• Ingen resultater fundet

Afhandling

N/A
N/A
Info
Hent
Protected

Academic year: 2022

Del "Afhandling"

Copied!
93
0
0

Indlæser.... (se fuldtekst nu)

Hele teksten

(1)

Cohomology of the Free Loop Spae

of a Projetive Spae

Ph.d. Thesis

Mia Hauge Dollerup

Thesis advisor: Marel Bökstedt

July 1, 2009

Department of Mathematis

Aarhus University

(2)
(3)

1 Projetive spae and geodesis 8

1.1 The quaternions . . . 8

1.2 Spaesof geodesis . . . 8

1.3 Fibrationsinvolvingspaes of geodesis . . . 12

1.4 Homotopy orbits of spaes of geodesis . . . 14

2 Cohomology of spaes of geodesis in

HP r

17 2.1 The parametrizedgeodesis . . . 17

2.2 The unparametrized geodesis . . . 21

2.3 Equivariantohomologyof spaes of geodesis . . . 30

3

K

-theory of spaes of geodesis in

CP r

35 3.1 The unparametrized geodesis . . . 35

3.2 Equivariant

K

-theory of spaes of geodesis . . . . . . . . . . 38

4 The free loop spae and Morse theory 47 4.1 The negative bundle . . . 49

4.2 The power map . . . 51

4.3 The Morse theory spetral sequene . . . 52

5

S 1

-equivariant ohomology of

LHP r

58 5.1 The Morse spetral sequenes . . . 58

5.2 The MainTheorem . . . 65

6

S 1

-equivariant

K

-theory of

LCP r

75 6.1 The rst dierential. . . 76

6.2 The MainTheorem for

r > 1

. . . . . . . . . . . . . . . . . . . 79

6.3 The MainTheorem for

r = 1

. . . . . . . . . . . . . . . . . . . 84

Notation 91

Referenes 92

(4)
(5)

Introdution

The free loopspae

LX

of a spae

X

is the spae of ontinuous maps from

S 1

to

X

. The irle group

S 1

ats on

LX

by rotation, and we study the

spaeofhomotopy orbits,

LX hS 1 = ES 1 × S 1 LX

,sometimesalled theBorel

onstrution. The main method for understanding this spae will be Morse

theory on the energy funtional, whih to a losed urve assoiates its en-

ergy. This version of Morse theory has been studied by W. Klingenberg in

[Klilngenberg1℄. Asonewouldexpet,theritialpointsofthisfuntionalare

the losed geodesis of

X

, soknowing those willbe animportantingredient

inunderstanding

LX hS 1

viaMorse theory.

Inthispaperwestudy

LX hS 1

forapartiularspae,namelytheprojetive

spae

X = FP r

, where

F = C

or

F = H

. The goal is to determine the

ohomology of

LHP r hS 1

and the omplex

K

-theory of

LCP r hS 1

. This is

alled

S 1

-equivariantohomology(or

K

-theory)of

LFP r

. In general,weget

a map

ES 1 × S 1 LX −→ BS 1

byprojetionontherstfator. Foraohomologytheory

h

,wethereforeget

a map

h (BS 1 ) −→ h (LX hS 1 )

, so

h (LX hS 1 )

beomes a

h (BS 1 )

-module.

The methods of Morse theory require the use of Thom isomorphism, whih

destroystheprodutstruture,soweannothopetoalulate

h (LFP r hS 1 )

as

a ring. But the

h (BS 1 )

-module struture is preserved by the Morse theory

mahinery, so the aim is to alulate

h (LFP r hS 1 )

as an

h (BS 1 )

-module,

where

h

iseither singularohomology

H

or omplex

K

-theory

K

.

We will now outline our main results. For

X = HP r

, we study the

ohomology with

F p

-oeients of

LX hS 1

, where

F p = Z/pZ

, and obtain a

omplete desription as an

H (BS 1 ; F p ) = F p [u]

-module:

Theorem 1. As a graded

H (BS 1 ; F p ) = F p [u]

-module,

H (LHP r hS 1 ; F p )

is

isomorphi to

F p [u] ⊕ M

2k ∈IF

F p [u]f 2k ⊕ M

2k ∈IF

F p [u]f 2k − 1 ⊕ M

2k ∈IT

(F p [u]/ h u i ) t 2k − 1 .

Here the lower index denotes the degree of the generator, and the index sets

IF

and

IT

are knowndisjointsubsets of

{ (4r + 2)i + 4j | 0 ≤ j ≤ r, i ≥ 0 }

.

In partiular, there is at most one generator in eah degree.

For

X = CP r

, we study the omplex

K

-theory of

LCP r hS 1

, and obtain

Theorem 2. As a

K (BS 1 ) = Z[[t]]

-module,

K 0 (LCP r hS 1 ) = K 0 (BS 1 ) = Z[[t]] .

As an abelian group,

K 1 (LCP r hS 1 )

is torsion-free.

(6)

This isone of the rst alulationsof

K (LM hS 1 )

for anon-trivial mani- fold

M

. Theresultisquitesurprisingwhenomparedto

H (LCP r hS 1 )

,whih

has a lotof torsion aording to[Bökstedt-Ottosen ℄.

Unfortunately, we have not been able to determine

K 1 (LCP r hS 1 )

as a

K (BS 1 )

-module. As a partial resultin this diretion, we have

Theorem 3. There is a spetralsequene of

K (BS 1 ) = Z[[t]]

-modules on-

verging strongly to

K (LCP r hS 1 )

, whih has

E 1

page,

E 1 0,j =

Z[[t]] ⊗ Z Z[h]/ h h r i ,

j even;

0,

j odd.

E 1 n,j =

Z[[t]] (n)R(S 1 ) Z[x, y ]/ h Q r , Q r+1 i ,

j odd;

0,

j even.

