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Fundamental polygon

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Fundamental polygon

In mathematics, each closed surface in the sense of geometric topology can be constructed from an even-sided oriented polygon, called a fundamental polygon, by pairwise identification of its edges.

Contents

This construction can be represented as a string of length 2g of g distinct symbols where each symbol appears twice with exponent either +1 or −1. The exponent −1 signifies that the corresponding edge has the orientation opposing the one of the fundamental polygon.

Examples

  • Sphere: A A 1 or A B B 1 A 1
  • Real projective plane: A A or A B A B
  • Klein bottle: A B A B 1 or A A B B
  • Torus: A B A 1 B 1 or A B C A 1 B 1 C 1
  • Group generators

    For the set of standard, symmetric shapes, the symbols of the edges of the polygon may be understood to be the generators of a group. Then, the polygon, written in terms of group elements, becomes a constraint on the free group generated by the edges, giving a group presentation with one constraint.

    Thus, for example, given the Euclidean plane R 2 , let the group element A act on the plane as A ( x , y ) = ( x + 1 , y ) while B ( x , y ) = ( x , y + 1 ) . Then A , B generate the lattice Γ = Z 2 , and the torus is given by the quotient space (a homogeneous space) T = R 2 / Z 2 . More generally, the two generators A , B can be taken to generate a parallelogram tiling, of fundamental parallelograms.

    For the torus, the constraint on the free group in two letters is given by A B A 1 B 1 = 1 . This constraint is trivially embodied in the action on the plane given above. Alternately, the plane can be tiled by hexagons, and the centers of the hexagons form a hexagonal lattice. Identifying opposite edges of the hexagon again leads to the torus, this time, with the constraint A B C A 1 B 1 C 1 = 1 describing the action of the hexagonal lattice generators on the plane.

    In practice, most of the interesting cases are surfaces with negative curvature, and are thus realized by a discrete lattice Γ in the group PSL ( 2 , R ) acting on the upper half-plane. Such lattices are known as Fuchsian groups.

    Standard fundamental polygons

    An orientable closed surface of genus n has the following standard fundamental polygon:

    A 1 B 1 A 1 1 B 1 1 A 2 B 2 A 2 1 B 2 1 A n B n A n 1 B n 1 = 1

    This fundamental polygon can be viewed as the result of gluing n tori together, and hence the surface is sometimes called the n-fold torus. ("Gluing" two surfaces means cutting a disk out of each and identifying the circular boundaries of the resulting holes.)

    A non-orientable closed surface of (non-orientable) genus n has the following standard fundamental polygon:

    A 1 A 1 A 2 A 2 A n A n

    Alternately, the non-orientable surfaces can be given in one of two forms, as n Klein bottles glued together (this may be called the n-fold Klein bottle, with non-orientable genus 2n), or as n glued real projective planes (the n-fold crosscap, with non-orientable genus n). The n-fold Klein bottle is given by the 4n-sided polygon

    A 1 B 1 A 1 1 B 1 1 A 2 B 2 A 2 1 B 2 1 A n B n A n 1 B n = 1

    (note the final B n is missing the superscript −1; this flip, as compared to the orientable case, being the source of the non-orientability). The (2n + 1)-fold crosscap is given by the 4n+2-sided polygon

    A 1 B 1 A 1 1 B 1 1 A 2 B 2 A 2 1 B 2 1 A n B n A n 1 B n 1 C 2 = 1

    That these two cases exhaust all the possibilities for a compact non-orientable surface was shown by Henri Poincaré.

    Fundamental polygon of a compact Riemann surface

    The fundamental polygon of a (hyperbolic) compact Riemann surface has a number of important properties that relate the surface to its Fuchsian model. That is, a hyperbolic compact Riemann surface has the upper half-plane as the universal cover, and can be represented as a quotient manifold H/Γ where Γ is a non-Abelian group isomorphic to the deck transformation group of the surface. The cosets of the quotient space have the standard fundamental polygon as a representative element. In the following, note that all Riemann surfaces are orientable.

    Metric fundamental polygon

    Given a point z 0 in the upper half-plane H, and a discrete subgroup Γ of PSL(2,R) that acts freely discontinuously on the upper half-plane, then one can define the metric fundamental polygon as the set of points

    F = { z H : d ( z , z 0 ) < d ( z , g z 0 ) g Γ , g 1 }

    Here, d is a hyperbolic metric on the upper half-plane. The metric fundamental polygon is more usually called the Dirichlet polygon .

