Icosahedral Polyhedra from 6 Lattice and Danzer's ABCK Tiling
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Systematic Narcissism
Systematic Narcissism Wendy W. Fok University of Houston Systematic Narcissism is a hybridization through the notion of the plane- tary grid system and the symmetry of narcissism. The installation is based on the obsession of the physical reflection of the object/subject relation- ship, created by the idea of man-made versus planetary projected planes (grids) which humans have made onto the earth. ie: Pierre Charles L’Enfant plan 1791 of the golden section projected onto Washington DC. The fostered form is found based on a triacontahedron primitive and devel- oped according to the primitive angles. Every angle has an increment of 0.25m and is based on a system of derivatives. As indicated, the geometry of the world (or the globe) is based off the planetary grid system, which, according to Bethe Hagens and William S. Becker is a hexakis icosahedron grid system. The formal mathematical aspects of the installation are cre- ated by the offset of that geometric form. The base of the planetary grid and the narcissus reflection of the modular pieces intersect the geometry of the interfacing modular that structures the installation BACKGROUND: Poetics: Narcissism is a fixation with oneself. The Greek myth of Narcissus depicted a prince who sat by a reflective pond for days, self-absorbed by his own beauty. Mathematics: In 1978, Professors William Becker and Bethe Hagens extended the Russian model, inspired by Buckminster Fuller’s geodesic dome, into a grid based on the rhombic triacontahedron, the dual of the icosidodeca- heron Archimedean solid. The triacontahedron has 30 diamond-shaped faces, and possesses the combined vertices of the icosahedron and the dodecahedron. -
E8 Physics and Quasicrystals Icosidodecahedron and Rhombic Triacontahedron Vixra 1301.0150 Frank Dodd (Tony) Smith Jr
E8 Physics and Quasicrystals Icosidodecahedron and Rhombic Triacontahedron vixra 1301.0150 Frank Dodd (Tony) Smith Jr. - 2013 The E8 Physics Model (viXra 1108.0027) is based on the Lie Algebra E8. 240 E8 vertices = 112 D8 vertices + 128 D8 half-spinors where D8 is the bivector Lie Algebra of the Real Clifford Algebra Cl(16) = Cl(8)xCl(8). 112 D8 vertices = (24 D4 + 24 D4) = 48 vertices from the D4xD4 subalgebra of D8 plus 64 = 8x8 vertices from the coset space D8 / D4xD4. 128 D8 half-spinor vertices = 64 ++half-half-spinors + 64 --half-half-spinors. An 8-dim Octonionic Spacetime comes from the Cl(8) factors of Cl(16) and a 4+4 = 8-dim Kaluza-Klein M4 x CP2 Spacetime emerges due to the freezing out of a preferred Quaternionic Subspace. Interpreting World-Lines as Strings leads to 26-dim Bosonic String Theory in which 10 dimensions reduce to 4-dim CP2 and a 6-dim Conformal Spacetime from which 4-dim M4 Physical Spacetime emerges. Although the high-dimensional E8 structures are fundamental to the E8 Physics Model it may be useful to see the structures from the point of view of the familiar 3-dim Space where we live. To do that, start by looking the the E8 Root Vector lattice. Algebraically, an E8 lattice corresponds to an Octonion Integral Domain. There are 7 Independent E8 Lattice Octonion Integral Domains corresponding to the 7 Octonion Imaginaries, as described by H. S. M. Coxeter in "Integral Cayley Numbers" (Duke Math. J. 13 (1946) 561-578 and in "Regular and Semi-Regular Polytopes III" (Math. -
Archimedean Solids
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln MAT Exam Expository Papers Math in the Middle Institute Partnership 7-2008 Archimedean Solids Anna Anderson University of Nebraska-Lincoln Follow this and additional works at: https://digitalcommons.unl.edu/mathmidexppap Part of the Science and Mathematics Education Commons Anderson, Anna, "Archimedean Solids" (2008). MAT Exam Expository Papers. 