R ENDICONTI
del
S EMINARIO M ATEMATICO
della
U NIVERSITÀ DI P ADOVA
J OST -H INRICH E SCHENBURG
R ENATO DE A ZEVEDO T RIBUZY
Constant mean curvature surfaces in 4-space forms
Rendiconti del Seminario Matematico della Università di Padova, tome 79 (1988), p. 185-202
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4-Space
JOST-HINRICH ESCHENBURG
(1) -
RENATO DE AZEVEDO TRIBUZY(2) (*)
1. Introduction : constant mean curvature in
3-space.
Consider the
following
classical theorems about constant mean curvature surfaces in euclidean3-space:
THEOREM
(a) (Ricci) [2, 12].
Let(.1~2, ds2)
be asimply
connectedsurface with Gaussian curvature 2L Then there exists an isometric immersion
f :
M -* R3 with constant mean curvature H without um-bilic
points
if andonly
if .H2 > .K and the metric _(H2 - .K)~ ds2
is flat.
THEOREM
(b) (H. Hopf) [9].
Let ~2 be a closed surface with Eulercharacteristic X
and an immersion with constant meancurvature. Then either is a round
sphere
or2x
= - N where Nis the number of umbilic
points,
counted withmultiplicities.
REMARK.
Hopf
does not stateexplicitly
this theorem butonly
its
corollary:
Atopological sphere
of constant mean curvature is round([9],
Ch.VI, 2.1). However,
the moregeneral
statement canbe read off from
VI, 2.3.,
p. 139: In the non-umbilic case thesingular-
ities of the
principal
linefields,
i.e. the umbilicpoints
are isolated andof
index j
= -n/2
where n is the order of the umbilicpoint (see below).
(*)
Indirizzodegli
AA.: J.-H. ESCHENBURG: Mathematisches InstitutMemminger
Str. 6, D-8900Augsburg,
WestGermany;
R. DE AZEVEDOTRI-BUZY :
Departamento
de Matemática, Universidade do Amazonas, 69000 Ma-naus, A.M., Brasil.
(1)
Partially supported by CNPq,
Brasil.(2)
Supported by CNPq,
Brasil, and GMD,Germany.
This
implies
Theorem(b) by
thePoinear6-Hopf
index theorem whichwas discussed before
([9],
Ch.III, 2.2).
At first
sight,
the two theorems seem to be unrelated since in(a)
the umbilics are
excluded,
in(b) they
are counted. But it turns out that asharpened
version of(a)
in factimplies (b).
To seethis,
we mustextend the local characterization of minimal surfaces
given
in(a)
to the umbilic
points.
First observe that the flatness of a metricd§2 = a ds2 is
expressed by
the differentialequation
where 4 is the
Laplacian
withrespect
to the metric ds2.Unfortunately,
in
general
the left hand side is undefined at the zeros of thefunction a,
and the zeros of a =
(H2 - K)i
areprecisely
the umbilicpoints.
How-ever, y for a certain
type
of zeros theexpression d log a
makes stillsense:
DEFINITION. A function
a : M --~ [o, oo)
on a surface(M, dS2)
is called of absolute value
type (A VT)
if everypoint
in M has aneigh-
borhood U such that a = on U where cco is smooth and
positive
and hoz-1 is
holomorphic
for some conformal coordinate z: U- C.Here, conformal
means that ds2 = £2 dzdi for somepositive
func-tion A,
calledconformal factor.
Note that then d = 4A-2a~ 8, .
If an absolute value
type
funct ion a does not vanishentirely
its zeros are
isolated,
and around each zero we have4 log a
=d log
a.which is still defined and smooth at the zeros. The order
ord, (a)
of aat a zero p E M
is, by definition,
the order of itsholomorphic part
h at p. If M is a
compact surface,
we define the number of zeros of a(with multiplicities)
to beThen we
get
as an easy consequence of thedivergence
theorem(see [7], 4.1 )
LEMMA. 1. Let
(M, d~2)
be acompact
surfaceand a 1
0 an AYT function on M. ThenREMARK. One may
generalize
the notion of A V T functionsby allowing
theholomorphic part h
to havepoles.
