The structural family of non-centrosymmetric Zr 2 Fe 12 P 7 -type pnictides, tetrelides and halides – structure–property relationships

Abstract The Zr 2 Fe 12 P 7 -type structure is one of the common structure types of transition metal-rich intermetallic compounds. This structural family is characterized through its broad coloring on the nine crystallographically independent Wyckoff sites. This diverse coloring leads to compounds with distinctly different bonding patterns, i.e., pnictides, tetrelides, halides, and even some hydrides. The Zr 2 Fe 12 P 7 -type phases can geometrically be explained through an easy condensation pattern of trigonal prisms, forming shamrock/windmill-like motifs. A central problem is the crystallographic disorder that can occur along the c axis. These structural features are reviewed in the present work, along with the broad magnetic and transport properties.

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Publication Details

Journal
Zeitschrift für Kristallographie - Crystalline Materials
Published
2026-11-04
DOI
https://doi.org/10.1515/zkri-2026-0051
Primary Topic
Inorganic Chemistry and Materials
Type
article
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article

The structural family of non-centrosymmetric Zr 2 Fe 12 P 7 -type pnictides, tetrelides and halides – structure–property relationships

Rainer Pöttgen, Eteri Svanidze, Oksana Karychort, Olga Zhak
Zeitschrift für Kristallographie - Crystalline Materials
Inorganic Chemistry and Materials
article

The structural family of non-centrosymmetric Zr 2 Fe 12 P 7 -type pnictides, tetrelides and halides – structure–property relationships

Rainer Pöttgen, Eteri Svanidze, Oksana Karychort, Olga Zhak
article en

Abstract

Abstract The Zr 2 Fe 12 P 7 -type structure is one of the common structure types of transition metal-rich intermetallic compounds. This structural family is characterized through its broad coloring on the nine crystallographically independent Wyckoff sites. This diverse coloring leads to compounds with distinctly different bonding patterns, i.e., pnictides, tetrelides, halides, and even some hydrides. The Zr 2 Fe 12 P 7 -type phases can geometrically be explained through an easy condensation pattern of trigonal prisms, forming shamrock/windmill-like motifs. A central problem is the crystallographic disorder that can occur along the c axis. These structural features are reviewed in the present work, along with the broad magnetic and transport properties.

Zeitschrift für Kristallographie - Crystalline Materials
Lviv University (UA), University of Münster (DE), Max Planck Institute for Chemical Physics of Solids (DE)
Openalex Percentile: Top 29%
Inorganic Chemistry and Materials
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