Existence and uniqueness for anisotropic and crystalline mean curvature flows

By Antonin Chambolle, Massimiliano Morini, Matteo Novaga, and Marcello Ponsiglione

Abstract

An existence and uniqueness result, up to fattening, for crystalline mean curvature flows with forcing and arbitrary (convex) mobilities, is proven. This is achieved by introducing a new notion of solution to the corresponding level set formulation. Such solutions satisfy a comparison principle and stability properties with respect to the approximation by suitably regularized problems. The results are valid in any dimension and for arbitrary, possibly unbounded, initial closed sets. The approach accounts for the possible presence of a time-dependent bounded forcing term, with spatial Lipschitz continuity. As a result of our analysis, we deduce the convergence of a minimizing movement scheme proposed by Almgren, Taylor, and Wang (1993) to a unique (up to fattening) “flat flow” in the case of general, including crystalline, anisotropies, solving a long-standing open question.

1. Introduction

In this paper we deal with anisotropic and crystalline mean curvature flows; that is, flows of sets (formally) governed by the law

where stands for the (outer) normal velocity of the boundary at , is a given norm on representing the surface tension, is the anisotropic mean curvature of associated with the anisotropy , is a norm evaluated at the outer unit normal to , and is a bounded spatially Lipschitz continuous forcing term. The factor plays the role of a mobility.⁠Footnote1 We recall that when is differentiable in , then is given by the surface divergence of a “Cahn-Hoffman” vector field Reference 17Reference 47Reference 48:

1

Strictly speaking, the mobility is .

However, in this work we will be interested mostly in the “crystalline case”, which is whenever the level sets of are polytopes and Equation 1.2 should be replaced with

as we will describe later on.

Equation Equation 1.1 is relevant in materials science and the study of crystal growth; see for instance Reference 43Reference 48Reference 49 and the references therein. Its mathematical well-posedness is classical in the smooth setting, that is, when , , , and the initial set are sufficiently smooth (and satisfies suitable ellipticity conditions). However, it is also well known that in dimensions singularities may form in finite time even in the smooth case. When this occurs the strong formulation of Equation 1.1 ceases to be applicable and one needs a weaker notion of solution leading to a (possibly unique) globally defined evolution.

Among the different approaches that have been proposed in the literature for the classical mean curvature flow (and for several other “regular” flows) in order to overcome this difficulty, we start by mentioning the so-called level set approach Reference 26Reference 29Reference 30Reference 37Reference 45, which consists in embedding the initial set in the one-parameter family of sets given by the sublevels of some initial function , and then in letting all these sets evolve according to the same geometric law. The evolving sets are themselves the sublevels of a time-dependent function , which turns out to solve a (degenerate) parabolic equation for (with the prescribed initial datum ). The crucial point is that such a parabolic Cauchy problem is shown to admit a global-in-time unique viscosity solution for many relevant geometric motions: in fact, one only needs the continuity⁠Footnote2 of the Hamiltonian of the level-set equation which corresponds to Equation 1.1 Reference 26Reference 36. When this happens, the evolution of the sublevels of defines a generalized motion (with initial set given by the corresponding sublevels of ), which exists for all times and agrees with the classical one until the appearance of singularities (see Reference 30). Moreover, such a generalized motion satisfies the comparison principle and is unique whenever the level sets of have an empty interior. Let us mention that the appearance of a nontrivial interior (the so-called fattening phenomenon) may in fact occur even starting from a smooth set (see for instance Reference 8). On the other hand, such a phenomenon is rather rare: for instance, given any uniformly continuous initial function , all its sublevels, with the exception of at most countably many, will not generate any fattening.

2

Which is of course weaker than the requirements for the existence of strong solutions, which at least include ellipticity properties.

