C OMPOSITIO M ATHEMATICA
A LBERT E. H EINS
On an integral equation in diffraction theory
Compositio Mathematica, tome 18, n
o1-2 (1967), p. 49-54
<http://www.numdam.org/item?id=CM_1967__18_1-2_49_0>
© Foundation Compositio Mathematica, 1967, tous droits réservés.
L’accès aux archives de la revue « Compositio Mathematica » (http:
//http://www.compositio.nl/) implique l’accord avec les conditions géné- rales d’utilisation (http://www.numdam.org/conditions). Toute utilisation commerciale ou impression systématique est constitutive d’une infrac- tion pénale. Toute copie ou impression de ce fichier doit contenir la présente mention de copyright.
Article numérisé dans le cadre du programme Numérisation de documents anciens mathématiques
http://www.numdam.org/
49
by
Albert E. Heins
The
following
remarks are intended to shed furtherlight
onrepresentation
theorems forpartial
differentialequations
of aspecial form,
inparticular
the two-dimensional waveequation.
Ithas
already
been shown in thepast
decade thataxially-symmetric boundary
valueproblems
of the Dirichlet or Neumanntype
forthe three dimensional-wave
equation
for the disk or a disk betweenparallel planes
may be formulated as aregular integral equation
of the second kind. The
advantage
to such a formulationrequires
no further comment. These Fredholm
integral equations
of thesecond kind are derived from the Poisson
representation
forsolutions of the wave
equation
and theanalytically
continuedaxis data of the Helmholtz
representation.
In a recent paper,J. Boersma
[1]
hasgiven
a similarrepresentation
for the twodimensional wave
equation by accepting
the three dimensionalrepresentation
as aguide
to construct the two dimensional one.We show here that this is
again
a result of theanalytically
continued data of the Helmholtz
representation
in two dimensionsand the
corresponding
version of the Poissonrepresentation
theorem.
The Poisson
representation
theorem[3]
for theequation
has the form
where the term
50
is even
in y
and the termis odd in y. The
symbols Jo
andIl
refer to the usual notation for theregular
and real Bessel functions of order zero and one respec-tively. Furthermore, (3)
in addition tosatisfying
theequation (1)
for
~(x, 0)
eC2,
reduces to~(x, 0) when y =
0 while~~/~y
vanishes at y = 0. On the other hand
(4)
vanishes at y = 0 while its y derivative reduces to03C8(x)
at y = 0. Hence(2)
describes aregular
initial-valueproblem
withrespect
to the line y = 0. Inparticular if ~(0, y )
vanishesfor Iyl b, (2) implies
thatand
We shall make use of these remarks to
provide integral equations
of the
type
which Boersma described.Let us now recall that the conventional Helmholtz
representa-
tion for a
plane
wave incident upon astrip
on which a Dirichletcondition is
satisfied,
thatis, ~(0, y)
= 0,Iyl
b isgiven by
where
A (t )
is thediscontinuity
of the x derivativeof ~(x, y )
onx
= 0, |y|
b.H(1)0
is thecustomary symbol
for the Hankelfunction of order zero and of the first
kind,
while the term exp(ixkx+iyky) represents
the incidentplane
wave. Theboundary
condition
~(0, y)
= 0,Iyl
bproduces
anintegral equation
ofthe Fredholm
type
and of the first kind. It is ourgoal
to showthat because of the
symmetry
of thestrip
about the line y = 0, that anotherintegral equation
may befound, although
it doesnot appear to possess the
simple
form which was found in theaxially-symmetric
case[2]. Nevertheless,
as Boersma hasshown,
it turns out to be useful.
