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c 2015 by Institut Mittag-Leffler. All rights reserved

Monotonicity formula for complete hypersurfaces in the hyperbolic space and

applications

Hil´ario Alencar and Greg´orio Silva Neto

Abstract. In this paper we prove a monotonicity formula for the integral of the mean curvature for complete and proper hypersurfaces of the hyperbolic space and, as consequences, we obtain a lower bound for the integral of the mean curvature and that the integral of the mean curvature is infinity.

1. Introduction and main results

Let Hn+1(ˇ) be the (n+1)-dimensional hyperbolic space with constant sec- tional curvatureˇ<0. The main result of this paper is the following

Theorem 1.1.(Monotonicity) Let Mn, n≥3, be a complete and proper hy- persurface of Hn+1(ˇ) with mean curvature H >0. If there exists a constant Γ0 such that scalar curvatureRsatisfiesˇ≤R≤nΓ1H+ˇ,then the functionϕ:R→R defined by

ϕ(r) = eΓ2r (sinh

−ˇr)n−12

MBr

(sinh

−ˇρ)H dM

is monotone non decreasing, whereρ is the geodesic distance function of Hn+1(ˇ) starting at p∈Hn+1(ˇ) and Br=Br(p) denotes the geodesic open ball of Hn+1(ˇ) with centerp∈Hn+1(ˇ)and radiusr. Moreover,if Γ<(n3)

−ˇ,then

M

H dM=∞.

Hil´ario Alencar was partially supported by CNPq of Brazil.

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The monotonicity of Theorem 1.1above implies the following estimate for the in- tegral of mean curvature:

Corollary 1.2. Let Mn, n≥3, be a complete and proper hypersurface of Hn+1(ˇ) with mean curvature H >0. If there exists a constant Γ0 such that the scalar curvature Rsatisfies ˇ≤R≤nΓ1H+ˇ, then

MBr

H dM≥(sinh

−ˇr)n−32 r

r0

CeΓ2τ

for allr>r0, whereC=C(r0, M, p) is a constant depending only onr0, M and p.

Remark 1.3. In this direction, we can cite the following result of H. Alencar, W. Santos and D. Zhou, see [3], proved in the context of higher order curvatures, whose version for mean curvature we state below.

LetMn+1(ˇ) be an (n+1)-dimensional, simply connected, complete Rieman- nian manifold with constant sectional curvature ˇ, and let Mn be a complete, noncompact, properly immersed hypersurface ofMn+1(ˇ). Assume there exists a nonnegative constantαsuch that

|R−ˇ| ≤αH.

If P1=nHI−A is positive semidefinite, where I:T MT M is the identity map, then for anyq∈M such thatH(q)=0 and anyμ0>0, there exists a positive constant C, depending only onμ0, qandM such that, for everyμ≥μ0,

MBμ(p)

H dM≥ μ

μ0

Ceατdτ,

whereBμ(p) is the closed ball of radius μand center q∈Mn+1(ˇ). In particular, if ˇ≤0,R=ˇ,H≥0 andH≡0, then

MH dM=.

Acknowledgements. The authors would like to thank the anonymous referee for his/her valuable comments.

2. Preliminary results

Let Hn+1(ˇ) be the (n+1)-dimensional hyperbolic space with constant sec- tional curvatureˇ.

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LetA:T MT M be the linear operator associated to the second fundamental form of the immersion. The first Newton transformationP1:T MT M is defined by

P1=nHI−A, whereI: T MT M is the identity map.

Notice that, sinceA is self-adjoint, thenP1 is also a self-adjoint linear opera- tor. Denote byk1, k2, ..., kn the eigenvalues of the operatorA, also called principal curvatures of the immersion. SinceP1is a self-adjoint operator, we can consider its eigenvaluesλ1, λ2, ..., λn given byλi=nH−ki,i=1,2, ..., n.

