Author: Eiko

Tags: quiver variety, algebraic geometry, representation theory, Dynkin, extended Dynkin

Time: 2024-12-08 23:28:08 - 2024-12-09 18:28:44 (UTC)

For the basic notions and results appearing in this example sheet, you should recall here.

A basic summary is put here for quick reminder.

  • There is an associated root system to a quiver.

  • For finite type quivers (i.e. for any α, only have finite many indecomposable reps. Finite type Dynkin)

    • Indecomposable Representations Positive roots

    • Using reflection functors one can obtain all indecomposable from simples, which is the same as obtaining all positive roots from simple roots ei.

  • Associated to a quiver Q we have a doubled quiver Q and associated to doubled quiver we have a moment map μQ,α:Rep(Q,α)Lie(Gα).

  • Quiver varieties

    Mθ(Q,α)=μQ,α1(0)//θGα,M(Q,α)=μQ,α1(0)//Gα.

  • Parameter function

    pQ(α)=1α,αQ=1+stQαsαtiαi2.

    When α is a root, 2pQ(α) is the dimension of Mθ(Q,α).

Examples Of Computations Of p(α)

The parameter p(α) conveys the meaning of number of parameters of representations of dimension α and is of fundamental importance. Let’s see some examples,

  • we will use Ai to denote the Dynkin quiver with i vertices,

  • use Ai^ to denote the extended Dynkin quiver with i+1 vertices,

  • and F(Ai^) to denote the framed extended Dynkin quiver with i+2 vertices.

A0^

The A0 quiver might sounds a bit too funny because it is empty. But we think of the extended A0 quiver A0^ to be the Jordan quiver which is a single vertex with exactly one loop. Whose representations are just assigning a vector space at that node.

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Here n is the dimension of that representation space.

If we compute the inner product we have

α,α=α0α0α02=n2n2=0

p(α)=1α,α=1.

So α corresponds to an isotropic imaginary root, and it has a single parameter.

F(A0^)

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α,α=1+a2aa2=1a. pQ(α)=1(1a)=a.

For θ=(a,1), this Mθ(Q,α) is our classical Hilbert scheme (C2)[a].

For θ=0, it reduces to M(Q,α) which is the symmetric product Syma(C2). You can see that the stratifications of Syma(C2) corresponds to the partitions of a, which perfectly matches the decomposition of the dimension vector α.

α=(1,0)+a1(0,1)++ak(0,1) Syma(C2)=a1++ak=aSa1,,aknC2=a1++ak=a{ikai[xi]:xi distinct}

F(A1^)

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α,α=1+a2+b2a2ab=1+(ab)2a

pQ(α)=a(ab)2.

F(A2^)

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α,α=1+a2+b2+c2aabbcac=1+(ab)2+(bc)2+(ca)22a.

pQ(α)=a(ab)2+(bc)2+(ca)22.

F(A3^)

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α,α=1+a2+b2+c2+d2aabbccdda=1+(ab)2+(bc)2+(cd)2+(da)22a.

pQ(α)=a(ab)2+(bc)2+(cd)2+(da)22.

Examples Of The Semistable Set Σλ,θ

Computing Σλ,θ(F(A1^))

The situation we are considering is λ=0, and θ=(n,1). The case θ=0 might also be interesting, we might consider it later.

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    p=n

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    p=n1

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    p=n4

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    p=nm2

Since all possible decompositions that can happen in Rθ+ look like

(1,n,a+b)=(1,n,a)+(0,0,b)

We conclude that

Σλ,θ(FA1^)={(1,n,nm):m2n}{(0,0,k):k0}.

And the canonical decomposition of α is just α.

Stratums corresponds to the decomposition of vectors

(1,n,n)=(1,n,nm)+m(0,0,1),0mn. p(1,n,nm)=nm2,p(0,0,1)=0.

therefore there will be n+1 strata.