Finite 2-arc-transitive strongly regular graphs and 3-geodesic-transitive graphs
Wei Jin
Wei Jin
School of Statistics
Jiangxi University of Finance and Economics
Nanchang, Jiangxi, 330013, P.R.China
Research Center of Applied Statistics
Jiangxi University of Finance and Economics
Nanchang, Jiangxi, 330013, P.R.China
[email protected]
Β andΒ
Cheryl E. Praeger
Cheryl E. Praeger
CMSC and Department of Mathematics and Statistics
The University of Western Australia
Crawley, WA 6009, Australia
[email protected]
Abstract.
We classify all the 2-arc-transitive strongly regular graphs, and use this classification
to study the family of finite (G,3)-geodesic-transitive graphs of girth 4 or 5 for some group G of automorphisms.
For this application we first give a reduction result on the latter family of graphs: let N be a normal subgroup of
G which has at least 3 orbits on vertices. We show that
Ξ is a cover of its quotient ΞNβ modulo the N-orbits, and that either
ΞNβ is (G/N,3)-geodesic-transitive of the same girth as Ξ, or
ΞNβ is a (G/N,2)-arc-transitive strongly regular graph, or
ΞNβ is a complete graph with G/N acting 3-transitively on vertices.
The classification of 2-arc-transitive strongly regular graphs allows us to characterise the (G,3)-geodesic-transitive covers Ξ
when ΞNβ is complete or strongly regular.
The first author acknowledges the hospitality of the Centre
for the Mathematics of Symmetry and Computation of UWA, where this research was carried
out.
The first author is supported by NSFC (11661039) and NSF of Jiangxi (2018ACB21001, 20171BAB201010,20171BCB23046,GJJ170321) and the second author acknowledges the Australian Research Council grant DP130100106.
Keywords: 3-geodesic-transitive graph, strongly regular graph, automorphism group.
Math. Subj. Class.: 05E18; 20B25
1. Introduction
A geodesic from a vertex u to a vertex v in a graph Ξ is
a path of the shortest length from u to v in Ξ, and is
called an s-geodesic if the distance between u and v is s.
Then Ξ is said to be (G,s)-geodesic-transitive if it has an s-geodesic, and for each iβ€s, the automorphism group
G is transitive on the set of i-geodesics of Ξ. The systematic investigation of s-geodesic-transitive graphs was initiated recently. The possible local structures of 2-geodesic-transitive graphs were determined in [13]. Then
Devillers, Li and the authors
[14] classified 2-geodesic-transitive graphs of valency 4. Later, in [15], a
reduction theorem for the family of normal
2-geodesic-transitive Cayley graphs was proved and
those which are complete multipartite graphs were also classified.
Our focus in this paper is on 3-geodesic-transitive graphs.
For a positive integer s, an s-arc of Ξ is a sequence of
vertices (v0β,v1β,β¦,vsβ) in Ξ such that
viβ,vi+1β are adjacent and vjβ1βξ =vj+1β where 0β€iβ€sβ1 and 1β€jβ€sβ1. In particular, 1-arcs are called
arcs. The graph Ξ is said to be (G,s)-arc-transitive
if, for each iβ€s, the automorphism group
G is transitive on the set of i-arcs of Ξ. Study of s-arc-transitive graphs originates
from Tutte [33, 34],
who proved that there are no 6-arc-transitive
cubic graphs, and for such graphs the order of the stabiliser of a vertex is at
most 48. This seminal result stimulated greatly the study of s-arc-transitive graphs.
About twenty years later, relying on the
classification of finite 2-transitive groups (which in turn depends on the finite
simple group classification), Weiss [35] proved that there
were no 8-arc-transitive graphs with valency at least three.
Moreover, for each sβ€5 and s=7, s-arc-transitive graphs exist which are not (s+1)-arc-transitive, but there are no such graphs for s=6.
Many other results have been proved for s-arc-transitive graphs,
see
[1, 23, 27].
On the other hand, there is no upper bound on s for s-geodesic-transitivity [24, Theorem 1.1].
Clearly, every s-geodesic is an s-arc, but some s-arcs
may not be s-geodesics, even for small values of s.
If Ξ has girth 3 (the girth of Ξ is
the length of the shortest cycle in Ξ), then 2-arcs contained in 3-cycles are
not 2-geodesics.
If Ξ has girth 4 or 5, then 3-arcs contained in 4-cycles or 5-cycles are
not 3-geodesics. The graph in Figure 1 is the Hamming graph H(3,2), and is
(G,3)-geodesic-transitive but not (G,3)-arc-transitive with
valency 3 and girth 4 where G is the full automorphism group. Thus the family of (G,3)-arc-transitive
graphs is properly contained in the family of (G,3)-geodesic-transitive graphs.
We study s-geodesic-transitive graphs that are not s-arc-transitive for s=3. This problem was studied earlier for the case s=2,
refer to [13, 14, 15, 16].
For s=3, the valency 4 examples have been classified in
[24], where it is shown also that there are examples with
unboundedly large diameter and valency.
In this paper, we introduce a general framework
for describing all the graphs with these properties.
We study normal quotients. Let Ξ be a G-vertex-transitive
graph. If N is a vertex-intransitive normal subgroup of G, then the quotient graph
ΞNβ of Ξ is the graph whose vertex set is the set of N-orbits,
such that two N-orbits Biβ,Bjβ are adjacent in ΞNβ if
and only if there exist xβBiβ,yβBjβ such that x,y are
adjacent in Ξ. Such quotients ΞNβ are often referred to as
G-normal quotients of Ξ relative to N.
Sometimes Ξ is a
cover of ΞNβ, that is to say, for each edge {Biβ,Bjβ} of
ΞNβ and vβBiβ, v is adjacent to exactly one vertex in Bjβ.
In this case we say that Ξ is a
G-normal cover of ΞNβ relative to N.
A connected regular graph is said to be strongly regular with parameters
(n,k,a,c) if it has valency k, vertex set of size n, every pair of adjacent vertices
has a common neighbours, and every pair of distinct non-adjacent vertices has c common neighbours.
Our first theorem is a reduction result on the family of 3-geodesic-transitive graphs of girth 4 or 5.
It describes the various possibilities for the girth and diameter of normal quotients.
Note that 3-geodesic-transitive graphs have diameter at least 3 and are therefore not
3-arc-transitive.
Theorem 1.1**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Let N be a normal subgroup of G with at least 3 orbits on the vertex set. Then Ξ is a cover of ΞNβ, ΞNβ is (G/N,sβ²)-geodesic-transitive where
sβ²=min{3,diam(ΞNβ)}, and one of the following holds:
ΞNβ* is a complete graph.*
ΞNβ* is a (G/N,2)-arc-transitive strongly regular graph with girth 4 or 5.*
ΞNβ* has diameter at least 3 and the same girth as Ξ.*
The normal quotient graphs in Theorem 1.1 (2) are
2-arc-transitive strongly regular graphs. In order to classify 3-geodesic-transitive graphs of girth 4 or 5,
we need to know the 2-arc-transitive strongly regular graphs, and our second theorem determines all such graphs.
Theorem 1.2**.**
Let Ξ be a 2-arc-transitive strongly regular graph. Then either
Ξ* has girth 4 and is one of the following graphs: Km,mβ with mβ₯2, the Higman-Sims graph, the Gewirtz graph, the M22β-graph, or the folded 5-cube β‘5β; or*
Ξ* has girth 5 and is one of the following graphs: C5β,
the Petersen graph, or the Hoffman-Singleton graph.*
Our third theorem, using the classification of 2-arc-transitive strongly regular graphs in Theorem 1.2, characterises all the (G,3)-geodesic-transitive covers Ξ
when ΞNβ is in part (1) or (2) of Theorem 1.1.
For each possible quotient ΞNβ, we obtain all normal covers Ξ explicitly, except for three cases for ΞNβ where we can only classify the graphs when Ξ is (G,4)-distance-transitive (see Table 2).
Theorem 1.3**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that G has a normal subgroup N such that N has at least 3 orbits on vertices and
ΞNβ has diameter at most 2.
Then Ξ is a cover of ΞNβ
and either Ξ,ΞNβ are as in Table 1
or Ξ is a non-(G,4)-distance-transitive graph of diameter at least 4 and ΞNβ is as in Table 2.
The graphs Ξ and ΞNβ in Tables 1 and 2 will be described in Section 2.
In particular, βSDCβ denotes the βstandard double coverβ (Definition 2.4).
We remark that in Theorem 1.3, if ΞNβ is strongly regular, then Ξ and ΞNβ may have distinct girths. For example, the Armanios-Wells graph is (G,3)-geodesic-transitive of girth 5 and it is a cover of the folded 5-cube β‘5β which has girth 4.
Note that the cycle Crβ, r=4 or 5, is a 2-arc-transitive graph of diameter 2. If Ξ is a 3-geodesic-transitive cover of Crβ, then Ξ has valency 2, and hence Ξ is a cycle with girth at least 8, and so is 3-arc-transitive.
In Theorem 1.1, we could choose N to be an intransitive normal subgroup of G which is maximal with respect to having at least 3 orbits on the vertex set of Ξ. Then
each non-trivial normal subgroup M of G, properly containing N,
has 1 or 2 orbits, and so M/N has 1 or 2 orbits on the vertices of ΞNβ.
In other words, G/N is quasiprimitive or bi-quasiprimitive on the vertex set of ΞNβ.
Hence this theorem suggests that to investigate the family of (G,3)-geodesic-transitive graphs that are not (G,3)-arc-transitive, we should
concentrate on the following two problems:
Problem 1.4**.**
determine (G,3)-geodesic-transitive graphs of girth 4 or 5 where G acts quasiprimitively or bi-quasiprimitively
on the vertex set;
investigate (G,3)-geodesic-transitive covers of
the graphs obtained from (1),
and also investigate the graphs Ξ in Table 2.
This paper is organised as follows.
After this Introduction, we give, in Section 2,
some definitions on groups and graphs that we need and also prove some elementary lemmas which will be used in the following analysis.
Theorem 1.1 is proved in Section 3. It
reduces the study of 3-geodesic-transitive graphs of girth 4 or 5 to the study of G-normal covers of complete graphs, of strongly
regular graphs, and of a class of 3-geodesic-transitive graphs of diameter at least 3 with the same girth.
Then in Section 4, we determine all the 2-arc-transitive strongly regular graphs and complete the proof of
Theorem 1.2.
In Section 5, we prove Theorem 1.3, that is, we
investigate 3-geodesic-transitive graphs of girth 4 or 5 which are covers of a 2-arc-transitive graph that is complete or strongly regular.
2. Preliminaries
In this section, we give some definitions concerning groups and graphs and also prove some results which will be used in our
analysis.
2.1. Graph theoretic notions
All graphs in this paper are finite, simple, connected and undirected. For a graph Ξ, we use V(Ξ) and Aut(Ξ) to denote
its vertex set and automorphism
group, respectively. For the group theoretic terminology not defined here we refer the reader to [9, 17, 36].
In a graph Ξ, dΞβ(u,v) denotes the distance between two vertices u and v in Ξ. The diameter diam(Ξ) of Ξ is the maximum distance between u,v
for all u,vβV(Ξ).
If Ξ is (G,s)-geodesic-transitive with G=Aut(Ξ), then Ξ is called s-geodesic-transitive; and if further
s=diam(Ξ), then Ξ is called geodesic-transitive.
A graph Ξ is said to be (G,s)-distance-transitive ((G,s)-DT) if Gβ€Aut(Ξ) and for each iβ€s, G is transitive on
the ordered pairs of vertices at distance i. Moreover, a (G,s)-distance-transitive graph is said to be G-distance-transitive (G-DT) if s=diam(Ξ), and
distance-transitive if G=Aut(Ξ).
By definition, every (G,s)-geodesic-transitive graph is (G,s)-distance-transitive.
Let G be a transitive permutation group on a set Ξ©.
Let B be a non-empty
subset of Ξ©. Then B is called a block of
G if, for any gβG, either Bg=B or
Bgβ©B=β
. The set Ξ© and singleton subsets are trivial blocks.
If N is a normal subgroup of G, then each N-orbit is a block of G on Ξ©, and the
set of N-orbits forms a
G-invariant partition of Ξ©.
The group G is said to be primitive on Ξ©, if G
has only trivial blocks. There is a remarkable classification of finite primitive permutation
groups (8 types), mainly due to M. OβNan and L. Scott, see
[28].
A subgraph X of Ξ is an induced subgraph if two
vertices of X are adjacent in X if and only if they are adjacent
in Ξ. When UβV(Ξ), we use [U] to denote the
subgraph of Ξ induced by U.
Let u be a vertex in a graph Ξ and let iβ€diam(Ξ).
Then Ξiβ(u) denotes the set of vertices at distance i from u.
In the characterisation of s-geodesic-transitive and s-distance-transitive
graphs, the following parameters are important.
Definition 2.1**.**
Let Ξ be an s-distance-transitive graph, let uβV(Ξ), and
let vβΞiβ(u), iβ€s. Then the number of edges
from v to Ξiβ1β(u), Ξiβ(u), and Ξi+1β(u)
does not depend on the choice of v and these numbers are
denoted, respectively, by ciβ, aiβ, biβ.**
Clearly aiβ+biβ+ciβ is equal to the valency of Ξ whenever the constants are well-defined. Note that for 3-geodesic-transitive graphs, the constants are always well-defined for i=1,2,3.
If Ξ is distance-transitive then the constants are well-defined for i=1,2,β¦,d where d
is the diameter of Ξ, and
the sequence (b0β,β¦,bdβ;c1β,β¦,cdβ), is called the intersection array of Ξ.
Some properties of these parameters are given in [4, Proposition 20.4].
2.2. The graphs occurring in Theorem 1.3
The Hoffman-Singleton graph HoS, is the unique strongly regular graph with parameters (50,7,0,1), automorphism group PSU(3,5).Z2β and vertex stabiliser S7β.
The Higman-Sims graph HiS, is the unique strongly regular graph with parameters (100,22,0,6), automorphism group HS.Z2β and vertex stabiliser M22β.Z2β.
The Gewirtz graph is the unique strongly regular graph with parameters (56,10,0,2), automorphism group PSL(3,4).Z22β and vertex stabiliser A6β.Z22β.
The Hamming graph H(d,2) has
vertex set Ξd={(x1β,x2β,β¦,xdβ)β£xiββΞ}, where
Ξ={0,1}, and two vertices v and vβ² are adjacent if and only if they differ
in exactly one coordinate. The Hamming graph H(d,2) is also called a d-cube;
it is 3-geodesic-transitive with girth 4 and diameter d whenever dβ₯3.
