Fe4P4Se4

Fe4P4Se4 is a metastable semiconducting skutterudite material used in research focused on thermoelectric energy conversion and electronic transport properties.

Crystal structure of Fe4P4Se4 (monoclinic, P21/c (No. 14))
Ground-state structure · Materials Project
Overview

About Fe4P4Se4

Fe4P4Se4 is a semiconducting member of the skutterudite family, a class of materials widely recognized for their complex crystal structures and potential in thermal energy conversion. As a metastable phase, it represents a specialized configuration within the iron-phosphorus-selenium system, offering distinct electronic characteristics that differentiate it from more common metallic or highly stable compounds.

This compound is of significant interest to researchers investigating the optimization of thermoelectric performance through structural tuning. Its semiconducting nature makes it a candidate for studying charge transport mechanisms in skutterudite frameworks, contributing to the broader understanding of how composition influences the efficiency of solid-state energy devices.

At a glance

Key Properties

Cross-validated computational properties for Fe4P4Se4, aggregated across 3 databases.

Band Gap

0.19 eV
Range across DFT structures

Energy Above Hull

0.074 eV/atom
Best (lowest) across sources

Stability

Metastable
2 DFT sources

Structures

6
3 databases, 1 space group
Crystallography

Reported Structures

Lowest-energy structures reported for Fe4P4Se4, ranked by energy above hull.

Space GroupCrystal SystemBand Gap (eV)E above hull (eV/atom)E/atom (eV)Density (g/cm³)
P21/c (No. 14)monoclinic0.190.0742-6.3226.27
6.05
6.05
4.13
P21/c (No. 14)
5.57
Uses

Applications

Where Fe4P4Se4 is used.

Thermoelectric energy conversion researchSolid-state electronic device studiesSemiconductor materials development
Reference

Frequently Asked Questions

Common questions about Fe4P4Se4, answered from cross-validated data.

What is Fe4P4Se4?

Fe4P4Se4 is a metastable semiconducting skutterudite material used in research focused on thermoelectric energy conversion and electronic transport properties.

More questions
What is Fe4P4Se4 used for?
Fe4P4Se4 is used in thermoelectric energy conversion research, solid-state electronic device studies, and semiconductor materials development.
What is the band gap of Fe4P4Se4?
Fe4P4Se4 has a DFT-computed band gap of 0.19 eV across 6 reported structures.
Is Fe4P4Se4 a metal, semiconductor, or insulator?
With a band gap up to 0.19 eV it is a semiconductor.
Is Fe4P4Se4 thermodynamically stable?
Fe4P4Se4 has a lowest energy above hull of 0.074 eV/atom (metastable).
What is the crystal structure of Fe4P4Se4?
The lowest-energy reported polymorph of Fe4P4Se4 is monoclinic symmetry, space group P21/c (No. 14).
What is the density of Fe4P4Se4?
The computed density of the ground-state structure of Fe4P4Se4 is 6.27 g/cm³.
How many polymorphs of Fe4P4Se4 are known?
6 structures of Fe4P4Se4 are reported across 3 databases, spanning 1 distinct space group.
What elements does Fe4P4Se4 contain?
Fe4P4Se4 contains Fe, P, and Se (3 elements).
Where does the data for Fe4P4Se4 come from?
Fe4P4Se4 data is cross-referenced from materials_project, omat24, aflow.
Comparison

How It Compares

Within the skutterudite thermoelectrics class.

Within the diverse skutterudite and pnictide class, Fe4P4Se4 occupies a distinct niche compared to more frequently studied binary phases like FeP or FeP2. While compounds such as FeP2 are often examined for their electrochemical stability and simpler stoichiometry, Fe4P4Se4 provides a more complex structural landscape that allows for nuanced electronic behavior, setting it apart from the more conventional phosphide members of the group.

Explore

Related Compounds

Other Skutterudite Thermoelectrics in the database.

Data sources & attribution
  • materials_project — Data from the Materials Project. Cite: Jain et al., APL Materials 1, 011002 (2013).
  • omat24 — Data from OMat24 (Meta FAIR). Cite: Barroso-Luque et al., arXiv 2410.12771 (2024).
  • aflow — Data from AFLOW. Cite: Curtarolo et al., Comp. Mater. Sci. 58, 218 (2012).

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