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Geodesic polyhedron

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3 constructions for a {3,5+}6,0
Geodesic icosahedral polyhedron example.png
Geodesic icosahedral polyhedron example2.png
Geodesic icosahedral polyhedron example5.png
A icosahedron and related symmetry polyhedra can be used to define a high geodesic polyhedron by dividing triangular faces into smaller triangles, and projecting all the new vertices onto a sphere. Higher order polygonal faces can be divided into triangles by adding new vertices centered on each face. The new faces on the sphere are not equilateral triangles, but they are approximately equal edge length. All vertices are valence-6 except 12 vertices which are valence 5.
Construction of {3,5+}3,3
Geodesic dodecahedral polyhedron example.png
Geodesic subdivisions can also be done from an augumented dodecahedron, dividing pentagons into triangles with a center point, and subdividing from that.
Construction of {3,5+}6,3
Geodesic icosahedral polyhedron example3.png
Chiral polyhedra with higher order polygonal faces can be augmented with central points and new triangle faces. Those triangles can then be further subdivided into smaller triangles for new geodesic polyhedra. All vertices are valence-6 except the 12 centered at the original vertices which are valence 5.
Construction of a mixed geodesic form
Geodesic icosahedral polyhedron example4.png
Geodesic subdivisions can also be done by augmented square faces, although the resulting triangles will be near right triangles rather than equilateral. This rhombicosidodecahedron example has 4 to 7 triangles around each vertex.

A geodesic polyhedron is a convex polyhedron made from triangles that approximates a sphere. They usually have icosahedral symmetry which have 6 triangles at a vertex, except 12 vertices which have 5 triangles. It is the dual of a corresponding Goldberg polyhedron, with mostly hexagonal faces.

Contents

Geodesic notationEdit

In Magnus Wenninger's Spherical models, polyhedra are given geodesic notation in the form {3,q+}b,c, where {3,q} is the Schläfli symbol for the regular polyhedron with triangular faces, and q-valance vertices. The + symbol indicates the valence of the vertices being increased. b,c represent a subdivision description, with 1,0 representing the base form. There are 3 symmetry classes of forms: {3,3+}1,0 for a tetrahedron, {3,4+}1,0 for a octahedron, and {3,5+}1,0 for a icosahedron.

The dual notation for Goldberg polyhedra is {q+,3}b,c, with valence-3 vertices, with q-gonal and hexagonal faces. There are 3 symmetry classes of forms: {3+,3}1,0 for a tetrahedron, {4+,3}1,0 for a cube, and {5+,3}1,0 for a dodecahedron.

Values for b,c are divided into 3 classes:

Class I (b=0 or c=0): {3,q+}b,0 or {3,q+}0,b represent a simple division with original edges being divided into b sub-edges.
Class II (b=c): {3,q+}b,b are easier to see from the dual polyhedron {q,3} with q-gonal faces first divided into triangles with a central point, and then all edges are divided into b sub-edges.
Class III: {3,q+}b,c have nonzero unequal values for b,c, and exist in chiral pairs. For b>c we can define it as a right-handed form, and c>b is a left-handed form.

Subdivisions in class III here do not line up simply with the original edges. The subgrids can be extracted by looking at a triangular tiling, positioning a large triangle on top of grid vertices and walking paths from one vertex b steps in one direction, and a turn, either clockwise or counterclockwise, and then another c steps to the next primary vertex.

For example, the icosahedron is {3,5+}1,0, and pentakis dodecahedron, {3,5+}1,1 is seen as a regular dodecahedron with pentagonal faces divided into 5 triangles.

The primary face of the subdivision is called a principal polyhedral triangle (PPT). Calculating a single PPT allows the entire figure to be created.

The frequency of a geodesic polyhedron is defined by the sum of ν = b + c. A harmonic is a subfrequency and can be any whole divisor of ν. Class II always have a harmonic of 2, since ν = 2b.

The triangulation number T = b2 + bc + c2. This number times the number of original faces expresses how many triangles the new polyhedron will have.

PPTs with frequency 8
 

ElementsEdit

The number of elements are specified by the triangulation number  . Two different geodesic polyhedra may have the same number of elements, for instance, {3,5+}5,3 and {3,5+}7,0 both have T=49.

