A NNALI DELLA
S CUOLA N ORMALE S UPERIORE DI P ISA Classe di Scienze
J. J. S TOKER
Uniqueness theorems for some open and closed surfaces in three-space
Annali della Scuola Normale Superiore di Pisa, Classe di Scienze 4
esérie, tome 5, n
o4 (1978), p. 657-677
<http://www.numdam.org/item?id=ASNSP_1978_4_5_4_657_0>
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http://www.numdam.org/
and Closed Surfaces in Three-Space (*).
J. J. STOKER
(**)
dedicated to .Hans
Lewy
1. - Introduction.
The
problems
considered are thefollowing:
1) Christo f f et’s problem.
The sumR2
of theprincipal
radii ofcurvature of a surface is
prescribed
as a function of the direction of its normals.2)
Minkowski’sproblem.
This the same as1 ) except
that the Gausscurvature g =
1/RlR2
isprescribed
as a function of the direction of the normals.3) Weyl’s problem.
The line element isprescribed
as a function ofGaussian
parameters
on the surface. ’4)
Liebmann’sproblem.
This is an infinitesimal version of3)
in whicha surface
S(0)
is embedded in a set ofneighboring
surfaces8(ë),
in one-to-one
correspondence
with,S(o),
with a few continuous derivatives in E near e = 0. It is assumed that the surfacesS(s)
areapproximately
iso-metric in the
correspondence
set up near e =0,
in the sense that corre-sponding
curves differ inlength by
aquantity
of order ë2.(*)
This paper is dedicated to HansLewy;
at the end of the introduction a few remarks about that are made. The author wishes to express thanks to theGug- genheim
Foundation for an award. The ideas that resulted in this paper came about in the course ofusing
it.(**)
New YorkUniversity,
Courant Institute of Mathematical Sciences, New York.Pervenuto alla Redazione il 6
Luglio
1977.In all of these
problems
it is to be shown that any solutions for a surfaceS(u, v),
with continuous thirdderivatives,
say, isuniquely
determined withinorthogonal transformations,
or,put differently,
that any two surfaces satis- -fying
the conditions of theproblems (which must,
of course, includeboundary
conditions in case the surfaces are not closed
surfaces)
can differonly by
arigid
motionplus
apossible
reflection in aplane.
In all cases the Gausscurvature .K is assumed not to
vanish, except possibly
atboundary points.
In the case of
problem 4) uniqueness
refersnaturally
to infinitesimalrigid motions,
which in effect means that0,
thedisplacement
field of sur-face
points
is that of arigid
motion within second order terms in E.These
problems
have been treated atlength by
many writers. Agood
deal of the relevant literature up to 1950 is cited in the author’s paper
[9],
in which the closed convex surfaces were
treated, together
with somehaving
boundaries of a very
special
character. Morerecently
the books ofPogo- relov [7], Efimov [1],
and a paperby Voss [14], give
discussions of these and various otherproblems concerning
surfaces withboundaries,
and withthe use of a considerable
variety
of methods.Only
references to papers cited here aregiven
in thebibliography.
In the paper of the author cited
above,
theobject
was togive
uni-queness
proofs
in all fourproblems by making
use of Minkowski’ssupport function,
which means that theproblems
are treatedusing homogeneous
functions in
three-space.
At the same time it was desired togive proofs
with a certain
unity
since theproblems
seemed to be in some senseclosely
related. This was
partially successful,
but not ascompletely
as was desired.The purpose of this paper is in
part
tobring
this out moreclearly by procedures using only
the maximumprinciple
inquite simple
ways whichavoid,
forexample,
the need for thesymmetry
relation between three arbi-trary homogeneous
functions ofdegree
one, followedby
anintegration
overthe unit
sphere
inthree-space
to obtain an invariantintegral
with an inte-grand
of onesign.
All four of theuniqueness problems
for closed surfacescan be treated with the aid of a
properly
chosencovariant
differentia,l form «of first
degree.
Its exterior derivative da vanishes when it isintegrated
overthe
surface,
and « is selected so that theintegrand
does notchange sign
andhence is
everywhere
zero, and inaddition,
is such that this leads to the desireduniqueness
theorems. In the author’s book[11] uniqueness proofs
for all four
problems
are treated in this way.They
arequite concise,
butsomewhat
mysterious,
since the choice of the differential « has little motiva-tion,
and the conciseness of theproofs
results from thecompactness
of thenotation,
which conceals agreat
deal of differentialgeometry.
The
present
paper also deals with variousproblems
for open surfaces whenboundaries
on the surfaces occur, orthey
extend toinfinity.