If H >0 and R≥ˇ, then P1 is semi-positive definite. This fact is known, and can be found in [1], Remark 2.1, p. 552. We include a proof here for the sake of completeness. IfR≥ˇ, then (nH)2=|A|2+n(n1)(R−ˇ)≥k2i, for alli=1,2, ..., n.

Thus 0(nH)2−ki2=(nH−ki)(nH+ki) which implies that all eigenvalues ofP1are non-negative, providedH≥0, i.e.,P1 is semi-positive definite. Let us denote by andthe connections ofHn+1(ˇ) andM, respectively. In order to prove our main theorem we will need the next two results.

Lemma 2.1. Letx: Mn→Hn+1(ˇ)be an isometric immersion,ρ(x)=ρ(p, x) be the geodesic distance function of Hn+1(ˇ) starting at p∈Hn+1(ˇ), and X=sinh−ˇρ

−ˇ ∇ρ the position vector of Hn+1(ˇ), where ∇ρ denotes the gradient ofρ onHn+1(ˇ). Then, for everyq∈M,

tr

E−P1

(EX)T

(q) =n(n−1)H(q) cosh

−ˇρ(q) .

Proof. Let γ be the only unit geodesic of Hn+1(ˇ) going from p to q. Let {e1(q), e2(q), ..., en(q)} a basis ofTqM made by eigenvectors ofP1, i.e., P1(ei(q))=

λi(q)ei(q), where λi, i=1, ..., n, are the eigenvalues of P1. Writing ei=biγ+ciYi, whereYi=1 and γ, Yi=0, we haveb2i+c2i=1, and

n

i=1

eiX, P1(ei)

= n

i=1

λieiX, ei= n

i=1

λibiγ+ciYiX, biγ+ciYi

= n

i=1

λi b2iγX, γ+biciγX, Yi +biciYiX, γ+c2iYiX, Yi

.

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On the other hand,

γX, γ=

γ

sinh

−ˇρ

√−ˇ γ

, γ

=

γ

sinh

−ˇρ

√−ˇ

γ+

sinh

−ˇρ

√−ˇ

γγ, γ

= (cosh

−ˇρ)γ, γ= cosh

−ˇρ,

γX, Yi=

γ

sinh

−ˇρ

√−ˇ γ

, Yi

= (cosh

−ˇρ)γ, Yi+

sinh

−ˇρ

√−ˇ

γγ, Yi

= 0,

YiX, γ=

Yi

sinh

−ˇρ

√−ˇ γ

, γ

=Yi

sinh

−ˇρ

√−ˇ

γ, γ+

sinh

−ˇρ

√−ˇ

Yiγ, γ

=

sinh

−ˇρ

√−ˇ

, Yi

+1

2

sinh

−ˇρ

√−ˇ

Yiγ, γ

=

sinh

−ˇρ

√−ˇ

, Yi

= (cosh

−ˇρ)γ, Yi= 0,

YiX, Yi=

Yi

sinh

−ˇρ

√−ˇ γ

, Yi

=Yi

sinh

−ˇρ

√−ˇ

γ, Yi+

sinh

−ˇρ

√−ˇ

Yiγ, Yi

=

sinh

−ˇρ

√−ˇ

Yi∇ρ, Yi.

Since

U∇ρ, V=

−ˇ(coth

−ˇρ)

U, V−∇ρ, U∇ρ, V ,

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for any vector fieldsU, V∈THn+1(ˇ), see [4], p. 713, and [2], p. 6, we have n

i=1

eiX, P1(ei)

= n

i=1

λi

b2i(cosh

−ˇρ)+c2i

sinh

−ˇρ

√−ˇ

Yi∇ρ, Yi

= n

i=1

λib2i(cosh

−ˇρ)

+ n

i=1

λic2isinh

−ˇρ

√−ˇ

√−ˇ(coth

−ˇρ) Yi, Yi

+∇ρ, Yi∇ρ, Yi

= (cosh

−ˇρ) n

i=1

λi b2i+c2i

= (cosh

−ˇρ) n

i=1

λi

=n(n−1)H(cosh

−ˇρ).

