Currents, Systoles, and Compactifications of Character Varieties
M. Burger, A. Iozzi, A. Parreau, M. B. Pozzetti

TL;DR
This paper investigates the structure of character varieties' boundaries, decomposes geodesic currents on surfaces, and identifies regions where the mapping class group acts discontinuously, extending previous results to finite-area surfaces with boundary.
Contribution
It introduces a canonical decomposition of geodesic currents, extends boundary analysis to finite-area surfaces, and demonstrates non-empty discontinuity regions for higher rank groups.
Findings
Decomposition of geodesic currents into lamination-associated and positive systole components.
Identification of an open set of discontinuity for the mapping class group action.
Explicit examples provided for the $SL(3,\mathbb{R})$-Hitchin component.
Abstract
We study the Weyl chamber length boundary both of the Hitchin and of the maximal character varieties and determine therein an open set of discontinuity for the action of the mapping class group. This result is obtained as consequence of a canonical decomposition of a geodesic current on a surface of finite type arising from a topological decomposition of the surface along special geodesics. We show that each component either is associated to a measured lamination or has positive systole. For a current with positive systole, we show that the intersection function on the set of closed curves is bi-Lipschitz equivalent to the length function with respect to a hyperbolic metric. The results of this paper on currents generalise the ones in arXiv:1710.07060v1 to the case of surfaces of finite area with geodesic boundary. Concerning the Weyl chamber boundary we improve on the results in…
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Currents, Systoles,
and Compactifications of Character Varieties
M. Burger
Department Mathematik, ETH Zentrum, Rämistrasse 101, CH-8092 Zürich, Switzerland
,
A. Iozzi
Department Mathematik, ETH Zentrum, Rämistrasse 101, CH-8092 Zürich, Switzerland
,
A. Parreau
Univ. Grenoble Alpes, CNRS, Institut Fourier, F-38000 Grenoble, France
and
M. B. Pozzetti
Mathematical Institute, Heidelberg University, Im Neuenheimer feld 205, 69120 Heidelberg, Germany
(Date: March 11, 2024)
Abstract.
We study the Weyl chamber length compactification both of the Hitchin and of the maximal character varieties and determine therein an open set of discontinuity for the action of the mapping class group. This result is obtained as consequence of a canonical decomposition of a geodesic current on a surface of finite type arising from a topological decomposition of the surface along special geodesics. We show that each component either is associated to a measured lamination or has positive systole. For a current with positive systole, we show that the intersection function on the set of closed curves is bilipschitz equivalent to the length function with respect to a hyperbolic metric.
2010 Mathematics Subject Classification:
32G15, 22E40
Marc Burger thanks Francis Bonahon and Kasra Rafi for enlightening conversations on geodesic currents and Kasra Rafi for suggesting to prove a decomposition theorem for geodesic currents. Beatrice Pozzetti thanks Anna Wienhard and Darryl Cooper for insightful conversations.
Beatrice Pozzetti was partially supported by SNF grant P2EZP2_159117, and by DFG project PO 2181/1. Marc Burger and Alessandra Iozzi were partially supported by SNF grant 2-77196-16. Alessandra Iozzi acknowledges moreover support from U.S. National Science Foundation grants DMS 1107452, 1107263, 1107367 "RNMS: Geometric Structures and Representation Varieties" (the GEAR Network). Anne Parreau thanks the Forschungsinstitut für Mathematik for their hospitality. Marc Burger thanks the Leverhulme Trust for supporting his visit to the University of Cambridge as Leverhulme Visiting Professor. Marc Burger, Alessandra Iozzi and Beatrice Pozzetti thank the Isaac Newton Institute for Mathematical Sciences, Cambridge, for support and hospitality during the program “Non-Positive Curvature Group Actions and Cohomology” where work on this paper was undertaken. This work was partially supported by EPSRC grant no P/K032208/1.
Contents
1. Introduction
Let be a geometrically finite surface, where is the hyperbolic plane and is a finitely generated torsion-free discrete group. A geodesic current on is a -invariant Radon measure on the space of unoriented, unparametrized geodesics. Geodesic currents occur in many different contexts. For instance they play a fundamental role in the study of hyperbolic structures [Bon01], of negatively curved metrics [Ota90], or of singular flat structures [DLR10]. A crucial fact is that length functions of these structures are intersection functions of geodesic currents. This has been recently extended to Hitchin and maximal representations by Martone and Zhang [MZ19] when is compact (see also [BCLS18]).
Let be the convex core of . Our main object of study are geodesic currents on whose support is contained in the subset of geodesics whose projection is in . We refer to these as geodesic currents on and we denote them by . The aim of this paper is to establish structural properties of geodesic currents on in terms of their intersection with closed geodesics, and in particular in terms of their systole. Our motivation comes from the study of compactifications of maximal and Hitchin character varieties: as an application, in the case in which is compact, we construct a natural open domain of discontinuity for the action of the mapping class group of on the Weyl chamber length boundary of these components and show that in the higher rank case this set is not empty (see § 1.3). We will also give explicit examples of actions of on -buildings whose orbit maps are quasi-isometric embeddings and whose length functions are in this set of discontinuity (see § 1.4).
The degree of generality adopted here in our treatment of currents, in particular allowing to have cusps, turns out to be needed in order to understand all the possible degenerations of maximal or Hitchin representations in higher rank groups. If is a non-Archimedean real closed field, the study of maximally framed representations of surface groups into was initiated in [BP17]. In a forthcoming paper we will show how to associate to such a representation a geodesic current whose intersection function on closed geodesics gives the length function, [BIPP21]. Together with the results of this current paper, the assignment is a key tool in the study of the “real spectrum” compactification of maximal and Hitchin character varieties and of its nice algebraic geometric properties (see [BIPP20] for an announcement of the results).
1.1. Decomposition of currents
Given a geodesic current on , we exhibit two laminations with corresponding decompositions of the current and show that the complementary regions are filled by the support of in a specific manner.
We say that a geodesic in is -short if no lift thereof intersects transversally a geodesic in the support of . The terminology reflects the fact that, in an appropriate sense, the topological intersection of two geodesics generalizes to a concept of length. Note that geodesic currents associated to points in the Hitchin and maximal character varieties of a compact surface are binding, that is, they have no -short geodesics. This is no longer the case for currents associated to points in the boundary of such character varieties and the study of -short geodesics will enable us to analyze the structure of such currents.
Given a geodesic lamination consisting of -short geodesics, the current decomposes as a finite sum
[TABLE]
that is orthogonal for the Bonahon-intersection form (see §2 for the definition), where the sum is taken over the complementary regions of , and (respectively ) denote the currents on given by the restriction of to the set of geodesics projecting into (respectively ).