All bound-aries are assumed to be
simple disjoint
closed curves on the surfaces. Theseproblems
are also solved inquite elementary
waysusing
the maximumprinciple.
Someproblems
forcomplete
open surfaces with 1£ > 0 aretreated
(these
are boundaries of unbounded three-dimensional convexbodies).
Papers by
Volkov andOliker [13]
andby Oliker [6], published
in 1970and
1971,
deal withuniqueness
theorems forproblems 1 )
and2)
when for-mulated as
boundary problems
for relevantpartial
differentialequations
onthe unit
sphere.
IThey
are treated in thespherical image
of the surfaces in terms of Minkowski’ssupport
function h asdependent
variable. The conditionimposed
for theuniqueness
theorems is h = 0 on theboundary
of SZ.
Uniqueness
theorems for suchproblems
alsolead,
of course, to uni- queness theorems for the surfaces inthree-space.
The author feels thatthey
can be obtained in a rather moreelementary
wayby working
in three-space.
Also, though
it isquite
natural from thepoint
of view ofuniqueness
theorems for
boundary problems
for a second order linearpartial
differentialequation
on thesphere
toprescribe
that solutions should take onprescribed
values at the
boundary,
it is not theonly
reasonable way to formulateboundary
conditions for the surfaces inthree-space.
Forexample,
in thepaper
by
Volkov and Olikersimple examples
aregiven showing
that thesolution of Christoffel’s
problem
for certain surfaces with boundaries is notalways uniquely
determinedby prescribing
the value of thesupport
func-tion on them. But in all cases the solution of these
problems
for the surfaces isuniquely
determined if any one of the Cartesian coordinates at itsboundary (rather
than the values of thesupport function)
has aprescribed value,
since it then follows
(as
will be shownlater)
that the other two coordinatesare
uniquely
determined within translations. The same remarkapplies
toMinkowski’s
problem.
It haslong
been known(apparently since- Darboux)
that the same
thing
holds forWeyl’s problem (and also,
within the infini- tesimalapproximation involved,
for Liebmann’sproblem).
The author has not seen this remark in the literature about the first twoproblems, although,
as will be seen, it is very easy to
verify
it.This paper is dedicated to Hans
Lewy.
He and I have been friends formore than
thirty
years. I At the time itbegan
we workedclosely
and fruit-fully together
for about a year onproblems
in fluid mechanics. HoweverI,
andstudents,
have been much influencedby
his two classic papers aboutWeyl’s
and Minkowski’sproblem,
in which he dealtmostly
with difficult existencequestions;
but he also gave the firstuniqueness proof
for the solu- tion of Minkowski’sproblem
for closedanalytic
surfaces. Thus it seemsappropriate
to me to write a paper for this occasion in the field of differen- tialgeometry
in thelarge.
I2. - Formulation of the
problems using
Minkowski’ssupport
function.The formulas needed for this paper will be set down without deriva- tions. These can be found in the paper
[9]
cited above or in the literature otherwise-in any case thetheory
isquite elementary
in character.The
support
function is defined as follows. Apoint
p of aregular
sur-face
8(u, v)
inthree-space
is considered and a Cartesian coordinatesystem xi,
i =
1, 2,
3 is chosen with itsorigin
not on S. The direction cosines of anormal to S at
point p
are denotedby
oci. The functionM2,
is definedas the distance from the
origin
to thetangent plane
at p. Since the Gaussian curvature .g is assumed not tovanish,
thepoints
of S in aneigh-
borhood of p are in one-to-one
correspondence
with the directions of the normals. I The functionM2, a3)
is then extended intothree-space
as ahomogeneous
functionx2, x3)
ofdegree
oneby setting
This is Minkowski’s
support
function. I It means that an infinite cone withvertex at the
origin
ismapped
on the surface in such a way that allpoints
on each ray from the
origin (except
theorigin itself)
map on asingle point
of ~S. This makes it
possible
toregard
the surface as definedby H,
withas
independent
variablesdefining
normal directions of the surface. I The Cartesian coordinates thepoints
of S are then shown to begiven by
In effect these are conditions that result because ~S is the
envelope
of itstangent planes.
The coordinates xi of thepoints
of S are therefore deter- minedby homogeneous
functions ofdegree
zero, since H ishomogeneous
of
degree
one, and that is as it should be because it means that everypoint
of a
given
ray from theorigin
does indeed map on auniquely
determinedpoint
of S. It is vital to observe that(2.2)
leads to thefollowing
conclusion:if
twosupport functions of surfaces differ by
a linearf unction
then the twosurfaces
are identical within a translation.Curvature
properties
of S are definedthrough
consideration of theprin- cipal
radii of curvatureR,, -R~
in connection with the formula ofRodrigues.