The rst dierential

d 1

is given by

d 1 (p(t) ⊗ h j ) = p(t) ⊗ (x j − y j )

, where

p(t) ∈ Z[[t]]

.

Theorem2statesthat

K 0 (LCP r hS 1 )

is(almost)trivial,while

K 1 (LCP r hS 1 )

is free abelian. This is rather similar to the well-known ase of

K 0 (BG)

as

the ompletion of the representation ring

R(G)

for a ompat Lie group

G

,

while

K 1 (BG) = 0

. This is a lassial result of M. Atiyah. One an also

ompare to e.g. [Freed-Hopkins-Teleman℄, who nd

K τ (LBG)

as the om-

pletion of ertain representations of the loopgroup

LG

, although it should

be remarked that they onsider

K

-theory twisted by a ohomologylass

τ

,

and not

S 1

-equivariant

K

-theory as we do. Still,this promptsthe following

Conjeture. The exists a representation theory type group, suh that

K 1 (LCP r hS 1 )

isa ompletion of this group.

The outline of this paper is as follows: The paper onsists of two main

parts,eahdividedinthreesetions. Therst setionofeahparttreatsthe

general theory needed and investigates the relevant spaes and strutures,

while the next two setions are more omputational and deal, respetively,

with the ohomologyfor

F = H

, and the

K

-theory for

F = C

.

Setion 1 investigates

FP r

and its geodesis, obtaining some useful -

brations. We onsider both the spae of parametrized and unparametrized

geodesis;the latter beingthe quotient of the former under the ation of

S 1

by rotation.

Setion 2 alulates the ohomology of the above spaes using Serre's

spetral sequene for the brations found in setion 1. We then turn to

S 1

-equivariant ohomology of the spae of parametrized geodesis, via two brationsandthe non-equivariantohomologyresultsfromthepreviousse-

(7)

Setion 3 obtains similar results for

K

-theory. We use the Atiyah-

Hirzebruh spetral sequene along with the known ohomology results for

CP r

to determine the

K

-theory of the spae of unparametrized geodesis.

The

S 1

-equivariant

K

-theory is determined using the same brations as for

ohomology,butthemethodisdierent,employingtheresultofAtiyahabout

K

-theory of lassifying spaes.

Setion 4 studies of the free loop spae,

LFP r hS 1

. First we explain the

workings of Morse theory in this setting, then we apply this to

LFP r

and

LFP r hS 1

toget the so-alledMorse spetral sequene.

Setion 5 is dediated to proving Theorem 1. The method is losely

baseduponasimilaralulationbyM.BökstedtandI.Ottosenintheirpaper

StringCohomologyGroupsofComplexProjetiveSpaes,[Bökstedt-Ottosen℄.

We extrat a lotof informationabout the Morse spetral sequene, its size,

itsdierentials,andtherelationbetweentheequivariantandnon-equivariant

ase. All this information is brought together to prove the Main Theorem

for ohomology, Theorem 1 above. But even then, it is neessary to turn

to other soures of information to omplete the proof. One is loalization,

the other is omparison with the Serre spetral sequene alsoonverging to

H (LHP r hS 1 )

.

Setion6isdediatedtoprovingTheorem2. Themethodsherearequite

dierent, relying on the fat that the Morse spetral sequene in Theorem

3 has a rather speial onguration, whih implies that all its non-trivial

dierentials start from the zeroth olumn. A very important point is the

alulation of the rst dierential

d 1

. The entral idea is then to twist the

rotationationof

S 1

withapositiveinteger,whihgivesnew Morse spetral

sequenes related to the standard one. This gives enough information to

prove Theorem

2

.

For the reader's onveniene, we have assembled a table of notation at

the end of this doument.

Aknowledgements. Finally,it is apleasure to thank my advisor, Marel

Bökstedt, forhishelp throughinnumerable fruitfuldisussions,whihadded

many new insights and ideas to this projet. Also, I would like to thank

Jørgen Tornehave for his time and valuable input when standing in as my

advisor for one year.

(8)

1 Projetive spae and geodesis

1.1 The quaternions

I start by introduing the quaternions,

H

, as an assoiative algebra of real

dimension

4

,generated by

1, i, j, k

with the followingmultipliation rules:

i 2 = j 2 = k 2 = − 1, ij = − ji = k, jk = − kj = i, ki = − ik = j.

Itshouldbestressed,eventhoughitisobviousfromthe aboverelations,that

H

is not ommutative. If one wants to be onrete, one an realize

H

as a

subalgebra of

M 2 (C)

generated over

R

by (inthe matrix entries,

i = √

− 1

):

i =

i 0 0 − i

, j =

0 1

− 1 0

, k =

0 i i 0

.

Itisstraightforward tohekthe abovemultipliationrules. Similartoom-

plexonjugation, there is an

R

-linear map, alsoalled onjugation,

H −→ H

z = x 0 + x 1 i + x 2 j + x 3 k 7→ z = x 0 − x 1 i − x 2 j − x 3 k,

satisfying the usual rule

(zw) = w z

. In the matrix desription, this is preisely the usual

-operation of taking the onjugate transpose. This an

beusedtodeneaninnerprodut

h z, w i H = w z

,whoserealpartistheusual

inner produt on

R 4

. Noting that

h z, z i H ∈ R

we an then dene a norm

| z | = p

h z, z i H

. This satises

| zw | = | z | | w |

and

| z | = | z |

. The unit sphere

in

H

is usually denoted

Sp(1) = { z ∈ H | | z | = 1 }

, and this is anonially

identied with

S 3

. Finally we note that if

z 6 = 0

then

z

is invertible this

is most easily seen by using the matrix desription, whih gives an expliit

inverse, and heking thatthis belongs to

H

.