4. https://digitalcommons.unl.edu/mathmidexppap/4 This Article is brought to you for free and open access by the Math in the Middle Institute Partnership at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in MAT Exam Expository Papers by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Archimedean Solids Anna Anderson In partial fulfillment of the requirements for the Master of Arts in Teaching with a Specialization in the Teaching of Middle Level Mathematics in the Department of Mathematics. Jim Lewis, Advisor July 2008 2 Archimedean Solids A polygon is a simple, closed, planar figure with sides formed by joining line segments, where each line segment intersects exactly two others. If all of the sides have the same length and all of the angles are congruent, the polygon is called regular. The sum of the angles of a regular polygon with n sides, where n is 3 or more, is 180° x (n – 2) degrees. If a regular polygon were connected with other regular polygons in three dimensional space, a polyhedron could be created. In geometry, a polyhedron is a three- dimensional solid which consists of a collection of polygons joined at their edges. The word polyhedron is derived from the Greek word poly (many) and the Indo-European term hedron (seat). -
Shape Skeletons Creating Polyhedra with Straws
Shape Skeletons Creating Polyhedra with Straws Topics: 3-Dimensional Shapes, Regular Solids, Geometry Materials List Drinking straws or stir straws, cut in Use simple materials to investigate regular or advanced 3-dimensional shapes. half Fun to create, these shapes make wonderful showpieces and learning tools! Paperclips to use with the drinking Assembly straws or chenille 1. Choose which shape to construct. Note: the 4-sided tetrahedron, 8-sided stems to use with octahedron, and 20-sided icosahedron have triangular faces and will form sturdier the stir straws skeletal shapes. The 6-sided cube with square faces and the 12-sided Scissors dodecahedron with pentagonal faces will be less sturdy. See the Taking it Appropriate tool for Further section. cutting the wire in the chenille stems, Platonic Solids if used This activity can be used to teach: Common Core Math Tetrahedron Cube Octahedron Dodecahedron Icosahedron Standards: Angles and volume Polyhedron Faces Shape of Face Edges Vertices and measurement Tetrahedron 4 Triangles 6 4 (Measurement & Cube 6 Squares 12 8 Data, Grade 4, 5, 6, & Octahedron 8 Triangles 12 6 7; Grade 5, 3, 4, & 5) Dodecahedron 12 Pentagons 30 20 2-Dimensional and 3- Dimensional Shapes Icosahedron 20 Triangles 30 12 (Geometry, Grades 2- 12) 2. Use the table and images above to construct the selected shape by creating one or Problem Solving and more face shapes and then add straws or join shapes at each of the vertices: Reasoning a. For drinking straws and paperclips: Bend the (Mathematical paperclips so that the 2 loops form a “V” or “L” Practices Grades 2- shape as needed, widen the narrower loop and insert 12) one loop into the end of one straw half, and the other loop into another straw half. -
Rhombic Triacontahedron
Rhombic Triacontahedron Figure 1 Rhombic Triacontahedron. Vertex labels as used for the corresponding vertices of the 120 Polyhedron. COPYRIGHT 2007, Robert W. Gray Page 1 of 11 Encyclopedia Polyhedra: Last Revision: August 5, 2007 RHOMBIC TRIACONTAHEDRON Figure 2 Icosahedron (red) and Dodecahedron (yellow) define the rhombic Triacontahedron (green). Figure 3 “Long” (red) and “short” (yellow) face diagonals and vertices. COPYRIGHT 2007, Robert W. Gray Page 2 of 11 Encyclopedia Polyhedra: Last Revision: August 5, 2007 RHOMBIC TRIACONTAHEDRON Topology: Vertices = 32 Edges = 60 Faces = 30 diamonds Lengths: 15+ ϕ = 2 EL ≡ Edge length of rhombic Triacontahedron. ϕ + 2 EL = FDL ≅ 0.587 785 252 FDL 2ϕ 3 − ϕ = DVF ϕ 2 FDL ≡ Long face diagonal = DVF ≅ 1.236 067 977 DVF ϕ 2 = EL ≅ 1.701 301 617 EL 3 − ϕ 1 FDS ≡ Short face diagonal = FDL ≅ 0.618 033 989 FDL ϕ 2 = DVF ≅ 0.763 932 023 DVF ϕ 2 2 = EL ≅ 1.051 462 224 EL ϕ + 2 COPYRIGHT 2007, Robert W. Gray Page 3 of 11 Encyclopedia Polyhedra: Last Revision: August 5, 2007 RHOMBIC TRIACONTAHEDRON DFVL ≡ Center of face to vertex at the end of a long face diagonal 1 = FDL 2 1 = DVF ≅ 0.618 033 989 DVF ϕ 1 = EL ≅ 0.850 650 808 EL 3 − ϕ DFVS ≡ Center of face to vertex at the end of a short face diagonal 1 = FDL ≅ 0.309 016 994 FDL 2 ϕ 1 = DVF ≅ 0.381 966 011 DVF ϕ 2 1 = EL ≅ 0.525 731 112 EL ϕ + 2 ϕ + 2 DFE = FDL ≅ 0.293 892 626 FDL 4 ϕ ϕ + 2 = DVF ≅ 0.363 271 264 DVF 21()ϕ + 1 = EL 2 ϕ 3 − ϕ DVVL = FDL ≅ 0.951 056 516 FDL 2 = 3 − ϕ DVF ≅ 1.175 570 505 DVF = ϕ EL ≅ 1.618 033 988 EL COPYRIGHT 2007, Robert W. -
Can Every Face of a Polyhedron Have Many Sides ?
