Equivariant Fiber Polytopes

Equivariant Fiber Polytopes

Documenta Math. 113 Equivariant Fiber Polytopes To the memory of Rodica Simion. Victor Reiner Received: February 15, 2002 Communicated by GunÄ ter M. Ziegler Abstract. The equivariant generalization of Billera and Sturmfels' ¯ber polytope construction is described. This gives a new relation between the associahedron and cyclohedron, a di®erent natural con- struction for the type B permutohedron, and leads to a family of order-preserving maps between the face lattice of the type B permu- tohedron and that of the cyclohedron 2000 Mathematics Subject Classi¯cation: 52B12, 52B15 Keywords and Phrases: ¯ber polytope, associahedron, cyclohedron, equivariant Contents 1. Introduction 114 2. Equivariant polytope bundles 115 2.1. Group actions on polytope bundles 115 2.2. Equivariant ¯ber polytopes 119 2.3. Equivariant secondary polytopes 120 3. Small, visualizable examples 121 3.1. The standard example. 121 3.2. Triangulations of a regular hexagon. 122 4. Application examples. 124 4.1. Cyclohedra and associahedra. 124 4.2. The type B permutohedron. 125 4.3. Maps from the type B permutohedron to the cyclohedron. 126 5. Remarks/Questions 129 Acknowledgements 131 References 131 Documenta Mathematica 7 (2002) 113{132 114 Victor Reiner (a) (b) Figure 1. The 3-dimensional associahedron, containing the 2-dimensional cyclohedron as a planar slice. 1. Introduction Much of this paper is motivated by a new relationship between two families of convex polytopes which have appeared in diverse places within topology, geometry, and combinatorics [4, 10, 12, 13, 16]: the associahedra (or Stashe® polytopes), and the cyclohedra (or type B associahedra). There is already a well-known relation between these two families: any face in a cyclohedron is combinatorially isomorphic to a Cartesian product of a lower- dimensional cyclohedron along with a collection of lower-dimensional associa- hedra [16, 3.3], [6, Proposition 3.2.1]. Our point of departure is a di®erent relationship,x illustrated in Figure 1. The 3-dimensional associahedron is de- picted in Figure 1(a), with its vertices indexed by triangulations of a (centrally symmetric) hexagon. Figure 1(b) shows inside it a hexagonal slice representing the 2-dimensional cyclohedron, with vertices indexed by the subset of triangu- lations possessing central symmetry { this slice is the invariant subpolytope for a reection symmetry acting on the associahedron, which swaps two vertices if they correspond to triangulations that di®er by 180± rotation. Our main result (Theorem 2.10) asserts a similar relationship generally when one considers subdivisions of a polytope which are invariant under some ¯nite group of symmetries. The theory of ¯ber polytopes introduced by Billera and Sturmfels [1] shows that whenever one has a linear surjection of convex poly- topes P ¼ Q, there is an associated convex polytope §(P ¼ Q), called the ¯ber polytop! e. This ¯ber polytope has dimension dim P dim!Q, and its faces correspond (roughly) to the subdivisions of Q by cells ¡which are projections of families of faces of P . Our result says that when the projection P ¼ Q is G-equivariant for some ¯nite group G acting as symmetries on both P!and Q, then G acts as a group of symmetries on §(P ¼ Q), and the G-invariant ! Documenta Mathematica 7 (2002) 113{132 Equivariant Fiber Polytopes 115 subpolytope §G(P ¼ Q) (the equivariant ¯ber polytope) is a polytope of di- mension dim P G dim! QG whose faces correspond to those subdivisions which are G-invariant. ¡ The paper is structured as follows. Section 2 proves the main results, with Subsection 2.1 containing the technical details needed to generalize ¯ber poly- topes to the equivariant setting. Theorem 2.10 on the existence and dimension of the equivariant ¯ber polytope is deduced in Subsection 2.2. The special case of equivariant secondary polytopes is discussed in Subsection 2.3. Section 3 contains some low-dimensional examples that are easily visualized, while Section 4 gives some general examples as applications. In particular, Example 4.1 explains the above relation between associahedra and cyclohedra, and Example 4.2 explains how the type B permutohedron (that is, the zono- tope generated by the root system of type B) occurs as an equivariant ¯ber polytope. In Section 4.3 we answer a question of R. Simion, by exhibiting a family of natural maps between the face lattices of the Bn-permutohedron and n-dimensional cyclohedron. Section 5 lists some remarks and open questions. 