It is found in a
straightforward
way thatRl
andI~2
are roots of thefollowing
algebraic equation:
Here
Hik
is asymbol
for second derivatives of H. Thisequation, seemingly
cubic in
R,
isreally quadratic,
since the constant term init,
i.e. the deter- minantIHikl,
y vanishessimply
because H ishomogeneous
ofdegree
one.It then follows that the
support
function satisfies two differential equa- tionscontaining R~
andR2
in coefficients. One of them iswhich results from consideration of the sum of the roots of
(2.3).
Thesecond results because the
product
of the roots of(2.3)
isRIR2 = I.K,
andbecause H is
homogeneous
ofdegree
one:The
following
identities occurlater; they
hold when H and Ware anyhomogeneous
functions ofdegree
one(not necessarily
derived from asurface):
If H and W were
identical,
the three ratios in(2.6)
would all beequal
to
1/r2K
in view of(2.5);
thus eachequation
of(2.5)
isequivalent
to the others. For the sake ofready
reference some of Euler’s relations for a homo- geneous function H ofdegree
one are setdown; they
are used inderiving
the above identities:
The second results because the first derivatives
Hi
arehomogeneous
ofdegree
zero.Suitable
partial
differentialequations
forproblems 1)
and2)
are,clearly, given by (2.4)
and(2.5).
ForWeyl’s
and for Liebmann’sproblem
the formulation in terms of asupport
function is less direct. IfX(u, v), Y(u, v)
are two surfaces
~51, ,S2
which are isometric in the sameparameters (u, v),
it follows that dX ~ dX =
dY ~ dY,
the differential d to be taken withrespect
to
(u, v).
Introduction of V = X - Y and Z =-E- Y),
the so-called meansurface,
y leads to the condition dV.dZ = 0. It can then be shown that auniquely
determined rotation vector8(u, v)
exists such thatin which X means the vector
product; provided
that the mean surface Zis a
regular
surface in theparameters (u, v).
It iseasily
seen that this con-dition on Z will be satisfied if the two surfaces
~~1
and~2
are soplaced
inthree-space
that nopair
oftangent
vectors thatcorrespond by
theisometry
are
parallel
inthree-space,
butoppositely
directed. In the book ofPogo- relov [7]
theregularity
of the mean surface is verified in aspecial
case;in a recent letter to the author he states that this
intriguing question
remainsunsettled in the
general
case.However,
if the two surfaces areplaced
soas to be
tangent
to each other at apair
ofcorresponding points,
it is clear that the mean surface will beregular
even if not toolarge
finitedisplace-
ments of
corresponding points
inthree-space
occur. IThis,
of course, y means that an unwanted restriction isimposed
if the mean surface isused,
butnevertheless
WeyFs problem
rather than Liebmann’sproblem
is involved:in the second
problem
theoriginal
surfaceS(o)
can be usedlegitimately
inplace
of a mean surface.The connection of this with a
support
function W resultsby defining
W as the scalar
product
5. n of the rotation vector with the unit normal n of the meansurface,
hence first as apoint
function on a unitsphere (the spherical image
of the meansurface),
y which is then extended into three- space as ahomogeneous
function ofdegree
one. Anelementary
discus-sion
(carried
out in[9]
forWeyl’s problem)
shows that if 8 is a constant vector in theparameters (u, v)
that then the isometric surfaces can differonly by
arigid
motion. It turns out that theuniqueness
theorems forproblems 2), 3),
and4)
then all lead to the same linear differentialequations
for a relevant
homogeneous
function(in spite
of the fact that the differentialequations
for2)
and3)
areMonge-Amp6re equations,
hence not evenquasi-
linear).
This isbasically
the reasonwhy
a unified treatment of the uni- quenessproblems
would seem feasible and worthlooking
for.3. - Christoffel’s
problem.
Consider two surfaces
~51, 82, possibly
withboundaries,
such thatT~ ~’.
0holds,
but K 0 as well asK >
0 may occur. Forboth,
thesupport
func- tions H~2~ are then sometimes assumed to have the same values at any boundaries of theirspherical images.
This is theassumption
madeby
Volkovand Oliker
[13],
andby
Oliker[6].
Ineffect,
and .H«> are assumed to beprescribed
at boundaries of thespherical image.
