A NNALI DELLA
S CUOLA N ORMALE S UPERIORE DI P ISA Classe di Scienze
K OK S ENG C HUA
Absolute gradient bound for surfaces of constant mean curvature
Annali della Scuola Normale Superiore di Pisa, Classe di Scienze 4
esérie, tome 21, n
o1 (1994), p. 1-9
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of Constant
MeanCurvature
KOK SENG CHUA
In 1977, Finn and Giusti
proved
in[5]
thefollowing
theorem:There exists an absolute constant
Ro
= 0.565406 ... and anondecreasing function A(R) for Ro
R 1 withA( 1 )
= 0, such thatif u(x, y)
is a solutionOf
~in a disc
of
radius R centered at 0,then A(R).
The main idea in
[5]
is acomparison principle,
and theA(R) occuring
inthe above theorem is the
gradient
at certainpoints
of one of afamily
of universalcomparison
surfaces: the moon surfaces whose existence has been established in[4].
TheA(R)’s
are however notexplicitly
known. In this paper weemploy
similar ideas of
comparison
as in[5] together
with afamily
ofexplicitly
knowncomparison
surfaces: afamily
of surfaces discoveredby Delaunay
in[2]
withthe aim of
giving
an upper bound forA(R).
Thisgives
us anexplicit gradient
bound in the Finn-Giusti theorem above.
In section 1 we introduce the moon surfaces and
study
the geometry ofa
particular
moon domain which is essential later. In section 2 we consider theDelaunay
surfaces: afamily
ofexplicitly
knowncomparison
surfaces ofconstant mean curvature. We are
particularly
interested in theirgradients,
whichcan be
computed explicitly.
In section 3 we obtain our main result: a form of ,the Finn-Giusti theorem with
explicit gradient
bound.1. - Moon Surfaces and the Finn-Giusti Theorem
In this section we consider the moon surface introduced in
[5],
westudy
Pervenuto alla Redazione il 15 Novembre 1990 e in forma definitiva il 21 Luglio 1992.
2
the
geometry
of aparticular
moon domain and we fix the notations. We will also recall the main result in[5]
in a moreexplicit
way.For
1/2
R 1 the moon domainDR
is the domain shown inFig. 1,
where 11 and E- are circular arcs of radius R and1/2 respectively.
The moonsurface
MR
is a formal solution overDR
ofFigure
1: The moon domainDR
such thatwhere v is the unit exterior normal.
Integrating
theabove,
we obtainand this determines the center of E-
uniquely
on the center line.We remark that the moon surfaces are all
symmetric
about thesymmetry line,
as follows fromuniqueness (see [3]).
We refer the reader to[4]
for existence and construction of the moon surfaces.We will be
mainly
concerned with aparticular
moon surfacecorresponding
to R =
Ro
= 0.565406 ... when E- passesthrough
the center 0 of 11. We referthe reader to
[5]
for the determination of the value of We will denote thisparticular
moon surfaceby
M and thecorresponding
moon domainby
D. Wewill also denote
by x
apoint
at distance x to theright
of 0 on the symmetry line of D(see Fig. 2).
We defineFigure
2: The moon domain D =D&
With these
notations,
the arguments in[5] give:
THEOREM 1.1
(Finn-Giusti).
Let R >Ro
= 0.564606 ... andy)
be aC2
solutionof
nn,
in the disc
BR of
radius R centered at 0; thenWe
strongly
urge the reader to read[5]
for aproof
of the above theoremas it also contains the main idea of this paper in a different context.
4
The main purpose of this paper is to
give
anexplicit
upper bound for the above functionA,
thusgiving
anexplicit gradient
bound in the Finn-Giusti theorem.Now we discuss some
geometric properties
of the moon domain D(see Fig. 3)
which we willrequire
later.LEMMA 1.2. Let R E PO be such then
Figure
3: Illustrationof
Lemmas 1.2 and 1.3PROOF. We first note that T > 0152 since
Ro
>1 /2,
so that thepoint
R existsbetween P and O.
Clearly
d= ~ PR ~
= cos T =1-2R5 by
the cosine ruleapplied
to the isosceles
triangle
V RP ..LEMMA 1.3.
If
0 x d the circleof
radius1 /2
centered at thepoint
Sat distance x to the
right of
P intersects theboundary of
D in ~+(.see Fig. 3).
PROOF. This is clear for small
positive
x. As xincreases,
the circle intersects ~- when it passesthrough
thepoints
V and w. This occurs when thecenter is at R with VR =
1 /2
and PR = d..The
key
fact on which our method is based is thefollowing:
LEMMA 1.4. Let 0 x d and c =
1/2 - Vl/4 - xed -
x). The annulus A,placed
over D so that its center S is at distance x to theright of
P intersectsthe
boundary of
Dentirely
in E+(see Fig. 4).
Figure
4: Illustrationof
Lemma 1.4PROOF.
By
Lemma 1.3 the circle of radius1/2
does not intersect I- sothat the
configuration
ispossible
for someAc.
Thelargest possible
suchAc
musthave inner
boundary passing through
V and W. The inner radius is thereforedetermined from the
triangle
PSVby
the cosinerule,
and it is~1 /4 + x2 -
xd..