  • This fundamental polygon is a fundamental domain.
  • This fundamental polygon is convex in that the geodesic joining any two points of the polygon is contained entirely inside the polygon.
  • The diameter of F is less than or equal to the diameter of H/Γ. In particular, the closure of F is compact.
  • If Γ has no fixed points in H and H/Γ is compact, then F will have finitely many sides.
  • Each side of the polygon is a geodesic arc.
  • For every side s of the polygon, there is precisely one other side s' such that gs=s' for some g in Γ. Thus, this polygon will have an even number of sides.
  • The set of group elements g that join sides to each other are generators of Γ, and there is no smaller set that will generate Γ.
  • The upper half-plane is tiled by the closure of F under the action of Γ. That is, H = g Γ g F ¯ where F ¯ is the closure of F.
  • Fricke canonical polygon

    Given a Riemann surface of genus g greater than one, Fricke described another fundamental polygon, the Fricke canonical polygon, which is a very special example of a Dirichlet polygon. The polygon is related to the standard presentation of the fundamental group of the surface. Fricke's original construction is complicated and described in Fricke & Klein (1897). Using the theory of quasiconformal mappings of Ahlfors and Bers, Keen (1965) gave a new, shorter and more precise version of Fricke's construction. The Fricke canonical polygon has the following properties:

  • The vertices of the Fricke polygon has 4g vertices which all lie in an orbit of Γ. By vertex is meant the point where two sides meet.
  • The sides are matched in distinct pairs, so that there is an unique element of Γ carrying a side to the paired side, reversing the orientation. Since the action of Γ is orientation-preserving, if one side is called A , then the other of the pair can be marked with the opposite orientation A 1 .
  • The edges of the standard polygon can be arranged so that the list of adjacent sides takes the form A 1 B 1 A 1 1 B 1 1 A 2 B 2 A 2 1 B 2 1 A g B g A g 1 B g 1 . That is, pairs of sides can be arranged so that they interleave in this way.
  • The sides are geodesic arcs.
  • Each of the interior angles of the Fricke polygon is strictly less than π, so the the polygon is strictly convex, and the sum of these interior angles is 2π.
  • The above construction is sufficient to guarantee that each side of the polygon is a closed (non-trivial) loop in the Riemann surface H/Γ. As such, each side can thus an element of the fundamental group π 1 ( H / Γ ) Γ . In particular, the fundamental group π 1 ( H / Γ ) has 2g generators A 1 , B 1 , A 2 , B 2 , A g , B g , with exactly one defining constraint,

    A 1 B 1 A 1 1 B 1 1 A 2 B 2 A 2 1 B 2 1 A g B g A g 1 B g 1 = 1 .

    The genus of the Riemann surface H/Γ is g.

    Area

    The area of the standard fundamental polygon is 4 π ( g 1 ) where g is the genus of the Riemann surface (equivalently, where 4g is the number of the sides of the polygon). Since the standard polygon is a representative of H/Γ, the total area of the Riemann surface is equal to the area of the standard polygon. The area formula follows from the Gauss–Bonnet theorem and is in a certain sense generalized through the Riemann–Hurwitz formula.

    Explicit form for standard polygons

    Explicit expressions can be given for the regular standard 4g-sided polygon, with rotational symmetry. In this case, that of a genus g Riemann surface with g-fold rotational symmetry, the group may be given by 2 g generators a k . These generators are given by the following fractional linear transforms acting on the upper half-plane:

    a k = ( cos k α sin k α sin k α cos k α ) ( e p 0 0 e p ) ( cos k α sin k α sin k α cos k α )

    for 0 k < 2 g . The parameters are given by

    α = π 4 g ( 2 g 1 )

    and

    β = π 4 g

    and

    p = ln cos β + cos 2 β sin β

    It may be verified that these generators obey the constraint

    a 0 a 1 a 2 g 1 a 0 1 a 1 1 a 2 g 1 1 = 1

    which gives the totality of the group presentation.

    Generalizations

    In higher dimensions, the idea of the fundamental polygon is captured in the articulation of homogeneous spaces.

    References

    Fundamental polygon Wikipedia