Then the lemma is still correct withN(a)
= number of zeros - number ofpoles.
Now we can
give
thesharpened
version of Ricci’s theorem(a)
for any
3-space
form of constant sectionalcurvature c, Q~ :
THEOREM 0. Let
(M, ds2)
be asimply
connected surface with Gaussian curvature g. Then there exists an isometric immersionf : M -~ Q~
with constant mean curvature .H if andonly
if c+
H2and a:=
(c +
H2 -K)i
is A VTsatisfying
0 and
f
istotally
umbilic. Infact,
there isexactly
a one-parameter family
of suchimmersions,
up to local congruence.Of course, for the «
only
if »part
we do not have to assumesimple connectivity. By
local congruence we mean that the lifts to the universal cover3
arecongruent.
This theorem has been stated
by
Lawson[12],
butavoiding
um-bilic
points. However,
forglobal applications
the umbilicpoints
areessential as we saw. In
fact,
from Theorem 0 and Lemma 1 weget immediately
Theorem(b), using
the Gauss-Bonnet theorem:COROLLARY. Let M be a
compact
surface and an im- mersion with constant mean curvature .H~. Then eitherf
istotally
umbilic or
where X
is the Euler number of M and a =(c +
H 2 -K)I.
Notethat the zeros of a are
precisely
the umbilicpoints,
yby
Gauss equa- tions.As a consequence, y a
topological sphere
of constant mean curva- ture inQ’
istotally
umbilic. This is well known: SeeAlmgren [1]
and Calabi
[4]
forQl c
= S3 and Chern[6]
forgeneral
space forms.Theorem 0 turns out to be a
special
case of a theorem in dimen- sion 4 which we will discuss in the next two sections. But the theo-rems and
(b)
stated at thebeginning
may serve as a model case aswell: Local characterization in terms of curvatures leads to
global
results. In the
present
paper we want to carry out this program for minimal surfaces in4-space
of constant sectional curvature(see
also[7]
for the case of constant
holomorphic curvature).
We wish to mention thateverything
can be done for branched immersions as well whichwe will discuss in a
subsequent
paper(*).
Part of this work was done while both. authors were
visiting
theFederal
University
of Ceara atFortaleza,
Brasil. It was finishedduring
the visit of the second author at the
University
ofMiinster, Germany.
We wish to express our thanks to these universities for their
hospitality
and to
CNPq
and GMD for financialsupport.
2. Constant mean curvature in
4-space.
In the
following sections,
y letQ’
be any 4-dimensional space of constant sectional curvature c and(M, ds2)
a surface with Gaussian curvature g which isalways
assumed to besimply
connected if weclaim existence of an immersion. One way of
carrying
over the notionof constant mean curvature surfaces to
4-space
is theassumption
ofparallel
mean curvature vector: Iff : M -~ Q~
is an immersion with2nd fundamental form
«(z, y)
==(Dx y)1, then q : = 2
trace oc is calledthe mean curvature vector
field,
and this is calledparallel
if it is aparallel
section of the normalbundle,
i.e. = 0.THEOREM 1. There exists an isometric immersion
f :
withparallel
mean curvature vector oflength
H > 0 if andonly
if I~~ c
+
.H’2 and a : _(c +
.H2 -K)l
is AVTsatisfying
In
fact,
up to local congruence, y there isexactly
atwo-parameter family - ~c
C1,T ~ ’JT,
of such immersions.REMARK. It is known
by
Yau[17]
that a surface of nonzeroparallel
mean curvature vector
always
lies in atotally
umbilichypersurface Q~. c Q~
with constant mean curvature H’=(H2 - (c’ - c))l,
for somec’ > c.