The second approach which is relevant for the present treatment is represented by the minimizing movements scheme devised by Almgren, Taylor, and Wang Reference 3 and, independently, by Luckhaus and Sturzenhecker Reference 44. It is variational in nature and hinges on the gradient flow structure of the geometric motion. More precisely, it consists in building a family of discrete-in-time evolutions by an iterative minimization procedure and in considering any limit of these evolutions (as the time step vanishes) as an admissible global-in-time solution to the geometric motion, usually referred to as a flat flow (or ATW flat flow). The problem which is solved at each step has the form Reference 3, §2.6

where denotes the symmetric difference of the two sets and , and the anisotropic perimeter is defined rigorously in Equation 2.1 below. (We generalize slightly the scheme later on, in particular to deal with noncompact boundaries, of possibly infinite mass.) This scheme is studied in great detail in Reference 3 and many convergence properties are proven, including to the previously mentioned viscosity solutions, under some technical assumption. If (and the initial set) is smooth enough, also convergence to strong solutions are proven. However, except in dimension 2 Reference 2, the convergence of this scheme in the crystalline case remains open.

In this paper, we show for the first time that, up to exceptional initial sets which might develop nonuniqueness, this discrete procedure converges to a unique motion in all cases, including crystalline. In practice, if we replace the distance in Equation 1.4 with an anisotropic distance based on a norm “compatible” with (“-regular”, Definition 4.1), it is relatively easy, though a bit technical, to extend our previous results in Reference 22 and show convergence of the scheme. Our main result in this work is a stability result which shows additionally that even if this -regularity is lost (as is always the case when the distance in Equation 1.4 is Euclidean and crystalline), the discrete-in-time flows remain close to -regular flows and their limit is still unique. While the stability for the limiting flow (only) is relatively simple Reference 20, the stability at the discrete level, for , which allows us to derive the uniqueness of the flat flow, is quite technical and requires precise estimates on the minimizers of Equation 1.4, established in Section 3.4. The remainder of this introduction describes more closely the technical content of this paper.

Practically, it is somewhat convenient to combine the variational approach with the level set point of view, by implementing the Almgren-Taylor-Wang scheme (ATW) for all the sublevels of the initial function (level set ATW). As already mentioned, it turns out that the two approaches produce in general the same solutions. A very simple proof of convergence of the level set ATW to the viscosity solution of the level set equation in the case of anisotropic mean curvature flows (with smooth anisotropy) is given in Reference 23 (see also Reference 3Reference 19); such a result implies in turn the convergence of the ATW to the aforementioned generalized motion whenever fattening does not occur.

When the anisotropy is crystalline, all the results mentioned before for regular anisotropies become much more difficult, starting from the very definition of crystalline curvature which cannot be given by Equation 1.2 anymore, but rather by Equation 1.3: one has to consider a suitable selection of the (multivalued) subdifferential map (of “Cahn-Hoffmann fields”), such that the tangential divergence has minimal -norm among all possible selections. The crystalline curvature is then given by the tangential divergence of the optimal Cahn-Hoffman field (see Reference 16Reference 35) and thus, in particular, has a nonlocal character.

We briefly recall what is known about the mathematical well-posedness of Equation 1.1 in the crystalline case. In two dimensions, the problem has been essentially settled in Reference 34 (when is constant) by developing a crystalline version of the viscosity approach for the level-set equation; see also Reference 2Reference 7Reference 33Reference 38Reference 48Reference 49Reference 50 for important former work. The viscosity approach adopted in Reference 34 applies in fact to more general equations of the form

with continuous and nondecreasing with respect to the second variable, however, without spatial dependence. Former studies were rather treating the problem as a system of coupled ODEs describing the relative motion of each facet of an initial crystal Reference 2Reference 7Reference 48Reference 49. We mention also the recent paper Reference 25, where short time existence and uniqueness of strong solutions for initial “regular” sets (in a suitable sense) is shown.

In dimension the situation was far less clear until very recently. Before commenting on the new developments, let us remark that before these, the only general available notion of global-in-time solution was that of a flat flow associated with the ATW scheme, defined as the limit of a converging subsequence of time discrete approximations. However, no general uniqueness and comparison results were available, except for special classes of initial data Reference 13Reference 18Reference 39 or for very specific anisotropies Reference 35. As mentioned before, substantial progress in this direction has been made only very recently, in Reference 41 and Reference 22.