In the papersquoted
thesignificance
of this for the surfacesSi
andS2
is mentionedonly
inpassing, probably
because theproblem
is dealt with as aboundary problem
on thesphere,
with differentialequations
also defined on it. It seems to the author easier to deal with theproblem
inthree-space
since the differentialequation
is
simpler
and theuniqueness
theorems areproved
in astraighforward
waythat is
quite elementary.
THEOREM
C1:
It has somepoint
to deal with the classicalproblem first,
i. e. the case in
which 81
and~S2
are closed convex sufaces with theorigin
in their
interiors,
and thus thespherical image
covers the wholesphere.
It is to be shown that
,S1 and S2
differonly by
a translation. Theirsupport
functions
H(l),
H(2) bothsatisfy (2.4)
with the sameright
hand sides. Thus isevidently
a harmonic function inthree-space (it
would bewhether
,Sl
and~2
are closed ornot,
and also whether T~ 0 or I~ > 0holds) :
The harmonic function H is defined in the entire
xl, x2, x3-space, except
atthe
origin. However,
theorigin
is an isolatedpoint
with H defined andsingle-valued
in itsneighborhood,
and H - 0 as r - 0 because .H is homo-geneous of
degree
one, hence H is bounded near theorigin. Consequently
the
origin
is a removablesingularity
and H is harmonic there if its value is defined to be zero. The function behaveslinearly
in r when r - 00; itfollows that H is a linear function of the variables xi
(from
Liouville’s theorem for harmonic functions in threedimensions),
and because of(2.2)
the coordinates Ti of the
points
of the two surfaces81
and~S2
differby
aconstant,
andthus 81
and~3
differby
a translation. Thus anexceedingly simple proof
ofuniqueness
of the solution of Christoffel’sproblem
forclosed convex surfaces results.
In the paper
by
Volkov and Oliker cited aboveexamples
aregiven (involving
surfaces with K0)
for which the solution of theproblem
withboundaries is not
uniquely
determined when thesupport
function H isprescribed
at boundaries.However,
the solutions areuniquely
determinedif any one of the Cartesian coordinates
Xi = Hi (cf. (2.2))
isprescribed,
aswill be shown next.
THEOREM
C2:
For surfaces with K> 0 or .KcO and any number of bound-aries,
theuniqueness proof
ishardly
morecomplicated
than it was for closedsurfaces if the
boundary
conditionimposed
is that a Cartesiancoordinate, x3
say, is
prescribed
at all boundaries. I Since H in(2.4),
hence also in(3.1),
israther
naturally
assumed to have at least continuous secondderivatives,
it follows that solutions of
(3.1)
would have continuous derivatives of all orders sincethey
are harmonic functions. Thus the derivativeH3
== H31’ - .H3 ’
would be a solution ofConsider the values of on the
spherical image Q, regarded
as an openset,
which lies on the unitsphere
centered at theorigin.
I At thepoints
of 8Qcorresponding
toboundary
curves of~’1
and~’2,
theboundary
conditionassumed means that the difference
Ng~ 2013 H32~
has the value zero at all bound- aries. Thus unlessH3 =-= 0
holds inQ,
apositive
maximum ofH3
could beassumed to exist at a
point
p in S~.H3
is ahomogeneous
function ofdegree
zero, hence is constant
along
each ray from theorigin
topoints
ofSZ;
ittherefore takes on a maximum in
three-space
at p. But that isimpossible
since
H3
is a harmonic function. I ThusH3 =
0holds,
and H =H~2~
isindependent
of x3.LEMMA C : From this it follows
readily
that the other Cartesian coordi- nates xl and x2 ofS’1 and S2
differby
constants at allcorresponding points.
The
proof
issimple.
Since H isindependent
ofx3,
it follows thatHII + -f- H22
= 0 holds. At the same time it follows from(2.8)
thatand since these are identities for
arbitrary
values of xland x2,
the deter-minant
Hl1H22- H;2
=0 ;
becauseHll
= -H22
it follows thatHIl = H22
.-=
I~x2 =
0 holdseverywhere.
Thusg’~
andH2
are constants and this meansthat the coordinates Tl and x2 at all
corresponding points
of81 and S2
differeverywhere by
aconstant,
and the desired lemma is obtained. With it theproof
of TheoremC2
iscompleted.
ITHEOREM
C3: Examples
of surfaces with boundaries for which this uni- queness theorem holds for .~ 0 as well as ~ > 0 arereadily given.