Weantakethediretprodutof

H

withitselftoform

H r

. Theoperations

h· , ·i H

and

|·|

from

H

areextendedto

H r

intheusualway: For

z = (z 1 , . . . , z r )

and

w = (w 1 , . . . , w r )

, we set

h z, w i H =

X r j=1

h z j , w j i H , | z | = q

| z 1 | 2 + . . . + | z r | 2 .

1.2 Spaes of geodesis

Let

F

denoteeither

C

or

H

. Toeasethenotationwedenotetheunitspherein

F

by

S(F)

. Wedenetheprojetivespae

FP r

astheset ofall

1

-dimensional

(9)

F

-subspaes

zF

of

F r+1

, for

z ∈ F r+1

. We dene the projetion map

π : F r+1 \ { 0 } −→ FP r

(1)

z = (z 0 , . . . , z r ) 7→ [z 0 , . . . , z r ] = zF,

so

π(z) = zF

is the subspae spanned by

z

. Note that for

F = H

it is im-

portantthatwespeify whihside wemultiplyon; Ihavehosen tomultiply

from the right. We give

FP r

the quotient topology from

π

. To show that

FP r

is a smooth manifold of real dimension

2r

(resp.

4r

) for

F = C

(resp.

F = H

), we display the expliit harts

h j : U j = { [z 0 , . . . , z r ] ∈ FP r | z j 6 = 0 } −→ F r , h j ([z 0 , . . . , z r ]) = (z 0 z j 1 , . . . , z \ j z j 1 , . . . , z r z j 1 ),

where the hat denotes omission;the harts have inverses

h j 1 (w 1 , . . . , w r ) = [w 1 , . . . , 1, . . . , w r ],

with the

1

atthe

j

thplae.

Example 1.1. We willshow

HP 1

is dieomorphi to

S 4

. This an be seen

by stereographi projetion. Think of

S 4 ⊆ R 5 = R × H

with north pole

p + = (1, 0)

and south pole

p = ( − 1, 0)

. Stereographi projetion are the maps

ψ ± : S 4 \ { p ± } −→ H,

whih takes a point

(t, z )

in

S 4

to the intersetion of the line through

(t, z)

and

p ±

with

0 × H

. This iseasily omputed:

ψ + (t, z) = z

1 − t , ψ (t, z) = z 1 + t ,

and arelearly smoothmaps. Now wewanttoompose

ψ +

and

ψ

withthe

h j 1

toget two maps to

HP 1

. When we dothis, wewould like the two maps

toagree when

t ∈ ] − 1, 1[

. To ahieve this, wereplae

ψ +

with itsonjugate

ψ + (t, z) = 1 z t

. Doing this, we get maps,

S 4 \ { p + } ψ

−→ + H h

− 1

−→ 0 HP 1 , S 4 \ { p } −→ ψ H h

− 1

−→ 1 HP 1 ,

given by

(t, z) 7→

1, z

1 + t

, (t, z) 7→

z 1 − t , 1

.

By multiplying the rst expression from the right by

z

1 − t

and using that

1 = | (t, z) | = t 2 + | z | 2 = t 2 + z z

, we see that these two maps agree when

t ∈ ] − 1, 1[

, so they ombine toa dieomorphism

S 4 −→ HP 1

.

(10)

We an modify the projetion map

π

in (1)toa map

π : S(F r+1 ) −→ FP r

where

S(F r+1 ) ⊆ F r+1

is the unit sphere. This an be used to desribe the

tangent bundle of

FP r

. Speially for

z ∈ S(F r+1 )

there is an

F

-linear

isometry,

t z : (zF) ⊆ T z S(F r+1 ) −→ π T π(z) FP r ,

where

(zF) = { w ∈ F r+1 | h w, z i F = 0 }

. This map satises

t (wλ) = t z (w)

for

λ ∈ S(F).

(2)

The above properties of

FP r

are rather elementary, and the reader an

see e.g. [Madsen-Tornehave℄ Chapter 14for proofs of the results in the ase

of

CP r

.

Consider the Riemannian metri on

FP r

given by the real part of the

inner produt on

F r+1

. This is the standard metri on

FP r

, and we will

use a metri

g

whih is a salar multiple of this metri. Take the unique

onnetion on

T (FP r )

ompatible with this metri, alled the Levi-Civita onnetion. We now dene

G(r) = G(FP r )

as the spae of parametrized, simple, losed geodesis

f : [0, 1] −→ FP r

with respet to this onnetion.

The salar determining

g

is speied by requiring that suh a geodesi has

length 1 with respet to

g

. Note that every geodesi in

FP r

is losed: The

group of

F

-orthogonal matries (

U (r + 1)

or

Sp(r + 1)

, respetively) ats transitively on

HP r

, so it is onlyneessary to hek it for one geodesi, e.g.

on

FP 1 ⊆ FP r

,andsine

CP 1 ∼ = S 2

and

HP 1 ∼ = S 4

, allgeodesis on

FP 1

are

known to be losed.

We also onsider the set of

n

times iterated geodesis

G n (r)

for every

integer

n ≥ 1

, whose elements

γ : [0, 1] −→ FP r

are given by

γ(t) = f(nt)

forsome

f ∈ G(r)

, wherewe makethe obviousidentiationof the intervals

[j − 1, j]

with

[0, 1]

for

j = 2, . . . , n

. There isanationon

G n (r)

by

S 1

given

by rotation;expliitly,

S 1 × G n (r) −→ G n (r) (e 2πiθ , f (t)) 7→ f (t − θ).

Wean twistthe rotationationon

G(r)

byaninteger

n ≥ 1

,and wedenote

the resulting

S 1

-spae

G(r) (n)

:

S 1 × G(r) (n) −→ G(r) (n)

(3)

(e 2πiθ , f(t)) 7→ f (t − nθ).