Therefore,
Theorem 0 and Theorem 1 areessentially
the same.The two
parameters
a and T are easy toexplain geometrically:
Oneparameter 7:
is obtainedby rotating
the second fundamental form in thetangent plane,
i.e.replacing
oc withwhere Rt
is the rotationof
angle
T. The otherparameter
a arises as theangle
between the (*) J.-H. ESCHENBURG and R. TRIBUZY, Branchpoints of conformal
map-pings of sur f aces,
Math. Ann., 279(1988),
pp. 621-633.normal vector of
Q:,
inQ:
and the mean curvaturevector n
in thenormal
plane
of M inQ~ .
In otherwords,
we have(Observe
that(c’- c)k
is the mean curvature ofQ’,
inQ").
Infact,
wesee that for
fixed Icrl,
theimmersions fct
allbelong
to the sametotally
umbilic
hypersurface Q’,,
up to local congruence, and that is con-gruent
to under a reflection inQ~~ .
There is
yet
another way ofgeneralizing
the notion of constantmean curvature to
higher codimension, namely by only assuming
that
]]
= .8’ = const. S. T. Yau hasinvestigated
this situation[17].
In
particular
he claimes: If .M isdiffeomorphic
to asphere,
thenany immersion
/:~f2013~(~
withII
= const > 0 istotally
umbilic.However,
9 hisproof
relies on the claim that for any surface withII
=const,
like in the minimal caseII =0,
thequartic
form~)=~’(~~)~2013~’(~J~)~ where
J denotes the 90 °-rotationon M is the real
part
of aholomorphic quartic form;
here we leta’(x, y)
:=a(x, y) - x,
the trace freepart
of the 2nd funda- mental form a. We will showby
acounterexample
that ingeneral
this is wrong
(see Appendix).
So thequestion
remains open whether there exists a non-trivial immersion of S2 intoQ§
withII
- const ~ 0.3.
Minimal
surfaces in4-space.
In this case, as a new
ingredience
we have the normal curvature which is defined as follows. Letf : M --~ Qc
be any isometric im- mersion. Let DN be the induced connection on the normal bundle NM and .RN its curvature tensor. Then RN is determinedby
asingle function,
called normalcurvature,
where and
(el,
e2, ea,e4)
is an oriented orthonormal basis of ei , e2tangent
and e~ normal.( T M
and NM arealways
considered as subbundles of
f* TQ’.)
Thus.gN
can be definedonly
if the bundle
f*TQ§
over M is orientable. If the mean curvaturevector ?7
isparallel
and non-zero, theplane
bundle NM has aparallel
section and hence = 0. But now we consider minimal
surfaces,
i.e. immersions
with q =
0. Then it follows from Gauss and Ricciequation
thatwith
equality exactly
at thosepoints
p E M where the so calledellipse of
curvaturein
N l’ M
is a circle(see
ch.4);
thesepoints
are called circular(or
semi-umbilic).
A minimal immersion is calledsuperminimal
if everypoint
is circular.
THEOREM 2. Let M-~ R be a smooth function
satisfying (3).
Then there exists an isometric minimal but not
superminimal
immer-sion
f : ..1V1-~ Q~
with normal curvatureKv
if andonly
if the func- tions at :_(c -
are AYT withIn
fact,
up to local congruence, there isexactly
aone-parameter family
- x
~ ~~
of such immersions.’
This theorem was obtained in
[16]
under theassumption IKNI
c - K and no circular
points.
If M is closed and oriented with oriented normal
bundle,
the Gauss-Bonnet-Chern-Weil theorem
gives
the Eulernumber XN
of the normal bundle:Hence
integrating (2)
andusing
Lemma1,
weget immediately:
COROLLARY. Let M be a closed oriented surface and
f :
if -*Q"
a minimal but not
superminimal
immersion with oriented normal bundle. Then weget
and in
particular
where
Recall that
N(a+ a_)
is the number of circularpoints (counted
withmultiplicities).
One mayinterpret (6)
as follows: At anyp E M
considerthe
longest principal
axis of theellipse
of curvature Since themapping x) :
hasdegree two,
there areexactly
four vectors with
xi) II
maximal. This defines a field of twoperpendicular
lines outside the circularpoints,
y and in the circularpoints
the index of this two-line field is -ordp (a+a_) (see [8]).