I Forexample,
any closed convex surface with holes cut outanywhere,
for exam-ple,
a band in the form of aring
with twoboundaries,
and thus notsimply connected,
would serve for the case K > 0. For .K C 0 such bands also exist. In addition the bandsmight
be such that thespherical image
couldhave a number of
sheets,
and the surfaces could have self-intersections. I The maximumprinciple
wouldagain
serve to establish theuniqueness theorems,
since that involves a
purely
localstatement,
and the fact that H wouldbe defined as a harmonic function in a multi-sheeted domain in
three-space
would cause no
difficulty.
IOther
uniqueness problems
have been consideredby
M.Tsuji [12],
in-cluding particular
kinds of closed surfaceshaving arbitrary
genus. Such surfaces have ofnecessity regions
in which K must bepositive,
as wellas
negative.
To construct suchexamples,
the surfaces were assumed to be built up ofpieces
ofnegative
curvaturejoined
topieces
withpositive
curvature across
special
curves where K = 0 holds. On theparts
withT~
0,
the Christoffel condition is assumed tohold,
whileon
apart
with-If > 0 either that condition or Minkowski’s condition is assumed. I
THEOREM
C4 :
Thebooks
ofPogorelov
and Efimov cited earlier dealextensively
with the case of bounded surfaces 8 in which.KT =
2aand the
spherical image
is ahemisphere.
For Christoffel’sproblem
suchcases are
readily
treated inthree-space
notonly
when a coordinate ofboundary
curves isfixed,
but also if thesupport
function isprescribed.
In case H is
prescribed
at theboundary
suppose that X3 = 0 contains thegreat
circle that bounds thespherical image.
It follows for two surfacesS1
and~2
that H = H~ 1 > - H(2) = 0 on the unit circle centered at theorigin
inthe
plane x3
= 0. Theorigin
is located so that H > 0 holdsgenerally.
ButH ~ 0 when r - 0 on any ray from the
origin,
and since H = 0 on each ray as it crosses the unit circle in x3 =0,
it follows since H ishomogeneous
of
degree
one that it vanisheseverywhere
in theplane X3
= 0. Since H is aharmonic function it can be continued
analytically by
reflection across theplane x3
=0,
andconsequently
can be defined as a harmonic function every- where inthree-space except
at theorigin,
where as in the earlier discussion it has a removablesingularity.
Asbefore,
H behaveslinearly
at oo, henceis a linear
function,
so that the derivativesHi
areconstants,
which meansthat
81
andS2
arecongruent.
I Theuniqueness
theoremC4
is thusproved.
4. - Minkowski’s
problem.
This
problem
is to be attacked on the basis of the threeequivalent
equa- tions(2.5),
with arepresentative example
of the formThe two others are found
by cyclic permutation
of thesubscripts.
IThe device used
by
the author in[9]
willagain
be used here. It con-sists in
introducing
the sum H = H(l)+ H(2) ,
and the difference W =- H(2) of the
support
functions of two convex surfacesS1 and S2 (K
> 0 holdsthroughout
thissection,
in otherwords)
such that(4.1)
is satisfied when g is the same for both. The result isreadily
found to be thefollowing
linear differential
equation
for W :The functions W and H are
both, evidently,
yhomogeneous
functions ofdegree
one, and H is thesupport
function of a closed surface withpositive
Gauss curvature since it is the sum of
support
functions for two such sur-faces,
y and the surface is then theboundary
of a bounded convex set(Hadamard’s theorem).
It follows thatif s3 # 0
holds,
in view of(4-1),
which is valid when H is thesupport
func-tion of any surface with .K > 0. As was
pointed
out earlier two other identi- ties like(4.2)
and(4.3)
hold when thesubscripts
arechanged cyclically.
Thus
always
one at least of theequations
of the form(4.2)
iselliptic
at agiven point
since xl = x2 = z3 = 0 never occurs.THEOREM
Mi:
As in thepreceding section,
the discussionbegins
withthe
uniqueness
theorem for the case of two closed convex surfacesS2
so that their
spherical images
cover the entire unitsphere.
In that caseH =
-+-
’2> is defined in the entirexl, x2, xs-space, except
for theorigin,
and yY = H(l) - H(2) as well. It is to be shown that81
and82
areidentical within a translation. This will be done
by considering
any one of the Cartesian coordinates xi =Hi
of~’1
andS2, x~,
say, andshowing
that
W,
=H31’ - H (2)
iseverywhere
constant. Once that is done it is clear fromsymmetry
that the same statement would hold for the other coor-dinates.
LEMMA J-1: If there are
boundaries, symmetry
in all three variables does not ingeneral exist,
and the latter statement is notnecessarily applicable.
