Synthesis and Characterization of High-Entropy-Alloy-Type Layered Telluride <i>M</i>Bi₂Te₄ (<i>M</i> = Ag, In, Sn, Pb, Bi).

Although those changes would be caused by chemical pressure effects, which is the shrinkage of unit cells and/or bonds by the decrease in the average ionic size at the M site, we found an interesting trend in the isotropic displacement parameter ( U iso ) at the M site.

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