We observe that
(5)
may bedecomposed
into the form~(x, y) = ~e(x, y)+~0(x, y)
where~e(x, y)
is even in y and~0(x, y)
is odd in y. Here we have from
(5)
thatand
In
particular
and this is an
analytic
function of thecomplex
variable z =x+iy
in the
complex plane
cutalong
the line x = 0. Indeed for 0 yb,
wehave,
if we take(x2+t2)1 2
to be real andpositive
for x
real,
that(z2+t2)1 2
=(t2-y2)1 2,
0 y tb, x ~
0±. Onthe other hand
(z2+t2)1 2
= exp(-i03C0/2)(y2-t2)1 2,
0 t y b for x ~ 0+ and it isequal
to exp(i03C0/2)(y2-t2)1 2,
0 t y b for z - 0-. Furthermoreif y
0, we have that(z2+t2)1
=(t2_y2)1,
0 -y tb,
z - 0:1: and it isequal
to exp(i03C0/2)
(y2-t2)1 2,
0t -y b, x ~
0+ and to exp(-i03C0/2)(y2-t2)1 2,
o
t -y b, x ~ 0-.
Hencefor x ~ 0+,
0y b,
weget
from
(6a)
where
B(t)
=A(t)+A(-t), Io (kÂ)
is theregular imaginary
Besselfunction of order zero and
K0(k03BB)
is the MacDonald function of order zero. For x ~0+,
0 -yb,
we haveHence
If we were to
repeat
this calculation for x -+ 0-,Iyl b,
we would52
get
the same result. Observe now that§6(iy, 0)+~e(-iy, 0)
= 0from the Poisson
representation
and hence we have thetype
ofintegral equation
that Boersma gave, that isUnlike Boersma’s
result, B(t)
can be identified as the evenpart
of the normal derivative
of ~
on x = 0,Iyl
b.Now we turn to the odd
component.
First it is noted thatwhere
C(t)
=A(t)-A(-t).
Now(7a)
may be rewritten asor
where a is a constant of
integration.
The constant can be evaluatedin terms of
C(t) by noting
that the left side of(8)
vanishes whenx = 0 and hence
Now we continue
(8) analytically
into the domain of thecomplex
variable z =
x+iy
as we did in the even case. The new term isthe
integral
on the left side of(8).
For 0 yb,
we haveso that for x ~ 0+, 0 y
b,
we havewhile for x ~ 0+, 0 -y
b,
we haveUpon replacing
-yby
y inequation (10)
weget
Hence upon addition of
(10)
and(11)
weget
Now we know from the odd
part
of the Poissonrepresentation
that
03C8(it)+03C8(-it)
= 0 and hence we are left with thefollowing
integral equation
54
Neumann
boundary
conditions may be dealt with in a similar fashion.If instead of a
plane
wave term in(5),
we had a term whichcould not be continued into the domain of the
complex
variablez =
z+iy,
forexample
a line source term, we could redefine~(x, y)
andproceed
as before.Suppose
that the source term isarbitrary
and has theform ~(x, y )
=~ei(x, y)+~ei(x, y )
where~ei(x, y)
and~ei(x, y)
are the even and oddparts
of~i(x, y).
Thenif we
put ~(x, y)-~i(x, y) = 03A6(x, y),
we have that03A6(0, y) =
~i(0, y), |y|
b. The Poissonrepresentation
is nowinhomogeneous
and may be solved as an
integral equation
toproduce ~(iy, 0)+
~(-iy, 0)
or03C8(iy)+03C8(-iy).
Theanalytic
continuation of the modified Helmholtzrepresentation proceeds
as before.Publication
sponsored by
the Air Force Office of ScientificResearch,
Office ofAerospace Research,
United States Air Force under AFOSR Grant No. 374-65.REFERENCES
J. BOERSMA
[1] Boundary value problems in diffraction theory and lifting surface theory, Compositio Mathematica, 16, 2052014293 (1964).
A. E. HEINS and R. C. MACCAMY
[2] On the scattering of waves by a disk, Z. Angew. Math. Phys. 11, 2492014264 (1960).
P. HENRICI
[3] Zur Funktionentheorie der Wellengleichung, Comment. Math. Helv. 27, 2352014293 (1953).
(Oblatum 20-1-66) c The University of Michigan
Ann Arbor, Michigan