Proposition 2.2. Let x:Mn→Hn+1(ˇ) be an isometric immersion, ρ(x)=

ρ(p, x) be the geodesic distance function of Hn+1(ˇ) starting at p∈Hn+1(ˇ), and X=sinh−ˇρ

−ˇ ∇ρthe position vector ofHn+1(ˇ),where ∇ρ denotes the gradient of ρonHn+1(ˇ). If f:M→Ris any smooth function, then

div P1

f XT

=X, P1(∇f)+n(n1)f H(cosh

−ˇρ)+n(n−1)(R−ˇ)fX, η, where ∇f denotes the gradient of f on M, XT=X−X, ηη is the component of X tangent toM andη is the unit normal vector field of the immersion.

Proof. Let {e1, e2, ..., en} be an adapted orthonormal frame tangent to M. SinceAandP1=nHI−Aare self-adjoint, we have

tr

E−P1

(Ef X)T

= n

i=1

P1

(eif X)T , ei

= n

i=1

ei(f X), P1(ei)

= n

i=1

ei

f XT

+ei(f X, ηη), P1(ei)

= n

i=1

ei

f XT

, P1(ei)

f X, ηn

i=1

η,∇ei

P1(ei)

= n

i=1

ei

f XT

, P1(ei)

−f X, η

n

i=1

A(ei), P1(ei)

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= n

i=1

ei

f XT

, P1(ei)

−f X, η

tr(A◦P1)

= n

i=1

P1

ei

f XT , ei

−f X, η

tr(A◦P1)

= n

i=1

ei

P1

f XT , ei

n

i=1

(eiP1) f XT

, ei

−fX, ηtr(A◦P1)

= div P1

f XT

(divP1) f XT

−fX, ηtr(A◦P1).

By using Gauss equation, we have tr(A◦P1) = tr

nHA−A2

=nHtrA−trA2=n2H2−|A|2=n(n−1)(R−ˇ) and, since divP10, see [5], p. 470 and [6], p. 225, we have

tr

E−P1

(EX)T

= div P1

f XT

−n(n−1)(R−ˇ)fX, η. (2.1)

On the other hand, by using Lemma2.1, we have tr

E−P1

(Ef X)T

= n

i=1

ei(f X), P1(ei)

= n

i=1

ei(f)X+feiX, P1(ei)

= n

i=1

X, P1

ei(f)ei

+f n

i=1

eiX, P1(ei)

=

X, P1(∇f) +ftr

E−P1

(EX)T

=X, P1(∇f)+n(n1)Hf(cosh

−ˇρ).

(2.2)

Replacing (2.2) in (2.1) we obtain the result.

Lemma 2.3. Let x:Mn→Hn+1(ˇ), n3,be a proper isometric immersion.

SupposeH >0andR≥ˇ. Letρ=ρ(p,·)be the geodesic distance function ofHn+1(ˇ) starting atp∈Hn+1(ˇ). Leth:R→Rbe a smooth function such thath(t)=0fort≤0 andh(t) is increasing fort>0. If f:M→Ris any non negative locally integrable,

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C1 function, then for allt>s>0, 1

(sinh

−ˇt)n−12

M

h(t−ρ)(sinh√

−ˇρ)f H dM

1

(sinh

−ˇs)n−12

M

h(s−ρ)(sinh√

−ˇρ)f H dM

1 2

t s

1 (sinh

−ˇr)n−12

M

h(r−ρ)(sinh√

−ˇρ)

∇ρ,1

nP1(∇f) +(n1)(R−ˇ)f η

dM dr.

Proof. Applying Proposition2.2to h(r−ρ(x))f(x), we have div

P1

h(r−ρ)f XT

=−h(r−ρ)f

X, P1(∇ρ)

+h(r−ρ)

X, P1(∇f) +n(n1)h(r−ρ)f H(cosh√

−ˇρ) +n(n1)(R−ˇ)h(r−ρ)fX, η. (2.3)

Since h(r−ρ)f XT is supported in M∩Br and M is proper, then h(r−ρ)f XT is compactly supported onM. Thus, by using divergence theorem, we have

M

div P1

h(r−ρ)f XT

dM= 0.

