FeAsO4

Scorodite · Ferric arsenate

FeAsO4 is a stable, semiconducting iron arsenate oxide utilized in the research and development of oxygen-evolution catalysts.

Crystal structure of FeAsO4 (orthorhombic, Imma (No. 74))
Ground-state structure · Materials Project
Overview

About Scorodite

FeAsO4 is a thermodynamically stable semiconducting oxide that plays a significant role in the study of oxygen-evolution catalysts. Its robust structural framework and electronic properties make it a subject of interest for researchers investigating efficient catalytic pathways in electrochemical environments.

With numerous reported structures, this compound serves as a critical material for understanding transition metal arsenates. Its stability on the convex hull suggests a reliable foundation for experimental applications in energy conversion and catalysis, where structural integrity is paramount for long-term performance.

At a glance

Key Properties

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

Band Gap

0.57–2.63 eV
Range across DFT structures · ground state: narrow gap

Energy Above Hull

0.000 eV/atom
Best (lowest) across sources

Stability

Stable
3 DFT sources

Structures

14
3 databases, 4 space groups
Validation

Cross-Source DFT Agreement

How well independent DFT databases agree on the thermodynamics of FeAsO4. Tight agreement means computed properties can be trusted without re-running calculations.

Agreement Score

0.75 / 1.00
Trust tier: medium

Hull Spread

0.062 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 FeAsO4, ranked by energy above hull.

Space GroupCrystal SystemBand Gap (eV)E above hull (eV/atom)E/atom (eV)Density (g/cm³)
——2.130.0000-1.564—
P21/c (No. 14)monoclinic1.560.0000-7.1884.30
——2.020.0005-1.563—
——1.810.0020-1.562—
Imma (No. 74)orthorhombic2.080.0221-7.1664.04
——2.630.0496-1.514—
P21/c (No. 14)monoclinic0.570.0619-1.239—
——1.810.0817-1.482—
——1.860.1133-1.450—
I-4 (No. 82)tetragonal0.000.3379-0.963—
P21/c (No. 14)monoclinic———4.45
R-3m (No. 166)trigonal———5.64
Uses

Applications

Where Scorodite is used.

Oxygen-evolution catalysisElectrochemical researchMaterials science studies
Reference

Frequently Asked Questions

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

What is FeAsO4?

FeAsO4 is a stable, semiconducting iron arsenate oxide utilized in the research and development of oxygen-evolution catalysts.

More questions
What is FeAsO4 used for?
Scorodite (FeAsO4) is used in oxygen-evolution catalysis, electrochemical research, and materials science studies.
What is the band gap of FeAsO4?
Scorodite (FeAsO4) has a DFT-computed band gap of 0.57–2.63 eV across 14 reported structures. Standard DFT underestimates band gaps, so the measured gap is typically larger.
Is FeAsO4 a metal, semiconductor, or insulator?
DFT predicts a band gap of up to 2.63 eV (a semiconductor). Measured gaps are typically larger.
Is FeAsO4 thermodynamically stable?
Yes — Scorodite (FeAsO4) sits on the convex hull (energy above hull 0 eV/atom), i.e. stable.
What is the crystal structure of FeAsO4?
The reference structure of Scorodite (FeAsO4) is orthorhombic symmetry, space group Imma (No. 74).
What is the density of FeAsO4?
The computed density of the ground-state structure of Scorodite (FeAsO4) is 4.04 g/cm³.
How many polymorphs of FeAsO4 are known?
14 structures of FeAsO4 are reported across 3 databases, spanning 4 distinct space groups.
What elements does FeAsO4 contain?
Scorodite (FeAsO4) contains As, Fe, and O (3 elements).
Where does the data for FeAsO4 come from?
FeAsO4 data is cross-referenced from oqmd, materials_project, jarvis, mpaloe, cod.
Comparison

How It Compares

Within the oxide oxygen-evolution catalysts class.

Unlike the highly conductive perovskite-based catalysts such as LaNiO3 or the layered lithium-intercalation oxides like LiCoO2, FeAsO4 offers a distinct semiconducting profile that differentiates it from the more metallic or purely ionic members of the oxygen-evolution catalyst class. While materials like BiFeO3 share similar transition metal-oxygen frameworks, FeAsO4 provides a unique chemical environment due to the presence of the arsenate group, offering a different catalytic landscape for oxygen-evolution reactions.

Explore

Related Compounds

Other Oxide Oxygen-Evolution Catalysts in the database.

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)
  • mpaloe — Data from MP-ALOE. Cite: Kuner et al., npj Comput. Mater. (2025), doi:10.1038/s41524-025-01834-9.
  • cod — Data from the Crystallography Open Database (crystallography.net/cod/). Cite: Grazulis et al., J. Appl. Cryst. 42, 726 (2009). (CC0-1.0)

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