2. Equivariant polytope bundles 2.1. Group actions on polytope bundles. For convenience, we work with the same notation as in [1, 1] in working out the equivariant versions of the same results. x Let Q be a polytope bundle, that is, Q is a convex polytope in Rd, and B ! n for each x in Q, the set x is a convex polytope in R , such that the graph B n+d x x : x Q is a bounded Borel subset of R . We further assume that fB £ 2 g we have a ¯nite group G acting linearly on both Rd and Rn. S Definition 2.1. Say that Q is a G-equivariant polytope bundle if B ! G acts as symmetries of Q, i.e. g(Q) = Q for all g in G. In particular, ² without loss of generality, the centroid of Q is the origin 0. for every x in Q and g in G one has = g( ). ² Bg(x) Bx Alternatively, equivariance of a polytope bundle is equivalent to G-invariance of Q, along with G-invariance of with respect to a natural G-action on polytope bundles: given Q and g inBG, let g( Q) be the polytope bundle de¯ned B ! B ! by g( Q) := g( 1 ). B ! x Bg¡ x The linear action of G on Rn induces a contragredient action on the dual space n 1 n n (R )¤ of functionals: g(Ã)(x) := Ã(g¡ (x)) for g G; y R ; à (R )¤. 2 2 2 A section of Q is a choice of (x) x for each x. If Q is B ! 2 B B !1 equivariant, there is a G-action on sections de¯ned by g()(x) := g(g¡ x). For any of these G-actions, de¯ne the averaging (or Reynolds) operator 1 ¼ = g G G g G j j X2 which is an idempotent projector onto the subset (or subspace) of G-invariants, n n G n n G e.g. ¼ maps R (R ) and maps (R )¤ ((R )¤) . ! ! Documenta Mathematica 7 (2002) 113{132 116 Victor Reiner It turns out that much of the reason that ¯ber polytopes interact well with ¯nite group actions boils down to ¼G being a linear operator which is a convex combination of the group operations g in G. Recall that for a polytope bundle Q, the Minkowski integral is the B ! Q B subset of n consisting of all integrals of measurable sections , and that R Q R this is a non-empty compact, convex subset of n. R R Proposition 2.2. Integration commutes with the G-action on sections of a G-equivariant polytope bundle Q: B ! g = g ZQ ZQ ¶ for all g in G. Proof. 1 g = g((g¡ x))dx ZQ ZQ 1 = g (g¡ x)dx ZQ ¶ = g (u)du ZQ ¶ Here the second equality uses linearity of g and linearity of integration. The third equality comes from the change of variable x = g(u), using the fact that the Jacobian determinant for this change of variable is det(g), which must be 1, since g is an element of ¯nite order in GL(Rn). § ¤ Corollary 2.3. For any G-equvariant polytope bundle Q, the group G acts on the convex set . B ! Q B Furthermore, one has R G n G := (R ) B B \ ZQ ¶ ZQ ¶ (2.1) = ¼ G B ZQ ¶ = : G-equivariant, measurable sections ; ½ZQ Proof. Proposition 2.2 implies the ¯rst assertion. For the second equality in (2.1), we claim more generally that n G C (R ) = ¼G(C) \ for any convex G-invariant subset C Rn. To see this, note that the left-hand ½ side is contained in the right because of idempotence of ¼G. The right-hand side is obviously contained in (Rn)G. It also lies in C since for any x in C, the 1 convex combination ¼G(x) = G g G g(x) will also lie in C. j j 2 P Documenta Mathematica 7 (2002) 113{132 Equivariant Fiber Polytopes 117 For the third equality in (2.1), note that the right-hand side is contained in the left since the integral Q of any G-equivariant section will be a G-invariant point of n by Proposition 2.2. Conversely, a typical point on the left-hand R R side is where is a section such that g( ) = for all g G, and Q Q Q 2 one can check using Proposition 2.2 that the G-equivariant section ¼ has the R R R G same integral: 1 ¼ = g G G Q g G Q Z j j X2 Z 1 = g G g G Q ¶ j j X2 Z = ZQ ¤ G We wish to interpret faces of in terms of face bundles. Recall that a Q B face bundle Q of Q ³isRa p´olytope bundle in which x is a face of x for every x inF Q!. A coheB r!ent face bundle of Q is one of theF form à BQ à à n B ! ÃB ! having x := ( x) , where à (R )¤ is any linear functional and P denotes the faceBof P onB which the functio2 nal à is maximized. When Q is G-equivariant, the G-action on bundles restricts to a G-action on faceBbundles,! and as before, a face bundle is G-equivariant if and only if it is invariant under the G-action.

View Full Text

Details

  • File Type
    pdf
  • Upload Time
    -
  • Content Languages
    English
  • Upload User
    Anonymous/Not logged-in
  • File Pages
    20 Page
  • File Size
    -

Download

Channel Download Status
Express Download Enable

Copyright

We respect the copyrights and intellectual property rights of all users. All uploaded documents are either original works of the uploader or authorized works of the rightful owners.

  • Not to be reproduced or distributed without explicit permission.
  • Not used for commercial purposes outside of approved use cases.
  • Not used to infringe on the rights of the original creators.
  • If you believe any content infringes your copyright, please contact us immediately.

Support

For help with questions, suggestions, or problems, please contact us