Thus we may
get (6)
from thePoincare-Hopf
index theorem. Thisargument
is very similar toHopf’s proof
of Theorem( b ) (see
ch.1).
In
particular
it follows from(6)
that a minimalsphere
inQ"
isalways superminimal
which wasproved
firstby
Calabi[4]
and thata minimal torus is either
superminimal
or has no circularpoints
at all.Now consider
superminimal
immersions inQ~.
For these we haveand the
following
intrinsic characterization:THEOREM 3. There exists an isometric
superminimal
immersionf : M --~ Q~
which is nottotally geodesic
if andonly
if c and thefunction a : =
(c - Kl’
is withEquation (7)
was known to Calabi[4].
The theorem was obtainedby Tribuzy
andGuadalupe [16]
in the case K c(i.e.
nopoints
forwhich a
vanishes).
For c =0, Q ~
==11~4,
the theorem shows that thesuperminimal
immersions areexactly
those which areholomorphic
with
respect
to a suitableisometry
between R4 andC2,
andthey
arealso
totally
real withrespect
to another suchisometry (see 3.6,
3.8and the
concluding
note in[7]).
For c =1, Q4 = ~54,
we see that thereis
only
onesuperminimal
immersion of constant curvature which is nottotally geodesic, namely
the Veroneseembedding
of RP2 with .K =3.
The
superminimal
surfaces in 54 have beeninvestigated by
R.Bryant ([3],
see also[10]).
As a
global
consequence of(3), (3’)
and Theorem 3 weget
immedi-ately
a theorem ofRodriguez
andGuadalupe [13]:
COROLLARY
(see [13]).
Let M be a closed oriented surface andf :
a minimal immersion with orientable normal bundle. Thenwith
equality
if andonly
iff
issuperminimal.
In this case we havewhere a =
(c
-unless f
istotally geodesic.
Recall that
N(a)
counts the number oftotally geodesic points (a
=0)
withmultiplicities.
One consequence of this
corollary
is a theorem of E. Ruh[14]:
A minimal
2-sphere (which
has to besuperminimal
as wesaw)
with trivial normal bundle(xN
=0)
istotally geodesic. E.g.
it is well knownthat
xN = 0
for an embedded oriented closed surface in S4( [11],
Cor.
3.2);
hence an embedded minimalsphere
in S4 is agreat sphere.
4. Structure
equations
of surfaces in4-space
forms.Let be a surface and an immersion. Let
(el,
e2, e3,e4)
be a Darboux framealong f ,
i.e. an orthonormal frame with et, e2tangent
e4normal,
and which is understood to be oriented if orientations of and NM aregiven.
Then the 1-forms on M1 a, b 4, satisfy
= (t)4 =0,
COab = - COba and the Cartan struc-ture
equations
and the induced metric is ds2
= C02 + C 1)2.
Vice versa, if 1-forms coab with theseproporties
aregiven
on asimply
connected surface .D~l and if thequadratic
form ds2 =+ co2
isnondegenerated,
there existsan immersion
f : .~--~ Q~
with Darboux frame ei , ..., e4 such that Wa,are the
corresponding 1-forms,
and this immersion isunique
up to local congruence(e.g.
seeSpivak [15]).
We will call two immersionsf , ,~ : .~C --~ Q~ locally congruent
if their lifts to the universal cover4
are
congruent.
where we assume
always i,
Then we have
Now we
put
Note that the mean curvature vector so
11 nil ||
-The functions
kj:
areclosely
related to theellipse
of curvature which consists of the normal vectorswhere c = cos = sin r for
arbitrary angles
r. Thisellipse
is a circleif and
only
if(x’ (el, e1 )
and(X( e1, e2 )
areperpendicular
and of the samelength,
i.e. iffl~+
= 0 or l~_ - 0 at theparticular point.