Can Every Face of a Polyhedron Have Many Sides ? Branko Grünbaum Dedicated to Joe Malkevitch, an old friend and colleague, who was always partial to polyhedra Abstract. The simple question of the title has many different answers, depending on the kinds of faces we are willing to consider, on the types of polyhedra we admit, and on the symmetries we require. Known results and open problems about this topic are presented. The main classes of objects considered here are the following, listed in increasing generality: Faces: convex n-gons, starshaped n-gons, simple n-gons –– for n ≥ 3. Polyhedra (in Euclidean 3-dimensional space): convex polyhedra, starshaped polyhedra, acoptic polyhedra, polyhedra with selfintersections. Symmetry properties of polyhedra P: Isohedron –– all faces of P in one orbit under the group of symmetries of P; monohedron –– all faces of P are mutually congru- ent; ekahedron –– all faces have of P the same number of sides (eka –– Sanskrit for "one"). If the number of sides is k, we shall use (k)-isohedron, (k)-monohedron, and (k)- ekahedron, as appropriate. We shall first describe the results that either can be found in the literature, or ob- tained by slight modifications of these. Then we shall show how two systematic ap- proaches can be used to obtain results that are better –– although in some cases less visu- ally attractive than the old ones. There are many possible combinations of these classes of faces, polyhedra and symmetries, but considerable reductions in their number are possible; we start with one of these, which is well known even if it is hard to give specific references for precisely the assertion of Theorem 1. -
Enhancing Strategic Discourse Systematically Using Climate Metaphors Widespread Comprehension of System Dynamics in Weather Patterns As a Resource -- /
Alternative view of segmented documents via Kairos 24 August 2015 | Draft Enhancing Strategic Discourse Systematically using Climate Metaphors Widespread comprehension of system dynamics in weather patterns as a resource -- / -- Introduction Systematic global insight of memorable quality? Towards memorable framing of global climate of governance processes? Visual representations of globality of requisite variety for global governance Four-dimensional requisite for a time-bound global civilization? Comprehending the shapes of time through four-dimensional uniform polychora Five-fold ordering of strategic engagement with time Interplay of cognitive patterns in discourse on systemic change Five-fold cognitive dynamics of relevance to governance? Decision-making capacity versus Distinction-making capacity: embodying whether as weather From star-dom to whizdom to isdom? From space-ship design to time-ship embodiment as a requisite metaphor of governance References Prepared in anticipation of the United Nations Climate Change Conference (Paris, 2015) Introduction There is considerable familiarity with the dynamics of climate and weather through the seasons and in different locations. These provide a rich source of metaphor, widely shared, and frequently exploited as a means of communicating subtle insights into social phenomena, strategic options and any resistance to them. It is however now difficult to claim any coherence to the strategic discourse on which humanity and global governance is held to be dependent. This is evident in the deprecation of one political faction by another, the exacerbation of conflictual perceptions by the media, the daily emergence of intractable crises, and the contradictory assertions of those claiming expertise in one arena or another. The dynamics have been caricatured as blame-gaming, as separately discussed (Blame game? It's them not us ! 2015). -
The Truncated Icosahedron As an Inflatable Ball
