KPrTe2

KPrTe2 is a stable semiconducting compound composed of potassium, praseodymium, and tellurium.

KPrTe
Crystal structure of KPrTe2 (trigonal, R-3m (No. 166))
Ground-state structure · Materials Project
Overview

About KPrTe2

KPrTe2 is a ternary telluride compound that exhibits semiconducting electronic behavior. As a thermodynamically stable phase located on the convex hull, it represents a robust structural arrangement of potassium, praseodymium, and tellurium atoms.

This material is of interest for researchers investigating rare-earth chalcogenides. Its stable nature makes it a reliable candidate for fundamental studies into the electronic and magnetic properties inherent to praseodymium-based semiconductors.

At a glance

Key Properties

Cross-validated computational properties for KPrTe2, aggregated across 4 databases.

Band Gap

0.45–1.41 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

5
4 databases, 1 space group
Validation

Cross-Source DFT Agreement

How well independent DFT databases agree on the thermodynamics of KPrTe2. Tight agreement means computed properties can be trusted without re-running calculations.

Agreement Score

1.00 / 1.00
Trust tier: high

Hull Spread

0.000 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 KPrTe2, ranked by energy above hull.

Space GroupCrystal SystemBand Gap (eV)E above hull (eV/atom)E/atom (eV)Density (g/cm³)
——1.410.0000-1.421—
R-3m (No. 166)trigonal1.280.0000-23.2484.71
R-3m (No. 166)trigonal1.260.0000-1.489—
——0.450.2849-1.136—
R-3m (No. 166)trigonal———4.85
Uses

Applications

Where KPrTe2 is used.

Semiconductor researchSolid-state chemistry studiesRare-earth material development
Reference

Frequently Asked Questions

Common questions about KPrTe2, answered from cross-validated data.

What is KPrTe2?

KPrTe2 is a stable semiconducting compound composed of potassium, praseodymium, and tellurium.

More questions
What is KPrTe2 used for?
KPrTe2 is used in semiconductor research, solid-state chemistry studies, and rare-earth material development.
What is the band gap of KPrTe2?
KPrTe2 has a DFT-computed band gap of 0.45–1.41 eV across 5 reported structures. Standard DFT underestimates band gaps, so the measured gap is typically larger.
Is KPrTe2 a metal, semiconductor, or insulator?
DFT predicts a band gap of up to 1.41 eV (a semiconductor). Measured gaps are typically larger.
Is KPrTe2 thermodynamically stable?
Yes — KPrTe2 sits on the convex hull (energy above hull 0 eV/atom), i.e. stable.
What is the crystal structure of KPrTe2?
The reference structure of KPrTe2 is trigonal symmetry, space group R-3m (No. 166).
What is the density of KPrTe2?
The computed density of the ground-state structure of KPrTe2 is 4.71 g/cm³.
How many polymorphs of KPrTe2 are known?
5 structures of KPrTe2 are reported across 4 databases, spanning 1 distinct space group.
What elements does KPrTe2 contain?
KPrTe2 contains K, Pr, and Te (3 elements).
Where does the data for KPrTe2 come from?
KPrTe2 data is cross-referenced from oqmd, materials_project, jarvis, cod.
Comparison

How It Compares

As a distinct ternary telluride, KPrTe2 serves as a foundational example of this specific chemical family, offering a stable structural framework for exploring the interplay between rare-earth elements and chalcogenide anions.

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)

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