(11)

This ation is the rotation ation preomposed with the

n

th power map

P n : S 1 −→ S 1

,

P n (z) = z n

in omplex notation. Then

G n (r)

and

G(r) (n)

are isomorphias

S 1

-spaesvia theobviousmap

G(r) (n) −→ G n (r)

given by

f (t) 7→ f(nt)

, so from now on, we will hiey use

G(r) (n)

instead of

G n (r)

.

We also onsider the quotient

∆(r) = S 1 \ G(r)

under the rotation ation,

whih is the spae of oriented, unparametrized, simple, losed geodesis on

FP r

.

We now want to get a more onrete desription of

G(r)

and

∆(r)

, fol-

lowing [Bökstedt-Ottosen ℄, Ÿ2. Let

V 2 = V 2 (F r+1 )

be the Stiefel manifold of

F

-orthonormal2-frames in

F r+1

,so

V 2 =

(v, w) ∈ F r+1 × F r+1 | k v k = k w k = 1, h v, w i F = 0 ,

and let

P V 2

be the quotient manifold by the right diagonal

S(F)

ation,

(v, w) ∗ z = (vz, wz)

. On

V 2

we have a left ation of

S 1

by rotation by an

angle

θ

: For

θ ∈ R

, the ation is

w v

7→ R(θ) w v

, where

R(θ) =

cos(θ) − sin(θ) sin(θ) cos(θ)

For eah

n ∈ N

, we an dene an ation of

S 1

on

P V 2

, and we denote the

resulting

S 1

-spae by

P V 2 (n)

:

S 1 × P V 2 (n) −→ P V 2 (n) ; e 2πiθ ∗ [x, y] = [R(nπθ)(x, y)].

This gives awell-dened

S 1

-ationon

P V 2

, beause we multiplythe matrix

R

onthe left,while

P V 2 = V 2 /

diag

S(F)

, wherewemultiplyontheright. We

an now make an

S 1

-equivariant dieomorphism

ϕ 1 : P V 2 (n) −→ G(r) (n)

(4)

[x, y] 7→ π ◦ c(x, y)

where

π : S(F r+1 ) −→ FP r

is the projetion, and

c(x, y )

isthe simple losed

geodesi startingat

x

in diretion

y

; expliitly,

c(x, y)(t) = cos(πt)x + sin(πt)y,

for

t ∈ [0, 1].

This iswell-dened,and abijetionbeauseeverygeodesion

FP r

islosed.

Clearly,

ϕ 1

isa dieomorphism,and it isstraightforward to hek that it is

S 1

-equivariant, using the trigonometriformulas.

Another very useful model for

G(r)

is

S(τ ) = S(T (HP r ))

, the sphere

bundle of the tangent bundle

τ

of

FP r

. There isa dieomorphism

ψ : P V 2 −→ S(τ )

[x, y] 7→ t x (y) ∈ T π(x) FP r

(12)

This is well-dened beause of (2), and we an give an expliit inverse:

Given

y ∈ T π(x) FP r

,

ψ 1 (y) = [x, t x 1 (y)]

. Thus we an give

S(T (FP r ))

a rotation ation of

S 1

, namely the ation that makes this dieomorphism

S 1

-equivariant. Combining this with (4), we have an

S 1

-equivariant dieo- morphism

ψ 1 ◦ ϕ 1 : S(τ ) −→ G(r).

(5)

The last desription only works for

CP r

. Going bak to

P V 2 (C r+1 )

, we

rst hange oordinates as follows

ϕ 2 : P V 2 (C r+1 ) −→ g P V 2 (C r+1 ), [x, v] 7→

x + iv

√ 2 , x − iv

√ 2

.

Here

P V g 2

is

P V 2

equipped the

S 1

-ationindued fromthis hangeofoordi-

nates. Itis easilyomputed that the ation of

θ ∈ [0, 1]

is

θ ∗ [a, b] = [za, zb]

where

z = e πiθ ∈ S 1

.

We are interested in

∆(CP r )

, i.e. we divide out the rotation ation.

Therefore we now onsider the following spae: Let

γ 2

be the standard 2-

dimensional bundle over the Grassmannian Gr

2 (C r+1 )

of

2

-planes in

C r+1

,

and let

p : P(γ 2 ) −→

Gr

2 (C r+1 )

be the assoiated projetive bundle. Then

P(γ 2 ) = { V 1 ⊆ V 2 ⊆ C r+1 | dim C (V j ) = j }

. Wean make adieomorphism,

ϕ 3 : S 1 \ P V g 2 (C r+1 ) −→ P(γ 2 ), [a, b] 7→

span

C { a } ⊆

span

C { a, b } .

This is well-dened, but only for

F = C

. In onlusion we get a omposite

S 1

-equivariant dieomorphism

ϕ : ∆(CP r ) ϕ

− 1

1 // S 1 \ P V 2 (C r+1 ) ϕ 2 // S 1 \ P V g 2 (C r+1 ) ϕ 3 // P(γ 2 ).

(6)

1.3 Fibrations involving spaes of geodesis

We are going to ompute the ohomology and

K

-theory of the spaes

G(r)

and

∆(r)

. In ohomology, our most important tool will be Serre's spe-

tralsequene. I will write down the most important part; for the omplete

formulationand proof, see e.g [Hather2 ℄ Thm 1.14 pp.

Theorem 1.2 (Serre's Spetral Sequene). Let

F −→ X −→ B

be a -

bration, with

B

a path-onneted CW omplex, and

π 1 (B )

ating trivially

on

H (F ; G)

. Then there is a spetral sequene

{ E r p,q , d r }

onverging to

H (X; G)

with

E 2 p,q ∼ = H p (B; H q (F ; G)).