We consider the set of solitary -short geodesics, namely -short geodesics that don’t intersect any other -short geodesic
[TABLE]
and the set of closed -short solitary geodesics:
[TABLE]
Then is a finite collection of pairwise disjoint simple closed geodesics containing the boundary components of . In particular is a geodesic lamination, and is a geodesic lamination refining .
Example 1.1** (See Figure 3).**
Let be a hyperbolic surface of finite area with at least one cusp, and let be a finite lamination consisting of geodesics with all their endpoints in cusps. Let be the geodesic current that corresponds to the measured lamination with a Dirac mass along every leaf of . In this case is the set of boundary components of the smallest subsurface with geodesic boundary containing and .
Theorem 1.2**.**
Let be a geodesic current on the convex core of a geometrically finite hyperbolic surface.
- (1)
*Let be the lamination and let us consider the corresponding decomposition (1.1) of . For every complementary region of , either or every lift of every closed geodesic in intersects transversally the support of . * 2. (2)
Let be the lamination and let us consider the corresponding decomposition (1.1) of . For every complementary region of , either or every lift of every geodesic in intersects transversally .
If is compact, part (1) of Theorem 1.2 has been established independently by Erlandsson and Mondello [EM, § 1.5].
1.2. Systole of a current
In the first decomposition in Theorem 1.2 let , where is the convex hull of the limit set of and let be a complementary region of ; its metric completion is then the quotient of a closed convex subset by a finitely generated subgroup . We can then restrict to the set of geodesics contained in and obtain a current on such that for every closed geodesic contained in . Thus, because of Theorem 1.2(1), in order to study currents on a surface with boundary it is enough to consider currents for which for every closed geodesic contained in the interior of the surface.
For a current on , define then its systole
[TABLE]
where the infimum is taken over all closed geodesics contained in the interior of . Our next results analyze the structure of depending on the vanishing or the non-vanishing of . These results are stated in terms of the intersection properties of with geodesic currents with compact carrier and with compactly supported measured laminations. The carrier of a current on is the closed subset obtained by projecting to all the points lying on the geodesics in the support of . For a compact subset , let
[TABLE]
and let
[TABLE]
Observe that the condition means that any corresponds to a measured geodesic lamination.
It is easy to see that there is a compact set such that any simple geodesic with compact closure in is contained in , so that . Thus we have the following:
Theorem 1.3**.**
Assume that is not the thrice punctured sphere. Let be a compact subset such that . Let be a geodesic current on . Then the following are equivalent:
- (1)
; 2. (2)
the function does not vanish on ; 3. (3)
the function does not vanish on ; 4. (4)
Every geodesic recurrent in intersects transversely some geodesic in the support of .
We say that a geodesic is recurrent in if the projection map from into is not proper. If has no cusps, then property (4) in Theorem 1.3 is equivalent to the current being binding in the sense of [EM, Definition 3.1]. If is compact and , every geodesic is recurrent.
Example 1.4**.**
- (1)
Unlike the case where is closed, in general there are geodesic currents with positive systole and whose support is a lamination: for example if in Example 1.1 we take the lamination such that the complementary regions are ideal polygons, the corresponding current will have positive systole. 2. (2)
The Patterson-Sullivan current (see Example 2.1 (3)) has positive systole.
For the next result we endow the space of geodesic currents on , and hence , with the weak*-topology coming from the dual of the topological vector space of continuous compactly supported functions on . The space of projectivized geodesic currents is then endowed with the quotient topology and, as such, it is compact metrizable (see Proposition 2.6).
Corollary 1.5**.**
- (1)
The systole function is continuous. 2. (2)
For every current on , with and every compact subset , there are constants such that
[TABLE]
for every closed geodesic . Here denotes the hyperbolic length. 3. (3)
The set is open in and the mapping class group of acts properly discontinuously on it.
Remark 1.6**.**
If is a compact surface, in [MZ19] the authors establish interesting systolic inequalities for period minimizing currents with full support, that is, currents with full support such that
[TABLE]
is finite for every . In fact our results imply that the first condition is redundant, that is, every current with full support is period minimizing. Indeed by Theorem 1.3 a current with full support has necessarily positive systole. By Corollary 1.5(3) with this implies the finiteness of the set in (1.2).
Assume now that is a geodesic current on such that for all closed geodesics . Then is the set of boundary components of and is the unique complementary region. According to (1.1) we have a decomposition
[TABLE]
and the next result gives the structure of the geodesic current if the systole of vanishes.
Theorem 1.7**.**
Let be a geodesic current on with positive intersection with every closed geodesic . Then the following are equivalent:
- (1)
; 2. (2)
* corresponds to a measured lamination, compactly supported in , minimal and surface filling.*
We say that a geodesic lamination is surface filling if every complementary region is either an ideal polygon, or an ideal polygon bounding either a boundary geodesic or a cusp.
Remark 1.8**.**
The relation between our results and the ones in [EM] is the following. If is compact, it follows from Theorem 1.2(1) that a current of full hull in the sense of [EM] is one such that for every closed geodesic . Then Theorem 1.3 and Theorem 1.7 show that the dichotomy “" or “” gives for of full hull the dichotomy “ is binding” or “ is a measured lamination". That this is a dichotomy for currents of full hull is the content of [EM, Theorem 3.19].
In general we consider the decompostion
[TABLE]
as a union of subsurfaces with geodesic boundary induced by the set closed -short solitary geodesics. For any such a subsurface and for a geodesic current let
[TABLE]
Combining Theorem 1.3 and Theorem 1.7 we deduce
Corollary 1.9**.**
Let be a geodesic current on a complete hyperbolic surface of finite area , and let be as in (1.3). We have
[TABLE]
where is the geodesic current associated to the closed geodesic . Furthermore, for every for which precisely one of the following holds:
- (1)
either , 2. (2)
or is the geodesic current associated to a measured lamination compactly supported in and surface filling in .
1.3. Positive systole and a domain of discontinuity in the Weyl chamber length boundary
Let be a (not necessarily torsion-free) cocompact lattice and let be either or . Let be the space of -conjugacy classes of representations of in that are Hitchin if or maximal if (see § 7). Our objective is to apply our results on currents to the study of the action of the mapping class group on the Weyl chamber length boundary . Recall (see [Par12]) that is a compact subset of the space of projective classes of functions from to a closed Weyl chamber of , and that a diverging sequence in converges to the projective class of a nonzero function if and only if converges to in , where is the Jordan projection, see (7.2). Let denote a Weyl group invariant norm on the Cartan subalgebra and define the systole of a function by
[TABLE]
Observe that the positive systole subset
[TABLE]
of is well-defined and independent of the choice of the norm .
The next result is a consequence of Corollary 1.5 and [MZ19, Theorem 1.1]:
Corollary 1.10**.**
Let be a cocompact lattice and let be the character variety of representations of in that are either Hitchin or maximal.
