Poincaré residue explained

In mathematics, the Poincaré residue is a generalization, to several complex variables and complex manifold theory, of the residue at a pole of complex function theory. It is just one of a number of such possible extensions.

Given a hypersurface

X\subsetPn

defined by a degree

d

polynomial

F

and a rational

n

-form

\omega

on

Pn

with a pole of order

k>0

on

X

, then we can construct a cohomology class

\operatorname{Res}(\omega)\inHn-1(X;C)

. If

n=1

we recover the classical residue construction.

Historical construction

When Poincaré first introduced residues[1] he was studying period integrals of the form

\underset{\Gamma}\iint\omega

for

\Gamma\in

2
H
2(P

-D)

where

\omega

was a rational differential form with poles along a divisor

D

. He was able to make the reduction of this integral to an integral of the form

\int\gammaRes(\omega)

for

\gamma\inH1(D)

where

\Gamma=T(\gamma)

, sending

\gamma

to the boundary of a solid

\varepsilon

-tube around

\gamma

on the smooth locus

D*

of the divisor. If

\omega=

q(x,y)dx\wedgedy
p(x,y)
on an affine chart where

p(x,y)

is irreducible of degree

N

and

\degq(x,y)\leqN-3

(so there is no poles on the line at infinity[2] page 150). Then, he gave a formula for computing this residue as

Res(\omega)=-

qdx
\partialp/\partialy

=

qdy
\partialp/\partialx
which are both cohomologous forms.

Construction

Preliminary definition

Given the setup in the introduction, let

p
A
k(X)
be the space of meromorphic

p

-forms on

Pn

which have poles of order up to

k

. Notice that the standard differential

d

sends

d:

p-1
A
k-1

(X)\to

p
A
k(X)

Define

l{K}k(X)=

p
A
k(X)
p-1
dA(X)
k-1

as the rational de-Rham cohomology groups. They form a filtration

l{K}1(X)\subsetl{K}2(X)\subset\subsetl{K}n(X)= Hn+1(Pn+1-X)

corresponding to the Hodge filtration.

Definition of residue

Consider an

(n-1)

-cycle

\gamma\inHn-1(X;C)

. We take a tube

T(\gamma)

around

\gamma

(which is locally isomorphic to

\gamma x S1

) that lies within the complement of

X

. Since this is an

n

-cycle, we can integrate a rational

n

-form

\omega

and get a number. If we write this as

\intT(-)\omega:Hn-1(X;C)\toC

then we get a linear transformation on the homology classes. Homology/cohomology duality implies that this is a cohomology class

\operatorname{Res}(\omega)\inHn-1(X;C)

which we call the residue. Notice if we restrict to the case

n=1

, this is just the standard residue from complex analysis (although we extend our meromorphic

1

-form to all of

P1

. This definition can be summarized as the map

Res:Hn(Pn\setminusX)\toHn-1(X)

Algorithm for computing this class

There is a simple recursive method for computing the residues which reduces to the classical case of

n=1

. Recall that the residue of a

1

-form
\operatorname{Res}\left(dz
z

+a\right)=1

If we consider a chart containing

X

where it is the vanishing locus of

w

, we can write a meromorphic

n

-form with pole on

X

as
dw
wk

\wedge\rho

Then we can write it out as

1
(k-1)

\left(

d\rho
wk-1

+d\left(

\rho
wk-1

\right)\right)

This shows that the two cohomology classes

\left[

dw
wk

\wedge\rho\right]=\left[

d\rho
(k-1)wk-1

\right]

are equal. We have thus reduced the order of the pole hence we can use recursion to get a pole of order

1

and define the residue of

\omega

as

\operatorname{Res}\left(\alpha\wedge

dw
w

+\beta\right)=\alpha|X

Example

For example, consider the curve

X\subsetP2

defined by the polynomial

Ft(x,y,z)=t(x3+y3+z3)-3xyz

Then, we can apply the previous algorithm to compute the residue of

\omega=

\Omega
Ft

=

xdy\wedgedz-ydx\wedgedz+zdx\wedgedy
t(x3+y3+z3)-3xyz

Since

\begin{align} -zdy\wedge\left(

\partialFt
\partialx

dx+

\partialFt
\partialy

dy+

\partialFt
\partialz

dz\right)&=z

\partialFt
\partialx

dx\wedgedy-z

\partialFt
\partialz

dy\wedgedz\\ ydz\wedge\left(

\partialFt
\partialx

dx+

\partialFt
\partialy

dy+

\partialFt
\partialz

dz\right)&=-y

\partialFt
\partialx

dx\wedgedz-y

\partialFt
\partialy

dy\wedgedz\end{align}

and

3Ft-z

\partialFt
\partialx

-y

\partialFt
\partialy

=x

\partialFt
\partialx

we have that

\omega=

ydz-zdy
\partialFt/\partialx

\wedge

dFt
Ft

+

3dy\wedgedz
\partialFt/\partialx

This implies that

\operatorname{Res}(\omega)=

ydz-zdy
\partialFt/\partialx

See also

References

  1. Poincaré. H.. 1887. Sur les résidus des intégrales doubles. Acta Mathematica. FR. 9. 321–380. 10.1007/BF02406742. 0001-5962. free.
  2. Griffiths. Phillip A.. 1982. Poincaré and algebraic geometry. Bulletin of the American Mathematical Society. en. 6. 2. 147–159. 10.1090/S0273-0979-1982-14967-9. 0273-0979. free.

Introductory

References