The folded d-cube β‘dβ, is the graph obtained by identifying antipodal vertices of H(d,2), i.e., vertices at distance d.
Hence H(d,2) is the antipodal cover of β‘dβ with antipodal parts of size 2.
The folded d-cube has diameter β2dββ and valency d, and if dβ₯4, then β‘dβ has girth 4.
Let Ξ be the Hoffman-Singleton graph and let uβV(Ξ). Then the induced subgraph [Ξ2β(u)], denoted by [HoS]2β, is a distance-transitive graph with diameter 3, girth 5, see [7, p.223], and it is a 3-geodesic-transitive 6-cover of K7β.
Let Ξ=HiS and let uβV(Ξ). Then the induced subgraph [Ξ2β(u)] is called the M22β-graph.
It is the unique strongly regular graph with parameters (77,16,0,4), automorphism group M22β.Z2β and vertex stabiliser Z24β:S6β,
see [7, p.369].
A distance-regular graph with intersection array (2ΞΌ,2ΞΌβ1,ΞΌ,1;1,ΞΌ,2ΞΌβ1,2ΞΌ)
is called a * Hadamard graph* of valency
2ΞΌ (for definition of distance-regular graph see [7, page 1], and intersection array is defined in the next subsection).
Hence a Hadamard graph of valency 2ΞΌ has 8ΞΌ vertices.
The Armanios-Wells graph is the unique distance-regular graph with intersection array (5,4,1,1;1,1,4,5), automorphism group Z21+4β.A5β, and vertex stabiliser A5β.
It is 2-arc-transitive, and also 3-geodesic-transitive.
The dodecahedron has both girth and diameter 5, automorphism group A5βΓZ2β and intersection array (3,2,1,1,1;1,1,1,2,3), see [7, p.1] and [20];
it is geodesic-transitive.
A divisible design GD(k,Ξ»,n,kn) is a triple (X,P,B)
where X is a set of kn βpointsβ, P is a partition of X into classes of size n, and
B is a collection of k-subsets of X (called βblocksβ) such that each block meets every class
in precisely 1 point, and any two points of X from different classes are contained in Ξ»
blocks. A design is called resolvable when its set of blocks can be partitioned into parallel classes, that is,
into partitions of the point set. We use RGD(k,Ξ»,n) to denote a resolvable divisible design GD(k,Ξ»,n,kn)
(see [7, page 439]).
Let D=(X,P,B) be a resolvable divisible design RGD(r,Ξ»,m) such that r=Ξ».m.
Counting triples (u,v,B), such that u,v are distinct points contained in BβB, yields β£Bβ£=m2Ξ»=rm=β£Pβ£. Thus each parallel class of blocks contains m blocks, and it follows that B is a disjoint union of r parallel classes of blocks,
and then, since each point lies in exactly one block from each parallel class, each point lies in exactly r blocks, that is to say, D is a 1-(rm,r,r) design. Let B={B1β,B2β,β¦,Brmβ}. The incidence graph Inc(D) of D is defined as follows:
the vertex set is V1ββͺV2β where V1β=X and V2β=B, and a vertex x of V1β is adjacent to a vertex Biβ of V2β
if and only if xβBiβ.
Lemma 2.2**.**
Let D=(X,P,B) be a resolvable divisible design RGD(r,Ξ»,m) with r=Ξ».m,
and define Inc(D) as above. Suppose moreover that any two blocks from different parallel classes contain exactly
Ξ» common points. Then Inc(D) is a distance-regular bipartite antipodal cover of Kr,rβ with diameter 4 and antipodal block size m, written Inc(D)=mKr,rβ.
Proof.
By definition Inc(D) is a bipartite graph with bipartition {V1β,V2β}.
Moreover, β£V1ββ£=β£V2ββ£=rm.
Now P is a partition of V1β into r classes of size m, say P={P1β,P2β,β¦,Prβ}, where each β£Piββ£=m.
As any two points of V1β from different classes are contained in Ξ»
blocks, it follows that vertices of V1β from distinct classes are at distance 2 in Inc(D).
Also B is a disjoint union of r parallel classes of blocks.
Let C={C1β,C2β,β¦,Crβ} be the set of parallel classes, where each Ciβ contains m blocks of B.
By assumption, any two blocks from different parallel classes contain exactly Ξ» common points, and hence
vertices of V2β from distinct parallel classes are at distance 2 in Inc(D).
Further, for each i, each vertex of V1β is adjacent to exactly one vertex of Ciβ,
and each vertex of V2β is adjacent to exactly one vertex of Piβ.
Let xβV1β and CβC. Then x lies in a unique block BβC. Let Bβ²β²βCβ{B}, and Cβ²βCβ{C},
so x also lies in a unique block Bβ²βCβ². By assumption β£Bβ²β©Bβ²β²β£=Ξ». Let yβBβ²β©Bβ²β². Then (x,Bβ²,y,Bβ²β²) is a path of length 3 in
Inc(D), and hence the distance between x and Bβ²β² in Inc(D) is 3. It follows that x has distance 1 or 3 from
each vertex of V2β. If xβPβP, then as mentioned above, x is at distance 2 from each point
yβV1ββP. If xβ²βPβ{x}, then xβ² also has distance 2 from y, and hence x,xβ² are at distance 4 in
Inc(D). By a similar argument, each vertex of V2β is at distance 1 or 3 from vertices of V1β, and at distance 2 or 4 from vertices of V2β.
Thus Inc(D) has diameter 4, and two vertices of Inc(D) are at distance 4 if and only if they are distinct blocks in the same parallel class, or distinct points in the same class P.
Hence the classes of V1β and the parallel classes of V2β are antipodal blocks of Inc(D).
It is straightforward, using the properties of the design D, to show that Inc(D) is distance-regular with intersection array
(r,rβ1,rβΞ»,1;1,Ξ»,rβ1,r).
Finally, we examine the antipodal quotient graph, that is, the graph Ξβ² with vertex set PβͺC, such that
a vertex PiββP is adjacent to a vertex CjββC
if and only if some vertex of Piβ is adjacent to some vertex of Cjβ in Inc(D).
Since, in fact, each vertex xβPiβ is contained in a unique block in Cjβ, and vice versa, it follows that Ξβ²β
Kr,rβ.
Moreover, since β£Piββ£=β£Cjββ£, we see that the edges of Inc(D) joining vertices of Piβ and Cjβ form a perfect matching
between these two sets. Thus Inc(D) is a cover of Ξβ².
β
2.3. Some results
We will use the following remark frequently throughout the paper. It is especially useful for studying small valency s-geodesic-transitive graphs.
Recall DefinitionΒ 2.1.
Remark 2.3**.**
(1) Let Ξ be a 2-geodesic-transitive graph with b2ββ€1.
If b2β=0, then as Ξ is 2-geodesic-transitive,
Ξ has diameter 2 and so is geodesic-transitive.
Suppose that b2β=1, so in particular, d:=diam(Ξ)β₯3. Let (u0β,β¦,udβ) be a d-geodesic. Then for each jβ€dβ3, it follows from the 2-geodesic-transitivity of Ξ that β£Ξ3β(ujβ)β©Ξ(uj+2β)β£=1.
Note that, Ξj+3β(u0β)β©Ξ(uj+2β)βΞ3β(ujβ)β©Ξ(uj+2β),
and so
β£Ξj+3β(u0β)β©Ξ(uj+2β)β£=1. Hence the 2-geodesic (u0β,u1β,u2β) has a unique continuation to an r-geodesic in Ξ for all r such that 3β€rβ€d.
Since Ξ is 2-geodesic-transitive, each 2-geodesic of Ξ has a unique continuation to an r-geodesic for 3β€rβ€d.
Thus Ξ is geodesic-transitive, and hence also distance-transitive.
(2) Let Ξ be a 3-geodesic-transitive graph with b3ββ€1.
If b3β=0, then since Ξ is 3-geodesic-transitive,
Ξ has diameter 3 and so is geodesic-transitive.
Suppose that b3β=1. So in particular, d:=diam(Ξ)β₯4.
Let (u0β,β¦,udβ) be a d-geodesic. Then for each jβ€dβ4, it follows from the 3-geodesic-transitivity of Ξ that β£Ξ4β(ujβ)β©Ξ(uj+3β)β£=1.
Note that, Ξj+4β(u0β)β©Ξ(uj+3β)βΞ4β(ujβ)β©Ξ(uj+3β), and so
β£Ξj+4β(u0β)β©Ξ(uj+3β)β£=1.
Hence the 3-geodesic (u0β,u1β,u2β,u3β) has a unique continuation to an r-geodesic in Ξ for all r such that 4β€rβ€d.
Since Ξ is 3-geodesic-transitive, each 3-geodesic of Ξ has a unique continuation to an r-geodesic for 4β€rβ€d.
Thus Ξ is geodesic-transitive, and hence also distance-transitive.
Definition 2.4**.**
For be a graph Ξ with vertex set V(Ξ) and arc set A(Ξ), let
Ξ be the graph with vertex set V(Ξ)Γ{1,2}, such that two vertices (x,1) and (y,2) adjacent if and only if (x,y)βA(Ξ). Then Ξ is called the standard double cover (SDC) of Ξ; Ξ is bipartite with bipartite halves V(Ξ)Γ{i} for i=1,2.
Some of our examples are standard double covers of distance-transitive graphs, and we use the following observation to identify them.
Lemma 2.5**.**
Suppose that Ξ is a finite distance-transitive graph of odd diameter which is both bipartite and antipodal with antipodal blocks of size 2. Let Ξ£ denote the antipodal quotient of Ξ. Then Ξ is isomorphic to the standard double cover of Ξ£.
Proof.
Let d=diam(Ξ), let Ξ1β,Ξ2β be the parts of the bipartition of Ξ, and identify V(Ξ£) with the set of antipodal blocks. Let B={u,v}βV(Ξ£). Then Ξdβ(u)={v}, and since d is odd we have, say, uβΞ1β,vβΞ2β. Let CβV(Ξ£) be adjacent to B in Ξ£.
Then C={x,y}, and u is adjacent to exactly one vertex of C, say x. Thus xβΞ(u)βΞ2β and yβΞ(v)=Ξdβ1β(u)βΞ1β.
Define a map Ο:V(Ξ)β¦V(Ξ£)Γ{1,2} by Ο(u)=(B,i) where B is the antipodal block containing u and Ξiβ is the part of the bipartition containing u. Then Ο is a well defined bijection. We claim that Ο is a graph isomorphism from Ξ to Ξ£, the standard double cover of Ξ£: for if {u,x} is an edge of Ξ and Ο(u)=(B,i),Ο(x)=(C,j) then iξ =j (as u,x lie in different parts of the bipartition) and {B,C} is an edge of Ξ£ (by definition of Ξ£). Conversely if
Ο(u)=(B,i),Ο(x)=(C,j) form an edge of Ξ£, then iξ =j and {B,C} is an edge of Ξ£, by the definition of Ξ£. As Ξ covers Ξ£, there are exactly two edges of Ξ joining vertices of B and C. Now u is the
unique vertex in Bβ©Ξiβ, and since Ξ is bipartite, the edge involving u must join u to the unique vertex in Cβ©Ξjβ, namely x. This proves the claim and hence Ξβ
Ξ£.
β
If Gβ€Aut(Ξ), then G also acts as a group of automorphisms of the standard double cover Ξ with
the action g:(x,i)β¦(xg,i). If G is vertex-transitive on Ξ, then G has two orbits
on the set of vertices of Ξ, namely the sets V(Ξ)Γ{i} for i=1,2.
Furthermore, Gvβ=G(v,i)β for each i=1,2 and vβV(Ξ),
the action of Gvβ on Ξ(v) is equivalent to the action of
G(v,i)β on Ξ((v,i)), and if Ξ is (G,2)-arc-transitive, then Ξ is locally (G,2)-arc-transitive.
Define
[TABLE]
Then Ο is a graph automorphism of Ξ of order 2. Further, for any vertex (v,i), we have (v,i)gΟ=(vg,i)Ο=(vg,3βi)=(v,3βi)g=(v,i)Οg.
Hence gΟ=Οg for every gβG. Let G=GΓβ¨Οβ©. Then Gβ€Aut(Ξ).
Moreover, Ξ is (G,2)-arc-transitive, then Ξ is (G,2)-arc-transitive.
Now (x,1) is adjacent to (y,2) if and only if (y,1) is adjacent to (x,2). If Ξ is connected, then for distinct x,yβV(Ξ) there exists a path P in Ξ
from x to y. The path P lifts to a path in Ξ from (x,1) to (y,1) if P has
even length, and to one between (x,1) and (y,2) if P has odd length. In particular, there is a
path from (y,1) to (y,2) if and only if y lies in a cycle in Ξ of odd length. Thus Ξ is connected if and only if Ξ is connected and contains an odd cycle,
that is, if and only if Ξ is connected and not bipartite.
We mention a few more properties of these standard double covers. When we say that a (non-complete)
graph Ξ βhas c2β=cβ we mean that β£Ξ(u)β©Ξ(w)β£=c whenever
dΞβ(u,w)=2.
Lemma 2.6**.**
Let Ξ be a non-bipartite graph of girth 4 with vertex-transitive group Gβ€Aut(Ξ), and let Ξ be its standard double cover with group G as above.
Then the following hold.
For an integer cβ₯2, Ξ has c2β=c if and only if Ξ has c2β=c.
For a positive integer sβ€diam(Ξ), Ξ is (G,s)-distance-transitive if and only if Ξ is (G,s)-distance-transitive.
If a2β=0 for Ξ, then Ξ is (G,3)-geodesic-transitive if and only if Ξ is (G,3)-geodesic-transitive.
Proof.
(1) Suppose that Ξ has c2β=c. Let dΞβ(u,w)=2 and, say, Ξ(u)β©Ξ(w)={v1β,β¦,vcβ}. Then for each i,
[(u,1),(viβ,2),(w,1)] is a 2-arc of Ξ, so {(v1β,2),β¦,(vcβ,2)} βΞ((u,1))β©Ξ((w,1)). Equality holds, since if
Ξ((u,1))β©Ξ((w,1)) contains a vertex (u,2), then uβΞ(u)β©Ξ(w). Similarly {(v1β,1),β¦,(vcβ,1)}=Ξ((u,2))β©Ξ((w,2)). Thus Ξ has parameter c2β=c.
