j. differential geometry 59 (2001) 353-437
THE INVERSE MEAN CURVATURE FLOW AND THE RIEMANNIAN PENROSE INEQUALITY
GERHARD HUISKEN & TOM ILMANEN
Abstract Let M be an asymptotically flat 3-manifold of nonnegative scalar curvature. The Riemannian Penrose Inequality states that the area of an outermost minimal surface N in M is bounded by the ADM mass m according to the formula |N|≤16πm2. We develop a theory of weak solutions of the inverse mean curvature flow, and employ it to prove this inequality for each connected component of N using Geroch’s monotonicity formula for the ADM mass. Our method also proves positivity of Bartnik’s gravitational capacity by computing a positive lower bound for the mass purely in terms of local geometry.
0. Introduction In this paper we develop the theory ofweak solutions forthe inverse mean curvature flow of hypersurfaces in a Riemannian manifold, and apply it to prove the Riemannian Penrose Inequality for a connected horizon, to wit: the total mass ofan asymptotically flat 3-manifoldof nonnegative scalar curvature is bounded below in terms ofthe area of each smooth, compact, connected, “outermost” minimal surface in the 3-manifold. A minimal surface is called outermost ifit is not separated from infinity by any other compact minimal surface. The result was announced in [51].
The first author acknowledges the support of Sonderforschungsbereich 382, T¨ubingen. The second author acknowledges the support of an NSF Postdoctoral Fellowship, NSF Grants DMS-9626405 and DMS-9708261, a Sloan Foundation Fellowship, and the Max-Planck-Institut for Mathematics in the Sciences, Leipzig. Received May 15, 1998.
353 354 g. huisken & t. ilmanen
Let M be a smooth Riemannian manifold of dimension n ≥ 2 with metric g =(gij). A classical solution ofthe inverse mean curvature flow is a smooth family x : N × [0,T] → M ofhypersurfaces Nt := x(N,t) satisfying the parabolic evolution equation ∂x ν (∗) = ,x∈ N , 0 ≤ t ≤ T, ∂t H t where H, assumed to be positive, is the mean curvature of Nt at the point x, ν is the outward unit normal, and ∂x/∂t denotes the normal velocity field along the surface Nt. Without special geometric assumptions (see [29, 105, 49]), the mean curvature may tend to zero at some points and singularities develop. In §1 we introduce a level-set formulation of (∗), where the evolving surfaces are given as level-sets of a scalar function u via
Nt = ∂{x : u(x)