E/atom (eV)Density (g/cm³)
——2.700.0000-2.588—
——2.820.0335-2.555—
Pnma (No. 62)orthorhombic2.600.0379-7.4883.85
Pnma (No. 62)orthorhombic0.000.1161-2.324—
Pnma (No. 62)orthorhombic———3.97
Pnma (No. 62)orthorhombic———3.98
Pnma (No. 62)orthorhombic———3.97
Pnma (No. 62)orthorhombic———3.92
Pnma (No. 62)orthorhombic———3.97
Pnma (No. 62)orthorhombic———3.97
Pnma (No. 62)orthorhombic———3.82
Pnma (No. 62)orthorhombic———3.88
Synthesis

Synthesis Routes

Literature-extracted synthesis procedures targeting MgCoSiO4.

Sol Gel
Procedure available · ceder_sol_gel
Solid State
Procedure available · ceder_solid_state
Uses

Applications

Where MgCoSiO4 is used.

Solid-state researchMaterials science explorationFundamental crystallographic studies
Reference

Frequently Asked Questions

Common questions about MgCoSiO4, answered from cross-validated data.

What is MgCoSiO4?

MgCoSiO4 is a metastable semiconducting silicate compound containing magnesium and cobalt.

More questions
What is MgCoSiO4 used for?
MgCoSiO4 is used in solid-state research, materials science exploration, and fundamental crystallographic studies.
What is the band gap of MgCoSiO4?
MgCoSiO4 has a DFT-computed band gap of 2.70–2.82 eV across 6 reported structures. Standard DFT underestimates band gaps, so the measured gap is typically larger.
Is MgCoSiO4 a metal, semiconductor, or insulator?
DFT predicts a band gap of up to 2.82 eV (a semiconductor). Measured gaps are typically larger.
Is MgCoSiO4 thermodynamically stable?
Yes — MgCoSiO4 sits on the convex hull (energy above hull 0 eV/atom), i.e. stable.
What is the crystal structure of MgCoSiO4?
The reference structure of MgCoSiO4 is orthorhombic symmetry, space group Pnma (No. 62).
What is the density of MgCoSiO4?
The computed density of the ground-state structure of MgCoSiO4 is 3.85 g/cm³.
How many polymorphs of MgCoSiO4 are known?
6 structures of MgCoSiO4 are reported across 3 databases, spanning 1 distinct space group.
How is MgCoSiO4 synthesized?
Literature-reported routes for MgCoSiO4 include sol gel, solid state (2 procedures documented).
What elements does MgCoSiO4 contain?
MgCoSiO4 contains Co, Mg, O, and Si (4 elements).
Where does the data for MgCoSiO4 come from?
MgCoSiO4 data is cross-referenced from oqmd, materials_project, jarvis, cod, mpaloe.
Comparison

How It Compares

As a unique silicate phase, MgCoSiO4 occupies a specialized niche within its compound class. While it lacks direct siblings in this specific dataset, its metastable nature distinguishes it from more common, highly stable silicate minerals, positioning it as a candidate for research into non-equilibrium material synthesis.

Data sources & attribution
  • oqmd — Data from the OQMD (oqmd.org). Cite: Saal et al., JOM 65, 1501 (2013); Kirklin et al., npj Comp. Mater. 1, 15010 (2015). (CC-BY-4.0)
  • materials_project — Data from the Materials Project (materialsproject.org). Cite: Jain et al., APL Materials 1, 011002 (2013). (CC-BY-4.0)
  • jarvis — Data from JARVIS (jarvis.nist.gov), NIST. Cite: Choudhary et al., npj Comp. Mater. 6, 173 (2020). (LicenseRef-US-Gov-PD)
  • cod — Data from the Crystallography Open Database (crystallography.net/cod/). Cite: Grazulis et al., J. Appl. Cryst. 42, 726 (2009). (CC0-1.0)
  • mpaloe — Data from MP-ALOE. Cite: Kuner et al., npj Comput. Mater. (2025), doi:10.1038/s41524-025-01834-9.

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