https://doi.org/10.3311/PPar.12375 Creative Commons Attribution b |99 Periodica Polytechnica Architecture, 49(2), pp. 99–108, 2018 The Truncated Icosahedron as an Inflatable Ball Tibor Tarnai1, András Lengyel1* 1 Department of Structural Mechanics, Faculty of Civil Engineering, Budapest University of Technology and Economics, H-1521 Budapest, P.O.B. 91, Hungary * Corresponding author, e-mail: [email protected] Received: 09 April 2018, Accepted: 20 June 2018, Published online: 29 October 2018 Abstract In the late 1930s, an inflatable truncated icosahedral beach-ball was made such that its hexagonal faces were coloured with five different colours. This ball was an unnoticed invention. It appeared more than twenty years earlier than the first truncated icosahedral soccer ball. In connection with the colouring of this beach-ball, the present paper investigates the following problem: How many colourings of the dodecahedron with five colours exist such that all vertices of each face are coloured differently? The paper shows that four ways of colouring exist and refers to other colouring problems, pointing out a defect in the colouring of the original beach-ball. Keywords polyhedron, truncated icosahedron, compound of five tetrahedra, colouring of polyhedra, permutation, inflatable ball 1 Introduction Spherical forms play an important role in different fields – not even among the relics of the Romans who inherited of science and technology, and in different areas of every- many ball games from the Greeks. day life. For example, spherical domes are quite com- The Romans mainly used balls composed of equal mon in architecture, and spherical balls are used in most digonal panels, forming a regular hosohedron (Coxeter, 1973, ball games. -
Polyhedral Harmonics
value is uncertain; 4 Gr a y d o n has suggested values of £estrap + A0 for the first three excited 4,4 + 0,1 v. e. states indicate 11,1 v.e. för D0. The value 6,34 v.e. for Dextrap for SO leads on A rough correlation between Dextrap and bond correction by 0,37 + 0,66 for the'valence states of type is evident for the more stable states of the the two atoms to D0 ^ 5,31 v.e., in approximate agreement with the precisely known value 5,184 v.e. diatomic molecules. Thus the bonds A = A and The valence state for nitrogen, at 27/100 F2 A = A between elements of the first short period (with 2D at 9/25 F2 and 2P at 3/5 F2), is calculated tend to have dissociation energy to the atomic to lie about 1,67 v.e. above the normal state, 4S, valence state equal to about 6,6 v.e. Examples that for the iso-electronic oxygen ion 0+ is 2,34 are 0+ X, 6,51; N2 B, 6,68; N2 a, 6,56; C2 A, v.e., and that for phosphorus is 1,05 v.e. above 7,05; C2 b, 6,55 v.e. An increase, presumably due their normal states. Similarly the bivalent states to the stabilizing effect of the partial ionic cha- of carbon, : C •, the nitrogen ion, : N • and racter of the double bond, is observed when the atoms differ by 0,5 in electronegativity: NO X, Silicon,:Si •, are 0,44 v.e., 0,64 v.e., and 0,28 v.e., 7,69; CN A, 7,62 v.e. -
A Tourist Guide to the RCSR
A tourist guide to the RCSR Some of the sights, curiosities, and little-visited by-ways Michael O'Keeffe, Arizona State University RCSR is a Reticular Chemistry Structure Resource available at http://rcsr.net. It is open every day of the year, 24 hours a day, and admission is free. It consists of data for polyhedra and 2-periodic and 3-periodic structures (nets). Visitors unfamiliar with the resource are urged to read the "about" link first. This guide assumes you have. The guide is designed to draw attention to some of the attractions therein. If they sound particularly attractive please visit them. It can be a nice way to spend a rainy Sunday afternoon. OKH refers to M. O'Keeffe & B. G. Hyde. Crystal Structures I: Patterns and Symmetry. Mineral. Soc. Am. 1966. This is out of print but due as a Dover reprint 2019. POLYHEDRA Read the "about" for hints on how to use the polyhedron data to make accurate drawings of polyhedra using crystal drawing programs such as CrystalMaker (see "links" for that program). Note that they are Cartesian coordinates for (roughly) equal edge. To make the drawing with unit edge set the unit cell edges to all 10 and divide the coordinates given by 10. There seems to be no generally-agreed best embedding for complex polyhedra. It is generally not possible to have equal edge, vertices on a sphere and planar faces. Keywords used in the search include: Simple. Each vertex is trivalent (three edges meet at each vertex) Simplicial. Each face is a triangle. -