(2.4)

Integrating (2.3) and by using (2.4) above we have

M

h(r−ρ)f

X, P1(∇ρ) dM =

M

h(r−ρ)

X, P1(∇f) dM

+n(n1)

M

h(r−ρ)f H(cosh√

−ˇρ)dM +n(n1)

M

h(r−ρ)f(R−ˇ)X, ηdM.

(2.5)

Letk1, k2, ..., kn be the principal curvatures of the immersion andλi=nH−ki

the eigenvalues of P1. From H >0 and R≥ˇ, P1 is semi-positive definite, that is, λi0 (i=1,2, ..., n). Since

λi=nH−ki≤nH+|ki| ≤nH+

k12+k22+...+k2n

≤nH+|A| ≤nH+

n2H2−n(n−1)(R−ˇ)

2nH,

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we have

M

h(r−ρ)f

X, P1(∇ρ) dM=

M

h(r−ρ)f(sinh

−ˇρ)

√−ˇ

∇ρ, P1(∇ρ) dM

2n

M

h(r−ρ)f(sinh

−ˇρ)

√−ˇ H dM

= 2nd dr

M

h(r−ρ)f(sinh

−ˇρ)

√−ˇ H dM

. (2.6)

From (2.5) and (2.6) we obtain 2n d

dr

M

h(r−ρ)f(sinh

−ˇρ)

√−ˇ H dM

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ

∇ρ, P1(∇f) dM

+n(n1)

M

h(r−ρ)f H(cosh

−ˇρ)dM +n(n1)

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ (R−ˇ)∇ρ, ηdM.

Since cothx is a decreasing function, we can estimate the second integral in the right hand side of inequality above by

M

h(r−ρ)f H(cosh

−ˇρ)dM

>√

−ˇ(coth

−ˇr)

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ Hf dM,

which implies d

dr

M

h(r−ρ)f(sinh

−ˇρ)

√−ˇ H dM

≥n−1 2

√−ˇ(coth

−ˇr)

M

h(r−ρ)f(sinh

−ˇρ)

√−ˇ H dM +1

2

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ

∇ρ,1

nP1(∇f)+(n1)(R−ˇ)f η

dM.

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Since sinh

−ˇρ

√−ˇ

n−12 d dr

sinh

−ˇρ

√−ˇ

n−12

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ Hf dM

=−n−1 2

√−ˇ(coth

−ˇr)

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ Hf dM + d

dr

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ Hf dM

, we have

sinh

−ˇρ

√−ˇ

n−12 d dr

sinh

−ˇρ

√−ˇ

n−12

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ Hf dM

1 2

M

h(r−ρ)(sinh

−ˇρ)

√−ˇ

∇ρ,1

nP1(∇f)+(n−1)(R−ˇ)f η

dM.

Dividing expression above by (sinh−ˇρ

−ˇ )n−12 ×(

−ˇ)n−32 and integrating onrfrom stot we obtain the result

1 (sinh

−ˇt)n−12

M

h(t−ρ)(sinh√

−ˇρ)f H dM

1

(sinh

−ˇs)n−12

M

h(s−ρ)(sinh√

−ˇρ)f H dM

1 2

t s

1 (sinh

−ˇr)n−12

M

h(r−ρ)(sinh√

−ˇρ)

∇ρ,1

nP1(∇f) +(n1)(R−ˇ)f η

dM dr.