(13)

If

G = R

is a ring, then there is a produt

E r p,q × E r s,t −→ E r p+s,r+t

, and the

dierentials are derivations, i.e.

d(xy) = (dx)y + ( − 1) p+q x(dy)

. For

r = 2

the produt is

( − 1) qs

times the standard up produt. The produt struture

on

E

oinide with that indued by the up produt on

H (X; R)

.

Forthe denitionofabration,and theuseful fatthatberbundlesare

brations, see [Hather1 ℄, p. 375 and Prop. 4.48.

Thereisasimilarresultforabrationin

K

-theory,butIamhiey going

tousetheimportantspeialasewherethebrationis

∗ −→ X −→ X

,alled

the Atiyah-Hirzebruhspetralsequene, see [Atiyah-Hirzebruh ℄:

Theorem1.3(Atiyah-HirzebruhSpetralSequene). Let

X

be aniteCW

omplex. Then there is a spetral sequene

{ E r p,q , d r }

onverging to

K (X)

with

E 2 p,q ∼ = H p (X; K q ( ∗ )).

We will need a way tobuild brations fromother brations, and this is

provided by the following theorem.

Theorem1.4. Let

F −→ X −→ B

bea bration,andassumethatthegroup

G

ats freely on

X

. Then,

(i)

Ifthe

G

-ationpreservesthebres,

F/G −→ X/G −→ B

isabration.

(ii)

If

G

ats freely on

B

, then

F −→ X/G −→ B/G

is a bration.

Proof. This follows from the fat that

G −→ X −→ X/G

is a bration,

whihis aonsequene of the slie theorem, [Bredon ℄ Thm. 5.4.

To applythe spetral sequenes, wemust knowsome brationsinvolving

the spaes of geodesis. Firstby denition we have the bration

S 1 −→ G(r) −→ ∆(r).

(7)

For the appliation of Serre's spetral sequene, note that the base is 1-

onneted. This an be seen from the long exat sequene of homotopy

groups, usingthat

G(r) ∼ = S(τ )

is 1-onneted.

Then there is the map

P V 2 (F r+1 ) −→

Gr

2 (F r+1 )

indued by the map

V 2 (F r+1 ) −→

Gr

2 (F r+1 )

,

(x, y) 7→ { xλ + yµ | λ, µ ∈ F }

,

whih is well-dened on

P V 2

. The bre is

P V 2 (F 2 )

. Bythe dieomorphism (4), this means we havethe bration

G(1) −→ G(r) −→

Gr

2 (F r+1 ).

(14)

Sinethe left

S

ationonthe totalspae isfreeand preservesthe bres,we

an divide by it in the total spae and bre, by Theorem 1.4

(i)

obtaining

the bration

∆(1) −→ ∆(r) −→

Gr

2 (F r+1 ).

(8)

Againwe note that the base is 1-onneted.

1.4 Homotopy orbits of spaes of geodesis

In this setion we are going to study the so-alled homotopy orbits of the

spaes of geodesis we have studied so far. For this denition we need the

following onepts: Let

G

be a group, and suppose we have a ontratible

spae with a free

G

ation. It turns out that all suh spaes are homotopy

equivalent, so we an dene

EG

to be any suh spae. We an then dene

BG = EG/G

to bethe lassifying spae of

G

. Notethat this isa working

denition; atually

BG

is dened for a ategory, but this is all I willneed.

For

G = S 1

we nd

ES 1 ≃ S

, sine this is ontratible. Thus we get

BS 1 ≃ S /S 1 = CP

.

Denition1.5. Let

X

beatopologialspaewith a(left)ationof

S 1

. We

denethe spae of homotopy orbits of

X

by

X hS 1 = ES 1 × S 1 X = ES 1 × X/

(e, tx) ∼ (et, x), t ∈ S 1 .

Projetion onthe rst fator givesamap

X hS 1 −→ BS 1

, and fora oho-

mologytheory

h

(weonsiderohomologyand

K

-theory),wegetanindued

map

h (BS 1 ) −→ h (X hS 1 ).

As explained in the introdution, this gives

h (X hS 1 )

the struture of an

h (BS 1 )

-module.

Reall that

G(r)

is the spae of simple parametrized geodesis with the free left ation of

S 1

given by rotation. The spae of

n

-times iterated

geodesis,

G n (r)

, we have identied as an

S 1

-spae with

G(r) (n)

, whih is

G(r)

with therotationationtwistedby the

n

thpowermap

P n : S 1 −→ S 1

,

see (3).

(15)

horizontal maps are brations with 1-onneted base spaes:

G(r)

BC n // ES 1 × S 1 G(r) (n) //

∆(r)

BS 1 B P n // BS 1

Here

C n ⊆ S 1

denotes the group of

n

th roots of unity.

Proof. To see that the vertial map is a bration, use the produt bundle

G(r) (n) −→ ES 1 × G(r) (n) −→

pr

1 ES 1

, and divide out by the free ation of

S 1

onboth total spae and base,aording toTheorem 1.4

(ii)

. Usingthe long

exat homotopy sequene for the bration

S 1 −→ ES 1 −→ BS 1

shows that

the base

BS 1

is 1-onneted.

The horizontal bration is built up in steps: We start with the produt

bre bundle,

ES 1 −→ ES 1 × G(r) (n) −→

pr

2 G(r) (n) .

Clearly,

C n ⊆ S 1

ats freely on

ES 1 × G(r) (n)

, preserving the bres. So by

Theorem 1.4

(i)

, dividing out by

C n

in the total spae and bre yields the

bration:

BC n −→ ES 1 × C n G(r) (n) −→ G(r) (n) .