The Crystal Forms of Diamond and Their Significance
THE CRYSTAL FORMS OF DIAMOND AND THEIR SIGNIFICANCE BY SIR C. V. RAMAN AND S. RAMASESHAN (From the Department of Physics, Indian Institute of Science, Bangalore) Received for publication, June 4, 1946 CONTENTS 1. Introductory Statement. 2. General Descriptive Characters. 3~ Some Theoretical Considerations. 4. Geometric Preliminaries. 5. The Configuration of the Edges. 6. The Crystal Symmetry of Diamond. 7. Classification of the Crystal Forros. 8. The Haidinger Diamond. 9. The Triangular Twins. 10. Some Descriptive Notes. 11. The Allo- tropic Modifications of Diamond. 12. Summary. References. Plates. 1. ~NTRODUCTORY STATEMENT THE" crystallography of diamond presents problems of peculiar interest and difficulty. The material as found is usually in the form of complete crystals bounded on all sides by their natural faces, but strangely enough, these faces generally exhibit a marked curvature. The diamonds found in the State of Panna in Central India, for example, are invariably of this kind. Other diamondsJas for example a group of specimens recently acquired for our studies ffom Hyderabad (Deccan)--show both plane and curved faces in combination. Even those diamonds which at first sight seem to resemble the standard forms of geometric crystallography, such as the rhombic dodeca- hedron or the octahedron, are found on scrutiny to exhibit features which preclude such an identification. This is the case, for example, witb. the South African diamonds presented to us for the purpose of these studŸ by the De Beers Mining Corporation of Kimberley. From these facts it is evident that the crystallography of diamond stands in a class by itself apart from that of other substances and needs to be approached from a distinctive stand- point. -
Rhombic Dodecahedron
Rhombic Dodecahedron Figure 1 Rhombic Dodecahedron. Vertex labels as used for the corresponding vertices of the 120 Polyhedron. COPYRIGHT 2007, Robert W. Gray Page 1 of 14 Encyclopedia Polyhedra: Last Revision: September 5, 2007 RHOMBIC DODECAHEDRON Figure 2 Cube (blue) and Octahedron (green) define rhombic Dodecahedron. Figure 3 “Long” (green) and “short” (blue) face diagonals. COPYRIGHT 2007, Robert W. Gray Page 2 of 14 Encyclopedia Polyhedra: Last Revision: September 5, 2007 RHOMBIC DODECAHEDRON Topology: Vertices = 14 Edges = 24 Faces = 12 diamonds Lengths: EL ≡ Edge length of rhombic Dodecahedron. 22 FDL ≡ Long face diagonal = EL ≅ 1.632 993 162 EL 3 1 FDS ≡ Short face diagonal = FDL ≅ 0.707 106 781 FDL 2 2 FDS = EL ≅ 1.154 700 538 EL 3 DFVL ≡ Vertex at the end of a long face diagonal 1 2 = FDL = EL ≅ 0.816 496 581 EL 2 3 DFVS ≡ Vertex at the end of a short face diagonal 1 = FDL ≅ 0.353 553 391 FDL 22 1 = EL ≅ 0.577 350 269 EL 3 COPYRIGHT 2007, Robert W. Gray Page 3 of 14 Encyclopedia Polyhedra: Last Revision: September 5, 2007 RHOMBIC DODECAHEDRON 3 DFE = FDL ≅ 0.306 186 218 FDL 42 1 = EL 2 1 DVVL = FDL ≅ 0.707 106 781 FDL 2 2 = EL ≅ 1.154 700 538 EL 3 3 DVVS = FDL ≅ 0.612 372 4 FDL 22 = EL 11 DVE = FDL ≅ 0.586 301 970 FDL 42 11 = EL ≅ 0.957 427 108 EL 23 1 DVF = FDL 2 2 = EL ≅ 0.816 496 581 EL 3 COPYRIGHT 2007, Robert W. Gray Page 4 of 14 Encyclopedia Polyhedra: Last Revision: September 5, 2007 RHOMBIC DODECAHEDRON Areas: 2 2 1 Area of one diamond face = FDL ≅ 0.353 553 391 FDL 22 22 2 2 = EL ≅ 0.942 809 042 EL 3 2 2 Total face area = 32 FDL ≅ 4.242 640 687 FDL 2 2 = 82 EL ≅ 4.242 640 687 EL Volume: 16 3 3 Cubic measure volume equation = EL ≅ 3.079 201 436 EL 33 3 Synergetics' Tetra-volume equation = 6 FDL Angles: Face Angles: ⎛⎞2 2arcsin θS ≡ Face angle at short vertex = ⎜⎟ ≅ 109.471 220 634° ⎝⎠3 ⎛⎞22 θ ≡ Face angle at long vertex = arcsin ≅ 70.528 779 366° L ⎜⎟ ⎝⎠3 Sum of face angles = 4320° Central Angles: ⎛⎞1 All central angles are = arccos ≅ 54.735 610 317° ⎜⎟ ⎝⎠3 Dihedral Angles: All dihedral angles are = 120° COPYRIGHT 2007, Robert W.