Symmetry Breakdown in Franckeite: Spontaneous Strain, Rippling, and Interlayer Moiré

Franckeite is a naturally occurring layered mineral with a structure composed of alternating stacks of SnS2-like and PbS-like layers. Although this superlattice is composed of a sequence of isotropic two-dimensional layers, it exhibits a spontaneous rippling that makes the material structurally anis...

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Bibliographic Details
Published in:Nano letters Vol. 20; no. 2; pp. 1141 - 1147
Main Authors: Frisenda, Riccardo, Sanchez-Santolino, Gabriel, Papadopoulos, Nikos, Urban, Joanna, Baranowski, Michal, Surrente, Alessandro, Maude, Duncan K, Garcia-Hernandez, Mar, van der Zant, Herre S. J, Plochocka, Paulina, San-Jose, Pablo, Castellanos-Gomez, Andres
Format: Journal Article
Language:English
Published: United States American Chemical Society 12-02-2020
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Summary:Franckeite is a naturally occurring layered mineral with a structure composed of alternating stacks of SnS2-like and PbS-like layers. Although this superlattice is composed of a sequence of isotropic two-dimensional layers, it exhibits a spontaneous rippling that makes the material structurally anisotropic. We demonstrate that this rippling comes hand in hand with an inhomogeneous in-plane strain profile and anisotropic electrical, vibrational, and optical properties. We argue that this symmetry breakdown results from a spatial modulation of the van der Waals interaction between layers due to the SnS2-like and PbS-like lattices incommensurability.
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ISSN:1530-6984
1530-6992
DOI:10.1021/acs.nanolett.9b04536