It does
hold, however,
as will now be shown.Suppose again,
as in LemmaC,
thatW3
is found to beidentically
constant so that Wdepends only
upon xl and x2. If X2 0 0 is assumed(the
0 can be treated in the samefashion)
then W wouldsatisfy
theappropriate equation
of thetype (4.2)
for this case, i.e.
Since
H,,,, =A
0 andW31
= 0 andW33
= 0hold,
it follows thatW11
=0,
firstfor r2 #
0,
then for all values of x2by continuity. Also,
as was noted in theprevious section,
it follows from Euler’s theorem for the first derivatives, ~2 (when W3
= constholds)
thatfor any values
xl, x2,
and as aresult IWikl
= 0. SinceWIl = 0,
it followsthat
Wi~ = 0. Finally,
for x3o0, (4.2 )
holds withHIIH22 - H 1 2 > 0;
thusW22
= 0everywhere, including X3
=0, again by continuity. Consequently WIt,
areidentically
zero, so that W is a linear function ofx1, x2, x3,
Iand its first derivatives are constants. In other
words, 81
andS2
woulddiffer
only by
a translation. This proves LemmaM,
and verifies a state-ment made in the first section to the effect that two surfaces
satisfying
the basic
condition,
i.e. thepartial
differentialequation, imposed
in Min-kowski’s
problem
would differ at mostby
a translation if it is assumed that any one of their Cartesian coordinates xi is the same for both atcorrespond- ing points.
THEOREM
Mi:
Theuniqueness
theorem for closed surfaces is now to beproved
with the aid of a maximumprinciple.
To this end consider the« ver- tical » Cartesian coordinates T3 of them atcorresponding points;
their differen-ce is the function
W3 (cf. (2.2)).
If this is noteverywhere
constant on the unitsphere
centered at theorigin (which implies
that it is constant on every ray from theorigin
since it ishomogeneous
ofdegree zero),
it may be assumed that it has apositive
maximum at apoint
p on thesphere,
andconsequently
a maximum at that
point
in thex1, X2, x3-space.
Consider first the case in which p does not lie on thex3-axis,
so that xl and x2 cannot vanish theresimultaneously. Assume,
say, 0 holds at p. The differential equa- tion(4.4)
is validthere,
and iselliptic
when it isregarded
as anequation
for W as a function of x1 and z3 in the
plane z2
= constthrough
thepoint
psince 01532 =F
0 at p is assumed. The maximumprinciple
does notimmediately apply
to thisequation
sinceyP, being homogeneous
ofdegree
one, does not
necessarily
have a maximum inthree-space
at p, and thus notnecessarily
so in theplane x2
= const.However,
a device can be intro-43 - Annali della Scuola Norm.. Sup. di Pisa
duced so that the maximum
principle
may be used. That is doneby
ob-serving
first that.H33 ~
0 holds. Theequation (4.3)
can therefore be dividedby
it and then a differentiation of theequation
withrespect
to 01533yields
the
following
second order differentialequation
for the derivativeW3:
Here the coefficient
B,
forexample,
isgiven by
Sincebeing homogeneous
ofdegree
one, has a maximum at p inthree-space,
ithas also a maximum
at p
in theplane x2
= const. Butthat,
as is wellknown
(and
not difficult toprove), is
notpossible
because the discriminant of the relevantquadratic
form for(4.5),
i.e.is
clearly positive.
ThusW~ =
const would holdeverywhere,
and Lem-ma if would
yield
theproof
of Theoremifi.
The
uniqueness proof
will therefore becompleted
once thespecial
case in which p is at the
point (0, 0, 1)
on the unitsphere
has been dealt with. This is doneby showing
that a contradiction results also in this case, as follows. It may be assumedthrough
anappropriate
translation of82
thatW3 = 0
at(0, 0, 1),
i.e. at p(it
islegitimate
to assume x3 =1at p since is in any case constant
along
thez3-axis).
3
Consider the function
Wa(x1, x2,1 ) ;
itsatisfies, from WiXi
=W,
therelation "~
in which
W1
andW2 depend only upon xl
and x2. Inaddition,
the equa- tion(4.2)
holds for W. The basic fact is thatW,
has~P3
= 0 as a max-imum at p, hence also in the
plane x3 = 1;
it follows from(4.6)
thatW = 0 at
xl = 0, X2= 0
1 i. e. at theorigin
in theplane
matter of
simple
direct verification to see that theright-hand
side of(4.6)
is unaltered if W is
replaced by
i.e. if anarbitrary
linearfunction is added to it.