Conversely, suppose that Ξ has parameter c2β=c. A distance-two pair is of the form (u,i),(w,i) for vertices u,wβV(Ξ) and iβ{1,2}. Then
Ξ((u,i))β©Ξ((w,i))={(v1β,3βi),β¦,(vcβ,3βi)} and a similar argument to the above shows that Ξ(u)β©Ξ(w)={v1β,β¦,vcβ}, and so Ξ has parameter c2β=c.
(2) Since G,G are vertex-transitive on Ξ,Ξ, respectively,
and since, for uβV(Ξ) and jβ{1,2} we have Guβ=G(u,j)β, it is sufficient to
examine the orbits of Guβ. For iβ€s, Ξiβ((u,j))={(v,jβ²)β£vβΞiβ(u)}, where jβ²=j if i is even and jβ²=3βj if i is odd. The actions of Guβ on
Ξiβ(u) and Ξiβ((u,j)) are therefore equivalent for each i, and part (2) follows.
(3) Suppose that a2β=0 for Ξ. Assume that Ξ is (G,3)-geodesic-transitive.
Then since Ξ has girth 4, Guβ is 2-transitive on Ξ(u), and so
G(u,1)β is 2-transitive on Ξ((u,1)), hence Ξ is
(G,2)-arc-transitive. Let [(u,1),(v1β,2),(v2β,1), (u4β,2)] and [(u,1),(v1β,2),(v2β,1),(u5β,2)] be two 3-geodesics of Ξ. Then
(u,v1β,v2β,u4β) and (u,v1β,v2β, u5β) are two 3-geodesics of Ξ, as a2β=0 for Ξ. Thus some element of G maps
(u,v1β,v2β,u4β) to (u,v1β,v2β,u5β), and so this element maps
[(u,1),(v1β,2),(v2β,1),(u4β,2)] to [(u,1),(v1β,2),(v2β,1),(u5β,2)] in Ξ. Hence Ξ is (G,3)-geodesic-transitive.
Conversely, suppose that Ξ is (G,3)-geodesic-transitive.
Then as Ξ is bipartite and
(G,2)-arc-transitive, G(u,1)β is 2-transitive on Ξ((u,1)), and so Guβ is 2-transitive on Ξ(u),
hence Ξ is (G,2)-arc-transitive. Let
(u,v1β,v2β,u4β) and (u,v1β,v2β,u5β) be two 3-geodesics of Ξ.
Then as a2β=0 for Ξ, [(u,1),(v1β,2), (v2β,1),(u4β,2)] and [(u,1),(v1β,2), (v2β,1),(u5β,2)] are two 3-geodesics of Ξ. Thus
some element of G maps
[(u,1),(v1β,2), (v2β,1),(u4β,2)] to [(u,1),(v1β,2),(v2β,1),(u5β,2)],
this element fixes V(Ξ)Γ{1} and so lies in G,
and hence
this element induces an element of G that maps
(u,v1β, v2β,u4β) to (u,v1β,v2β,u5β). Thus Ξ is (G,3)-geodesic-transitive.
β
3. Reduction result
In this section, we study normal quotients of 3-geodesic-transitive graphs of girth 4 or 5.
We will need the following result from [12, Lemma 5.3].
Lemma 3.1**.**
Let Ξ be a connected locally (G,s)-distance-transitive
graph with sβ₯2. Let 1ξ =Nβ²G be intransitive on
V(Ξ), and let B be the set of N-orbits on
V(Ξ). Then one of the following holds:
β£Bβ£=2.
Ξ* is bipartite, ΞNββ
K1,rβ with
rβ₯2 and G is intransitive on V(Ξ).*
s=2, Ξβ
Km[b]β, ΞNββ
Kmβ
with mβ₯3 and bβ₯2.
N* is semiregular on V(Ξ), Ξ is a cover
of ΞNβ, β£V(ΞNβ)β£<β£V(Ξ)β£ and ΞNβ is
locally (G/N,sβ²)-distance-transitive where sβ²=min{s,diam(ΞNβ)}.*
We derive from LemmaΒ 3.1 the following result for s-geodesic-transitive graphs.
Lemma 3.2**.**
Let Ξ be a connected (G,s)-geodesic-transitive graph where sβ₯2. Let 1ξ =Nβ²G be intransitive on V(Ξ).
Suppose that ΞβKm[b]β for any mβ₯3 and bβ₯2. Then either
N* has 2 orbits on
V(Ξ) and Ξ is bipartite; or*
N* has at least 3 orbits on
V(Ξ), N is semiregular on V(Ξ), Ξ is a cover of
ΞNβ and ΞNβ is (G/N,sβ²)-geodesic-transitive where
sβ²=min{s,diam(ΞNβ)}.*
Proof.
By assumption N is not transitive on V(Ξ). If N has exactly 2 orbits on
V(Ξ), say C0β and C1β, then as Ξ is connected and G-arc-transitive,
each Ciβ contains no edges of Ξ, and so
Ξ is a bipartite graph with C0β,C1β being the two bipartite halves, part (i) holds. Thus, we may suppose that
N has at least 3 orbits on
V(Ξ). Since Ξ is (G,s)-geodesic-transitive where sβ₯2, Ξ is also (G,s)-distance-transitive.
Since ΞβKm[b]β for any mβ₯3 and bβ₯2, it follows that part (iv) of
Lemma 3.1 holds. To prove that part (ii) is valid it remains to prove that
ΞNβ is locally (G/N,sβ²)-geodesic-transitive, where sβ²=min{s,diam(ΞNβ)}.
Let (B0β,B1β,B2β,β¦,Btβ) and
(C0β,C1β,C2β,β¦,Ctβ) be t-geodesics of ΞNβ
where tβ€sβ². Since Ξ is a
cover of ΞNβ, there exist xiββBiβ and yiββCiβ such
that (x0β,x1β,x2β,β¦,xtβ) and (y0β,y1β,y2β,β¦,ytβ)
are t-geodesics of Ξ. As tβ€sβ²β€s and Ξ
is (G,s)-geodesic-transitive, there exists gβG such that
(x0β,x1β,x2β,β¦,xtβ)g=(y0β,y1β,y2β,β¦,ytβ), and hence
g maps
(B0β,B1β,B2β,β¦,Btβ) to (C0β,C1β, C2β,β¦,Ctβ). Thus
ΞNβ is (G/N,sβ²)-geodesic-transitive, and (ii) holds. β
Lemma 3.3**.**
Let Ξ be a (G,2)-geodesic-transitive graph of girth at least 4.
Let N be an intransitive normal subgroup of G with at least 3 orbits on
V(Ξ). Then ΞNβ is a complete graph if and only if ΞNβ has girth 3.
Proof.
Note that ΞβKm[b]β for any mβ₯3 and bβ₯2, since
the girth of Ξ is at least 4.
If ΞNβ is a complete graph, then since N has at least 3 orbits on
V(Ξ), it follows that ΞNβ has girth 3. Conversely, suppose that ΞNβ has girth 3.
Then by Lemma 3.2, the graph Ξ is a cover of ΞNβ.
Let (B1β,B2β,B3β) be a triangle of ΞNβ.
Then there exist biββBiβ such that (b1β,b2β,b3β) is a 2-arc of Ξ. Further, (b1β,b2β,b3β) is a 2-geodesic of Ξ (as Ξ has girth at least 4).
Suppose that ΞNβ is not a complete graph. Then ΞNβ has a 2-geodesic (C1β,C2β,C3β). Since Ξ covers ΞNβ, we can find ciββCiβ such that (c1β,c2β,c3β) is a 2-geodesic of Ξ.
As Ξ is (G,2)-geodesic-transitive, there exists gβG
such that (b1β,b2β,b3β)g=(c1β,c2β,c3β), and so (B1β,B2β,B3β)g=(C1β,C2β,C3β), which is impossible.
Therefore ΞNβ is a complete graph. β
Now we prove Theorem 1.1 and
describe the various possibilities for the girth and diameter of ΞNβ.
Proof of Theorem 1.1.
Since Ξ has girth 4 or 5, we have ΞβKm[b]β for any mβ₯3 and bβ₯2.
Thus by Lemma 3.2, Ξ is a cover of ΞNβ and ΞNβ is (G,sβ²)-geodesic-transitive where
sβ²=min{3,diam(ΞNβ)}.
If ΞNβ is a complete graph, then (1) holds. Assume now that ΞNβ is not a complete graph.
Then by Lemma 3.3, ΞNβ has girth at least 4.
Moreover, since ΞNβ is covered by Ξ, it follows that the girth of ΞNβ is at most the girth of Ξ,
and hence ΞNβ has girth 4 or 5.
If ΞNβ has diameter 2, then (2) follows.
Now suppose that ΞNβ has diameter at least 3. If Ξ has girth 4, then by the previous paragraph ΞNβ has girth 4. Suppose that Ξ has girth 5.
Assume that the girth of ΞNβ is 4 and
let (B1β,B2β,B3β,B4β) be a 4-cycle. Then since Ξ is a cover of ΞNβ, there exist biββBiβ and bβ²βB1β such that (b1β,b2β,b3β,b4β,bβ²)
is a 4-arc of Ξ. Since Ξ has girth 5, b1βξ β{b4β,bβ²} and (b1β,b2β,b3β)
is a 2-geodesic. Furthermore, b4ββΞ2β(b1β)βͺΞ3β(b1β).
If b4ββΞ2β(b1β), then there exists vβΞ(b1β) such that (b1β,v,b4β) is a 2-geodesic.
Let B be the N-orbit containing v.
Then (B1β,B,B4β) is a triangle of ΞNβ, contradicting the assumption
that ΞNβ has girth 4.
Thus b4ββΞ3β(b1β), and so (b1β,b2β,b3β,b4β)
is a 3-geodesic of Ξ.
Let (C1β,C2β,C3β,C4β) be a 3-geodesic of ΞNβ. Then there exist ciββCiβ such that (c1β,c2β,c3β,c4β)
is a 3-geodesic, and there exists gβG such that (b1β,b2β,b3β,b4β)g=(c1β,c2β,c3β,c4β),
and hence (B1β,B2β,B3β,B4β)g=(C1β,C2β,C3β,C4β). This is impossible, as (B1β,B4β)
is an arc but C1β,C4β are at distance 3 in ΞNβ. Therefore, ΞNβ has girth 5, and (3) holds.
β
4. Finite 2-arc-transitive strongly regular graphs
The normal quotient graphs in Theorem 1.1 (2) are
2-arc-transitive strongly regular graphs. In order to classify (G,3)-geodesic-transitive graphs of girth 4 or 5,
we need to know all possibilities for these normal quotients explicitly, and determining them is the aim of this section.
Note that every 2-arc-transitive strongly regular graph Ξ has girth 4 or 5.
Also, for each uβV(Ξ) and distinct v,wβΞ(u), the triple (v,u,w) is a 2-arc, so if Ξ is (G,2)-arc-transitive then Guβ is 2-transitive on Ξ(u). We frequently uese this fact in our proofs. First we gather results from the literature to
determine all the girth 5 examples.
Lemma 4.1**.**
Let Ξ be a 2-arc-transitive strongly regular graph of girth 5. Then Ξ is C5β,
the Petersen graph, or the Hoffman-Singleton graph.
Proof.
Since Ξ is a 2-arc-transitive graph of diameter 2 and girth 5, it follows from [7, Theorem 6.7.1] that Ξ has valency 2, 3, 7 or 57.
By [2] and [7, p.207, Remark (i)],
the valency of Ξ is not 57, and so Ξ has valency 2, 3 or 7.
Moreover, by [7, p.207, Remark (i)] or [21, p.206], if Ξ has valency 2, then Ξ is C5β;
if Ξ has valency 3, then Ξ is the Petersen graph; and if Ξ has valency 7, then Ξ is the Hoffman-Singleton graph. β
Lemma 4.2**.**
Let Ξ be a 2-arc-transitive strongly regular graph. Then either Ξ is a complete bipartite graph, or Ξβ
C5β, or β£Ξ(u)β£<β£Ξ2β(u)β£ for each vertex u.
Proof.
Let k=β£Ξ(u)β£, and note that k is independent of the choice of u. Suppose that kβ₯β£Ξ2β(u)β£.
Since Ξ is 2-arc-transitive and not a complete graph, it follows that Ξ has girth at least 4, and
so there are k(kβ1) edges between Ξ(u)
and Ξ2β(u). Hence k(kβ1)=c2βΓβ£Ξ2β(u)β£β€c2βk, so
c2β=kβ1 or k.
If c2β=k, then Ξ is complete bipartite.
Suppose that c2β=kβ1. Then β£Ξ2β(u)β£=k, and since Ξ has diameter 2, we obtain a2β=1.
Thus for vβΞ2β(u) and X=Aut(Ξ), Xuvβ fixes Ξ(u)βΞ(v)={x}, say, and Ξ2β(u)β©Ξ(v)={w}, say. Thus Xuvβ=Xuxβ (as they have the same order), and since Xuβ is 2-transitive on Ξ(u), it follows that
Xuvβ is transitive on Ξ(u)β©Ξ(v). Similarly, Xuvβ=Xuwβ and Xuvβ is transitive on Ξ(u)β©Ξ(w). If the valency k is greater than 2 then we must have Ξ(u)β©Ξ(v)=Ξ(u)β©Ξ(w) and Ξ contains a 3-cycle, which is a contradiction. Hence k=2 and c2β=1, and therefore Ξβ
C5β. β
The socle of a finite 2-transitive permutation group is either elementary abelian or a nonregular nonabelian simple group, see [17, Theorem 4.1B]. Moreover, in the latter case, the socle is primitive, see [17, p.244].
Now we prove Theorem 1.2 to determine the class of 2-arc-transitive strongly regular graphs.
Proof of Theorem 1.2.
Since Ξ is a 2-arc-transitive graph of diameter 2, Ξ has girth 4 or 5.
If Ξ has girth 5, then by Lemma 4.1, case (2) holds. Assume now that
Ξ has girth 4.
Let X:=Aut(Ξ) and let uβV(Ξ).
The 2-arc-transitivity of Ξ implies that the stabiliser Xuβ is transitive on both Ξ(u) and Ξ2β(u).
Case 1. X imprimitive:
Suppose that X is not primitive on V(Ξ). Then X has a non-trivial block on V(Ξ) containing u, say Ξ. Since
Ξ is arc-transitive and connected, Ξ does not contain any edge of Ξ. Thus Ξβ{u}βͺΞ2β(u), as Ξ
has diameter 2. Since Xuβ fixes the block Ξ setwise
and acts transitively on Ξ2β(u), it follows that Ξ={u}βͺΞ2β(u).
