Artikel

Slab Rotation by Transition‐Metal Relocation in the Layered Zintl Phase Li2ZnSi

05.08.2025

Layered crystal structure of Li2ZnSi with honeycomb-like [ZnSi]2− networks and interlayer Li atoms forming a Lonsdaleite-type substructure. Despite local stacking faults corresponding to 60° rotations of individual layers, the average structure retains P63/mmc symmetry. The Zintl phase forms congruently from the melt and features metallic conductivity.


The layered Zintl phase Li2ZnSi is a structural analog of intercalated graphite with hexagonal layers of Zn and Si atoms separated by Li atoms (space group P63/mmc, a = 4.2458(2) Å, c = 8.224(1) Å). Single-crystal X-ray diffraction reveals Zn relocation into the center of the Zn3Si3 rings in 4% of the hexagonal layers. The Zn relocation is coupled with Li migration. The resulting 2D defects can be modeled either as 60° slab rotations or, alternatively, as layer translations by k  = 1/3 [1,−1,0]. Li2ZnSi shows metal-type electrical resistivity (ρ = 1.18 μΩ m at 300 K) and exhibits significantly enhanced diamagnetism, suggesting orbital contributions akin to those in graphite. This study demonstrates transition-metal mobility in a layered Zintl phase, generating localized 2D defects that leave the local coordination of each atom unchanged. This mechanism is relevant for understanding defect tolerance in structurally related electrode materials.

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Slab Rotation by Transition‐Metal Relocation in the Layered Zintl Phase Li2ZnSi
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Slab Rotation by Transition‐Metal Relocation in the Layered Zintl Phase Li2ZnSi
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Slab Rotation by Transition‐Metal Relocation in the Layered Zintl Phase Li2ZnSi
Aus den Fachgruppen
Slab Rotation by Transition‐Metal Relocation in the Layered Zintl Phase Li2ZnSi
EuChemS Policy Workshop „PFAS”
Slab Rotation by Transition‐Metal Relocation in the Layered Zintl Phase Li2ZnSi
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