Symmetry Icosahedral Octahedral Tetrahedral
Base Icosahedron
{3,5} = {3,5+}1,0
Octahedron
{3,4} = {3,4+}1,0
Tetrahedron
{3,3} = {3,3+}1,0
Image      
Symbol {3,5+}b,c {3,4+}b,c {3,3+}b,c
Vertices      
Faces      
Edges      

ConstructionEdit

Geodesic polyhedra are constructed by subdividing faces of simpler polyhedra, and then projecting the new vertices onto the surface of a sphere. A geodesic polyhedron has straight edges and flat faces that approximate a sphere, but it can also be made as a spherical polyhedron (A tessellation on a sphere) with true geodesic curved edges on the surface of a sphere. and spherical triangle faces.

Conway u3I = (kt)I (k)tI ktI
Image        
Form 3-frequency
subdivided icosahedron
Kis truncated icosahedron Geodesic polyhedron (3,0) Spherical polyhedron

Relation to Goldberg polyhedraEdit

Geodesic polyhedra are the dual of Goldberg polyhedra. Goldberg polyhedra are also related in that applying a kis operator (dividing faces triangles with a center point) creates new geodesic polyhedra, and truncating vertices of a geodesic polyhedron creates a new Goldberg polyhedron. For example, Goldberg G(2,1) kised, becomes {3,5+}4,1, and truncating that becomes G(6,3). And similarly {3,5+}2,1 truncated becomes G(4,1), and that kised becomes {3,5+}6,3.

ExamplesEdit

Class I geodesic polyhedra
Frequency (1,0) (2,0) (3,0) (4,0) (5,0) (6,0) (7,0) (8,0) (m,0)
T 1 4 9 16 25 36 49 64 m2
Face
triangle
                ...
Icosahedral                 more
Octahedral                 more
Tetrahedral                 more
Class II geodesic polyhedra
Frequency (1,1) (2,2) (3,3) (4,4) (5,5) (6,6) (7,7) (8,8) (m,m)
T 3 12 27 48 75 108 147 192 3m2
Face
triangle
                ...
Icosahedral                 more
Octahedral     more
Tetrahedral   more
Class III geodesic polyhedra
Frequency (1,2) (1,3) (2,3) (1,4) (2,4) (3,4) (1,5) (2,5) (m,n)
T 7 13 19 21 28 37 31 39 m2+mn+n2
Face
triangle
                ...
Icosahedral         more
Octahedral   more
Tetrahedral   more

Spherical modelsEdit

Magnus Wenninger's book Spherical Models explores these subdivisions in building polyhedron models. After explaining the construction of these models, he explained his usage of triangular grids to mark out patterns, with triangles colored or excluded in the models.[1]

Example model
 
An artistic model created by Father Magnus Wenninger called Order in Chaos, representing a chiral subset of triangles of a 16-frequency icosahedral geodesic sphere, {3,5+}16,0
 
A virtual copy showing icosahedral symmetry great circles. The 6-fold rotational symmetry is illusionary, not existing on the icosahedron itself.
 
A single icosahedral triangle with a 16-frequency subdivision

See alsoEdit

ReferencesEdit

  1. ^ Spherical Models, pp. 150–159
  • Robert Williams The Geometrical Foundation of Natural Structure: A source book of Design, 1979, pp. 142–144, Figure 4-49,50,51 Custers of 12 spheres, 42 spheres, 92 spheres
  • Antony Pugh, Polyhedra: a visual approach, 1976, Chapter 6. The Geodesic Polyhedra of R. Buckminster Fuller and Related Polyhedra
  • Wenninger, Magnus (1979), Spherical Models, Cambridge University Press, ISBN 978-0-521-29432-4, MR 0552023, archived from the original on July 4, 2008  Reprinted by Dover 1999 ISBN 978-0-486-40921-4
  • Edward S. Popko, Divided spheres: Geodesics & the Orderly Subdivision of the Sphere (2012) Chapter 8 Subdivision schemas, 8.1 Geodesic Notation, 8.2 Triangulation number 8.3 Frequency and Harmonics 8.4 Grid Symmetry 8.5 Class I: Alternates and fords 8.5.1 Defining the Principal triangle 8.5.2 Edge Reference Points