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柏拉图立体与自然碎片几何

Plato's cube and the natural geometry of fragmentation.

机构信息

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.

出版信息

Proc Natl Acad Sci U S A. 2020 Aug 4;117(31):18178-18185. doi: 10.1073/pnas.2001037117. Epub 2020 Jul 17.

Abstract

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.

摘要

柏拉图设想地球的基本构成是立方体,这种形状在自然界中很少见。然而,太阳系中到处都是扭曲的多面体——由无处不在的碎裂作用产生的岩石和冰的碎片。我们应用凸镶嵌理论表明,从泥裂到地球板块等自然二维(2D)碎片的平均几何形状有两个吸引子:“柏拉图”四边形和“沃罗诺伊”六边形。在三维(3D)中,柏拉图吸引子占主导地位:值得注意的是,天然岩石碎片的平均形状是长方体。通过凸镶嵌的视角来看,天然碎片确实是柏拉图形式的几何阴影。模拟表明,一般的二元断裂会将所有镶嵌体推向柏拉图吸引子,从而解释了长方体平均值的普遍性。二元断裂的偏差会产生更多与形成应力场有基因联系的奇特模式。我们为 2D 和 3D 碎裂计算了建立这种联系的通用模式生成器。

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