Plato's cube and the natural geometry of fragmentation.

Gömböc fracture mechanics pattern formation statistical physics

Journal

Proceedings of the National Academy of Sciences of the United States of America
ISSN: 1091-6490
Titre abrégé: Proc Natl Acad Sci U S A
Pays: United States
ID NLM: 7505876

Informations de publication

Date de publication:
04 08 2020
Historique:
pubmed: 19 7 2020
medline: 19 7 2020
entrez: 19 7 2020
Statut: ppublish

Résumé

Plato envisioned Earth's building blocks as cubes, a shape rarely found in nature. The solar system is littered, however, with distorted polyhedra-shards of rock and ice produced by ubiquitous fragmentation. We apply the theory of convex mosaics to show that the average geometry of natural two-dimensional (2D) fragments, from mud cracks to Earth's tectonic plates, has two attractors: "Platonic" quadrangles and "Voronoi" hexagons. In three dimensions (3D), the Platonic attractor is dominant: Remarkably, the average shape of natural rock fragments is cuboid. When viewed through the lens of convex mosaics, natural fragments are indeed geometric shadows of Plato's forms. Simulations show that generic binary breakup drives all mosaics toward the Platonic attractor, explaining the ubiquity of cuboid averages. Deviations from binary fracture produce more exotic patterns that are genetically linked to the formative stress field. We compute the universal pattern generator establishing this link, for 2D and 3D fragmentation.

Identifiants

pubmed: 32680966
pii: 2001037117
doi: 10.1073/pnas.2001037117
pmc: PMC7414180
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S.

Langues

eng

Sous-ensembles de citation

IM

Pagination

18178-18185

Déclaration de conflit d'intérêts

The authors declare no competing interests.

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Auteurs

Gábor Domokos (G)

MTA-BME Morphodynamics Research Group, Budapest University of Technology and Economics, 1111 Budapest, Hungary.
Department of Mechanics, Materials and Structure, Budapest University of Technology and Economics, 1111 Budapest, Hungary.

Douglas J Jerolmack (DJ)

Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104; sediment@sas.upenn.edu.
Mechanical Engineering and Applied Mechanics, University of Pennsylvania, Philadelphia, PA 19104.

Ferenc Kun (F)

Department of Theoretical Physics, University of Debrecen, 4032 Debrecen, Hungary.

János Török (J)

MTA-BME Morphodynamics Research Group, Budapest University of Technology and Economics, 1111 Budapest, Hungary.
Department of Theoretical Physics, Budapest University of Technology and Economics, 1111 Budapest, Hungary.

Classifications MeSH