Octomino

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The 369 free octominoes The 369 Free Octominoes.svg
The 369 free octominoes

An octomino (or 8-omino) is a polyomino of order 8; that is, a polygon in the plane made of 8 equal-sized squares connected edge to edge. [1] When rotations and reflections are not considered to be distinct shapes, there are 369 different free octominoes. When reflections are considered distinct, there are 704 one-sided octominoes. When rotations are also considered distinct, there are 2,725 fixed octominoes. [2] [3]

Contents

Symmetry

The figure shows all possible free octominoes, coloured according to their symmetry groups:

Reflection symmetrical octominoes 90 deg.svg
Reflection symmetrical octominoes 45 deg.svg
Rotation symmetrical octominoes (C2).svg
Rotation symmetrical octomino (C4).svg
Rotation and reflection symmetric octominoes h.svg

The set of octominoes is the lowest polyomino set in which all eight possible symmetries are realized. The next higher set with this property is the dodecomino (12-omino) set. [3]

If reflections of an octomino are considered distinct, as they are with one-sided octominoes, then the first, fourth and fifth categories above double in size, resulting in an extra 335 octominoes for a total of 704. If rotations are also considered distinct, then the octominoes from the first category count eightfold, the ones from the next three categories count fourfold, the ones from categories five to seven count twice, and the last octomino counts only once. This results in 316 × 8 + (23+5+18) × 4 + (1+4+1) × 2 + 1 = 2,725 fixed octominoes.

Packing and tiling

Of the 369 free octominoes, 320 satisfy the Conway criterion and 23 more can form a patch satisfying the criterion. [4] The other 26 octominoes (including the 6 with holes) are unable to tessellate the plane. [5]

Since 6 of the free octominoes have a hole, it is trivial to prove that the complete set of octominoes cannot be packed into a rectangle, and that not all octominoes can be tiled.

Octominoes with holes.svg

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<span class="mw-page-title-main">Polyomino</span> Geometric shapes formed from squares

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<span class="mw-page-title-main">Dihedral group</span> Group of symmetries of a regular polygon

In mathematics, a dihedral group is the group of symmetries of a regular polygon, which includes rotations and reflections. Dihedral groups are among the simplest examples of finite groups, and they play an important role in group theory, geometry, and chemistry.

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<span class="mw-page-title-main">Hexomino</span> Geometric shape formed from six squares

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<span class="mw-page-title-main">Polyhex (mathematics)</span> Polyform with a regular hexagon as the base form

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In geometry, a point group in three dimensions is an isometry group in three dimensions that leaves the origin fixed, or correspondingly, an isometry group of a sphere. It is a subgroup of the orthogonal group O(3), the group of all isometries that leave the origin fixed, or correspondingly, the group of orthogonal matrices. O(3) itself is a subgroup of the Euclidean group E(3) of all isometries.

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A decomino, or 10-omino, is a polyomino of order 10; that is, a polygon in the plane made of 10 equal-sized squares connected edge to edge. When rotations and reflections are not considered to be distinct shapes, there are 4,655 different free decominoes. When reflections are considered distinct, there are 9,189 one-sided decominoes. When rotations are also considered distinct, there are 36,446 fixed decominoes.

References

  1. Golomb, Solomon W. (1994). Polyominoes (2nd ed.). Princeton, New Jersey: Princeton University Press. ISBN   0-691-02444-8.
  2. Weisstein, Eric W. "Octomino". From MathWorld – A Wolfram Web Resource. Retrieved 2008-07-22.
  3. 1 2 Redelmeier, D. Hugh (1981). "Counting polyominoes: yet another attack". Discrete Mathematics. 36 (2): 191–203. doi: 10.1016/0012-365X(81)90237-5 .
  4. Rhoads, Glenn C. (2005). "Planar tilings by polyominoes, polyhexes, and polyiamonds". Journal of Computational and Applied Mathematics. 174 (2): 329–353. doi:10.1016/j.cam.2004.05.002.
  5. Gardner, Martin (August 1975). "More about tiling the plane: the possibilities of polyominoes, polyiamonds and polyhexes". Scientific American . 233 (2): 112–115.