As Ξ is 2-distance-transitive, it follows from
[12, Lemma 5.2] that either Ξβ
Km[b]β for some mβ₯3,bβ₯2, or V(Ξ)βΞ=Ξ(u)
is the only X-image of Ξ different from Ξ.
However the graph Ξβ
Km[b]β has girth 3 (since mβ₯3), and so we
conclude that there are just two blocks of imprimitivity, namely Ξ and Ξ(u), and hence Ξβ
Km,mβ
for some mβ₯2 as in part (1).
Case 2. X primitive:
In the remainder, we suppose that X acts primitively on V(Ξ), and as Xuβ is transitive on Ξ(u) and Ξ2β(u),
X is a primitive rank 3 group. By 2-arc-transitivity, we know that Xuβ is 2-transitive on Ξ(u). It then follows from [30, Theorem A] that X is primitive on V(Ξ) of type either
affine or almost simple.
Note that the 2-transitive group XuΞ(u)β induced by Xuβ on Ξ(u) is also of type either affine or almost simple.
Let the valency of Ξ be n. Then since Ξ is a 2-arc-transitive graph of diameter 2,
it follows that
[TABLE]
Case 2A. X affine:
If X is an affine group, then Ξ is among the graphs listed in [23, Table 1] where the Column 3 entry is βpβ. Thus Ξ is one of the following graphs:
β‘nβ, Pmβ(a) where mβ₯3 and a=1 or 2, Ξ(C23β) or
Ξ(C22β).
The graph
Ξ(C23β) has 211 vertices of valency 23, however
232+1<211, so Ξ is not Ξ(C23β); Ξ(C22β) has 210 vertices of valency 22, and
222+1<210, and so Ξ(C22β) is also not a candidate.
The graph
Pmβ(a) has 2ma vertices of valency n=2aβ12amβ1β.
By [23, (1.3)], if a=1, then
Pmβ(a)=K2mβ has diameter 1, which is not the case; if a=2 and mβ₯3, then an easy inductive argument yields n2+1<2ma, and so
Ξ is not Pmβ(a).
Finally, for the folded n-cube β‘nβ, only β‘5β has diameter 2, and β‘5β is an example, as in case (1).
Case 2B. X almost simple:
From now on we suppose that X is an almost simple group with nonabelian simple socle L.
If L is an alternating group, then a classification of the possible rank 3 actions appears in [3], while the rank 3 representations of the classical
groups are listed in [26], and
the rank 3 primitive
groups in which L is either an exceptional group of Lie type or a sporadic group are listed in [29].
(A summary of this classification can also be found in [8], which provides also
a list of the smallest possible groups in the various families.) We now inspect the groups case by case to identify the remaining three examples in (1).
Note that the socle L of an almost simple primitive group is not regular, so Luβξ =1 for uβV(Ξ), and since Ξ is connected, LuΞ(u)βξ =1.
L* exceptional:*
Assume that L is an exceptional
simple group of Lie type. Then L,Luβ and the subdegrees k=β£Ξ(u)β£,l=β£Ξ2β(u)β£ are listed in [29, Table 1].
By Lemma 4.2, we have k<l.
In each case, k is not a prime power. Hence XuΞ(u)β is a 2-transitive group on Ξ(u) of almost simple type, and
the socle soc(XuΞ(u)β) is its unique minimal normal subgroup.
Since, as we observed above, 1ξ =LuΞ(u)ββ΄XuΞ(u)β, it follows that
soc(XuΞ(u)β)β€LuΞ(u)β.
Moreover, since kξ =28,
it follows from the classification of the 2-transitive groups XuΞ(u)β that
soc(XuΞ(u)β) induces a 2-transitive action on Ξ(u).
Hence LuΞ(u)β acts 2-transitively on Ξ(u).
Checking the candidates in [29, Table 1], we see that none of the groups Luβ induces a
2-transitive action on degree k. Thus L is not exceptional of Lie type.
L* sporadic:*
For the sporadic
simple groups L,
we inspect the groups in [29, Table 2], and find that (L,Luβ)=(M22β,Z24β.A6β) and (L,Luβ)=(HS,M22β) are the only two candidates. Moreover, (L,Luβ)=(M22β,Z24β.A6β), provides the example M22β-graph; and (L,Luβ)=(HS,M22β) yields the Higman-Sims graph.
L* alternating:*
Suppose that L=Acβ, cβ₯5, as in [3]. Recall that n=β£Ξ(u)β£.
Then since XuΞ(u)β is 2-transitive on Ξ(u), it follows from
[31, Main Theorem] that one of the
following holds:
X is 3-transitive on V(Ξ);
Xβ€Scβ, n=2c+1β and Xuββ
(SnβΓSnβ1β)β©X;
X=Scβ, c is prime, and Xuβ=Zcβ:Zcβ1β is a sharply 2-transitive Frobenius group;
Xβ°Scβ, c=6, and Xuβ is the normaliser of a Sylow 5-subgroup;
Xuβ is almost simple and primitive in the natural action of Scβ of degree c, and XuΞ(u)ββ
Xuβ.
Since Ξ is not a complete graph, case (1) does not occur.
If case (2) holds, then by [3, p.476, I], X has rank n on V(Ξ), and so n=3 and c=5.
In this case, Ξ is the Petersen graph of girth 5, a contradiction since Ξ has girth 4.
Suppose that case (3) holds. Then β£V(Ξ)β£=β£Xuββ£β£Xβ£β=(cβ2)!, and the only 2-transitive action for Xuβ has degree c (since the valency is not 2), so the valency is n=c. Recall that
β£V(Ξ)β£β€n2+1. Hence (nβ2)!β€n2+1, and so nβ€6. Since n=c is a prime power, we get n=5,
β£V(Ξ)β£=6, and Ξβ
K6β, which is a contradiction.
In case (4), we have c=6 and Xuβ=NXβ(Z5β). Since X=L.Xuβ, it follows that
β£V(Ξ)β£=β£Xuββ£β£Xβ£β=β£XuβL.Xuβββ£=β£Lβ©XuβLββ£=2.5.26!β=36. Also, the only 2-transitive action of Xuβ is of degree 5, so the valency is n=5, giving
β£V(Ξ)β£>n2+1, a contradiction.
Thus case (5) holds. Then by
Tables 1-2 of [3, p.484β485], we have cβ€12. Since Xuβ is primitive in the natural action of degree c, it follows from
[3, Section 2, I and II] that
there is a unique graph and it satisfies: c=9, β£V(Ξ)β£=120, X=A9β and Xuβ=PSL(2,8):Z3ββ
Ree(3). Since
XuΞ(u)β is 2-transitive on Ξ(u) of degree n and β£V(Ξ)β£β€n2+1, it follows that n=28. This implies, however, that Xuβ is transitive on Ξ2β(u) of degree 120β1β28=91, which is impossible since β£Xuββ£ is not divisible by 13.
Thus L is not an alternating group.
X* classical:*
It remains to consider the case where X is a classical almost simple group with a rank 3 action. Such groups are classified in [26, Theorems 1.1 and 1.2]. We consider first the case of [26, Theorem 1.1] which assumes that a group G is semilinear with quasisimple normal subgroup M=Sp(2mβ2,q),Ω±(2m,q),Ξ©(2mβ1,q), or SU(m,q), where mβ₯3 and q is a prime power (and hence M has a possibly non-trivial centre Z), so that the socle L=M/Z and the group X=G/Zβ€Aut(M/Z).
In cases (i)β(iv) of [26, Theorem 1.1], the action is on an orbit of totally singular (or isotropic) subspaces, or nonsingular subspaces, and one checks as follows that these do not produce examples: in all cases Xuβ acts faithfully on each of its orbits Ξ(u),Ξ2β(u) and one sees, either group theoretically that the action of Xuβ on Ξ(u) is not 2-transitive, or geometrically
that Ξ(u) contains an edge. (Some additional information from [8, p.18,Table 6, or the discussion on p.32β36] is helpful.)
The remaining quasisimple groups M in cases (v)β(x) of [26, Theorem 1.1]
are listed in TableΒ 3, together with the stabiliser Muβ, and the subdegrees (lengths of the Guβ-orbits in V(Ξ)) many of which were computed using MAGMA [5]. In most cases we determine that Guβ does not act 2-transitively on either Ξ(u) or
Ξ2β(u) (often using MAGMA to confirm) - we denote this fact by an entry βnot 2-trans.β in the column headed βCommentsβ of TableΒ 3. In one case, case (vi), we find the 2-arc-transitive Hoffman-Singleton graph, but it is excluded here since it has girth 5, while we are assuming that Ξ has girth 4.
Finally, we treat the groups from [26, Theorem 1.2]. Here
L=PSL(n,q)β€Xβ€Aut(L). In case (i) of [26, Theorem 1.2], nβ₯4
and the X-action on V(Ξ) is equivalent to its action on lines of the projective space PG(nβ1,q). For a line u, the sets Ξ(u),Ξ2β(u) are the sets of lines that either
intersect u in a single point, or are disjoint from u. In either case it is easy to see that the corresponding graph contains a triangle, and hence we obtain no girth 4 example. Of the remaining groups in cases (ii)β(iv) of [26, Theorem 1.2], we do not need to consider
L=PSL(2,4),PSL(2,9) or PSL(4,2) as these groups are isomorphic to alternating groups, which were treated above. With these exclusions,
the remaining groups L in these cases are listed in
TableΒ 4, together with the stabiliser Luβ, and the subdegrees. In all but one
case Xuβ does not act 2-transitively on either Ξ(u) or
Ξ2β(u) - denoted as above by βnot 2-trans.β in the column headed βCommentsβ. In the exceptional case, case (iii) of [26, Theorem 1.2] with L=PSL(3,4), the stabiliser is 2-transitive on its orbit of length 10, and we obtain the 2-arc-transitive Gewirtz graph of girth 4, as in Part (1). This completes the proof of Theorem 1.2. β
As a corollary of Theorem 1.2, we observed a group theoretic characterisation of the Petersen graph.
A primitive group on a set X is 2-primitive if for every uβX, the stabiliser of u is primitive on Xβ{u}. In particular, each 3-transitive group
is 2-primitive.
Corollary 4.3**.**
Let Ξ be a connected (G,2)-arc-transitive graph of girth 4 or 5,
and let uβV(Ξ). Assume that the Guβ-action on Ξ(u) is 2-primitive and unfaithful. Then
Ξ is either the Petersen graph or a complete bipartite graph.
Proof.
Let (u,v) be an arc of Ξ.
Since Guβ is 2-primitive on Ξ(u),
Guvβ acts primitively on Ξ(u)β{v}.
Let K be the kernel of Gvβ acting on Ξ(v). Then Kβ΄Gvβ and Kβ΄Guvβ.
Since Guvβ is primitive on Ξ(u)β{v}, either K fixes all the vertices of
Ξ(u)β{v} or K is transitive on
Ξ(u)β{v}. If K fixes all the vertices in
Ξ(u)β{v}, then K=1 as Ξ is connected, and so Guβ is faithful on Ξ(u), contradicting our assumption. Hence K is transitive on
Ξ(u)β{v}. Note that Kβ€Guvwβ for each 2-geodesic (u,v,w). Thus Guvwβ
is transitive on Ξ(u)β{v}.
Suppose first that Ξ has girth 4. Then since G is transitive on 2-arcs, Ξ has a cycle of length 4
containing u,v,w, and so w is adjacent to at least one vertex of Ξ(u)β{v}.
Since Guvwβ
is transitive on Ξ(u)β{v}, it follows that
Ξ(u)=Ξ(w), and since this holds for all w, it follows that Ξ is a complete bipartite graph.
Suppose then that Ξ has girth 5. Then, for each of the vertices
xβΞ(u)β{v} there exists a vertex y(x)βΞ(w)β{v} such that (u,v,w,y(x),x) is a 5-cycle. Since Ξ contains no 4-cycles, distinct x,xβ² correspond to distinct y(x),y(xβ²) and it follows that Ξ(w)β{v}βΞ2β(u)
so Ξ has diameter 2.
Then by Theorem 1.2, Ξ is one of the following three graphs: C5β,
the Petersen graph, and the Hoffman-Singleton graph. However, if Ξ is C5β or the Hoffman-Singleton graph, then the vertex stabilisers (in the full
automorphism group) act faithfully on their neighbours, a contradiction. Hence
Ξ is the Petersen graph.
β
5. Proof of Theorem 1.3
In this section, we investigate the class of 3-geodesic-transitive graphs of girth 4 or 5 which are normal covers of a 2-arc-transitive graph of diameter at most 2.
The first subsection determines such covers of complete graphs. We use the parameters aiβ,biβ,ciβ introduced in DefinitionΒ 2.1.
5.1. Covers of complete graphs
Lemma 5.1**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that Ξ is a G-normal cover of the complete graph Krβ for some
rβ₯3, relative to a normal subgroup N of G.
Then Ξ is a distance-transitive antipodal cover of Krβ of diameter 3,
and either
- (i)
Ξ=Kr,rββrK2β* for some rβ₯4, or*
2. (ii)
Ξ* is the distance 2 graph [HoS]2β of the HoffmanβSingleton graph, with r=7.*
Proof.
Let B={B1β,β¦,Brβ} be the set of N-orbits in V(Ξ), so that
Ξ£:=ΞBββ
Krβ with rβ₯3.
Since Ξ is a cover of Ξ£, the valency of Ξ is rβ1β₯2.
Since Ξ has girth 4 or 5, Ξ is not a complete graph, and in particular β£Biββ£β₯2. For the same reason,
if r=3, then Ξ has valency 2 and so Ξ is C4β or C5β, neither of which is a cover of K3β. Hence rβ₯4.
Let (u1β,u2β,u3β) be a 2-geodesic of Ξ with uiββBiβ, for i=1,2. Since Ξ is a cover of Ξ£, u3ββ/B1β, so we may suppose that u3ββB3β. As Ξ£ is a complete graph, it follows that
B1β and B3β are adjacent in Ξ£, and so u3β is adjacent in Ξ to a vertex u1β²ββB1β. Now u1β²βξ =u1β since Ξ has girth at least 4, and since Ξ
is G-arc-transitive, B1β does not contain an edge of Ξ and hence u1β²βξ βΞ(u1β). Thus
u1β²ββΞ2β(u1β)βͺΞ3β(u1β).
