Natural Quasicrystals

Quasicrystals are solids whose atomic arrangements have symmetries that are forbidden for periodic crystals, including configurations with fivefold symmetry. All examples identified to date have been synthesized in the laboratory under controlled conditions. Here we present evidence of a naturally o...

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Main Authors: Luca Bindi, Paul J. Steinhardt, Nan Yao, Peter J. Lu
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.672.9541
http://physics.princeton.edu/%7Esteinh/BindiSCIENCE.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.672.9541 2023-05-15T17:05:20+02:00 Natural Quasicrystals Luca Bindi Paul J. Steinhardt Nan Yao Peter J. Lu The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.672.9541 http://physics.princeton.edu/%7Esteinh/BindiSCIENCE.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.672.9541 http://physics.princeton.edu/%7Esteinh/BindiSCIENCE.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://physics.princeton.edu/%7Esteinh/BindiSCIENCE.pdf text ftciteseerx 2016-01-08T17:27:52Z Quasicrystals are solids whose atomic arrangements have symmetries that are forbidden for periodic crystals, including configurations with fivefold symmetry. All examples identified to date have been synthesized in the laboratory under controlled conditions. Here we present evidence of a naturally occurring icosahedral quasicrystal that includes six distinct fivefold symmetry axes. The mineral, an alloy of aluminum, copper, and iron, occurs as micrometer-sized grains associated with crystalline khatyrkite and cupalite in samples reported to have come from the Koryak Mountains in Russia. The results suggest that quasicrystals can form and remain stable under geologic conditions, although there remain open questions as to how this mineral formed naturally. Solids, including naturally forming min-erals, are classified according to the orderand rotational symmetry of their atomic arrangements. Glasses and amorphous solids have disordered arrangements with no exact rota-tional symmetry. Crystals have atomic structures with long-range periodic order that can be de-scribed by a single atom or atomic cluster that repeats at regular intervals. According to the well-known theorems of crystallography derived nearly two centuries ago, the rotational symme-tries of crystals are highly restricted: Two-, three-, four-, and sixfold symmetry axes are allowed, but five-, seven-, and all higher-fold symmetry axes are forbidden. Quasicrystals (1, 2) (short for quasiperiodic crystals) have a more subtle kind of long-range order. In a quasiperiodic structure, the atomic positions along each symmetry axis are described by a sum of two or more periodic functions whose wavelengths have an irrational ratio (inexpressible as a ratio of integers). This difference exempts quasicrystals from the crys-tallographic restrictions: They can exhibit all the rotational symmetries forbidden to crystals, in-cluding fivefold symmetry. Just as square or hex-agonal tilings are commonly used as geometric analogs for periodic crystals, the Penrose tiling ... Text Koryak Unknown
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description Quasicrystals are solids whose atomic arrangements have symmetries that are forbidden for periodic crystals, including configurations with fivefold symmetry. All examples identified to date have been synthesized in the laboratory under controlled conditions. Here we present evidence of a naturally occurring icosahedral quasicrystal that includes six distinct fivefold symmetry axes. The mineral, an alloy of aluminum, copper, and iron, occurs as micrometer-sized grains associated with crystalline khatyrkite and cupalite in samples reported to have come from the Koryak Mountains in Russia. The results suggest that quasicrystals can form and remain stable under geologic conditions, although there remain open questions as to how this mineral formed naturally. Solids, including naturally forming min-erals, are classified according to the orderand rotational symmetry of their atomic arrangements. Glasses and amorphous solids have disordered arrangements with no exact rota-tional symmetry. Crystals have atomic structures with long-range periodic order that can be de-scribed by a single atom or atomic cluster that repeats at regular intervals. According to the well-known theorems of crystallography derived nearly two centuries ago, the rotational symme-tries of crystals are highly restricted: Two-, three-, four-, and sixfold symmetry axes are allowed, but five-, seven-, and all higher-fold symmetry axes are forbidden. Quasicrystals (1, 2) (short for quasiperiodic crystals) have a more subtle kind of long-range order. In a quasiperiodic structure, the atomic positions along each symmetry axis are described by a sum of two or more periodic functions whose wavelengths have an irrational ratio (inexpressible as a ratio of integers). This difference exempts quasicrystals from the crys-tallographic restrictions: They can exhibit all the rotational symmetries forbidden to crystals, in-cluding fivefold symmetry. Just as square or hex-agonal tilings are commonly used as geometric analogs for periodic crystals, the Penrose tiling ...
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Luca Bindi
Paul J. Steinhardt
Nan Yao
Peter J. Lu
spellingShingle Luca Bindi
Paul J. Steinhardt
Nan Yao
Peter J. Lu
Natural Quasicrystals
author_facet Luca Bindi
Paul J. Steinhardt
Nan Yao
Peter J. Lu
author_sort Luca Bindi
title Natural Quasicrystals
title_short Natural Quasicrystals
title_full Natural Quasicrystals
title_fullStr Natural Quasicrystals
title_full_unstemmed Natural Quasicrystals
title_sort natural quasicrystals
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.672.9541
http://physics.princeton.edu/%7Esteinh/BindiSCIENCE.pdf
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