3. Proof of Theorem 1.1

Proof of Theorem1.1. Choosingf≡1 in the inequality of Lemma2.3, we have, for everyt>s>0,

1 (sinh

−ˇt)n−12

M

h(t−ρ)(sinh√

−ˇρ)H dM

1

(sinh

−ˇs)n−12

M

h(s−ρ)(sinh√

−ˇρ)H dM

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1 2

t s

1 (sinh

−ˇr)n−12

M

h(r−ρ)(sinh√

−ˇρ)

∇ρ,(n1)(R−ˇdM dr

≥ −1 2

t s

1 (sinh

−ˇr)n−12

M

h(r−ρ)(sinh√

−ˇρ)(n−1)(R−ˇ)dM dr

≥ −Γ 2

t s

1 (sinh

−ˇr)n−12

M

h(r−ρ)(sinh√

−ˇρ)H dM dr.

Lettingg(r)= 1

(sinh

−ˇr)n−12

Mh(r−ρ)(sinh√

−ˇρ)H dM, inequality above beco- mes

g(t)−g(s)≥ −Γ 2

t s

g(r)dr,

which implies

g(t)≥ −Γ 2g(t), i.e.,

d dt

eΓ2tg(t)

0 and thus

eΓ2rg(r) =eΓ2r(sinh

−ˇr)n−12

M

h(r−ρ)(sinh√

−ˇρ)H dM

is monotone non-decreasing. Now, let us apply this result to the sequence of smooth functions hm: R→R such that hm(t)=0 for t≤0, hm(t)=1 for t≥m1 and hm is increasing for t∈(0,m1). Taking m→∞, sequence hm tends to the characteristic function of (0,) and the first part of the theorem follows.

To prove that

MH dM= for Γ<(n3)

−ˇ, notice that monotonicity of ϕ(r) implies

MBr

(sinh

−ˇρ)H dM

≥eΓ2(r0r)

sinh

−ˇr sinh

−ˇr0 n−12

MBr0

(sinh

−ˇρ)H dM, for allr>r0>0. Since sinhxis an increasing function, we have

MBr

(sinh

−ˇρ)H dM≤(sinh

−ˇr)

MBr

H dM,

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which implies

MBr

H dM≥(sinh

−ˇr)n−32

eΓ2r × eΓ2r0 (sinh

−ˇr0)n−12

MBr0

(sinh

−ˇρ)H dM.

Since sinh

−ˇr=12(e−ˇr−e−ˇr), takingr→∞, and by using that Γ<(n3)

√−ˇ, we obtain

MH dM=.

References

1. Alencar, H.,do Carmo, M.andSantos, W., A gap theorem for hypersurfaces of the sphere with constant scalar curvature one,Comment.Math.Helv.77(2002), 549–562. doi:10.1007/s00014-002-8351-1. MR1933789 (2003m:53098).

2. Alencar, H. and Frensel, K., Hypersurfaces whose tangent geodesics omit a nonempty set, in Differential Geometry 52, pp. 1–13, Longman Sci. Tech., Harlow, 1991. MR1173029 (93f:53048).

3. Alencar, H.,Santos, W.,Zhou, D., Curvature integral estimates for complete hy- persurfaces,Illinois J.Math.55(2012), 185–203. MR3006685.

4. Jorge, L.andKoutroufiotis, D., An estimate for the curvature of bounded subman- ifolds,Amer.J.Math.103(1981), 711–725. doi:10.2307/2374048. MR623135 (83d:53041b).

5. Reilly, R. C., Variational properties of functions of the mean curvatures for hypersur- faces in space forms,J.Differential Geom.8(1973), 465–477. MR0341351 (49

#6102).

6. Rosenberg, H., Hypersurfaces of constant curvature in space forms, Bull.Sci.Math.

117(1993), 211–239. MR1216008 (94b:53097).

Hil´ario Alencar

Instituto de Matem´atica Universidade Federal de Alagoas Macei´o, AL

57072-900 Brasil

hilario@mat.ufal.br

Greg´orio Silva Neto Instituto de Matem´atica Universidade Federal de Alagoas Macei´o, AL

57072-900 Brasil

gregorio@im.ufal.br

Received February 7, 2015 in revised form April 1, 2015 published online May 27, 2015

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