- (1)
* is an open subset of .* 2. (2)
For every there are constants such that, for every hyperbolic element ,
[TABLE]
where is the translation length of in . 3. (3)
Assume that is torsion-free. Then the mapping class group of acts properly discontinuously on .
Note that if and is torsion-free, is the Thurston boundary of the Teichmüller space of and it is well-known that for every . It is a striking fact that it is not anymore the case when has higher rank.
Corollary 1.11**.**
*Let be any compact hyperbolic surface, and with or with . Then the positive systole subset is non-empty. *
It is a natural question whether length functions if correspond to some kind of geometric structures on the surface . In the case where , one can show using [GM91] that corresponds to the Teichmüller space of semi-translation structures . We will study this case in further details in a forthcoming paper.
Another interesting feature of the positive systole subset is its relationship with entropy. This uses [MZ19, Corollary 1.5].
Corollary 1.12**.**
Let be a compact hyperbolic surface and or . Assume that is a sequence in converging to a point of . Then we have for the entropy of :
[TABLE]
The first examples of such sequences were obtained by X. Nie [Nie15] for and by T. Zhang in [Zha15a] for (see also [Zha15b]). Examples 1.15 and 1.16 below satisfy this property.
Corollary 1.11 is in fact a consequence of next theorem (Theorem 1.13) concerning the Weyl chamber length boundary of the Hitchin component of a hyperbolic triangle group
[TABLE]
Theorem 1.13**.**
Let be a hyperbolic triangle group and or . Then for every
[TABLE]
1.4. Actions on buildings
Recall that any projectivized function in is the -valued length function of an action of on an affine Bruhat-Tits building, that is typically not simplicial, see [Par12]. In the case where has positive systole, that is , by Corollary 1.10(2) the action of is displacing in the sense of [DGLM11], and in particular orbit maps are quasi-isometric embeddings.
Explicit examples of -actions on a simplicial building whose length function belongs to can be obtained as follows from representations , where is the field of rational functions. Let be the field of Laurent series endowed with its canonical non-Archimedean -valued valuation for which . Let be the Bruhat-Tits building of . The -valued length of in is its Jordan projection
[TABLE]
where are the eigenvalues of (see § 7).
Corollary 1.14**.**
Assume that is a representation such that
- (i)
* has a pole at infinity for some , and* 2. (ii)
for all large enough, the specialization of at is a Hitchin representation.
Then
- (1)
. 2. (2)
*Any -orbit in is a quasi-isometric embedding. *
We now give explicit examples of representations of triangle groups satisfying the hypotheses of Corollary 1.14.
Example 1.15**.**
For , define
[TABLE]
According to the main result of [LRT11], belongs to the -Hitchin component of for every . In addition one verifies that
[TABLE]
Example 1.16**.**
The following example is due to Goldman, [Gol88, §6]. Let with . Consider the following matrix with coefficients in , where for ,
[TABLE]
Define where are the canonical basis vectors of . Then
[TABLE]
define a representation , whose specialization at all is Hitchin. In addition a computation gives
[TABLE]
hence satisfies the hypotheses of Corollary 1.14, provided .
1.5. Outline of the paper
After some preliminaries on currents in § 2, we study in § 3 a general set of geodesics in and associate to it a lamination using the intersection graph of . If is invariant under , we deduce, using the structure of complementary regions of laminations in , general results from which Theorem 1.2 follows.
The main goal of § 4 is to show that the systole of a current can be computed using only simple closed geodesics, provided is not the thrice punctured sphere. To this end we associate to any geodesic current on a pseudo-distance on that is a modification of a pseudo-distance introduced by Glorieux [Glo] and which has the advantage of being additive on colinear triples of points. When is a geodesic current on a hyperbolic surface , this pseudo-distance leads to a pseudo-length for paths and closed curves on and the main point consists then in showing a Length-Shortening-Under-Surgery Lemma (Lemma 4.9). This is essential in the proof of Theorem 1.3 and Theorem 1.7.
In § 5 we deal with currents of positive systole. The main point in the proof of Theorem 1.3 consists in showing that positive systole currents do not admit -short recurrent geodesics. This is shown in Proposition 5.1 using the classical Closing Lemma.
In § 6, we prove Theorem 1.7, which follows essentially from a study of geodesic laminations consisting of -short geodesics.
In § 7 we apply the results on currents to the study of the Weyl chamber length boundary of the Hitchin or maximal components of a cocompact lattice . Beside the results of [MZ19], an essential input is Theorem 7.2 establishing that for a hyperbolic triangle group , -invariant non-vanishing currents have positive systole. The basis for the construction of the explicit examples in § 1.4 is Corollary 1.14, which relies on Theorem 7.2 as well as on Puiseux’s theorem on the representability of elements of a specific real closure of by convergent Puiseux series.
2. Preliminaries on currents
A geodesic current is a positive Radon measure on the space of unoriented, unparametrized, geodesics in . The topology on is obtained by identifying this space with the quotient by the flip of the space of pairs of distinct points in the boundary of the hyperbolic plane . Via this identification we will think of a geodesic current as a -invariant positive Radon measure on the locally compact space .
Let be a torsion-free discrete subgroup and be the quotient hyperbolic surface. We denote by the corresponding projection.
A geodesic current on is a -invariant geodesic current.
Examples 2.1**.**
The following examples of geodesic currents will play an important role in the rest of the paper:
- (1)
The Liouville current is the unique (up to positive scaling) -invariant Radon measure on . It is of course -invariant for every subgroup . 2. (2)
Let be a geodesic in . Then the set of lifts of to is a -orbit in , which is discrete in if and only if is closed as a subset of . Then the sum of the Dirac masses along this orbit is a geodesic current on . 3. (3)
Let be the unit disk model of and be a discrete subgroup. For a -density on is a probability measure such that where
[TABLE]
For instance the round measure
[TABLE]
is a 1-density for . Given a -density , the measure on given by
[TABLE]
is then a -invariant current.
When is finitely generated, and is the critical exponent of , there is a unique -density on ; its support is precisely the limit set and the corresponding measure is the Patterson–Sullivan current. It is thus a current on the convex core of and every recurrent geodesic in intersects transversely a geodesic in the support of . It follows from Theorem 1.3 that and satisfy the conclusion of Corollary 1.5 (2).
Recall that if are two geodesics, their intersection number is defined as
[TABLE]
Then the intersection of two currents on is defined as follows (see [Bon01] or [Mar]). Let
[TABLE]
then acts properly on the open set and so does . The intersection is then the -measure of any Borel fundamental domain for the -action on . We will often denote by .