2. -
Delaunay
Surfaces: the UnduloidsIn this section we construct an
explicitly
knownfamily
of surfaces of constant mean curvature which will serve ascomparison
surfaces togive
us6
explicit
upper bounds for A. These surfaces were discoveredby Delaunay
in1841.
Delaunay
in[2]
showed that if one rolls anellipse along
a line L, theneach focus generates a curve which when rotated about L
gives
arotationally symmetric
surface of constant mean curvature H. If the center of theellipse
isat distance
1/2
from L then H = 1. We consider asingle period
as shown inFig.
5.Figure
5:Delaunay surfaces
The
defining height
function then satisfies:on a circular annulus
Ac: 1 /2 - c r 1 /2 + c
and itpoints vertically upwards
on the outer curve r = rb =
1 /2 + c
andvertically
downwards on the inner curver=7-a=l/2-c(0c 1/2).
As c tends to 0 this surface tends to a finitepiece
of a verticalcylinder,
while as c tends to1/2
itapproaches
a lower unithemisphere.
If 0
is theangle
ofinclination,
we haveanalytically
which
gives
This
equation
admits a firstintegral
Thus and
the
positive sign
holds when r exceeds the inflexion(ri,
whereIf r ri the
negative sign
holds. The inclination achieves a minimum at ri. We haveWe have thus shown:
LEMMA 2.1. For each c with 0 c
1/2
there exists arotationally symmetric surface Uc of
constant mean curvature 1defined
over an annularregion Ac : 1/2 -
c r1/2
+ c withoutward-pointing gradient.
The minimumof
thisgradient
is attained at ri1 /2 from
the center, and it isWe note that me decreases
monotonically
frominfinity
to 0 as c increasesfrom 0 to
1/2.
8
3. - An
Explicit
Gradient BoundIn this section we obtain an
explicit
form of the Finn-Giusti theorem. The main idea is that we are able togive
anexplicit
upper bound for the function A in Theorem 1.1by comparing
the moon surface M with theDelaunay
surface~7c for a suitable value of c and then
applying essentially
the same argumentsas in Lemma 1.1 of
[5].
Moreprecisely,
we have thefollowing:
THEOREM 3.1. Let Then
PROOF.
By
Lemma 1.4, for thegiven
values of x and c, one canplace A,
over Dsymmetrically
in such a way that the intersection of A, and D doesnot meet I-
(see Fig. 4).
IfA(x) =
0 there isnothing
to prove.Otherwise,
the symmetry of M and the fact that it
points vertically
downwards as itapproaches
I-implies
that thegradient DM(y)
mustpoint
to theright (in
thesame direction as
DUe)
for 0 y x. Let T be thepoint
of Dcorresponding
to the
point
ri ofAc.
It suffices to provethat
me since T comesbefore x
along
the symmetry line(recall
the definition ofA).
If, by contradiction, IDM(T)I
> mc, the intermediate value theorem im-plies
that there exists apoint z
on the symmetry line such thatDM(z)
=DUc(z) (recall that ¡DUel
is infinite on the innerradius).
Now weapply
the same ar-gument as in Lemma 1.1 of
[5]
to obtain a contradiction. We note that Mapproaches
a finite limit for anyapproach
to E+(see [4])
so that the function7y used in the
proof
of Lemma 1.1 of[5]
can be defined. It is not difficult toshow that the arguments of
[5]
can be carried out, and we have a contradiction.COROLLARY 3.2. Let Then:
PROOF. Since me is
decreasing
in c, we maximise c and it iseasily
seenthat this occurs at c = co
corresponding
to x =d/2.
Since A isdecreasing
wehave,
for x >d/2,
We now combine Theorem
3.1, Corollary
3.2 and Theorem 1.1 to obtainour main result:
THEOREM 3.3. Let R > Ro = 0.565406 ... and
u(x, y) be a C2
solutionof
div T u = 2 in a disc
of
radius R centered at 0.If
thenOtherwise let ; and set
then:
REMARKS. It is
possible
to obtain aslightly
better result than that stated above since we knowexactly
thepoint
of minimumgradient
of theDelaunay
surfaces.
However,
even in theimproved form,
we are not able to obtain thesharp
bound which wouldimply
thatDu(O)
vanishes as R tends to 1. We havethus
preferred
the above theorem which issimpler
to state. Thesharp
boundwould be obtained if one could prove that
DM(x)
vanishes at somepoint;
butunfortunately
we have not been able to do this. Our main contribution is that anexplicit gradient
bound in the Finn-Giusti theorem asgiven
above ispossible.
REFERENCES
[1] R. COURANT - D. HILBERT, Methods of Mathematical Physics, Vol. II. Interscience Publishers, New York, 1962.
[2] C.E. DELAUNAY, Sur la surface de revolution dont la courbure moyenne est constante.
J. Math. Pures Appl. 6 (1841), 409-415.
[3] R. FINN, Equillibrum Capillary Surface. Springer-Verlag, New York, 1986.
[4] R. FINN, Moon surfaces and boundary behaviour of Capillary surfaces for perfect wetting and non wetting. Proc. London Math. Soc. 57 (1988), 542-576.
[5] R. FINN - E. GIUSTI, On nonparametric surfaces of constant mean curvature. Ann.
Scuola Norm. Sup. Pisa 4 (1977), 13-31.
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