Weget

ES 1 /C n = BC n

beause

ES 1

is a ontratiblespae uponwhih

C n

ats freely, and so

ES 1 ≃ EC n

. Now onsider the quotient group

S 1 /C n

,

whih isisomorphi to

S 1

by the

n

'th powermap. Sine

C n

ats triviallyon

G(r) (n)

, we have an ation of

S 1 /C n

on

G(r) (n)

. By denition, this ats on

G(r) (n)

exatly as

S 1

ats on

G(r)

, so

(S 1 /C n ) \ G(r) (n) ∼ = S 1 \ G(r)

. By

Theorem1.4

(ii)

,dividingoutbythis freeationinthe totaland basespaes

gives usthe bration

BC n −→ ES 1 × C n G(r) (n)

/(S 1 /C n ) −→ S 1 \ G(r).

Now

ES 1 × C n G(r) (n)

/(S 1 /C n ) ∼ = ES 1 × S 1 G(r) (n)

,bythe denitionofthe

ations, sowe get the desired bration. As noted inSetion 1.3, the base is

1

-onneted.

To get the ommutative square, note that we have the homotopy equiv-

alene pr

2 : ES 1 × G(r) −→ G(r)

, sine

ES 1

is ontratible. Sine this is an

S 1

map and

S 1

ats freely on both spaes, we an use [tomDiek℄

Prop. 2.7 to onlude that

ES 1 × S 1 G(r) −→ S 1 \ G(r) = ∆(r)

is also a

(16)

homotopy equivalene. The upper vertial map in the square is dened as

pr

2 : ES 1 × S 1 G(r) −→ ∆(r)

usingthis homotopyequivalene. Fortheiden- tiation

S 1 /C n

with

S 1

above,we usedthe

n

thpowermap

P n : S 1 −→ S 1

,

so for the diagram to ommutate, the lower horizontal map

BS 1 −→ BS 1

must also be the one indued by

P n

. Note: This is well-dened on

BS 1

beause

S 1

is ommutative.

Remark 1.7. If we let

n = 1

, the vertial bration beomes

G(r) −→

ES 1 × S 1 G(r) −→ BS 1

. Asnotedintheproof,

ES 1 × S 1 G(r) −→ S 1 \ G(r)

is

ahomotopyequivalene. So, uptohomotopy,wehaveinpratieabration

G(r) −→ ∆(r) −→ BS 1 .

(9)

(17)

2 Cohomology of spaes of geodesis in

HP r

2.1 The parametrized geodesis

Inthissetionwendthe ohomologyofthespaeofparametrizedgeodesis

on

HP r

,

G(r) = G(HP r )

, followed by some Lemmasneessary to determine

thespaeoforiented,unparametrizedgeodesis,

∆(r) = ∆(HP r ) = S 1 \ G(r)

.

Theorem 2.1. As a graded ring,

H (G(HP r ); Z) ∼ = Z[y, τ ]/

(r + 1)y r , y r+1 , τ 2 ,

where

y ∈ H 4 (G(HP r ); Z)

and

τ ∈ H 4r+3 (G(HP r ); Z)

.

Let

p

be a prime number. Then

H (G(HP r ); F p ) ∼ =

F p [y, σ]/ h y r+1 = 0, σ 2 = 0 i , p | r + 1;

F p [y, τ ]/ h y r = 0, τ 2 = 0 i , p ∤ r + 1.

where

y ∈ H 4 (G(HP r ); F p )

,

σ ∈ H 4r 1 (G(HP r ); F p )

,

τ ∈ H 4r+3 (G(HP r ); F p )

.

Proof. We use the dieomorphismfrom(5),

G(r) ∼ = S(τ )

, where

S(τ)

isthe

sphere bundleof the tangentbundle,

S 4r 1 −→ S(τ ) −→ HP r .

Sine

HP r

is 1-onneted, we an use Serre'sspetral sequene,

H p (HP r ; H q (S 4r 1 )) ⇒ H p+q (S(τ ))

(10)

(here the oeients will be

Z

atrst, and

F p

toprove the lastpart) whih

has the following

E 2

page:

4r − 1 σ yσ y 2 σ y r σ

0 1 y y 2 y r

0 4 8 . . . 4r

We an see for dimensional reasons that there an only be one non-trivial

dierential,namely

d 4r (σ)

. Forthespherebundle,itisageneraltheoremthat

this dierentialismultipliation by the Euler harateristi of the manifold,

here

HP r

, so

d 4r (σ) = (r + 1)y r

. This is proved in [Milnor-Stashe℄, Cor.

(18)

11.12and Thm. 12.2. This is an injetivemap

Z −→ Z

, sowhen passing to

the

E 4r+1

page, the result is

4r − 1 0 yσ y · yσ y r 2 · yσ y r 1 · yσ

0 1 y y 2 y r 1 y r

0 4 8 . . . 4r − 4 4r

Asmentioned,therearenoothernon-trivialdierentials,sothisis

E

. Also,

therearenoextensionproblemssinethereisatmostonenon-trivialgroupon

eahdiagonal

p + q = n

,so

denesalassin

H 4r+3 (S(τ); Z)

whihweall

τ

. We an then read o the lasses

y ∈ H 4 (S(τ ); Z)

and

τ ∈ H 4r+3 (S(τ ); Z)

with the relations

y r+1 = 0

,

(r + 1)y r = 0

,and

τ 2 = 0

.

Toprovetheresultwith

F p

oeients,weusethesamespetralsequene

(10), now with

F p

-oeients. In ase

p | r + 1

,

d 2 (σ) = 0

, so there are no

non-trivial dierentials, and

E = E 2

. As above, there are no extension

problems, and

σ

denes an element in

H 4r 1 (S(τ); F p )

. So we an read o

thedesiredresult. Inase

p ∤ r + 1

,

r + 1

isaunit in

F p

,so

d 2 : F p σ −→ F p y r

is an isomorphism. So when passing to the

E 4r+1

page, these two groups

disappear. The result follows.