Examples 2.2**.**
- (1)
Given two distinct closed geodesics in , the intersection is the minimal geometric intersection number between two closed curves in the free homotopy classes represented by and . Instead is the number of self intersections of the geodesic , so for example if and only if is simple. 2. (2)
If is a closed geodesic in and is its hyperbolic length, then we have
[TABLE]
The set of geodesic currents on is a convex cone in the dual of the space of compactly supported functions on ; the latter is provided with the topology of inductive limit of Banach spaces and will be equipped with the corresponding weak* topology. Given a geodesic current on , its support is a closed -invariant subset; as mentioned in the introduction, we call the carrier of and denote by the closed subset of consisting of the projection to of the union of all points on all geodesics in . For , we denote by the subset of geodesic currents on with carrier included in .
It is straightforward to verify that if is any current on and has compact carrier, then .
Example 2.3**.**
The geodesic current on from Example 2.1(2) is a geodesic current on if and only if is either a closed geodesic or an ideal geodesic, that is a geodesic connecting two cusps of . This is the case in Figure 3.
One of the most fundamental facts concerning the intersection is the following continuity property due to Bonahon:
Theorem 2.4** ([Bon86, § 4.2]).**
For every compact subset , the intersection
[TABLE]
is continuous.
This continuity relies on the following crucial technical point that we will use in this paper and that can be found for example in [Mar, Proposition 8.2.8]. It rules out a situation in which a geodesic current may have a “one-sided” atom. Recall that a pencil is a subset of of the form where is a Borel subset not containing . The lemma holds as stated for any hyperbolic surface . If is geometrically finite, then a point in the limit set is conical if and only if it is not a cusp.
Lemma 2.5**.**
Let be a geodesic current on . Assume that is a conical limit point and the pencil does not contain the axis of a hyperbolic element. Then
[TABLE]
For our purposes we will need the following compactness property, which can be derived from the arguments in [Bon88, Proposition 4].
Proposition 2.6**.**
- (1)
Let be compact and let be the Liouville current on . Then the set
[TABLE]
is compact and hence is compact. 2. (2)
The space is compact.
Proof.
The proof of (1) follows the one in [Bon88, Proposition 4] observing that, since , any non-zero current on has positive intersection with . For the second assertion replace [Bon88, Proposition 4] by the following lemma. ∎
Lemma 2.7**.**
Let be a current on with compact carrier such that every geodesic in projecting into intersects transversally a geodesic in the support of . Let be continuous with compact support such that for every boundary component of , for some lift of . Then the set
[TABLE]
is compact.
The proof of Lemma 2.7 is a straightforward modification of the proof of [Bon88, Proposition 4]. The lemma implies Proposition 2.6(2) by observing that the set
[TABLE]
is compact and the projection map is a continuous bijection.
We refer for instance to [Mar, §8.3.4] for the notion of measured geodesic lamination on a general hyperbolic surface , and the bijective correspondence between geodesics currents on with , equivalently such that no two geodesics in the support of intersect transversally, and measured geodesic laminations on .
3. Decompositions
Let be a hyperbolic surface (not necessarily complete) and a subset. We denote by the set of unoriented, unparametrized geodesics of that are contained in . Given a geometrically finite surface with convex core and an arbitrary subset of geodesics, our aim is to show how one can associate two laminations and respectively, such that their complementary regions are either completely avoided by or filled by in two specific ways (see Proposition 3.2 and 3.3). Applying these propositions to the support of a geodesic current on will imply Theorem 1.2. In § 3.1 we start by studying the case of a subset of , then move to geometrically finite surfaces in § 3.2, where we establish the main propositions. We show in § 3.3 how to deduce Theorem 1.2.
3.1. The lamination associated to a subset of geodesics in
Given a subset its intersection graph, , is the graph whose vertex set is and two vertices are adjacent if . We say that is -connected if is connected; an -connected component (-cc) is then the set of vertices of a connected component of . We proceed to define the lamination associated to , this relies on classical properties of convex hulls in .
For let be the convex hull of the union of the geodesics in , namely the intersection of all convex subsets containing . Whenever , then is in general neither open nor closed but its closure is the closed convex hull of the set of extremities of geodesics in . Each connected component of is an interval to which we can associate the geodesic connecting its endpoints; the boundary of in is the disjoint union of the set of all such geodesics.
Let
[TABLE]
be the closure in the space of the set of the boundary geodesics of convex hulls of -connected components of . Notice that the boundary of the closure of is a lamination for every -cc and the gist of next proposition is to show that is a lamination as well.
Given any subsets we set
[TABLE]
Observe that if and only if some intersects transversally some . Then
[TABLE]
is a closed subset of and if , then . Setting , then , and is a lamination, since .
Lemma 3.1**.**
Let be a geodesic and an -cc of . If , then . As a consequence
[TABLE]
for every two -cc of .
Proof.
If for every , every is contained in one of the two closed half planes defined by , and since is -connected, the same holds for , implying for every .
Let be distinct -cc, , and assume . By the claim there is with and hence with , a contradiction. Thus . ∎
Proposition 3.2**.**
Let be a set of geodesics and as defined in (3.1). Then
- (1)
* is a lamination and . In particular ;* 2. (2)
for any complementary region of one of the following holds
- (a)
either no geodesic of meets , or 2. (b)
* is an -connected component of , and . In particular every geodesic meeting must intersect transversally some geodesic in .*
Proof.
It is immediate from Lemma 3.1 that is a lamination and . We will prove that after having proven (2).
If is a complementary region and intersects then since . Thus, the -cc-component of is formed of geodesics all in and hence . Since , we conclude that , thus proving (2).
We now complete the proof of (1). Since , it follows that . If , then there is an -cc with which by Lemma 3.1 would imply that , a contradiction. Thus .
Conversely, if , then since is a lamination, there is a complementary region of with . Since , if follows from (2b) and Lemma 3.1 that no geodesic of intersects nontrivially and hence . Since , the region must have a least four ideal vertices and hence there is with implying , a contradiction. ∎
3.2. The structure of subsets of geodesics in
Let now be a geometrically finite hyperbolic surface and its convex core. The covering projection induces a map still denoted by . For we define as the sum of where runs through a fundamental domain for the -action on ; if are distinct closed geodesics this recovers the usual intersection number. For subsets we extend the definition of to as in §3.1, and define analogously. Given we consider the set of solitary elements among the set of closed geodesics in , that is
[TABLE]
Observe that if is the support of a geodesic current on , is nothing but the set defined in the introduction. In general consists of simple, closed, pairwise disjoint geodesics and contains all the boundary components of . In particular is a geodesic lamination and furthermore it induces a partition of :
[TABLE]
where the disjoint union is over all complementary regions of and .
Proposition 3.3**.**
Let be a subset of , and let be as in (3.2). Then for every complementary region of precisely one of the following holds:
- (1)
either no geodesic of meets , 2. (2)
or any closed geodesic meeting must intersect transversely some geodesic of .