If u1β²ββΞ2β(u1β), then there exists a vertex v such that (u1β,v,u1β²β) is a 2-geodesic. This implies that {u1β,u1β²β}βΞ(v)β©B1β, so β£Ξ(v)β©B1ββ£β₯2,
contradicting the fact that Ξ is a cover of Ξ£. Thus
u1β²ββΞ3β(u1β), so u1β²ββΞ3β(u1β)β©B1β. Since Ξ is (G,3)-geodesic-transitive, the stabiliser Gu1ββ is transitive on Ξ3β(u1β) and fixes B1β setwise, so Ξ3β(u1β)βB1β.
Furthermore, as B1β does not contain an edge of Ξ, the induced subgraph [Ξ3β(u1β)] is an empty graph.
Since the diameter of Ξ is at least 3, we have b2β=β£Ξ(u3β)β©Ξ3β(u1β)β£β₯1.
On the other hand, as Ξ is a cover of Ξ£=Krβ and Ξ3β(u1β)βB1β, it follows that β£Ξ(u3β)β©B1ββ£=1. Thus b2β=1.
Since Ξ is (G,3)-geodesic-transitive, it is easy to see that b3ββ€b2β=1, and so
b3β=0 or 1.
Suppose that b3β=1. Then Ξ has diameter at least 4. As [Ξ3β(u1β)] is an empty graph, we obtain a3β=0, and so c3β=(rβ1)βb3β=rβ2. Let (u1β,u2β,u3β,u4β,u5β) be a 4-geodesic of Ξ. Then u4ββB1β and u5ββ/B1β. Hence β£Ξ(u5β)β©B1ββ£=1, and so Ξ(u5β)β©B1β={u4β}, and β£Ξ(u5β)β©Ξ3β(u1β)β£=1 (since Ξ3β(u1β)βB1β). However,
since (u2β,u3β,u4β,u5β) is a 3-geodesic and c3β=rβ2, we have β£Ξ(u5β)β©Ξ2β(u2β)β£=rβ2. We note that Ξ(u5β)β©Ξ2β(u2β)βΞ(u5β)β©Ξ3β(u1β) (since u5ββΞ4β(u1β)). Thus rβ2=β£Ξ(u5β)β©Ξ2β(u2β)β£β€1, contradicting the fact that rβ₯4.
Thus b3β=0, and Ξ has diameter 3. Hence Ξ is G-geodesic-transitive.
Since Ξ has valency rβ1 and girth 4 or 5, it follows that b0β=rβ1,b1β=rβ2 and c1β=1, and we have shown that b2β=1. Furthermore, 2β€c2ββ€rβ2 if the girth is 4 and c2β=1 if the girth is 5.
Since Ξ has diameter 3 and [Ξ3β(u1β)] is an empty graph (since Ξ3β(u1β)βB1β), it follows that a3β=0=b3β, and so c3β=rβ1. Hence
Ξ has intersection array
[TABLE]
Further, for distinct z,zβ²βΞ3β(u1β), the distance
dΞβ(z,zβ²)ξ =1 since a3β=0 and
dΞβ(z,zβ²)ξ =2 since b2β=1, and hence dΞβ(z,zβ²)=3. This implies that
Ξ is a G-distance-transitive antipodal cover of Ξ£, with antipodal blocks of size β£Biββ£=1+β£Ξ3β(u1β)β£=1+(rβ2)/c2β.
Thus, Ξ is listed in [22, Main Theorem].
Moreover, since Ξ is (G,3)-geodesic-transitive with girth 4 or 5, it follows that for each vertex u, Guβ is 2-transitive on Ξ(u), and hence G induces a 3-transitive group on V(Ξ£).
We inspect the candidates in [22, Main Theorem].
The graph in case (1) of [22, Main Theorem] is Ξ=Kr,rββrK2β,
as in part (i), and the graph in case (2) is Ξ=[HoS]2β with r=7 (see also
[7, p.223]). Both are geodesic-transitive. None of the groups G in part (3) (a)β(e)
of [22, Main Theorem] induce a 3-transitive group on V(Ξ£).
Let Ξ be a graph in case (4)(a). Then Ξ is also in [7, Propositon 12.5.3], its intersection array is
(q,qβrqβ1ββ1,1;1,rqβ1β,q), so
Ξ has girth 3, a contradiction.
For graphs in Main Theorem (4)(b) and (5) of [22], G/Nβ€Aut(Ξ) does not induce a
3-transitive action on V(Ξ£), where N is the kernel of G acting on V(Ξ£).
Finally, let Ξ be a graph in case (6). Then Ξ is described in Example 3.6 and Section 6 of
[22]. By Lemma 6.1 of [22], Ξ is a normal Cayley graph of some p-group P and Ξ is as in Proposition 6.2 or 6.3 of [22]. Let u=1Pβ. Since Guβ is 2-transitive on Ξ(u), we have p=2, and
hence the graphs in [22, Proposition 6.3] do not occur.
Thus Ξ is as in [22, Proposition 6.2]. Here r=22b and β£Biββ£=2a for some positive integers a,b,
and G induces an affine 3-transitive group on Ξ£=Krβ
contained in [22b].Sp(2b,2). Such a group is 3-transitive only when b=1, and in this case 2a=β£Biββ£=1+(rβ2)/c2β=1+2/c2β,
so that c2β=2 and β£Biββ£=2. It follows that Ξβ
H(3,2)β
Q3ββ
K4,4ββ4K2β, as in (i).
β
5.2. Covers of the Petersen graph and β‘5β, and a general lemma
First we determine the 3-geodesic-transitive covers of
the Petersen graph and the folded 5-cube.
Lemma 5.2**.**
Let Ξ be a connected 3-geodesic-transitive graph of girth 4 or 5. Then the following hold.
(1)* Ξ is not a cover of Crβ for r=4,5.*
(2)* If Ξ is a cover of the Petersen graph, then Ξ is the dodecahedron.*
(3)* If Ξ is a cover of β‘5β, then Ξ is either H(5,2) or the Armanios-Wells graph.*
Proof.
(1) If Ξ is a cover of Crβ where r=4,5, then Ξ has valency 2 and girth 4 or 5, and so Ξβ
C4β or C5β which have no 3-geodesics, a contradiction.
(2) Suppose that Ξ is a cover of the Petersen graph.
Then Ξ has valency 3 and girth 5, and so c2β=1 and a2β=1 or 2.
Since Ξ has diameter at least 3, we must have a2β=1 and b2β=1. Then by Remark 2.3, Ξ is a geodesic-transitive graph of valency 3, so Ξ is listed in [7, p.221]. By inspecting the candidates, we conclude that Ξ is the dodecahedron.
(3) Suppose that Ξ is a cover of β‘5β. Since β‘5β has valency 5 and girth 4, it follows that Ξ has valency 5 and girth 4 or 5.
Then by Theorem 1.1 of [25], Ξ is either H(5,2) or
the Armanios-Wells graph. β
The following lemma will be used frequently in the rest of our analysis.
Lemma 5.3**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that G has an intransitive normal subgroup N with at least 3 orbits
on V(Ξ) such that
ΞNβ has diameter 2. Let (B0β,B1β,B2β) be a
2-geodesic of ΞNβ. Then there exist uiββBiβ, for each i
such that (u0β,u1β,u2β) is a 2-geodesic of Ξ, and for each such 2-geodesic
the following statements hold.
ΞNβ* has girth at least 4.*
GB0ββ=NGu0ββ, GB0βB1ββ=NGu0βu1ββ and GB0βB1βB2ββ=NGu0βu1βu2ββ.
If BβΞNβ(B0β)β©ΞNβ(B2β) such that Bξ =B1β, then
Ξ(u2β)β©BβΞ(u0β)βͺΞ3β(u0β). Moreover if
Ξ(u2β)β©Bβ©Ξ3β(u0β)ξ =β
, then all vertices of
Ξ3β(u0β) lie in blocks of ΞNβ(B0β) and β£Ξ3β(u0β)β£ is divisible by the valency
β£Ξ(u0β)β£.
If β£Ξ(u0β)β©Ξ(u2β)β£=β£ΞNβ(B0β)β©ΞNβ(B2β)β£ (that is if
Ξ and ΞNβ has βthe same c2ββ), then GB0βB2ββ=NGu0βB2ββ=NGu0βu2ββ.
Proof.
(1) Since Ξ has girth 4 or 5, Ξξ β
Km[b]β for any mβ₯3,bβ₯2.
Hence by LemmaΒ 3.2, Ξ is a cover of ΞNβ, N is semiregular on V(Ξ) (so each N-orbit has β£Nβ£ vertices), and ΞNβ is (G/N,2)-geodesic-transitive.
Since ΞNβ has diameter 2 it follows from LemmaΒ 3.3 that ΞNβ has girth at least 4.
(2) Also, since Ξ covers ΞNβ, each u0ββB0β determines a unique u1ββB1β and
u2ββB2β such that (u0β,u1β,u2β) is a 2-arc of Ξ, and indeed it must be
a 2-geodesic of Ξ since ΞNβ has girth at least 4.
Now B0ββV(ΞNβ) is the N-orbit containing u0β, that is,
B0β=u0Nβ, and B0β is a block of imprimitivity for G in V(Ξ).
Thus both Gu0βββ€GB0ββ and N<GB0ββ, and as N is transitive on B0β, it follows that GB0ββ=NGu0ββ.
For i=1,2, consider the transitive action of GB0ββ¦Biββ on B0β. The stabiliser of u0β is H:=GB0ββ¦Biβββ©Gu0ββ. Since u1β is the unique point of B1β adjacent to u0β, H also fixes u1β; and similarly, if i=2, since u2β is the unique point of B2β adjacent to u1β, H also fixes u2β. Thus Hβ€Gu0ββ¦uiββ, and conversely Gu0ββ¦uiβββ€GB0ββ¦Biβββ©Gu0ββ. Hence the stabiliser H=Gu0ββ¦uiββ. Since the subgroup N of
GB0ββ¦Biββ is transitive on B0β, it follows that GB0ββ¦Biββ=NGu0ββ¦uiββ.
(3) Let BβΞNβ(B0β)β©ΞNβ(B2β) such that Bξ =B1β and let uβΞ(u2β)β©B.
Since (u0β,u1β,u2β) is a 2-geodesic of Ξ, the distance dΞβ(u0β,u2β)=2 and so dΞβ(u0β,u)β€3. If dΞβ(u0β,u)=2, then some element of Gu0ββ maps u to u2β, and hence maps B to B2β, which is impossible since B,B2β have distances 1, 2 from B0β in ΞNβ, respectively.
Thus uβΞ(u0β)βͺΞ3β(u0β). Finally suppose that dΞβ(u0β,u)=3. Since Ξ is (G,3)-geodesic-transitive, Gu0ββ is transitive on Ξ3β(u0β), and so all points of
Ξ3β(u0β) lie in blocks of ΞNβ(B0β). Since Gu0ββ is transitive on ΞNβ(B0β),
it follows that β£ΞNβ(B0β)β£=β£Ξ(u0β)β£ divides β£Ξ3β(u0β)β£.
(4) Suppose that Ξ and ΞNβ have the same value of c2β. Since G is transitive on the 2-geodesics of both Ξ and ΞNβ, we have c2β=β£GB0βB2ββ:GB0βB1βB2βββ£=β£Gu0βu2ββ:Gu0βu1βu2βββ£. Hence using this and part (2), we have
[TABLE]
and it follows that GB0βB2ββ=NGu0βu2ββ. Since NGu0βu2βββNGu0βB2βββGB0βB2ββ, equality holds and part (4) is proved.
β
5.3. Covers of the Higman-Sims graph
Recall that the Higman-Sims graph is strongly regular with parameters (100,22,0,6).
The following lemma determines the unique 3-geodesic-transitive cover of the Higman-Sims graph.
Lemma 5.4**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5 such that Ξ is a
G-normal cover of the Higman-Sims graph Ξ£. Then Ξ is the standard double cover of Ξ£, and
G=HΓZ2β, where H is the Higman-Sims group HS or HS.Z2β.
Proof.
By assumption there is a non-trivial normal subgroup Nβ΄G such that Ξ is a cover of the Higman-Sims graph Ξ£=ΞNβ. Since Ξ£ is strongly regular with parameters (100,22,0,6), the graph
Ξ has valency 22 and c2ββ€6.
Let uβV(Ξ), and let B=uN be the N-orbit (vertex of Ξ£) containing u, so GBβ=NGuβ (LemmaΒ 5.3 (2)). By LemmaΒ 3.2,
N is semiregular on V(Ξ), the subgroup induced by G on Ξ£ is G/N and this group acts transitively on the 2-geodesics of Ξ£. In particular, GBβ acts 2-transitively on Ξ£(B), and it follows that G/Nβ
HS or HS.Z2β, and Guββ
GBβ/Nβ
M22β or M22β.Z2β, respectively (see [11, p.39, 80], for example).
Let (B0β,B1β,B2β) be a 2-geodesic of Ξ£. Since Ξ covers Ξ£, there are vertices uiββBiβ, for i=0,1,2
such that (u0β,u1β,u2β) is a 2-geodesic of Ξ. It follows from the parameters of Ξ£ that the
set Ξ:=Ξ£(B0β)β©Ξ£(B2β)
has size 6 and contains B1β. Moreover, exactly c2ββ₯1 of the Ξ£-vertices in Ξ (including B1β) contain a vertex of Ξ(u0β)β©Ξ(u2β). In particular, this c2β-subset of Ξ is fixed setwise by Gu0βu1βu2ββ. By LemmaΒ 5.3 (2), GB0βB1βB2ββ=NGu0βu1βu2ββ, and hence GB0βB1βB2ββ leaves invariant a c2β-subset of Ξ containing B1β.
Considering the G-action on Ξ£, we have (see [11, p.80]) GB0βB2ββ/N=Z24β.A6β or Z24β.S6β, and so GB0βB2ββ induces A6β or S6β on Ξ, so that GB0βB1βB2ββ is transitive on the 5-subset Ξβ{B1β}. We conclude from the observation in the previous paragraph that c2β=1 or c2β=6. If c2β=6, then it follows from work of Cameron, see [10, Part (II) on p.4], that Ξ is the standard double cover of the Higman-Sims graph as in Definition 2.4, and the assertions of the lemma hold.
Assume to the contrary that c2β=1, so Ξ has girth 5. We shall obtain a contradiction.
Let B3ββ(Ξ£(B0β)β©Ξ£(B2β))β{B1β}
and B4ββΞ£2β(B0β)β©Ξ£(B2β).
