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This chapter describes Magma functions for computing with finite real root
systems.
A root system describes the reflections in a reflection group
(Chapter REFLECTION GROUPS).
Root systems are essential in the theories of finite Coxeter
groups
(Chapter COXETER GROUPS)
and Lie algebras
(Chapter LIE ALGEBRAS).
See [Bou68] for more details on the theory of root systems.
The closely related concept of a root datum is discussed in
Chapter ROOT DATA.
Let X and Y be vector spaces over a field k with bilinear pairing
< , >:X x Y -> k that
identifies Y with the dual of X.
Given nonzero α∈X and αstar∈Y,
the linear map sα:X -> X is defined by
x sα= x - < x, αstar >α
and the linear map sαstar:Y -> Y by
y sαstar= y - < α, y >αstar.
These maps are called reflections if one of
the following equivalent properties hold:
< α, αstar >=2; (sα)2=1;
< xsα, ysαstar > = < x, y > for all
x∈X and y∈Y; α sα= - α.
The mapping sαstar is also called a coreflection:
this just means it is a reflection defined on Y instead of X.
magma functions for computing with reflections are described in
Section Construction of Pseudo- reflections.
If X has an inner product, then we can take Y=X and use the inner
product as our pairing.
In magma, we generally take X=Y to be a row space,
with the bilinear pairing given by the standard inner product
< x, y > = xyT.
However, it is sometimes useful to allow X and Y to be distinct
subspaces of a row space.
For the purposes of this chapter, k will always be
the rational field (Chapter RATIONAL FIELD),
a number field (Chapter RATIONAL FIELD),
or a cyclotomic field (Chapter CYCLOTOMIC FIELDS).
The real field (Chapter REAL AND COMPLEX FIELDS)
is not allowed since it is not infinite precision.
Suppose Φ is a finite subset of X - {0}.
For each α in Φ, suppose a corresponding nonzero αstar in Y
is given; set Φstar={αstar | α∈Φ}.
The tuple R=(X, Φ, Y, Φstar) is called a root system if the following
conditions are satisfied for every α in Φ
- 1.
- sα and sαstar are reflections;
- 2.
- Φ is closed under the action of sα; and
- 3.
- Φstar is closed under the action of sαstar.
The set X is called the root space
and Y is called the coroot space.
The elements of Φ are called roots and the elements of
Φstar are called coroots.
A root system is said to be crystallographic if
< α, βstar > is integral for every root α
and coroot βstar.
A root system is reduced, if
α, β∈Φ with β a scalar product of α
implies α=∓β.
Note that it is possible for the set of roots to be empty, in which case the
system is called toral.
A subset Δ of Φ is called a set of
simple roots if
- 1.
- Δ is a basis for the span of the roots kΦ≤X; and
- 2.
- Φ = Φ^ + ∪Φ^ -, where Φ^ + is the set of
linear combinations of elements of Δ with nonnegative
coefficients, and Φ^ - = - Φ^ +.
Every root system has a set of simple roots.
Simple roots are frequently called fundamental
roots. The elements of
Φ^ + are called positive roots
and the elements of Φ^ - are called
negative roots. The
coroots corresponding to the simple (respectively, positive, negative)
roots are the simple (respectively, positive, negative)
coroots.
The rank of a root system
is the size of Δ, i.e. the dimension of the subspace kΦ.
The rank cannot be larger than the dimension of the root system (i.e. the
dimension of X); if the rank and dimension are equal, the root system is
said to be semisimple.
Choose a basis e1, ..., ed for X and a dual basis
f1, ..., fd for Y, so that < ei, fj >=δij.
A reduced root system is determined by a pair of real matrices A and
B where the rows of A are the simple roots and the rows of B
are the corresponding coroots; i.e. Aij=< αi, fj > and
Bij=< ej, αistar >.
The group W generated by the reflections sα, for α a simple
root, is a finite Coxeter group.
The Cartan matrix of a root system is
C =
(< αi, αjstar >)i, j=1n =
ABt.
Note that the root system is crystallographic if, and only if, its Cartan
matrix is crystallographic. As in Chapter COXETER SYSTEMS, the Cartan
matrix is used to define the Coxeter matrix, Coxeter graph, and Dynkin
digraph of a root system.
The classification of Section Finite and Affine Coxeter Groups applies to reduced
semisimple root systems.
The isomorphism class of a reduced root system is determined by its Coxeter
graph and its dimension.
A Coxeter form is a W-invariant bilinear form on
X.
If R is reduced and irreducible, then the roots can have at most two
different lengths with respect to this form.
We call the roots long or short accordingly.
The Coxeter form is normalised so that the short roots in each
component have length one.
Note that, even if X=Y, this form will generally not be the same as the
pairing < , >; however it can be arranged for them to be
the same (see StandardRootSystem).
A root system is reduced, if
α, β∈Φ with β a scalar product of α
implies α=∓β.
A root α with the property 2α∉Φ is called reduced.
A root α with the property (1/2)α∈Φ is called
divisible.
If R is a root system, then the set R0 of indivisible roots in R form the
indivisible subsystem.
Let R be a nonreduced irreducible crystallographic root system of
rank n.
It can be shown that R0 is irreducible of type of type Bn
and every root is either in R0, or is two times a short root of R0.
The Cartan type of R in this case is BCn.
For noncrystallographic root systems the situation is more complex.
Note that the Cartan matrix, Coxeter matrix, Coxeter diagram, Coxeter group and
Dynkin diagram are the same for R and R0.
Thus, when creating a non-reduced crystallographic root system for a given
Cartan matrix, Coxeter matrix, Coxeter diagram, Coxeter group or Dynkin diagram,
one must specify the set of nonreduced simple roots.
For example, let C be a cartan matrix of type B2 x B3. Then the
set of non-reduced fundamental roots can be one of
emptyset, {2}, {5}, or {2, 5}, in which cases the root system
will be of types B2 x B3, BC2 x B3, B2 x BC3, or BC2 x BC3
respectively.
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