In Reference 41, the authors succeed in extending the viscosity approach of Reference 34 to . They are able to deal with very general equations of the general form Equation 1.5 establishing existence and uniqueness for the corresponding level set formulations. In an article just appeared Reference 42, they show how to extend their approach to any dimension, which is a major breakthrough (moreover the new proof is considerably simpler than before). It seems that their method, as far as we know, still requires a purely crystalline anisotropy (so mixed situations are not allowed), bounded initial sets, and the only possible forcing term is a constant.

In Reference 22, the first global-in-time existence and uniqueness (up to fattening) result for the crystalline mean curvature flow valid in all dimensions, for arbitrary (possibly unbounded) initial sets, and for general (including crystalline) anisotropies was established, but under the particular choice (and ) in Equation 1.1. It is based on a new stronger distributional formulation of the problem in terms of distance functions, which is reminiscent of, but not quite the same as, the distance formulation proposed and studied in Reference 46 (see also Reference 4Reference 6Reference 11Reference 18Reference 28). Such a formulation enables the use of parabolic PDE arguments to prove comparison results, but of course makes it more difficult to prove existence. The latter is established by implementing the variant of the ATW scheme devised in Reference 18Reference 19. The methods of Reference 22 yield, as a byproduct, the uniqueness, up to fattening, of the ATW flat flow for the equation Equation 1.1 with and . But it leaves open the uniqueness issue for the general form of Equation 1.1 and, in particular, for the constant mobility case

originally appearing in Reference 3, which is approximated by Equation 1.4. The main reason is technical: the distributional formulation introduced in Reference 22 becomes effective in yielding uniqueness results only if, roughly speaking, the level sets of the -distance function from any closed set ( being the norm polar to the mobility ) have (locally) bounded crystalline curvatures. This is certainly the case when (and explains such a restriction in Reference 22).

As said, we remove in this paper the restriction and extend the existence and uniqueness results of Reference 22 to the general equation Equation 1.1. In order to deal with general mobilities, we cannot rely anymore on a distributional formulation in the spirit of Reference 22, but instead we extend the notion of solution via an approximation procedure by suitable regularized versions of Equation 1.1.

We now describe in more detail the contributions and the methods of the paper. Before addressing the general mobilities, we consider the case where may be different from but satisfies a suitable regularity assumption, namely we assume that the Wulff shape Equation 2.3 associated with (in short the -Wulff shape) admits an inner tangent -Wulff shape at all points of its boundary. We call such mobilities -regular (see Definition 4.1). The -regularity assumption implies in turn that the level sets of the -distance function from any closed set have locally bounded crystalline curvatures and makes it possible to extend the distributional formulation (and the methods) of Reference 22 to Equation 1.1 (Definition 2.2), to show that such a notion of solution bears a comparison principle (Theorem 2.7) and that the ATW scheme converges to it (Theorem 4.3). As is classical, we then use these results to build a unique level set flow (and a corresponding generalized motion), which satisfies comparison and geometricity properties (Theorem 4.8).

Having accomplished this, we deal with the general case of being any norm. As mentioned before, the idea here is to build a level set flow by means of approximation, after the easy observation that for any norm there exists a sequence of -regular mobilities such that . More precisely, we say that is a solution to the level set flow associated with Equation 1.1 if there exists an approximating sequence of -regular mobilities such that the corresponding level set flows constructed in Section 4 locally uniformly converge to (Definition 5.6).

In Theorems 5.7 and 5.9 we establish the main results of the paper: we show that for any norm a solution-via-approximation always exists; moreover satisfies the following properties:

(i)

(Uniqueness and stability) The solution-via-approximation is unique in that it is independent of the choice of the approximating sequence of -regular mobilities . In fact, it is stable with respect to the convergence of any sequence of mobilities and anisotropies.

(ii)

(Comparison) If , then the corresponding level set solutions and satisfy .

(iii)

(Convergence of the level set ATW) is the unique limit of the level set ATW.

(iv)

(Generic nonfattening) As in the classical case, for any given uniformly continuous initial datum all but countably many sublevels do not produce any fattening.

(v)

(Comparison with other notions of solutions) Our solution-via-approximation coincides with the classical viscosity solution in the smooth case and with the Giga-Požár viscosity solution Reference 41Reference 42 whenever such a solution is well-defined, that is, when is constant, is purely crystalline, and the initial set is bounded.