The proof of Proposition 3.3 uses the structure of complementary regions of a compactly supported geodesic lamination in a complete finite area hyperbolic surface. Namely that the complement is a finite union of components of the following types [CEG06, Theorem I.4.2.8]:
- (1)
an ideal polygon; 2. (2)
an ideal polygon containing one cusp; 3. (3)
a totally geodesic subsurface with geodesic boundary to which one has added a crown to some boundary geodesic (such a subsurface can possibly be reduced to a single geodesic).
A crown is an infinite cylinder bounded by a geodesing on one side and by finitely many ideal sides on the other. We will need the following
Lemma 3.4**.**
Let be a geodesic bounding a crown . Any closed geodesic intersecting intersects a leaf of .
Proof.
Assume by contradiction that there exists a closed geodesic that intersects but doesn’t intersect any leaf of . We choose intersecting lifts of in . The lift of which is bounded by on one side is an infinite strip, bounded on the other side by countably many geodesics indexed so that shares the endpoint with . Since doesn’t intersect any leaf of , there exists such that is an endpoint of . We denote by the hyperbolic element with axis , and assume without loss of generality that . Then for a sufficiently high power of , intersects and . This implies that intersects the lamination , a contradiction. ∎
Proof of Proposition 3.3.
Let : is a closed geodesic and . We apply Proposition 3.2 to the -invariant set of geodesics and let be the corresponding lamination. Set . Since , we have the following inclusion: .
Claim**.**
In fact .
Proof.
∎Note that, denoting , we have , hence . Since \widetilde{B}=\widetilde{A}^{0}\cap\{\text{closed geodeiscs of \Sigma}\}, this implies that a leaf of is in if and only if projects to a closed geodesic. Recall now that
[TABLE]
As is closed, it is then enough to show that for all .
Let be an -cc of and assume first that . Then and , so that . Assume now that and let . Then is a complementary region in of the lamination . For the sake of contradiction, assume that the boundary of contains a leaf that does not close in ; by the structure of complementary regions [CEG06, Theorem I.4.2.8], the projection of this leaf is then part of a crown bounded by a simple closed geodesic ; moreover since , contains at least a pair of intersecting closed geodesics and hence the region is not reduced to a crown, implying . Let be a lift of . Since , where , Proposition 3.2 (2) implies that no geodesic in meets , hence . If is a closed geodesic with , then for a suitable lift of we have and thus by Lemma 3.4. This implies , hence and which shows that , a contradiction.
Let now be a complementary region of and assume that some geodesic of intersects . Let be a closed geodesic intersecting . Let be a complementary region of lifting and a lift of intersecting . Since intersects no geodesic of can intersect (Proposition 3.2(2)) and hence , that is , hence . ∎
We now combine Proposition 3.2 and Proposition 3.3 to obtain a refined decomposition of associated with analogous to Theorem 1.2.
Proposition 3.5**.**
Let be a subset of and . Let , where is the lamination associated to by Proposition 3.2 and . Then is a lamination and we have
- (1)
*; in particular *
[TABLE]
where runs over the complementary regions of and . 2. (2)
For every complementary region of precisely one of the following holds:
- (a)
either does not meet any geodesic of . 2. (b)
or every geodesic of meeting intersects transversely some geodesic in . 3. (3)
* does not meet any of the complementary regions of meeting no geodesic of .* 4. (4)
For every closed geodesic , if , then . 5. (5)
* is the set of closed leaves of .*
Proof.
We implicitly use that the assertions of Proposition 3.2 hold true verbatim once projected to .
First observe that, because of Lemma 3.1, we have , hence is a lamination. The statements (1) and (5) are clear as and are included in by definition, and the closed geodesics in are in .
The dichotomy (2) is true for by Proposition 3.2, hence also for as refines and is contained in .
To see (3), observe that if is a complementary region of such that , then there is a geodesic in contained in , since is a lamination refining . But then on one side of there must be a geodesic in that meets .
Assertion (4) follows from (3) as, by Proposition 3.3, any closed geodesic with is either in or contained in a complementary region of meeting no geodesic of . ∎
3.3. Proof of Theorem 1.2
Let be a geodesic current on , its support and . Observe that by definition a geodesic in is -short if some (and hence every) lift of satisfies . This implies that and . Then Theorem 1.2(1) follows from Proposition 3.3 and Theorem 1.2(2) follows from Proposition 3.5.
4. Straight pseudo-distance, length shortening and systole
The main objective of this section is to show that the systole of a current on a finite area surface with geodesic boundary can be computed using simple closed geodesics, provided is not the thrice punctured sphere (Corollary 4.8). This relies on two main ingredients:
- (1)
the fact that a geodesic current gives rise to an appropriate pseudo-distance on and that the length function associated to this pseudo-distance behaves very much like the hyperbolic length. A similar study, in the case of closed surfaces, was carried out by Glorieux in [Glo]. 2. (2)
A Length-Shortening-Under-Surgery Lemma in the spirit of [MZ19], with the additional difficulty due to the presence of boundary components.
A pseudo-distance on is a symmetric function vanishing on the diagonal and verifying the triangle inequality. We say that a pseudo-distance is straight if whenever three points lie on a geodesic segment on (for the hyperbolic metric) in this order, we have
[TABLE]
We emphasize that such a pseudo-distance is not necessarily continuous for the standard topology on .
We now turn to the construction of a straight pseudo-distance associated to a geodesic current on . Given a geodesic current on , define for :
[TABLE]
where for a possibly empty geodesic segment we define
[TABLE]
Proposition 4.1**.**
The function is a straight pseudo-distance.
Proof.
By definition is symmetric and vanishes on the diagonal.
In order to check the triangle inequality we may assume that the points are pairwise distinct.
If , then either or . If , then either or . If on the other hand , then either or otherwise contains the segment which implies that don’t lie on a geodesic and hence .
x$$y$$z
This shows the inclusion
[TABLE]
An analogous argument shows the corresponding statement for and concludes the proof of the triangle inequality.
If the three points lie on a geodesic in this order, then is the disjoint union of and and analogously for . This implies that and hence is straight.
∎
Example 4.2**.**
- (1)
If is the Liouville current on , the corresponding pseudo-distance is the hyperbolic metric . 2. (2)
If is a geodesic current on such that is a geodesic lamination, a standard argument shows that the quotient metric space , obtained by identifying points at -distance zero, is [math]-hyperbolic in the sense of Gromov and can therefore be canonically embedded in a complete -tree (see [MS91] for instance).
Given a straight pseudo-distance on we define as usual the length of a continuous path , by
[TABLE]
Of course is invariant by monotone continuous reparametrization. The statements in the following lemma are straightforward verifications.