Now we an deal with the smallest ase,

HP 1

, whih we have shown in

Example1.1isdieomorphito

S 4

. This isgoingtobeuseful, sine wehave

the bration

∆(HP 1 ) −→ ∆(HP r ) −→

Gr

2 (H r+1 )

from(8).

Lemma 2.2.

H (∆(HP 1 ); Z) ∼ = Z[x, t]/

2t − x 2 , t 2 ,

where

x ∈ H 2 (∆(HP 1 ); Z)

and

t ∈ H 4 (∆(HP 1 ); Z)

.

Proof. Weusethebration

S 1 −→ G(HP 1 ) −→ ∆(HP 1 )

fromthe

S 1

ation.

Hereweknowtheohomologyofthebreandthetotalspae,thelatterfrom

Theorem 2.1,

H n (G(HP 1 )) =

 

Z, n = 0, 7

;

Z/2Z, n = 4

;

0,

else.

We an use the Serre'sspetralsequene,

H p (∆(HP 1 ); H q (S 1 ; Z)) ⇒ H p+q (G(HP 1 ); Z),

to nd the ohomology of the base. Let

σ ∈ H 1 (S 1 )

denote a generator.

The

E 2

page has only two non-zero rows. We see that the only possible

(19)

non-trivial dierentials are

d 2

, so

E 3 = E

. We know the total spae has

nothing in degree 1, so there must be zero at

(1, 0)

sine this annot be

killedby anything. So

H 1 (∆(HP 1 )) = 0

, whih meansthereiszero at

(1, 1)

,

too. Also,

σ

must be killed by an outgoing dierential, so

d 0,1 2

is injetive.

Atually it must be an isomorphism, otherwise something would survive in

degree2,and thereisnothing. Sowehave a

H 2 (∆(HP 1 ); Z) ∼ = Z

generated,

say, by

x = d 2 (σ)

. Letus take a look atthe

E 2

page as we knowit now:

1 σ 0 σx ? ? ? ? ? ? · · · 0 1 0 x ? ? ? ? ? ? · · · 0 1 2 3 4 5 6 7 8 · · ·

Continuinginthisfashionweseethereiszeroat

(3, 0)

sine

H 3 (G(HP 1 ); Z) = 0

, and so also at

(3, 1)

. Likewise, there are zeroes at

(5, 0)

and

(5, 1)

. Now

onsider

d 2,1 2

. This must be injetive, sine it starts in degree 3, where the

total spae has nothing. Also,

d 2,1 2

ends at

(4, 0)

, and must besuh that we

get

H 4 (G(HP 1 ); Z) = Z/2Z

when taking the okernel of it. This means it

must be multipliation by

± 2

; we might as well say 2 for onreteness. So

H 4 (∆(HP 1 ); Z) ∼ = Z

generated by some

t

, whih we an hoose suh that

d 2 (σx) = 2t

. A quik summary:

1 σ 0 σx 0 σt 0 ? ? ? · · · 0 1 0 x 0 t 0 ? ? ? · · · 0 1 2 3 4 5 6 7 8 · · ·

Nowwehavegottensomethingat

(4, 1)

,butthetotalspaehaszeroindegree

5,so

σt

must bekilledby the outgoingdierential

d 4,1 2

. Againitmust bean

isomorphism. Note that by the derivation property of

d 2

,

d(σt) = d(σ)t − σd(t) = d(σ)t = xt

so

xt

is agenerator of

H 6 (∆(HP 1 ); Z)

. This givesusa

Z

at

(6, 1)

generated

by

σxt

. Now to see what further happens, we note that

∆(HP 1 )

is at most

7

-dimensional, sine

G(HP 1 ) = S(T (HP 1 ))

is a

7

-manifold. So we know

that

H (∆(HP 1 ); Z)

is zero above degree

7

. This means that

σxt

annot

be killed, soit survives to

E

, meaningthere an be nothing else in degree

7

. So from olumn 7 and onwards there are zeroes in the

E 2

page. Now we

know the full story:

1 σ 0 σx 0 σt 0 σxt 0 0 · · ·

0 1 0 x 0 t 0 xt 0 0 · · ·

0 1 2 3 4 5 6 7 8 · · ·

(20)

Toget tothe bottomof the multipliativestruture wealulate:

2t = d(σx) = d(σ)x − σd(x) = d(σ)x = x 2 .

Fordimensional reasons

t 2 = 0

, and all other relationsome from these two

(e.g.

x 3 = x 2 · x = 2xt

). This proves the result.

Wenowturntothegeneralaseof

∆(r)

. Wehavethe brationfrom(8),

∆(HP 1 ) −→ ∆(HP r ) −→

Gr

2 (H r+1 ).

So in order to apply Serre's spetral sequene, we need to know the oho-

mology of Gr

2 (H r+1 )

. This is taken are of by the following Lemma, whih

isthe quaternion version of [Bökstedt-Ottosen ℄ Thm. 3.1:

Lemma 2.3. For

r ≥ 1

,

H (

Gr

2 (H r+1 ); Z) ∼ = Z[p 1 , p 2 ]/ h ϕ r , ϕ r+1 i ,

where

p 1 , p 2

arethePontryaginlassesofthestandardbundle

γ 2 ց

Gr

2 (H r+1 )

,

and

ϕ i = ϕ i (p 1 , p 2 )

is the polynomial given indutively by

ϕ 0 = 1, ϕ 1 = p 1 , ϕ i = − p 1 ϕ i − 1 − p 2 ϕ i − 2 ,

for

i ≥ 2.