Let uiββBiβ (i=3,4) such that (u0β,u1β,u2β,u3β)
and (u0β,u1β,u2β,u4β) are 3-arcs. Then as c2β=1, the two vertices u3β and u4β are in Ξ2β(u0β)βͺΞ3β(u0β).
By LemmaΒ 5.3(3), it follows that u3ββΞ3β(u0β), and since this holds for each of the 5 blocks
B3ββ(Ξ£(B0β)β©Ξ£(B2β))β{B1β}, it follows that b2β=β£Ξ3β(u0β)β©Ξ(u2β)β£β₯5.
Moreover, by LemmaΒ 5.3(3), all points of
Ξ3β(u0β) lie in blocks of Ξ£(B0β), and therefore u4ββΞ2β(u0β).
Since this holds for each of the 16 blocks B4ββΞ£2β(B0β)β©Ξ£(B2β), it follows that
a2β=β£Ξ2β(u0β)β©Ξ(u2β)β£β₯16 for Ξ. Thus 22=β£Ξ(u2β)β£=a2β+b2β+c2ββ₯16+5+1=22, and so a2β=16 and b2β=5.
Since B3ββΞ£(B0β), there exists a vertex u0β²ββB0β such that
(u3β,u0β²β) is an arc of Ξ. Further u0β²βξ =u0β, as Ξ has
girth 5. The sequence (u0β,u1β,u2β,u3β,u0β²β) is a 4-arc, so 1β€dΞβ(u0β,u0β²β)β€4. Further Gu0ββ fixes Ξ£(B0β) and Ξ£2β(B0β) setwise, and there are blocks
in Ξ£(B0β)βͺΞ£2β(B0β) that contain vertices from Ξiβ(u0β) for i=1,2 or 3 (such as u1β,u2β,u3β respectively). Since
Ξ is (G,3)-geodesic-transitive, Gu0ββ is transitive on Ξiβ(u0β) for each i=1,2,3, and hence
dΞβ(u0β,u0β²β)=4, and Ξ has diameter at least 4..
Consider Ξ¦:=Ξ2β(u1β)β©Ξ(u3β). Then Ξ¦βΞ2β(u0β)βͺΞ3β(u0β). Since dΞβ(u1β,u3β)=2, it follows that β£Ξ¦β£=a2β=16.
Let uβΞ¦ and let B be the block containing u. If uβΞ3β(u0β),
then B would lie in Ξ£(B0β) and (B0β,B3β,B) would be a triangle in Ξ£,
contradicting the fact that Ξ£ has girth 4. Thus Ξ¦β©Ξ3β(u0β)=β
, and
hence Ξ¦βΞ2β(u0β), so c3β=β£Ξ2β(u0β)β©Ξ(u3β)β£β₯β£Ξ¦β£=16. Also c3ββ€21 since Ξ has diameter at least 4.
Counting the edges between Ξ2β(u0β) and Ξ3β(u0β), we find β£Ξ3β(u0β)β£β
c3β=β£Ξ2β(u0β)β£β
b2β=22β
21β
5, and as 16β€c3ββ€21 we conclude that c3β=21.
Since Ξ has valency 22 and diameter at least 4, this implies that b3β=1, a3β=0.
Thus by Remark 2.3 (2), Ξ is G-distance-transitive.
Furthermore, β£Ξ3β(u0β)β£=22β
5, and so the number of edges between Ξ3β(u0β) and Ξ4β(u0β)
is 22β
5=β£Ξ3β(u0β)β£β
b3β=β£Ξ4β(u0β)β£β
c4β. Thus c4β divides 22β
5 and by [4, Proposition 20.4],
c4ββ₯c3β=21, so c4β=22,β£Ξ4β(u0β)β£=5, and Ξ has diameter 4. The set of N-orbits is a block system for G which is not a bipartition, and it follows from [32, Theorem 2] that it is a set of antipodal blocks and Ξ is antipodal.
Thus B0β={u0β}βͺΞ4β(u0β) and GB0βB0ββ is 2-transitive on B0β of degree 6. However as N is semiregular on V(Ξ), NB0β is a regular normal subgroup of GB0βB0ββ, which is a contradiction since β£B0ββ£=6 is not a prime power.
β
5.4. Covers of the Gewirtz graph
Next we consider covers of the Gewirtz graph. Our first step identifies two substantial cases to be analysed.
Lemma 5.5**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that Ξ is a G-normal cover of the Gewirtz graph Ξ£, that is, G has a normal subgroup N such that ΞNββ
Ξ£. Then the following hold:
Ξ* has girth 4 and c2β=2;*
PSL(3,4)β€G/Nβ€PSL(3,4).Z22β* and, for u0ββV(Ξ), either*
- (a)
Gu0ββ=PSL(2,9)* or PΞ£L(2,9), and (a2β,b2β)=(4,4); or*
2. (b)
Gu0ββ=PGL(2,9),M10β* or PΞL(2,9), and (a2β,b2β)=(0,8).*
Proof.
We identify ΞNβ=Ξ£. Since Ξ£ is strongly regular
with parameters (56,10,0,2), it follows that Ξ has valency 10 and c2ββ€2. So either Ξ has girth 4 and c2β=2, or Ξ has girth 5 and c2β=1.
Let (B0β,B1β,B2β) be a 2-geodesic of Ξ£ and let B3ββΞ£(B0β)β©Ξ£(B2β)
such that B3βξ =B1β. Let uiββBiβ, for each i, such that (u0β,u1β,u2β,u3β) is a 3-arc of Ξ.
Since Ξ has girth 4 or 5, it follows that (u0β,u1β,u2β) is a 2-geodesic.
Let B4ββΞ£2β(B0β)β©Ξ£(B2β) and let u4ββB4β so that (u0β,u1β,u2β,u4β) is a 3-arc.
Suppose for a contradiction that the girth of Ξ is 5, that is, c2β=1. By LemmaΒ 5.3(3), the vertex u3ββΞ3β(u0β) so (u0β,u1β,u2β,u3β) is a 3-geodesic,
and Ξ3β(u0β) is contained in the union of the blocks of Ξ£(B0β). This implies that u4ββ/Ξ3β(u0β), and so u4ββΞ2β(u0β). Since this holds for each choice of B4β and β£Ξ£2β(B0β)β©Ξ£(B2β)β£=8,
it follows that a2β=β£Ξ2β(u0β)β©Ξ(u2β)β£β₯8, and since Ξ has valency 10
and Ξ(u2β) contains also u1β,u3β, we must have a2β=8, b2β=1 and c2β=1.
Thus by Remark 2.3(1), Ξ is a G-distance-transitive graph of valency 10. However, by inspecting the candidates in [7, p.224], such a graph does not exist.
Hence Ξ has girth 4 and so c2β=2, and Part (1) holds.
Also, since Ξ£(B0β)β©Ξ£(B2β)={B1β,B3β}, we have Ξ(u0β)β©Ξ(u2β)={u1β,u3β},
(u0β,u1β,u2β,u3β) is a 4-cycle, and (u0β,u1β,u2β,u4β) is a 3-geodesic for at least one choice of B4β,u4β.
The group G induces a subgroup G/N of Aut(Ξ£)=PSL(3,4).Z22β, and by [11, p.23], the only vertex-transitive proper subgroups of Aut(Ξ£) contain PSL(3,4). Thus PSL(3,4)β€G/N. By LemmaΒ 5.3 (2), Gu0βββ
GB0ββ/N and so
PSL(2,9)β€Gu0βββ€PSL(2,9).Z22β (see [11, p.23]), as in Part (2).
Since Ξ is (G,3)-geodesic-transitive, Gu0βu1βu2ββ is transitive on the b2β-subset
Ξ3β(u0β)β©Ξ(u2β). The possible stabiliser subgroups Gu0ββ give us two possibilities for the parameters a2β,b2β as follows:
(a) if Gu0ββ=PSL(2,9) or PΞ£L(2,9) then Gu0βu2ββ has two orbits in
Ξ(u2β)β{u1β,u3β}, each of length 4, and so a2β=β£Ξ2β(u0β)β©Ξ(u2β)β£=4 and b2β=β£Ξ3β(u0β)β©Ξ(u2β)β£=4;
(b) in all other cases (namely Gu0ββ=PGL(2,9),M10β or PΞL(2,9)), Gu0βu2ββ is
transitive on Ξ(u2β)β{u1β,u3β}, and we have a2β=β£Ξ2β(u0β)β©Ξ(u2β)β£=0 and b2β=β£Ξ3β(u0β)β©Ξ(u2β)β£=8.
β
We now show that case (2)(a) of LemmaΒ 5.5 leads to no examples.
Lemma 5.6**.**
There are no (G,3)-geodesic-transitive graphs Ξ satisfying the conditions of
LemmaΒ \refcoverβgβ1A(2)(a).
Proof.
Let Ξ,Ξ£,G be as in LemmaΒ 5.5 and suppose that part (2)(a) holds
so that (a2β,b2β,c2β)=(4,4,2) and Ξ has valency 10.
Let B,Bβ²βV(Ξ£) such that dΞ£β(B,Bβ²)=2, and let uβB and uβ²βBβ² such that dΞβ(u,uβ²)=2. In our case (LemmaΒ 5.5(2)(a)), Guββ
GBβ/N=PSL(2,9) or PΞ£L(2,9), and Ξ:=Ξ(uβ²)β©Ξ2β(u) is an orbit of Guuβ²β of length 4.
Let Ξ© be the set of four blocks of Ξ£2β(B)β©Ξ£(Bβ²) containing a point of
Ξ, and let Ξ©β² be the set consisting of the remaining four blocks of Ξ£2β(B)β©Ξ£(Bβ²). Then Guuβ²β and GBBβ²β leave Ξ£2β(B)β©Ξ£(Bβ²)=Ξ©βͺΞ©β² invariant, and both are transitive on Ξ©. Moreover, the set Ξ© is the set of blocks adjacent to Bβ² in a (GBβ/N)-invariant subgraph of valency 4 of the induced subgraph
[Ξ£2β(B)].
We consider the action of GBBβ²β/Nβ€Aut(Ξ£) on Ξ£2β(B). Now Aut(Ξ£)=PSL(3,4).Z22β has a subgroup Y such that β£Y:(G/N)β£=2 and
YBβ=PGL(2,9) or PΞL(2,9) according as Guβ=PSL(2,9) or PΞ£L(2,9), respectively. The group YBβ is transitive on Ξ£2β(B) of degree 45 and
the stabiliser YBBβ²β is a Sylow 2-subgroup of YBβ. Similarly its index 2 subgroup GBβ/N
is transitive on Ξ£2β(B) and its stabiliser GBBβ²β/N is a Sylow 2-subgroup of GBβ/N. Thus each of YBβ and GBβ/N has a unique transitive representation of degree 45 up to permutational isomorphism. A computation using MAGMA [5] shows that, in this representation, YBBβ²β has a unique orbit of size 8, and this orbit must be
Ξ£2β(B)β©Ξ£(Bβ²). A further computation shows that this YBBβ²β-orbit
is the union of two orbits of GBBβ²β/N of length 4.
Now YBβ has a transitive action on the 45 flags (incident point-line pairs) of the
generalised quadrangle GQ(2,2), and the uniqueness of this representation discussed above means that we may identify the vertices of [Ξ£2β(B)] with the flags of GQ(2,2).
Let us define two flags (p,L) and (q,M) (where p,q are points and L,M are lines of GQ(2,2) incident with p,q, respectively) to be adjacent if and only if pξ =q, Lξ =M, and either p lies on M or q lies on L. Then (p,L) is adjacent to exactly eight flags and YBβ is transitive on ordered pairs of adjacent flags.
Thus this definition of adjacency defines an arc-transitive graph on [Ξ£2β(B)] of valency 8,
and the uniqueness of Ξ£2β(B)β©Ξ£(Bβ²) as a YBBβ²β-orbit of size 8 implies that the induced subgraph [Ξ£2β(B)] has precisely this adjacency rule. Further, taking Bβ² to be the flag (p,L), one may check that
GBBβ²β/N leaves invariant, and acts transitively on the sets {(q,M)β£qξ =p,Mξ =L,qβL} and
{(q,M)β£qξ =p,Mξ =L,pβM}, each of size 4. It follows that Ξ© is equal to one of these sets. However the sets
{(q,M)β£qξ =p,Mξ =L,qβL} and
{(q,M)β£qξ =p,Mξ =L,pβM} are paired orbits of GBBβ²β/N, and therefore do not correspond to undirected graphs of valency 4. (Instead they correspond to (GBβ/N)-invariant orientations of the edge set of [Ξ£2β(B)].) This is a contradiction, since when a2β=4, the set Ξ© is the neighbourhood of Bβ² in a (GBβ/N)-invariant valency 4 (undirected) subgraph of [Ξ£2β(Bβ²)].
Therefore (a2β,c2β)ξ =(4,2) for Ξ and there are no examples satisfying the conditions of LemmaΒ 5.5(2)(a).
β
Finally we deal with case (2)(b) of LemmaΒ 5.5.
Lemma 5.7**.**
Let Ξ be a (G,3)-geodesic-transitive graph, and suppose that the conditions of
LemmaΒ \refcoverβgβ1A(2)(b) hold. Then either
Ξ* is the standard double cover of the Gewirtz graph, or*
Ξ* has diameter at least 4 and is not (G,4)-distance-transitive.*
Proof.
First we show that the standard double cover Ξ£ of the Gewirtz graph Ξ£ is an example.
Let G=AΓβ¨Οβ©, where A=Aut(Ξ£) and Ο is
the map defined before LemmaΒ 2.6. Then since Ξ£ is connected and non-bipartite with c2β=2,
it follows from LemmaΒ 2.6 that Ξ£ is connected with c2β=2. Also it follows from the definition that
Ξ£ is a G-normal cover of Ξ£Nββ
Ξ£, where N=1Γβ¨Οβ©β΄G.
Finally, it follows from the discussion at the end of the proof of LemmaΒ 5.5 that G is transitive on the s-geodesics
of Ξ£, for each sβ€3. Thus all conditions hold and Ξ£ is an example.
If Ξ,G satisfy the hypotheses of the lemma, and if Ξ has diameter at least 4 and is not
(G,4)-distance-transitive, then (2) holds. So we assume that this is not the case, and hence we assume that Ξ,G have the following properties:
Ξ is connected, (G,3)-geodesic-transitive, and (G,s)-distance-transitive for s=min{4,diam(Ξ)},
Ξ has girth 4 with (a2β,b2β,c2β)=(0,8,2), ΞNββ
Ξ£ for some non-trivial normal subgroup N of G,
and Gu0ββ=PGL(2,9),M10β or PΞL(2,9), for u0ββV(Ξ).