Lemma 4.3**.**
The length function associated to a straight pseudo-distance has the following properties:
- (1)
If is a continuous path, then and if parametrizes a geodesic segment, equality holds. 2. (2)
If a path is the concatenation of two paths , then
[TABLE]
Let now be a torsion-free discrete subgroup and be the corresponding quotient surface. Given a -invariant straight pseudo-distance on we define the length of a continuous path as the length of any continuous lift .
The following generalizes a fundamental property of hyperbolic length to length functions associated to straight pseudo-distances.
Proposition 4.4**.**
Let be a closed geodesic represented by a hyperbolic element and let be a point on the axis of . Then for every closed loop in the free homotopy class of
[TABLE]
Using the definitions of the length of a curve in and Lemma 4.3, the above proposition is a direct consequence of the following:
Lemma 4.5**.**
With the hypotheses of Proposition 4.4
[TABLE]
Proof.
Using that is straight, -invariant, and applying the triangle inequality we obtain for all :
[TABLE]
Dividing by and letting tend to infinity we obtain the lemma. ∎
Assume now that is finitely generated. Let be the closed convex hull of the limit set of and be the quotient surface, which is a complete hyperbolic surface with geodesic boundary and finite area, included in . Let be the interior of . Define
[TABLE]
Our objective is to show:
Proposition 4.6**.**
Let be a finite area surface with geodesic boundary and be the length function associated to a -invariant straight pseudo-distance on .
- (1)
If is not the thrice punctured sphere, . 2. (2)
If is the thrice punctured sphere
[TABLE]
Before indicating the proof of Proposition 4.6 we establish the link with the systole of a current. Let thus be a geodesic current on , and let be the invariant straight pseudo-distance on and be the corresponding length function on curves in .
Lemma 4.7**.**
Let be a closed geodesic. Then .
Proof.
Let be a hyperbolic element representing and let be a point on its axis . Then we have (by Proposition 4.4):
[TABLE]
Observe that as well as are Borel fundamental domains for the -action on and hence their -measure equals by definition. ∎
Lemma 4.7 and Proposition 4.6 now lead to the main result of this section concerning the systole of .
Recall that
[TABLE]
and
[TABLE]
Then
Corollary 4.8**.**
Let be a geodesic current on a finite area hyperbolic surface with geodesic boundary.
- (1)
If is not the thrice punctured sphere,
[TABLE] 2. (2)
If is the thrice punctured sphere and the carrier of is not included in ,
[TABLE]
Proof.
(1) This statement follows from Proposition 4.6(1) and Lemma 4.7.
(2) Since the carrier of is not contained in the boundary of , there is a geodesic in the carrier of . But intersects then transversally at least one closed geodesic with one self-intersection. The claim follows then from Proposition 4.6(2).∎
We now indicate the main steps in the proof of Proposition 4.6. It relies on a “Length-Shortening-Under-Surgery” property and standard arguments from surface topology. In the sequel we will use the notation for distinct loops as the minimum intersection number of loops in the free homotopy classes represented by and . Instead we will denote by the number of self-intersections of .
Let now be a closed geodesic with at least one self-intersection point . Choose a parametrisation and such that . Then is the concatenation of and ; let also denote the loop with opposite orientation and let be the concatenation of and .
<$$<$$c_{1}$$c_{2}$$p
Observe that
[TABLE]
The following is an immediate consequence of Proposition 4.4:
Lemma 4.9**.**
If for , if is freely homotopic to the closed geodesic , then .
Given a closed geodesic with positive self-intersection, let denote the subsurface filled by , that, we recall, is obtained by taking a regular tubular neighborhood of and adding to it all the components of the complement that are either simply connected or whose fundamental group is cyclic. Standard arguments in surface topology, combined with Lemma 4.9 then imply:
Lemma 4.10**.**
- (1)
If is a closed self-intersecting geodesic, we have for every connected component of :
[TABLE] 2. (2)
Given a closed geodesic with positive self-intersection, there exists a closed geodesic in with and . In particular is a thrice punctured sphere.
Proof of Proposition 4.6.
- (1)
Let be a closed geodesic with positive self-intersection; by Lemma 4.10(2) there is a closed geodesic in with and . Since is a thrice punctured sphere and is not, there is a boundary component of which is a simple closed geodesic contained in ; Lemma 4.10(1) implies then that and this shows that . 2. (2)
Follows immediately from Lemma 4.10(2).
∎
Remark 4.11**.**
Lemma 4.9 is Proposition 4.5 in [MZ19] for the case where is compact. We believe that the use of pseudo-distance associated to a current simplifies the arguments.
5. Currents with positive systole
This section is devoted to the proofs of Theorem 1.3 and Corollary 1.5.
Let then be finitely generated and torsion-free, the quotient surface and the corresponding finite area surface with geodesic boundary.
Let be a geodesic current on and recall that a geodesic is -short if some (and hence any) lift of does not intersect transversally any geodesic in the support of . The main ingredients in the proof of Theorem 1.3 are the results on systoles established in § 4 together with the following proposition, establishing the implication (1) (4) of Theorem 1.3.
Proposition 5.1**.**
Let be a geodesic current on and a -short geodesic that is recurrent in . Then for all , there exists a closed geodesic in such that .
The hyperbolic metric on and induces Riemannian metrics on the respective unit tangent bundles and , denoted , for which the projection maps are Riemannian submersions; as usual will denote the hyperbolic distance on and . We denote by the geodesic flow action on .
We will use:
Closing Lemma**.**
[Ebe96, 4.5.15]** Given a compact set and , there exist and such that if there is , and with , then there is with and with and .
Proof of Proposition 5.1.
We may suppose that is not closed (otherwise the statement is clear). Recall that is recurrent in if there exists a sequence in with and stays in a fixed compact subset of . Modulo reparametrizing with opposite orientation, we may assume that the sequence is monotone increasing with . Let be an accumulation point of the sequence ; enlarging we may assume . Let be the unit speed geodesic with , and be a lift of .
Claim**.**
For all , and for all except at most countably many, there exists so that .
Proof.
∎Let be such that . Then for any , is an accumulation point of the sequence . Let be a lift of ; we claim that the set of points such that is at most countable. Indeed, the family of Borel subsets are pairwise disjoint; since is -finite, the claim follows. Thus replacing by for some appropriate we may assume that is the projection of a point such that . Since , we may now choose such that , where is the closed ball centered at of radius for the hyperbolic metric.
Possibly decreasing we may in addition assume that is smaller than and the injectivity radius at . In particular, the projection sends isometrically to , the corresponding metric ball in , and . As is not closed, is never tangent to , so we may assume that never belongs to . Passing to a subsequence we may now assume that all points are on the same side of in .
Claim**.**
If is a closed loop obtained by concatenation of and the geodesic segment joining and in , then
[TABLE]
where is the length function corresponding to .