Proof. We use a result of Borel, [Borel℄ Prop. 31.1. Let

γ 2 ց

Gr

2 (H r+1 )

denote the standard 2-dimensional bundle, i.e. the bre over

V ⊆ H r+1

is

V

. Let

p i

,

i ≥ 0

be the Pontryagin lasses,

p i ∈ H 4i (

Gr

2 (H r+1 )

, whih

satisfy

p i = 0

for

i > 2

, sine

γ 2

is 2-dimensional. Let

γ ¯ r − 1

denote its

(r − 1)

-dimensional orthogonal omplement, i.e. the bre over

V ⊆ H r+1

is

V ⊆ H r+1

. Denote the Pontryagin lasses of this bundleby

p ¯ j

,

j ≥ 0

,

p ¯ j ∈ H 4j (

Gr

2 (H r+1 ))

,and note that

p ¯ j = 0

for

j > r − 1

. Then

γ 2 ⊕ γ ¯ r − 1 ∼ = ε r+1

,

thetrivialbundleofdimension

r + 1

. ThesumformulaforPontryagin lasses

gives the relations

X

i+j=k

p i p ¯ j = ¯ p k + ¯ p k − 1 p 1 + ¯ p k − 2 p 2 = 0,

for

k > 0

(11)

Borel'stheoremstatesthat

H (

Gr

2 (H r+1 ); Z)

isgeneratedbythePontryagin

lasses of

γ 2

and

¯ γ r − 1

, subjet tothe relations mentioned above:

H

Gr

2 (H r+1 ); Z ∼ = Z[p i , p ¯ j | i, j > 0]/ h{ p i } i>2 , { p ¯ j } j>r − 1 , X

i+j=k

p i p ¯ j

k>0 i .

By(11) we see thatwean indutivelyexpress

p ¯ k

asa polynomialin

p 1

and

p 2

. Callthat polynomial

ϕ k

, so

p ¯ k = ϕ k (p 1 , p 2 )

, and we get from (11)

ϕ 0 = 1, ϕ 1 = p 1 , ϕ i = − p 1 ϕ i − 1 − p 2 ϕ i − 1 , i ≥ 2.

(21)

Then we get

H (

Gr

2 (H r+1 ); Z) ∼ = Z[p 1 , p 2 , p ¯ j | j > 0]/

*

{ p ¯ j } j>r 1 , X

i+j=k

p i p ¯ j

k>0

+

∼ = Z[p 1 , p 2 , p ¯ 1 , p ¯ 2 , . . .]/ D

{ p ¯ j } j>r 1 , { p ¯ k − ϕ k (p 1 , p 2 ) } k>0

E

∼ = Z[p 1 , p 2 ]/ h ϕ k | k ≥ r i .

From the indutive formula for

ϕ k

it is seen that

h ϕ k | k ≥ r i = h ϕ r , ϕ r+1 i

,

and this proves the lemma.

2.2 The unparametrized geodesis

Reall

H (BS 1 ) ∼ = H (CP ) ∼ = Z[u]

where

u

has degree 2; a fat that an

be dedued from

H (CP n ) ∼ = Z[u]/ h u n+1 i

.

Theorem 2.4. The spae of unparametrized oriented geodesis,

∆(HP r )

,

has the following ohomology:

H (∆(HP r ); Z) ∼ = Z[x, t]/ h Q r , Q r+1 i ,

where

x ∈ H 2 (∆(HP r ); Z)

istheimageofthegenerator

u ∈ H (BS 1 ) ∼ = Z[u]

and

t ∈ H 4 (∆(HP r ); Z)

.

Q k

for

k ∈ N

isapolynomialin

x

and

t

indutively

given by

Q 0 = 1, Q 1 = 2t − x 2 , Q s = (2t − x 2 )Q s − 1 − t 2 Q s − 2 ,

for

s ≥ 2.

Note that Lemma 2.2 is a speial ase of this with

r = 1

:

Q 1 = 2t − x 2

,

and

Q 2 = (2t − x 2 )Q 1 − t 2 ≡ t 2 (mod Q 1 )

. TheproofofTheorem2.4for

HP r

isnot atalllikethe

CP r

ase, sine

∆(HP r )

isnot isomorphito

P(γ 2 )

, and

the proof willtakequite sometime. First we show that the ohomologyisa

polynomial algebragenerated by lasses

x

and

t

asinthe Theorem, modulo

ertain relations. It will follow from Lemma 2.3 that the polynomials

Q r

,

Q r+1

are among these relations. Then we use a purely algebrai ounting

argumentto showthat there an beno further relations.

Proposition 2.5 (Theorem 2.4, Part1). There is a surjetive map

Z[x, t]/ h Q r , Q r+1 i ։ H (∆(HP r ); Z).

Proof of Theorem 2.4,Part 1. We write down the

E 2

page of the Serre's

spetral sequene for the bration

∆(HP 1 ) −→ ∆(HP r ) −→

Gr

2 (H r+1 )

,

Referencer

RELATEREDE DOKUMENTER

No Creation [B-multicast]: if a correct process p delivers a message m with sender s, then m was previously multicast by process

• FIFO ordering: if a correct process p i issues multicast(g, m) and then multicast (g, m’) (multicast(g, m) ➝ i multicast(g, m’)), then every correct process that

In this case, we either have a normal P 2 -constraint, and then the generate rule does not create problems, or a constraint of type special, in which case the message m to de- rive

› Intuitivt giver det mening, at kvalitet af asfalt kan påvirke mængden af ophvirvlet vejstøv. påvirke mængden af

We start by defining the category of models LTS 4 , then the subcategory of observations P , and finally we characterise the P -open maps and prove that P -bisimilarity coincides

We do not replace S m by S m 0 in the CDD (which would mean we would replace it for all subgraphs which share it), but we only replace it in the node the constraint J(i, j) came

This means that the simulator knows the opening of all the commit K (m) commitments and the opening of the commit K E (m) and commit K (m + m) commitments for the perfect

We rst present the type system (Section 3), and we then prove that the type inference problem is log space equivalent to a constraint problem (Section 4) and a graph problem