Now we introduce the
complex
valued 1-formsThen one
easily
checks that the Cartanequations (C)
areequivalent
to the
following
set ofequations:
REMARK. Under the usual
isomorphism
of the Liealgebra
~’0(4)
onto the Lie
algebra
the connection form co ==(Wab)
ismapped
onto thepair
where
(i, ~, ij)
is the usual basis ofSp (1),
viewed as the space of im-aginary quaternions.
Theequations (9)-(12)
arejust
a translation of(0)
into the Liealgebra (compare [10]).
Moreover,
from the structureequations
of the bundles TM and with induced connections we haveHence
together
with(11)
and the definition of the "PI weget
where H ’ °
1Ir¡11
_In
particular,
the immersion is minimal if andonly
if ’ijJ+ and Y -are
(1, 0)-forms,
i.e.multiples
of q. Note that for any conformal co- ordinatepreserving
the orientationgiven by (e1, e2),
wehave q
= for somecomplex
valued function Iz. Since ds2 =990
=- so is the conformal factor.
The mean curvature vector field is
parallel
if andonly
ifhence
So
by (9),
this isequivalent
to =Or,
in otherwords,
the(1, 0)-form
the
(1, 0)-part
of "PI’ satisfiesIt is easy to check that for an
arbitrary immersion ,
an oriented surface the
quartic
formis
independent
of the choice of the Darboux frame and henceglobally
defined. In
fact,
its realpart
is~R(x) _ x) ~~ 2 - II oc’ (x, JX) 11 2
where J denotes the almost
complex
structure on M. If the immersion hasparallel
mean curvature vector oflength
.H >0,
this form is holo-morphic : if 99
=P, dz
for some conformalcoordinate z, putting
we
get
and from(9)
and
(12’):
Therefore,
which shows that is a holo-morphic
function. IfH # 0,
thisquartic
formsplits
as 0 ==where are
holomorphic quadratic
forms: We may choose in thiscase e3 = then e4 are
parallel
in the normal bundle. So Wa4 vanishes and hence the 2-forms~t : =
areholomorphic quadratic forms,
yby
a similarargument
as above.5. Proof of the theorems.
The link between the structure
equations (9)-(12)
andequations ( 1 ) , (4), (7)
isgiven by
thefollowing
lemma which isessentially
an easyspecial
case of a theorem of Chern[5].
Let(M, ds2)
be a surface. Acomplex
valued function p on M will be called ofholomorphic type
if
locally p
= po pl with po smooth and nowherevanishing
andholomorphic
for a suitable conformal coordinate z onClearly
then
Ipl
is an AYT function.LEMMA 2. Let p be a smooth
complex
valued function onM,
and (o a real valued 1-form on M. for some con-
formal coordinate z. Then the
equality
is valid if and
only
if p is ofholomorphic type
andMoreover,
thenREMARK. Note that
az log p
and4 log (p) I
are well defined evenat the zeros of p, if p is of
holomorphic type.
PROOF
(see [7]).
Since w isreal,
we have co = b dz+
for somecomplex
function b. Thus(*)
isequivalent
to the differential equa- tion for p:Let u be a solution of the
inhomogeneous Cauchy-Riemann equation az u = ib
andput
po := eu. Then po is a nowherevanishing
solutionof
(* *).
If p is any other solution of( ~ ~ ),
then is holo-morphic.
So p is ofholomorphic type
and(**)
isequivalent
tob = and hence to
(17). Differentiating (17),
weget (18).
(a)
The localequations (1 ), (4), (7).
Now let(M, ds2)
be a surfaceand
f :
an isometric immersion withparallel
mean curvaturevector field of
length
H > 0.Let e1,
... , e4 be a Darboux framealong f .
Then we may
apply
Lemma 2 to the forms ’ijJ:t = = re-placing (*)
with(12’).
So the functionis A VT
(since ¡,ul
_ ~ >0),
and if0,
weget
from(18)
since
4 log £
_ - g(which
also follows from(18), using (9)
and(13)).
On the other
hand,
weget
from(13)
and(14)
and
theref ore,
If
0,
the form W34 is exactby (16)
and therefore2~
=0, by (14);
so we
get (1).