Proof.
∎We have
[TABLE]
The first summand vanishes because is -short; for the second summand observe that since and are on the same side of in , the geodesic segment is disjoint from , contained in and as a result
[TABLE]
Now let and let be the compact set consisting of unit tangent vectors based at a point of ; let and be the corresponding constants given by the Closing Lemma. We may assume and choose such that . We can pick so that and we have
[TABLE]
Let be the closed loop obtained by concatenation of and the geodesic segment joining and in . Let be the unique lift with and let be such that . Then it follows from (5.1) that
[TABLE]
and hence it follows from the Closing Lemma that is hyperbolic and that its axis contains a point with , in particular . The projection to of the axis of gives us then a closed geodesic contained in and for which (see Proposition 4.4 and Lemma 4.7). This concludes the proof. ∎
Proof of Theorem 1.3.
We will show that the contrapositions of properties (1), (2), (3), (4), denoted (1)’, (2)’, (3)’, (4)’, are equivalent.
(1)’ (2)’: Assume . Since is not the thrice punctured sphere, we have by Corollary 4.8(1). Let thus be a sequence of simple closed geodesics in with , in particular
[TABLE]
Now the sequence of currents is contained in . Since the latter space is compact (see Proposition 2.6 and the remark preceding Theorem 1.3), this sequence has a accumulation point, say , in for which and , in particular . This shows the announced implication.
(2)’ (3)’: clear.
(3)’ (4)’: let , with and . Then any geodesic does not intersect transversally any geodesic of ; such a geodesic is -short by definition and recurrent since .
(4)’ (1)’: This is the content of Proposition 5.1. ∎
Proof of Corollary 1.5.
(1) If is the thrice punctured sphere the assertion follows from Proposition 4.6(2). We may hence assume that is not the thrice punctured sphere. Let be a convergent sequence in with limit . Since for every closed geodesic , then and hence is continuous if .
Let and assume by contradiction that
[TABLE]
For every , it follows from Proposition 4.6(1) that there exists a simple closed geodesic with
[TABLE]
If is unbounded, without loss of generality we may assume that and that the sequence converges to a compactly supported measured lamination . But then
[TABLE]
which, by Theorem 1.3, implies that , a contradiction.
Hence, by passing to a subsequence, we may assume that for all , and thus
[TABLE]
which is a contradiction.
(2) Assume that the first inequality does not hold. Then there is a sequence of closed geodesics contained in such that
[TABLE]
Using that
[TABLE]
is relatively compact (see Proposition 2.6(1)), let , for , be an accumulation point of this sequence. Then , which contradicts Theorem 1.3(3). An analogous argument leads to the second inequality.
(3) Let be a sequence of homeomorphisms fixing pointwise and such that in the mapping class group of . Since is locally compact, it suffices to show that if and is any accumulation point of , then . Let be a closed geodesic such that
[TABLE]
where is the closed geodesic in the free homotopy class of . Then it follows from the first inequality in (2) that
[TABLE]
Let be a subsequence and such that
[TABLE]
In particular we have that
[TABLE]
which implies that . using the continuity of the systole map, we get that
[TABLE]
∎
6. Currents with vanishing systoles and laminations
In this section we establish Theorem 1.7 which characterizes geodesic currents with vanishing systole that occur as components in the decomposition theorem.
The main tools are Theorem 1.3 and the following proposition that is of independent interest.
Proposition 6.1**.**
Let and be a geodesic lamination without isolated leaves and consisting of -short geodesics. Then for any closed geodesic bounding a crown of a complementary region of we have
[TABLE]
Let be the lift to a -invariant geodesic lamination of and let be a complementary region of . Then is bounded by leaves of whose endpoints in are the vertices of . We now make the following crucial observation: let be consecutive vertices of ordered such that is positively oriented; since has no isolated leaf, the pencil does not contain the axis of a hyperbolic element; in addition, is in the limit set of and cannot be a cusp since otherwise would have an isolated leaf. Therefore, the hypothesis of Lemma 2.5 are fulfilled and hence
[TABLE]
Lemma 6.2**.**
Let be a sequence of consecutive vertices of a complementary region labelled in such a way that is positively oriented. Then the geodesic is -short.
Proof.
The proof proceeds by recurrence. For the statement holds. Let us now suppose . We have the following equalities:
[TABLE]
Using that is -short, the induction hypothesis that is -short and the observation preceding Lemma 6.2, we get to the conclusion that is -short. ∎
Proof of Proposition 6.1.
Let be a crown in the complement of the lamination , and let be a geodesic bounding . We choose lifts to in such a way that the half plane to the left of contains a lift of the crown .
\mathcal{C}$$\gamma
\gamma_{+}$$\gamma_{-}$$x_{i+k}$$x_{i+k-1}$$x_{i}$$x_{i-k}$$\gamma^{-1}p$$p$$\gamma p$$\widetilde{\mathcal{C}}$$\gamma^{-1}\widetilde{\mathcal{C}}
Then has consecutive ideal sides , , labelled in such a way that is positively oriented. Now observe that
[TABLE]
By Lemma 6.2 is -short, so that is -short since the set of -short geodesics is a closed subset of . ∎
Proof of Theorem 1.7.
Let be a geodesic current as in the statement of Theorem 1.7 and in the remark preceding it.
(2) (1): Follows from Theorem 1.3 since and .
(1) (2): Since , Theorem 1.3 implies the existence of with and . Let be the corresponding geodesic lamination and observe that it consists of -short geodesics. The projection of to is a compact subset of by hypothesis. An isolated leaf of is necessarily a closed geodesic: but and by assumption , hence cannot be -short. Thus has no isolated leaves. Let be a minimal component of ; then satisfies all the assumptions of Proposition 6.1 and since for every closed geodesic we deduce that a complementary region of in is either an ideal polygon, an ideal polygon containing one cusp, or an ideal polygon bounding a component of [CEG06, Theorem I.4.2.8]. We show now how this fact implies that where is the lift of to .
Let and assume that is not a leaf of . Since all leaves of are -short, cannot intersect transversally a leaf of , hence it is contained in a complementary region of . The specific structure of implies that if are the endpoints of , one of has to be a vertex of . If corresponds to a complementary region of bounding a cusp or a crown, it has infinitely many vertices and if it is an ideal polygon it must have at least four vertices since is not a side of . In any case we can find a geodesic connecting two vertices of and intersecting in one point. By Lemma 6.2, is -short and this contradicts the assumption that . Thus and by minimality of we have equality. ∎
7. On the Weyl chamber length compactification
Let be a cocompact lattice and a representation. Recall that when , is Hitchin if it lies in the connected component of containing the restriction to of the irreducible -representation of , while if it is maximal if the restriction of to some (and hence any) torsion-free subgroup of finite index is maximal (see [BIW10, BIW14] for the relevant facts concerning maximal representations). The space is then the topological space obtained by taking the quotient by -conjugation of the set of representations that are Hitchin if or maximal if .
