Compressibility and High-Pressure Structure of CaMg2Bi2 and YbMg2Bi2

Abstract Compounds with the formula AM2X2 in the CaAl2Si2 structure type have garnered increasing interest across various solid-state research domains, such as quantum topological and thermoelectric materials. Prior studies have identified high-pressure phase transitions in several compounds, including Mg3Sb2, Mg3Bi2, CaMn2Bi2, and SrAl2Si2. In this study, we investigate the structural behavior of CaMg2Bi2 and YbMg2Bi2 under varying pressure conditions. We synthesized crystals using the molten metal flux method and examined them through single-crystal synchrotron X-ray diffraction, employing diamond anvil cells to exert pressures up to 20 GPa. Our analysis reveals insights into the anisotropic compressibility of these materials, highlighting the more compressible and flexible octahedral A-Bi bonds as the primary contributors to this anisotropy. Moreover, we observed a phase transition in both CaMg2Bi2 and YbMg2Bi2 at pressures above 9.6 and 8.7 GPa, respectively. The newly identified high-pressure phase exhibits a distortion of the original CaAl2Si2 structure with space group C2/m. This high-pressure structure is distinct from that of related compounds (e.g., CaMn2Bi2, MgMg2Bi2), the latter exhibiting a square pyramidal coordination for the M site. These results illustrate how pressure can reorganize bonding and coordination in AM2X2 Zintl phases, providing insight into the structural mechanisms that govern phase stability. The anisotropy in compressibility may also influence directional phonon transport, with implications for tuning lattice thermal conductivity through pressure, strain, or chemical substitution.

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Publication Details

Journal
Inorganic Chemistry
Published
2026-09-22
DOI
https://doi.org/10.1021/acs.inorgchem.6c02769
Primary Topic
Rare-earth and actinide compounds
Type
article
Field-Weighted Citation Impact
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Compressibility and High-Pressure Structure of CaMg2Bi2 and YbMg2Bi2

Susannah M. Dorfman, Alexandra Zevalkink, Megan Rylko, M. Calderón et al.
Inorganic Chemistry
Rare-earth and actinide compounds
article

Compressibility and High-Pressure Structure of CaMg2Bi2 and YbMg2Bi2

Susannah M. Dorfman, Alexandra Zevalkink, Megan Rylko, M. Calderón, Wanyue Peng, Allison Pease, Weiwei Xie, Cheng Peng
article en

Abstract

Abstract Compounds with the formula AM2X2 in the CaAl2Si2 structure type have garnered increasing interest across various solid-state research domains, such as quantum topological and thermoelectric materials. Prior studies have identified high-pressure phase transitions in several compounds, including Mg3Sb2, Mg3Bi2, CaMn2Bi2, and SrAl2Si2. In this study, we investigate the structural behavior of CaMg2Bi2 and YbMg2Bi2 under varying pressure conditions. We synthesized crystals using the molten metal flux method and examined them through single-crystal synchrotron X-ray diffraction, employing diamond anvil cells to exert pressures up to 20 GPa. Our analysis reveals insights into the anisotropic compressibility of these materials, highlighting the more compressible and flexible octahedral A-Bi bonds as the primary contributors to this anisotropy. Moreover, we observed a phase transition in both CaMg2Bi2 and YbMg2Bi2 at pressures above 9.6 and 8.7 GPa, respectively. The newly identified high-pressure phase exhibits a distortion of the original CaAl2Si2 structure with space group C2/m. This high-pressure structure is distinct from that of related compounds (e.g., CaMn2Bi2, MgMg2Bi2), the latter exhibiting a square pyramidal coordination for the M site. These results illustrate how pressure can reorganize bonding and coordination in AM2X2 Zintl phases, providing insight into the structural mechanisms that govern phase stability. The anisotropy in compressibility may also influence directional phonon transport, with implications for tuning lattice thermal conductivity through pressure, strain, or chemical substitution.

Inorganic Chemistry
Michigan State University (US)
Sustainable cities and communities
Openalex Percentile: Top 55%
Rare-earth and actinide compounds
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