If .H’ =0,
weget (4).
If a+a_ = 0 then either a+ n 0or a_ - 0 since a+, a- are both A VT. If a+ = a_ -
0,
the immersionis
totally
umbilic(i.e.
a’=0),
hencetotally geodesic
if .H’ = 0. Ifa- =
0, a+ =F 0,
we have H = 0(since
otherwise a+ =a_)
and there-fore
KN==c-K and ~ == (2(c2013 ~))~
andsimilarly
if a+ =0,
a_ ~ 0. This proves
(7).
(b) Uniqueness.
Let beoriented, Qc simply
connected and two isometricimmersions,
y both with the same normal curvatureKN
and withparallel
mean curvature vector field oflength H >
0. Assume thatf , f
induce the sameholomorphic quartic
form 0on .M. If
H # 0,
assume further that also0+
and0-
are the same forboth immersions. We claim that then
f == got
for some orientedisometry
of’
In
fact,
in case0,
the 1-forms ’ijJ+, are the same for bothimmersions,
so are the sameby (12’)
and hence the immersions arecongruent.
In case .g =0,
7 let e, 7 e4 and ei, 7 e2 , 7g3
7j,
be local oriented Darboux framesalong f
andf
resp.(We
consider TM as asubbundle of
f * TQ
and Then we have==
,k+ 1~-=1~+ k-,
and therefore
f or some real function i.
Rotating
the normal frameof f by
thisangle
7:,we
get 1pi:: ==
1Jli:: for this new frame. Asbefore,
weget
andso
f
andI
arecongruent.
In both cases, theisometry g
ofQf taking
f to f preserves
the orientation of both thetangent
and the normalbundle,
so it is oriented.REMARK. In
fact,
it is not necessary to assume thatKN =KN.
We have
~_~_==(c2013-Er)~2013-B~
and we have_ ~.KN .
In case.KN
the immersionf
andI
diff erby
anorientation
reversing isometry. Similar,
in the case0,
it isonly
necessary to assume
that 4% = W
andy~3
= where e3,e3
arepointing
in the direction of the mean curvature vector.
(c)
Existence. Let(M, dS2)
be asimply
connectedsurface,
some number and
KN
a function which is zero if H >0,
suchthat
is A VT
satisfying
unless a+ n 0. Let U c M be an open disk and z : t7-~ C a conformal coordinate. Choose an oriented orthonormal basis e1, e2 on U. Put Wi
= ~ , ei~ and
= WI+ Then =,udz
withjyj
_ ~, the con-formal factor.
By (17)
we have(recall
that4 log £ = 2013 .K).
Since b:_ ~,4a+a_
isA VT,
there existsa
holomorphie function g
with b =lgl (see [7], 3.12).
In fact we haveb =
bolhl I
with hholomorphic
andbo > 0
andd log bo
= 0. Solog bo
is the real
part
of aholomorphic
function 1 and thus g el - h is holo-morphic with lgl
= b. Infact, g
isuniquely
determined up to a con-stant factor ei7:. Choose any such g. Let
k+, k-
be functions of holo-morphic type satisfying Ik:i:1 == a:i:
and andput
"Px ===
+ Hip.
Then(10)
isautomatically
satisfied. Tosatisfy (12’)
and hence
(12), according
to Lemma 2 we have toput
whenever := is not the zero function. Then we have
On the other
hand,
this proves
Equation (11). Finitely, put
Since 99
= ,udz,
weget by
Lemma 2and hence
W12
= W12; Thus(9)
is satisfied.It remains to consider the case
a+ a_ = 0
whichimplies
H = 0.If a- =
0,
that meansJE~ -~-
K = c, weput
"P+, w- as above and1Jl- = 0,
= w_. Then co- still satisfies(11)
and henceas before.
Therefore,
and hence satisfies
(11). Equation (12)
is valid for co-, asbefore,
and it is trivial for
(9)
is satisfiedby
definition of W12(as
anintrinsic
quantity).