By
a proper choice of the constants a and b the first derivativesWi
andW2
of the new function would have the value zeroat the
origin.
It follows that W may be assumed to vanish to second order at theorigin.
The existence of the maximum ofW3 = 0
at p means thatthe
following inequality
holds:This can be
put
into a useful formby noting
thatso that
holds. From
(4.7)
it then follows thatis valid. Since W vanishes to second order for r =
0,
it follows thatas
r - 0,
and results sinceWjr
is anon-decreasing
func-tion of r in view of
(4.9) (*). Consequently W
also has thatproperty;
inother words W would take on the minimum value zero at r = 0. But that is
impossible
unless W = 0 holds since W satisfies(4.2)
in theplane
x3 = 1and
HllH22- Hi2
> 0 holds.For the closed surfaces
Si
and~2 therefore, W3 --- 0 holds,
andWl
andW2
would beconstant,
as wasproved
earlier. Thiscompletes
theuniqueness proof
of theorem~Il.
THEOREM
lVl2:
For surfacesSi
and82
withboundaries,
such that anyone of their Cartesian coordinates is assumed to be the same for both at
corresponding points,
theuniqueness
theorem isproved
in the same wayas above
by using
the maximumprinciple:
apositive
maximum of say, could be assumed to exist in thespherical image Q,
and the discussionabove would once more lead to a
uniqueness proof.
The observations madeconcerning
TheoremCg (but
restricted to the case K >0)
are also relevant here.(*)
This device isadapted
to the presentproblem
from a much moregeneral unpublished
lemmaby
D. Koutroufiotis and L.Nirenberg.
The lemma states:Let u(x, y) be such that 0 holds in a bounded
star-shaped
domain Drelative to the
origin.
Then the function u - xux - YU1/ takes on any maximum value in D also at somepoint
on theboundary
of D. The lemma has an intricateproof
except when the maximum occurs at theorigin (which
is the case in the pre- sentdiscussion).
In case it is the value of the
support
functions and H~2~ of~’1
andS,
that is
prescribed
atboundaries,
as is doneby
Oliker andVolkov,
ratherthan a Cartesian
coordinate,
it is alsopossible
andadvantageous
in somecases to
give uniqueness proofs by working
inthree-space
rather than onthe surface of the unit
sphere,
y since theproofs
thenrequire only
elemen-tary procedures,
rather than suchthings
as the use of Hilbert’stheorem, proved
with the aid of histheory employing integral equations,
to make astatement about relevant linear
eigenvalue problems
on thesphere.
A fewexamples
will begiven.
ITHEOREM
Suppose
that thespherical image ,S2
lies in ahemisphere
without
touching
thegreat
circle that bounds thehemisphere,
and this in turn is assumed to lie in theplane
x3 = 0. In that case the rays from theorigin
to D will cut out a bounded domain D in theplane 01533 = 1,
say, with any number of distinct curves
forming
theboundary
aD ofD,
on which W = H~1~-
H(2),
when solutions H(l) and H(2) aresupport
func-tions of two surfaces
satisfying
theboundary conditions,
would have the value zero. On thatplane (4.2) holds,
withHllH22- Hi2
>0,
when H isdefined as
H = H~1~ -+- H~2>
since x3 = 0 does not occur in ,5~.Multiplication
of
(4.2) by
W andintegration
over Dyields, evidently
The
parenthesis
can be written as adivergence expression,
i.e.(H22
-
(Hl1 W2- TV1)2
=O2
since third derivatives cancel out.Integration by parts
then results in theidentity:
with F and G defined as indicated above. Since W = 0 on 8D it follows that
1.J
and since the
integrand
is apositive
definitequadratic
form inW,
andW2,
it follows that
W1
andW2
vanisheverywhere,
andconsequently W3
also.Thus the
uniqueness proof
of Theoremjtfg
is carried out inelementary
classical
style.
THEOREM
M4 :
Anotherinteresting
case in which H isprescribed
at aboundary
is that of bounded surfaces with aspherical image
SZ that is ahemisphere,
and theuniqueness
within translations of such surfaces is tobe
proved.
Thisspecial
case has received agood
deal of attention in theliterature,
as waspointed
out earlier. If thegreat
circle arc that is theboundary
of D lies in theplane a;3 = 0,
1 it follows that W = .g 1 - H 2 va- nishes on every ray from theorigin lying
in thatplane,
as waspointed
outin the same situation in the
preceding
section. Thus W = 0 in theplane
s3 = 0 holds.