Let be the Jordan projection on a closed Weyl chamber and let be defined by , where refers to the -conjugacy class of , while is the projective class of the length function . The Weyl chamber length boundary of is then defined by
[TABLE]
where the intersection is over all compact subsets (see [Par12]). For our purposes we make the following choices of Weyl chamber and describe the corresponding Jordan projection as well as the specific norm we use:
- (1)
If ,
[TABLE]
and
[TABLE]
where are the eigenvalues of counted with multiplicity. Then for ,
[TABLE] 2. (2)
If ,
[TABLE]
and is defined as in (7.2), where here however are the eigenvalues of of absolute value . If , then
[TABLE]
We will make crucial use of the results in [MZ19] that establish a relation between length functions and geodesic currents. In fact, fix a torsion-free normal subgroup of finite index, and . Then acts on the space of currents on ; the action factors via the finite group and the space of -invariant currents is a closed subset of . The following is a direct consequence of [MZ19]:
Corollary 7.1**.**
For every there is a unique current such that for every
[TABLE]
where is the closed geodesic corresponding to .
Proof.
Assume is Hitchin. Then is Hitchin as well and there exists a unique -invariant Frenet curve into the variety of full flags (see [MZ19, Definition 3.2] and [Lab06, Theorem 4.1]). But then, given any , the assignment is -equivariant Frenet as well, and hence coincides with . The current associated to is uniquely determined by its value on rectangles, that is whenever is a positive -tuple in , then
[TABLE]
where is a specific -invariant of -tuples of complete pairwise transverse flags (see [MZ19, Lemma 3.6]). This, together with the -equivariance of , implies that is -invariant.
The argument for maximal representations is completely analogous by using the continuous -equivariant map into the space of Lagrangians that sends positive triples to positive triples. One concludes by uniqueness that is -equivariant, which implies that the current associated to (see [MZ19, § 3.2]) is -invariant. ∎
Proof of Corollary 1.10.
Observe that any is homogeneous, namely for . As a result, does not vanish identically and the map
[TABLE]
is well defined and continuous.
The map that to a projectivized current associates its projectivized intersection function is a homeomorphism onto its image [Ota90], and by [MZ19, Theorem 1.1, Theorem 3.4 and Corollary 3.11], its image contains and hence . Thus
[TABLE]
and the assertions of Corollary 1.10 follow from the corresponding ones in Corollary 1.5. ∎
Next we show how Corollary 1.11 can be deduced from Theorem 1.13 and [ALS18, Theorem B]. If and with or with , then is a positive dimensional cell, in particular . Since contains a torsion-free subgroup of index representing a genus surface, any as in Corollary 1.11 is isomorphic to a torsion-free subgroup of of finite index and Theorem 1.13 implies that .
In the case of one can take ; then is non-compact as it contains the Hitchin component that is homeomorphic to by [ALS18, Thm B], contains a torsion-free subgroup of index representing a genus surface and the same argument as above allows us to conclude. Theorem 1.13 is in turn an immediate consequence of Corollary 7.1 and the following:
Theorem 7.2**.**
Let be a hyperbolic triangle group, a torsion-free subgroup of finite index and . Then for any non-vanishing current ,
[TABLE]
Proof.
First we show that if with , then as current on it cannot be a measured lamination. Otherwise let be the -tree dual to . Since is -invariant, acts by isometries on the complete -tree . The subset and of -fixed, respectively -fixed, points are not empty. Since is complete and has a fixed point in , this implies that and hence has a fixed point in .
On the other hand pick representing a closed geodesic in with . Then in the tree the element acts as a translation of length along its axis. This is in contradiction with the fact that has a fixed point.
Now let , . Then the set of closed -short solitary geodesics is -invariant, and hence is a -invariant measured lamination on , which implies that . Since , Theorem 1.2(1) implies that for every closed geodesic . If now , Theorem 1.7 implies that is a measured lamination, which is impossible by the preceding discussion. Hence , which concludes the proof. ∎
Proof of Corollary 1.12.
Let be a sequence in converging to a point of . Let be the current with
[TABLE]
where is any hyperbolic element with corresponding closed geodesic . By [MZ19, Corollary 1.5], we have that
[TABLE]
where is a constant only depending on . We will now show that
[TABLE]
which will imply the corollary. Let be the geodesic current associated to a binding multicurve in . Then, by compactness of , up to extracting we have that converges to some non zero current . Then by continuity of we have
[TABLE]
for all hyperbolic with corresponding closed geodesic . As this implies that and for all for some representant of . In particular we have . By continuity of the systole (Corollary 1.5(1)) we have that
[TABLE]
As and , this implies that . ∎
Turning to Corollary 1.14, we define now the Jordan projection
[TABLE]
for . Let
[TABLE]
be an algebraic closure of . The valuation defined on extends uniquely to by
[TABLE]
if
[TABLE]
for . Given , we order the eigenvalues of so that
[TABLE]
Let be the Euclidean norm restricted to . We have:
Lemma 7.3**.**
Let denote the translation length of computed with respect to the CAT(0)-metric in . Then
[TABLE]
Proof.
Let be the splitting field in of the characteristic polynomial of . Since is complete with discrete valuation and is a Galois extension of , the building embeds -equivariantly in the building of as a convex subset, [Tit79, 2.6]. Therefore it suffices to show that
[TABLE]
Let be the Jordan decomposition of with diagonalizable in a basis of and unipotent upper triangular in this basis. As , we have that
[TABLE]
The action by on the apartment associated to the basis in the model of of good norms on (see [Par00, 3.2.2]) is given by translation by , which completes the proof of the lemma. ∎
Proof of Corollary 1.14.
Let
[TABLE]
endowed with the order
[TABLE]
if . This order is compatible with the valuation and is real closed. Observe that : thus, if , then is positive and we denote
[TABLE]
Let be the real closure of in . Given , its eigenvalues lie in and we order them so that
[TABLE]
Observe that any can be represented by a Puiseux series that is convergent at . As a result, if
[TABLE]
This implies that for every
[TABLE]
Since has a pole at infinity, we must have , from which it follows that . Since the latter coincides with by Theorem 1.13, this shows (1).
For the second assertion, let be a torsion-free finite index subgroup. By Lemma 7.3 we have that for all
[TABLE]
and Theorem 1.13 and Corollary 1.10(2) imply then that for some constants ,
[TABLE]
for all .
This says that the -action on is displacing and hence [DGLM11, Proposition 2.2.2 and Lemma 2.8.1] imply that the -orbits, and hence the -orbits, are quasi-isometric embeddings. ∎
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