If instead a+ =
0,
we arguesimilarly replacing +
with -. Ifboth a+
and a- are the zerofunctions,
i.e..K = c,KN - 0,
weput
1JJ+ = 1JJ- =0,
(0+ = co- = C012, andEquations (9)-(12)
are satisfied.Thus, by
thegeneral
existencetheorem,
weget
an isometric im- mersionf : U --~ Q~
withparallel
mean curvature vector oflength
H(since (12’)
issatisfied), together
with a Darboux frame e1, ... , e4along f .
Infact,
we recover anyquartic
form 0 and in the case 0 any twoquadratic
forms0+
10-, holomorphic
withgiven
absolutevalues, by choosing
the functions g,1~+,
7 7~_suitably.
Now cover if
by
open coordinate ballsUi .
Then weget
immersionsf t :
Choose these so that thecorresponding quartic
orquad-
ratic forms agree in the intersections
Ut
nU~. By simple connectivity
of
M,
this can be achieved. Then forsome proper motion g of
by
theuniqueness part (b). Thus f
andtogether
define an immersion ofUt
uUs . Continuing
this process,we
get
an immersionf:
with the desiredproperties.
It remains to
verify
the remarkfollowing
Theorem 1. Ifis an immersion with
parallel
mean curvature vector oflength 0,
the
holomorphic quadratic
forms0+
andø -
have the same absolutevalues
Ik+1
-Ik-I
-(c -~-
H2 -K), .
Sothey
diff erby
a constantfactor of unit
length: Say
gg+ =Hence ’
= andput-
ting
:= y~a -haip (see
ch.4),
weget
V+ = e
In other
words,
theparallel vector $ : = - (sin ~) e3 -~- (cos ~) e4
isumbilic,
i.e.~~
= 0(compare [17]).
It is easy to see([17]),
thatlies in a
totally
umbilichypersurface Q’ c
inQ~
with normalvector ~.
Thus a:=
ni2 -~--
ð is theangle
between the mean curvature vector 17 =He,
and$.
On the other
hand,
iff , f :
are isometric immersions withparallel
mean curvature vector oflength
H > 0with |O| = |O| 1
and1p+/ip-
=then
=e4Ti ø
for some constantangle
í. Hencey~t
= and so a= .R.*
a whereRT
denotes the rotationby i
inthe
tangent plane.
Appendix:
Mean curvature vector of constantlength.
We want to
give
anexample
of a surface in4-space
whose meancurvature vector has constant
length
but whosequartic
form 0(see
~ch.
4)
is notholomorphic (compare
ch.2).
Put e :
R2013~C, e(t)
= eit. Consider the immersionf :
IxJ C2 =R4, j(s, t)
==(e(s), g(s) e(t))
whereI,
J are open intervals and g: 1 ->(0, oo)
some smooth function. Let
f,
denote thepartial
derivatives. We havef
t and(1 + g’21’
= :h, ]]
= g. Let usput
this is a Darboux frame for the immersion
f .
For the 2nd fundamental form a weget
in terms of this frame:Therefore,
the mean curvature vector hasconstant
length
if andonly
ifOn the other
hand,
thecorresponding quartic
form iswith
and
= ccy-E- iw2
where Wi _d f,
Nowputting
du = dswe have and so
(u, t)
is a conformal coordinatesystem
for the metric on I X J inducedby f,
with conformal factor g.Since its coefficient function is is
holomorphic
if andonly
if(k 3 2+ k4 ) g4
=const,
hence iffSince h2 =
1 + g’ 2, Equations ( A1 )
and(A2)
are~2nd
order differentialequations
for g. Sincethey
areindependent,
y one finds afunction g
which solves
(A1)
but not(A2).
To be
specific,
let e1 = 5 and consider thesolution g
ofwith initial values
Then g solves also
(A1 ),
and it follows from(A1’ ) that g
is even withg"(0)
=3, g~4~(o)
= 78.Instead,
from(A2)
we wouldget g(4)(0)
=72,
so g does not solve
(A2).
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