We claim that, if Ξ is not bipartite, then its standard double cover Ξ and the
group G=GΓβ¨Οβ© (with Ο as defined before LemmaΒ 2.6),
satisfy all of these conditions.
To prove this claim, assume that Ξ is not bipartite. Then Ξ is connected.
Since Ξ is connected of girth 4 with c2β=2,
it follows from LemmaΒ 2.6 that Ξ has girth 4 with c2β=2, and also from LemmaΒ 2.6 it follows that
Ξ is (G,3)-geodesic-transitive (since a2β=0) and
Ξ is (G,4)-distance-transitive (since diam(Ξ)>diam(Ξ)β₯3).
Finally Ξ is a G-normal cover of ΞNββ
ΞNββ
Ξ£,
where N=NΓβ¨Οβ©β΄G, and the vertex stabilisers in G and G are isomorphic, implying, by LemmaΒ 5.5 that (a2β,b2β)=(0,8).
This proves the claim.
We now assume that Ξ is bipartite, if necessary replacing a non-bipartite graph with its standard double cover.
We will prove that, under this assumption, Ξ is Ξ£ as in part (1).
If in fact the original graph had been non-bipartite, then this would imply that Ξ=Ξ£ and hence that
Ξ=Ξ£, which is not the case since diam(Ξ£)=2. Hence to complete the proof of the lemma, it is sufficient to assume that
Ξ is bipartite and to prove that Ξ=Ξ£. So we assume that Ξ,G,N satisfy all the conditions
of the previous paragraph and in addition that Ξ is bipartite.
Note that the Gewirtz graph Ξ£ has valency 10, so also Ξ has valency 10 since it covers Ξ£.
As in the proof of LemmaΒ 5.5,
let (B0β,B1β,B2β) be a 2-geodesic of Ξ£ and let B3ββΞ£(B0β)β©Ξ£(B2β)
such that B3βξ =B1β. Let uiββBiβ, for each i, such that (u0β,u1β,u2β,u3β) is a 3-arc of Ξ; it was shown that this is a 4-cycle and Ξ(u0β)β©Ξ(u2β)={u1β,u3β}.
Let B4ββΞ£2β(B0β)β©Ξ£(B2β) and let u4ββB4β so that (u0β,u1β,u2β,u4β) is a 3-arc; it was shown that this is a 3-geodesic for
each of the 8 choices for B4β (since a2β=8).
Also in this case the stabiliser Gu0ββ is 3-transitive on Ξ(u0β).
Let Ξ£(B0β)β©Ξ£(B4β)={B5β,B6β} and, for iβ{5,6},
let uiββBiβ such that the sequence (u0β,u1β,u2β,u4β,uiβ) is a 4-arc.
Since (u0β,u1β,u2β,u4β) is a 3-geodesic, dΞβ(u0β,uiβ)β{2,3,4}, but since
Ξ is (G,3)-geodesic-transitive and B2β,B3ββΞ£2β(B0β), all vertices of
Ξ2β(u0β)βͺΞ3β(u0β) lie in blocks of Ξ£2β(B0β).
Hence uiββΞ4β(u0β), and since Ξ is (G,4)-distance-transitive,
all vertices of Ξ4β(u0β) lie in blocks of Ξ£(B0β). Now Ξ4β(u0β)β©Ξ(u4β) contains {u5β,u6β} so b3ββ₯2.
Since B5ββΞ£(B0β), u5β is adjacent to a vertex u0β²ββB0β, and so
(u0β,u1β,u2β,u4β,u5β,u0β²β) is a 5-arc. Thus dΞβ(u0β,u0β²β) is at most 5, and is greater than 4 since vertices of βͺi=14βΞiβ(u0β) lie in blocks in
Ξ£(B0β)βͺΞ£2β(B0β).
Hence dΞβ(u0β,u0β²β)=5 and Ξ has diameter at least 5.
Further, each vertex of Ξ4β(u0β)β©Ξ(u4β) lies in one of the two
blocks B5β,B6ββΞ£(B0β) adjacent to B4β.
Thus Ξ4β(u0β)β©Ξ(u4β)={u5β,u6β} (since Ξ is a cover of Ξ£), and b3β=2.
Since Ξ is bipartite of valency 10, a3β=0 and c3β=β£Ξ2β(u0β)β©Ξ(u4β)β£=10βb3β=8.
Thus we have β£Ξ2β(u0β)β£=c2β10Γb1ββ=290β=45,
β£Ξ3β(u0β)β£=c3β45Γb2ββ=845Γ8β=45, and
β£Ξ4β(u0β)β£=c4β45Γb3ββ=c4β90β, with c4ββ₯c3β=8.
Since vertices of Ξ4β(u0β) lie in blocks of Ξ£(B0β), Ξ4β(u0β) consists of a constant number of vertices from each of these blocks and so β£Ξ4β(u0β)β£ is divisible by 10.
It follows that c4β=9 and β£Ξ4β(u0β)β£=10. Then b4β=1 (as Ξ is bipartite),
Ξ is G-distance-transitive (Remark 2.3), and
β£Ξ5β(u0β)β£=c5β10Γb4ββ=c5β10β, with c5ββ₯c4β=9,
so c5β=10 and β£Ξ5β(u0β)β£=1.
Thus Ξ is an antipodal double cover of Ξ£ as well as bipartite, and has odd diameter.
Hence by LemmaΒ 2.5, Ξ is the standard double cover of the Gewirtz graph Ξ£.
β
5.5. Covers of the M22β graph
First we determine the value of c2β for a G-normal cover of the M22β-graph.
Lemma 5.8**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that Ξ is a G-normal cover of the M22β-graph Ξ£, that is, G has a normal subgroup
N such that ΞNββ
Ξ£.
Let uβV(Ξ). Then
- (1)
G/N=M22β* or M22β.2, and Guβ=Z24β:S6β or Z24β:A6β, respectively, and*
2. (2)
c2β=4.
Proof.
(1) The M22β-graph Ξ£ is
strongly regular with parameters (77,16,0,4). Let uβBβV(Ξ£).
By [6], A:=Aut(Ξ£)β
M22β.2
and ABββ
Z24β:S6β. Moreover, it follows from [11, p.39] that M22β
is the only proper subgroup of M22β.2 which is vertex transitive on Ξ£. Hence
G/N=M22β or M22β.2, and GBβ/N=Z24β:S6β or Z24β:A6β, respectively.
Since Ξ is (G,3)-geodesic-transitive of girth 4 or 5, it follows from Lemma 5.3 (2) that GBβ=NGuβ, and
by Lemma 3.2, N is semiregular on V(Ξ). Thus Guββ©N=1Gβ and
Guββ
Guβ/(Guββ©N)β
NGuβ/N=GBβ/N, proving part (1).
(2) Since Ξ covers Ξ£ it follows that Ξ has valency 16 and c2ββ€4.
Suppose that c2β<4. Let (B0β,B1β,B2β) be a 2-geodesic of Ξ£. Let uiββBiβ (0β€iβ€2) such that
(u0β,u1β,u2β) is a 2-arc of Ξ. Since Ξ has no triangles,
(u0β,u1β,u2β) is a 2-geodesic.
Let B3ββΞ£(B0β)β©Ξ£(B2β) be one of the
4βc2β blocks that contain no point of Ξ(u0β)β©Ξ(u2β),
and let B4β be one of the 12 blocks of Ξ£2β(B0β)β©Ξ£(B2β).
Let uiββBiβ (i=3,4) such that (u0β,u1β,u2β,u3β)
and (u0β,u1β,u2β,u4β) are 3-arcs of Ξ.
By LemmaΒ 5.3(3), u3ββΞ3β(u0β) so that
b2β:=β£Ξ(u2β)β©Ξ3β(u0β)β£β₯4βc2β; and also all vertices
of Ξ3β(u0β) lie in blocks of Ξ£(B0β) so that u4βξ βΞ3β(u0β).
Since the block B4β is not in Ξ£(B0β) it follows that u4ββΞ2β(u0β),
and hence that a2β:=β£Ξ(u2β)β©Ξ2β(u0β)β£β₯12. Since the
valency 16=a2β+b2β+c2β we conclude that a2β=12 and b2β=4βc2β.
Since B3ββΞ£(B0β), there exists a vertex u0β²ββB0β adjacent to u3β.
Further u0β²βξ =u0β, as u3βξ βΞ(u0β).
By the (G,3)-geodesic-transitivity of Ξ, Gu0ββ is transitive on Ξiβ(u0β) for i=1,2,3 and so vertices in these sets lie in blocks of Ξ£(B0β)βͺΞ£2β(B0β).
Hence u0β²ββΞ4β(u0β), and Ξ has diameter at least 4.
Next we claim that c3β:=β£Ξ(u3β)β©Ξ2β(u0β)β£=15. Consider
Ξ:=Ξ(u3β)β©Ξ2β(u1β). Since dΞβ(u1β,u3β)=2, β£Ξβ£=a2β=12. Since there are no Ξ-edges between blocks of Ξ£(B0β) and since all vertices of Ξ3β(u0β)
lie in bocks of Ξ£(B0β), it follows that Ξ is disjoint from Ξ3β(u0β).
Then since ΞβΞ2β(u1β) it follows that ΞβΞ2β(u0β). Thus
Ξ(u3β)β©Ξ2β(u0β) contains Ξ and so c3ββ₯12. To determine c3β exactly we use some divisibility arguments. Since all vertices of Ξ2β(u0β) lie in blocks of Ξ£2β(B0β), and since Gu0ββ is transitive on both Ξ2β(u0β) and Ξ£2β(B0β) (LemmaΒ 5.3), it follows that β£Ξ£2β(B0β)β£=60 divides β£Ξ2β(u0β)β£=c2β16Γ15β=c2β240β.
Since c2β<4, this implies that c2β=1 or 2. Again, by LemmaΒ 5.3(3), β£Ξ(u0β)β£=16 divides β£Ξ3β(u0β)β£=c2β240βΓc3β4βc2ββ, and this implies that c3β divides 45. It follows that c3β=15, as claimed.
Since Ξ has diameter at least 4, b3β:=β£Ξ(u3β)β©Ξ4β(u0β)β£=1 and
a3β:=β£Ξ(u3β)β©Ξ3β(u0β)β£=0, and so by Remark 2.3, Ξ is G-distance-transitive.
Since a2β=12, Ξ contains 5-cycles and hence is not bipartite, and since Ξ is also not vertex-primitive, it follows from [32, Theorem 2] that Ξ is antipodal.
We showed above that c2ββ€2.
If c2β=2 then β£Ξ2β(u0β)β£=c2β16Γ15β=120, β£Ξ3β(u0β)β£=2Γc3β240Γ2β=16, and β£Ξ4β(u0β)β£=c4β16Γ1β with c4ββ₯c3β=15, so we find that β£Ξ4β(u0β)β£=1, Ξ has diameter 4,
and Ξ has intersection array (16,15,2,1;1,2,15,16). However, by [7, p.421], such a graph does not exist.
Hence c2β=1, so b2β=3 and we obtain β£Ξ2β(u0β)β£=c2β16Γ15β=240,
β£Ξ3β(u0β)β£=c3β240Γ3β=48, and β£Ξ4β(u0β)β£=c4β48Γ1β with c4ββ₯c3β=15. Thus c4β=16, β£Ξ4β(u0β)β£=3. Hence Gu0ββ has a transitive action on Ξ4β(u0β) of degree 3, but this is impossible since by part (1), Gu0ββ=Z24β:S6β or Z24β:A6β.
β
Lemma 5.9**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that Ξ is a G-normal cover of the M22β-graph. Then
either
Ξ* is the standard double cover of the M22β-graph, or*
Ξ* has diameter at least 4 and is not (G,4)-distance-transitive.*
Proof.
Let Ξ£ be the M22β-graph, a strongly regular graph with parameters (77,16,0,4), and let Nβ΄G such that ΞNββ
Ξ£. Since Ξ is a cover of Ξ£, Ξ has valency 16, and by Lemma 5.8, G/N=M22β or M22β.2, and c2β=4. We identify ΞNβ with Ξ£.
Let (u0β,u1β,u2β,u3β) be a 3-geodesic of Ξ such that uiββBiββV(Ξ£). Then (B0β,B1β,B2β, B3β) is a 3-arc of Ξ£.
Since Ξ£ also has c2β=4, it follows that for each BβΞ£(B0β)β©Ξ£(B2β) such that Bξ =B1β, the unique vertex of Ξ(u2β)β©B is adjacent to u0β. Hence
B3ββ/Ξ£(B0β), and so B3ββΞ£2β(B0β).
Also by LemmaΒ 5.3(4), we have GB0βB2ββ=NGu0βB2ββ=NGu0βu2ββ (since c2β=4).
It can be easily checked using MAGMA [5] that GB0βB2ββ/Nβ
Z22β.S4β or Z22β.S4β.Z2β and acts transitively
on Ξ£2β(B0β)β©Ξ£(B2β), a set of 12 blocks including B3β. It follows that Gu0βu2ββ acts transitively on Ξ£2β(B0β)β©Ξ£(B2β). Therefore Ξ3β(u0β)β©Ξ(u2β) contains a point from each of these 12 blocks, and hence b2β:=β£Ξ3β(u0β)β©Ξ(u2β)β£β₯12. Since the valency 16=a2β+b2β+c2ββ₯a2β+12+4, we have a2β=0 and b2β=12.
Now β£Ξ£(B0β)β©Ξ£(B3β)β£=4, say Ξ£(B0β)β©Ξ£(B3β)={E1β,E2β,E3β,E4β}, and, for each i, let
Ξ(u3β)β©Eiβ={eiβ}. Then dΞβ(u0β,eiβ)β€4, and dΞβ(u0β,eiβ)ξ =1 since u3ββΞ3β(u0β). Since Gu0ββ is transitive on Ξiβ(u0β) for i=2,3 and u2β,u3β lie in blocks in Ξ£2β(B0β), it follows that dΞβ(u0β,eiβ)ξ =2,3 and hence dΞβ(u0β,eiβ)=4, so diam(Ξ)β₯4 and b3β=β£Ξ4β(u0β)β©Ξ(u3β)β£β₯4.
If Ξ is not (G,4)-distance-transitive then part (2) holds, so suppose now that Ξ is (G,4)-distance-transitive.