(This
is the main reasonwhy
this case is sospecial.)
But ifW == 0 holds for all
xl,
x2 in theplane 01533
=0,
its first derivativesWx
andW2
also vanisheverywhere
there.Consequently
bothWl
andW2,
ifnot zero
everywhere,
could be assumed to have apositive
maximum for x3 = on the unitsphere, hence
also in theplane
x3 = c. As a resultthe same discussion as was carried out on the basis of
equation (4.5),
y butwith
subscripts
1 and 2 rather than 1 and3,
would lead to aproof
ofuniqueness.
THEOREM
lVl5:
If thespherical image
S~ lies on ahemisphere
boundedby
r3 =0,
but apart
of 3~3 lies on x3 =0,
a morecomplicated
discussionis
required
to prove theuniqueness
theorem for bounded surfaces when thesupport
function isprescribed
at boundaries. The earlier discussion ofa similar case in which Green’s theorem sufficed to prove
uniqueness
wouldnot
yield
the desired result in this case since theprojection
on aplane
r3 = const
by
rays from theorigin
topoints
of SZ would result in an un-bounded domain D in the
plane 01533
=const,
and theboundary integrals
inGreen’s theorem would not
necessarily
tend to zero at oo.However,
thisdifficulty
can be overcome because the differentialequation
in thepresent
case has the
special
formfor W =
W(xl, x2)
in anyplane
x3 = const 00,
and because it is natural to make theassumption
that W - 0 uponapproaching boundary points
of S~in the
plane x3
= 0.The basic idea is to avoid
boundary integrals by introducing
an auxil-liary
C°°-functionCo(x, y)
= r2 =(xl)2 + (X2) 2,
that has the value 1 forr 1 and the value 0 for r > 2 and
integrating by parts
twice in order toget
rid ofboundary integrals altogether.
A functiony) (*)
is defined as(*) The basic idea of
getting
rid ofboundary integrals by
successiveintegra-
tion
by
parts is due to S. BERNSTEIN. Thegeneralization
of itthrough
the use of theauxiliary multiplier ~
in what follows is due to L. NIRENBERG,for a
positive
value of R. It follows that second derivativesof ~
are boundedfor R
large by const/.R2. Multiplication
of(4.10) by W~ (instead
ofW,
asin the
preceding)
and use of Green’s theorem leads toThe
integrals
are taken over apart
of the domain D that lies inside of asufficiently large
circle so that on itscircumference ~
= 0 holds andboundary integrals
vanish either because W = 0 on any boundaries in thatcircle,
y orbecause ~
= 0 on the intersection of D with it. The aboveidentity
can bewritten as follows:
The
symbols
I and J have an obvioussignificance.
I Green’s theorem is usedonce
again
withrespect
toJ,
with the resultThe limit of J when R - oo is now considered. The term behaves like
const/.R3
since(since Hii
ishomogeneous
ofdegree -1)
and’22"" l/r2,
as was noted above. Thus if W wereuniformly
bounded in theX2-plane
as R - oo the term would be such that .R2 W 2Hll’22 -+
0uniformly
as R - 00, and the same observation wouldapply
tothe other terms in the
integrand
of J. Thus for.R r C 2.R,
J -~ 0 asB -* oo.
Consequently
1 - 0 also. As aresult, since ~
= 1 in this range of r, it follows thathence W _--_ const =
0,
in case boundaries of D occur. If S~ is ahemisphere,
hence
2n,
so that D is the entireplane
x3 =const, only
W = constis
proved,
but the desireduniqueness
theorem for the surfaces results-provided
that the boundedness of W at oo is established.In the
present
case this can be done. At firstsight
it seems not reason-able since W is
homogeneous
ofdegree
one inthree-space
and hence becomeslinearly
unbounded at ooalong
rays from theorigin.
However in theplane
x3 = const. W is not
homogeneous.
The circumstance that its value on the unitsphere
is assumed to be zero where x3 =0, together
with the assump- tion(which
is nowmade)
that ~W has continuous first derivatives uponapproaching
theboundary
of SZ leads to the boundedness of W at oo in aplane x3
= const. In theaccompanying figure,
the r-axis passesthrough
aboundary point
of S~ in x3 = 0 at thepoint
in the intersection ofthe r, x3-plane
and theplane 01533
= a. It is known thate m
0-*0W(1, 0)
=0,
andW(p) =
-W((o, 0)
=0),
with O =a/sin 0.
The behaviour ofW(p)
is to beinvestigated
when8 --~ 0,
hence p - 001 Thus forW(e, 0)
theequation
holds and