Then all vertices in Ξ4β(u0β) lie in blocks of Ξ£(B0β), and hence
vertices in B0ββ{u0β} all have distance at least 5 from u0β. Since Ξ covers Ξ£ there is a unique vertex u0β²ββB0ββ{u0β} adjacent to e1β and this must satisfy dΞβ(u0β,u0β²β)=5. Further, since each vertex uβΞ4β(u0β)β©Ξ(u3β) lies in one of the 4 blocks of Ξ£(B0β)β©Ξ£(B3β), it follows that u is one of the eiβ, and so b3β=β£Ξ4β(u0β)β©Ξ(u3β)β£=4.
Suppose that Ξ is not bipartite, and let Ξ denote the standard double cover of Ξ and G=GΓZ2β, as in Lemma 2.6. Then, by Lemma 2.6,
Ξ is (G,3)-geodesic-transitive and (G,4)-distance-transitive and has c2β=4. Moreover
ΞNββ
Ξ£ where N=NΓZ2β. If LemmaΒ 5.9 holds for bipartite graphs, then Ξ is the standard double cover of Ξ£, and hence Ξ=Ξ£, which is a contradiction.
Thus it is sufficient to prove the lemma for bipartite graphs, and we therefore assume from now on that Ξ is bipartite.
Then, since Ξ is bipartite, a3β=β£Ξ3β(u0β)β©Ξ(u3β)β£=0,
so c3β=β£Ξ2β(u0β)β©Ξ(u3β)β£=16βa3ββb3β=12, β£Ξ3β(u0β)β£=c3β60Γb2ββ=60, and β£Ξ4β(u0β)β£=c4β60Γb3ββ=c4β240β with c4ββ₯c3β=12.
Since Ξ4β(u0β) is contained in the union of the blocks in Ξ£(B0β), and since Gu0ββ is transitive on Ξ£(B0β) and fixes
Ξ4β(u0β) setwise, it follows that Ξ4β(u0β) contains a constant number of vertices from each block of Ξ£(B0β). Thus β£Ξ4β(u0β)β£ is divisible by 16, and it follows that c4β=15 and β£Ξ4β(u0β)β£=16. Again, since Ξ is bipartite, a4β=β£Ξ4β(u0β)β©Ξ(e1β)β£=0
so b4β=β£Ξ5β(u0β)β©Ξ(e1β)β£=16βc4β=1. It follows that Gu0ββ is transitive on
Ξ5β(u0β) and that β£Ξ5β(u0β)β£=c5β16Γb4ββ=c5β16β with c5β=β£Ξ4β(u0β)β©Ξ(u0β²β)β£β₯c4β=15. Thus c5β=16, β£Ξ5β(u0β)β£=1, and Ξ
is a G-distance-transitive, bipartite and antipodal graph, with antipodal blocks of size 2 and with odd diameter 5. It follows from LemmaΒ 2.5 that Ξ is the standard double cover of Ξ£, as in part (1).
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5.6. Covers of complete bipartite graphs
Lemma 5.10**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Suppose that Ξ is a G-normal m-fold cover of Kr,rβ, where rβ₯3 and mβ₯2. Then Ξ is bipartite with girth 4 and diameter at least 4, and
one of the following holds:
Ξ* is a Hadamard graph of order r (so m=2); or*
Ξ* is a G-distance-transitive antipodal graph mKr,rβ which is the incidence graph of a resolvable divisible design
RGD(r,c2β,m), where r=mc2β, such that any two blocks from different parallel classes contain exactly c2β common points; Ξ has intersection array (r,rβ1,rβc2β,1;1,c2β,rβ1,r), and c2ββ₯2, mβ₯3; or*
Ξ* is not (G,4)-distance-transitive.*
There are examples of distance-transitive antipodal graphs mKr,rβ arising from resolvable divisible designs RGD(r,c2β,m) in case (2). Those with valency rβ€13 are classified and are listed in [7, p.223β225]. Moreover, by LemmaΒ 2.2, each RGD(r,c2β,m) with r=c2βm, such that any two blocks from different parallel classes contain exactly c2β common points, has an incidence graph which is distance-regular.
Proof.
Let Ξ£=Kr,rβ where rβ₯3, and let Nβ΄G be such that ΞNββ
Ξ£.
Since Ξ£ is bipartite it follows that Ξ is also bipartite, and hence contains no cycles of odd length, Then since
Ξ has girth 4 or 5, the girth of Ξ must be 4.
Set V(Ξ£)=B0ββͺB1β where
B0β={B01β,B02β,β¦,B0,rβ} and
B1β={B11β,B12β,β¦,B1,rβ}, and B0β, B1β are the two bipartite halves of Ξ£.
Let (u01β,u11β,u02β,u12β) be a 4-cycle of Ξ such that each uijββBijβ. Then u02ββΞ2β(u01β) and (B01β,B11β,B02β,B12β) is a 4-cycle of Ξ£.
Since Ξ is (G,3)-geodesic-transitive with diameter at least 3, u02β is adjacent to some vertex u13ββΞ3β(u01β). Let u13ββB13β. Since Ξ£=Kr,rβ, it follows that B13ββΞ£(B01β).
Let u01β²ββB01β be adjacent to u13β. Then dΞβ(u01β,u01β²β)β€4. As Ξ is bipartite
dΞβ(u01β,u01β²β) is even, and as Ξ is a cover of Ξ£, dΞβ(u01β,u01β²β)ξ =2. Hence
u01β²ββΞ4β(u01β), and in particular diam(Ξ)β₯4.
Since Ξ has girth 4, it follows that c2ββ₯2, and we have β£Ξ2β(u01β)β£=c2βrΓ(rβ1)β.
By LemmaΒ 3.2, it follows that GB01ββ is transitive on Ξ£2β(B01β)=B0ββ{B01β},
and by LemmaΒ 5.3, GB01ββ=NGu01ββ, and hence also Gu01ββ is transitive on
Ξ£2β(B01β). It follows that Ξ2β(u01β) contains equally many vertices from each block of Ξ£2β(B01β) and hence
that rβ1 divides β£Ξ2β(u01β)β£. Therefore c2β divides r. Since diam(Ξ)β₯4, we must have c2β<r, and hence
2β€c2ββ€r/2.
Suppose first that c2β=2rβ. Then by [7, Theorem 1.9.3] (since Ξ has diameter at least 4 and valency rβ₯3),
Ξ is a Hadamard graph of order r with intersection array
(r,rβ1,r/2,1;1,r/2,rβ1,r). Thus β£V(Ξ)β£=4r and so m=β£B01ββ£=2 and (1) holds.
Now suppose that 2β€c2β<2rβ, so c2ββ€r/3 since c2β divides r.
If Ξ is not (G,4)-distance-transitive then (3) holds, so
assume now that Ξ is (G,4)-distance-transitive.
Then since u01β²ββΞ4β(u01β)β©B01β, it follows that Ξ4β(u01β)βB01β.
Let uβΞ(u01β²β)β{u13β}. Then uβΞ3β(u01β)βͺΞ5β(u01β).
Further, (u13β,u01β²β,u) is a 2-geodesic, so β£Ξ(u13β)β©Ξ(u)β£=c2ββ₯2, say
{u01β²β,u03β}βΞ(u13β)β©Ξ(u).
Since u13ββΞ3β(u01β), it follows that u03ββΞ2β(u01β)βͺΞ4β(u01β). Moreover, since
Ξ4β(u01β)βB01β, we have u03ββ/Ξ4β(u01β), and so u03ββΞ2β(u01β). Hence
uβΞ3β(u01β), and it follows that Ξ(u01β²β)βΞ3β(u01β) so c4β=r and diam(Ξ)=4.
In particular Ξ is G-distance-transitive. Since Ξ is a cover of Ξ£, each vertex of B01ββ{u01β}
has even distance from u01β greater than 2, and therefore B01ββ{u01β}=Ξ4β(u01β) so Ξ is an antipodal graph.
Also Ξ2β(u01β)=βͺi=2rβB0iβ and Ξ3β(u01β)=(βͺi=1rβB1iβ)βΞ(u01β), so
β£Ξiβ(u01β)β£ is (rβ1)m,r(mβ1),mβ1 for i=2,3,4, respectively. In particular, since
β£Ξ2β(u01β)β£=c2βrβ(rβ1), it follows that r=c2βm so mβ₯3 since c2ββ€r/3. Also, counting the edges between Ξ3β(u01β) and
Ξ4β(u01β) we have r(mβ1)b3β=β£Ξ3β(u01β)β£b3β=β£Ξ4β(u01β)β£c4β=(mβ1)r and hence b3β=1.
Therefore c3β=rβb3β=rβ1 (since a3β=0),
and Ξ has intersection array
(r,rβ1,rβc2β,1;1,c2β,rβ1,r).
Moreover, by [18, Item 10 on p.316], a distance-regular graph with intersection array of this type
is an m-fold antipodal cover mKr,rβ where r=m.c2β.
Finally, we show that Ξ is the incidence graph of a resolvable divisible design with the properties specified in (2), and that each such design
determines a distance-regular m-fold antipodal cover of Kr,rβ.
Let V(Ξ)=V1ββͺV2β where V1β,V2β are the bipartite halves of V(Ξ). We construct the design
D=(V1β,P,B) with V1β being the set of points, P being the set of antipodal blocks of Ξ contained in V1β (that is, P=B0β), and B
being the set {Ξ(u)β£uβV2β} of neighbour-sets of vertices in V2β.
Then P consists of r antipodal blocks, each of size m, and is a partition of V1β.
Since Ξ is a bipartite graph of valency r that covers Ξ£, it follows that each block in B is adjacent to exactly one vertex of every antipodal block in P. Also, each pair of points from different antipodal blocks of P are at distance 2 in Ξ and therefore are contained in exactly c2β blocks of B.
Thus D is a divisible design GD(r,c2β,m,rm).
Moreover, the set B can be partitioned into r parts, namely B(i):={Ξ(u)β£uβB1iβ} for 1β€iβ€r.
Each of these parts has size m and distinct Ξ(u),Ξ(uβ²) in the same part must be disjoint since Ξ is a cover of Ξ£.
Thus βͺuβB1iββΞ(u) has size rm and hence is equal to V1β, that is, each B(i) is a partition of V1β β a parallel class of blocks of D. Thus D is a resolvable divisible design RGD(r,c2β,m). If Ξ(u)βB(i) and
Ξ(v)βB(j) with iξ =j, then u,v are at distance 2 in Ξ and hence β£Ξ(u)β©Ξ(v)β£=c2β. Thus D has all the properties specified in (2).
Conversely, by Lemma 2.2, if D is a resolvable divisible
design RGD(r,c2β,m), where r=c2β.m, such that any two blocks from different parallel classes contain exactly c2β common points, then
its incidence graph Inc(D) is an antipodal diameter 4 graph that is an m-fold cover mKr,rβ.
β
5.7. Covers of the Hoffman-Singleton graph
Recall that the automorphism group of the Hoffman-Singleton graph is PSU(3,5).Z2β. Its action on vertices has rank 3, with point stabiliser S7β, see [19, p.304].
Lemma 5.11**.**
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5.
Then Ξ is not a G-normal cover of the Hoffman-Singleton graph.
Proof.
Suppose that Ξ is a G-normal cover of the Hoffman-Singleton graph Ξ£, and let Nβ΄G
such that ΞNβ=Ξ£.
Since Ξ£ is a strongly regular graph with parameters (50,7,0,1),
it follows that Ξ has valency 7 and c2β=1. In particular, Ξ has girth 5.
Let (u0β,u1β,u2β,u3β) be a 3-geodesic of Ξ such that uiββBiββV(Ξ£). Then (B0β,B1β,B2β, B3β) is a 3-arc of Ξ£ and β£Ξ£2β(B0β)β£=42.
Since Ξ£ has c2β=1, B3β lies in Ξ£2β(B0β).
By LemmaΒ 3.2, Ξ£ is (G/N,2)-geodesic-transitive,
so GB0ββ/N is 2-transitive on Ξ£(B0β). By [11, p34], the only proper subgroup of
Aut(Ξ£) that is 2-geodesic-transitive is PSU(3,5), and so
G/N=PSU(3,5).Z2β or PSU(3,5) and
GB0ββ/N=S7β or A7β, respectively, acting faithfully on Ξ£(B0β).
For both cases, we check using MAGMA [5] that GB0βB2ββ/N is transitive on
Ξ£2β(B0β)β©Ξ£(B2β), a set of size 6.
By Lemma 5.3(4), GB0ββ=NGu0ββ and GB0βB2ββ=NGu0βu2ββ=NGu0βB2ββ.
Therefore, Gu0βu2ββ is transitive on Ξ£2β(B0β)β©Ξ£(B2β).
Let CβΞ£2β(B0β)β©Ξ£(B2β) with Cξ =B3β, and let Ξ(u2β)β©C={c}.
Then some element gβGu0βu2ββ maps B3β to C, and
so u3gβ=c. Thus cβΞ3β(u0β)β©Ξ(u2β).
Since β£Ξ£2β(B0β)β©Ξ£(B2β)β£=6, it follows that β£Ξ3β(u0β)β©Ξ(u2β)β£=6, that is, Ξ has b2β=6, and so a2β=0,
contradicting the fact that Ξ has girth 5. β
We are ready to prove the third theorem.
Proof of Theorem 1.3.
Let Ξ be a connected (G,3)-geodesic-transitive graph of girth 4 or 5, and let
Nβ΄G with at least 3 orbits on V(Ξ), and such that ΞNβ has diameter at most 2.
It follows from Theorem 1.1 that
Ξ is a cover of ΞNβ, and ΞNβ is either a complete graph or
a strongly regular graph of girth 4 or 5.
If ΞNβ is a complete graph, then by Lemma 5.1,
Ξ is isomorphic to Kk+1,k+1ββ(k+1)K2β, for some kβ₯3, or to [HoS]2β, as in Table 1.
Suppose that ΞNβ has diameter 2 and girth 4 or 5. Then by Theorem 1.2,
ΞNβ is one of the following graphs: C5β, Kr,rβ with rβ₯2, the Higman-Sims graph HiS, the Gewirtz graph, the M22β-graph, the folded 5-cube β‘5β,
the Petersen graph, and the Hoffman-Singleton graph. Further, by Lemmas 5.2(1) and 5.11,
ΞNβ is not C5β or the Hoffman-Singleton graph. All the other possibilities yield examples, and
by Lemmas 5.2 (2)-(3), 5.4, 5.7, 5.9 and 5.10, either Ξ
is one of the graphs in TableΒ 1, or Ξ is not (G,4)-distance-transitive, with ΞNβ as in TableΒ 2.
β