(vi)

(Phase-field approximation) When is constant, a phase-field Allen-Cahn type approximation of holds.

We finally mention that property (iii) implies the convergence of the ATW scheme, whenever no fattening occurs and thus settles the long-standing problem of the uniqueness (up to fattening) of the flat flow corresponding to Equation 1.1 (and in particular for Equation 1.6) when the anisotropy is crystalline. In our later paper Reference 20 we show that it is also possible to build crystalline flows by approximating the anisotropies with smooth ones and relying for existence on the standard viscosity theory of generalized solutions. However, this variant, even if slightly simpler, does not show that flat flows are unique.

The plan of the paper is the following. In Section 2 we extend the distributional formulation of Reference 22 to our setting and we study the main properties of the corresponding notions of sub- and supersolutions. The main result of the section is the comparison principle established in Section 2.3.

In Section 3 we set up the minimizing movements algorithm and we start paving the way for the main results of the paper by establishing some preliminary results. In particular, the density estimates and the barrier argument of Section 3.4, which do not require any regularity assumption on the mobility , will be crucial for the stability analysis of the ATW scheme needed to deal with the general mobility case and developed in Section 5.1.

In Section 4 we develop the existence and uniqueness theory under the assumption of -regularity for the mobility . More precisely, we establish the convergence of the ATW scheme to a distributional solution of the flow, whenever fattening does not occur. Uniqueness then follows from the results of Section 2.

Finally, in Section 5 we establish the main results of the paper, namely the existence and uniqueness of a solution via approximation by -regular mobilities. As already mentioned, the approximation procedure requires a delicate stability analysis of the ATW scheme with respect to varying mobilities. Such estimates are established in Section 5.1 and represent the main technical achievement of Section 5.

2. A distributional formulation of curvature flows

In this section we generalize the approach introduced in Reference 22 by introducing a suitable distributional formulation of Equation 1.1 and we show that such a formulation yields a comparison principle and is equivalent to the standard viscosity formulation when the anisotropy and the mobility are sufficiently regular.

The existence of the distributional solution defined in this section will be established in Section 4 under the additional assumption that the mobility satisfies a suitable regularity assumption (see Definition 4.1 below).

2.1. Preliminaries

We introduce the main objects and notation used throughout the paper.

Given a norm on (a convex, even,⁠Footnote3 one-homogeneous real-valued function with if ), we define a polar norm by and an associated anisotropic perimeter as

3

For simplicity we develop the theory in the symmetric case; see Remark 6.3.

As is well known, so that when the set is smooth enough one has

which is the perimeter of weighted by the surface tension . The notation , , stands for the -dimensional Hausdorff measure. It is also useful to recall the notion of relative perimeter: given an open set we will denote by the -perimeter of relative to ; i.e.,

As before, note that if is sufficiently regular, then

We will often use the following characterization of the subgradient:

(and the symmetric statement for ). In particular, if and , then and . For we denote

Such a set is called the Wulff shape (of radius and center ) associated with the norm and represents the unique (up to translations) solution of the anisotropic isoperimetric problem

see for instance Reference 32. We let , be the unit ball, and more generally, for , .

We denote by the distance from induced by the norm , that is, for any

if , and . Moreover, we denote by the signed distance from induced by , i.e.,

so that and , where we adopted the standard notation and . Note that by Equation 2.2 we have a.e. in . We will write and without any superscript to denote the Euclidean distance and signed distance from , respectively.

Finally we recall that a sequence of closed sets in converges to a closed set in the Kuratowki sense if the following conditions are satisfied:

(i)

if for each , any limit point of belongs to ;

(ii)

any is the limit of a sequence , with for each .

We write in this case:

It is easily checked that if and only if (for any norm ) locally uniformly in . In particular, the Ascoli-Arzelà Theorem shows that any sequence of closed sets admits a converging subsequence in the Kuratowski sense.

2.2. The distributional formulation

In this subsection we give the precise formulation of the crystalline mean curvature flows we will deal with. Throughout the paper the norms and will stand for the anisotropy and the mobility, respectively, appearing in Equation 1.1. Note that we do not assume any regularity on (nor on ) and in fact we are mainly interested in the case when is crystalline, that is, when the associated unit ball is a polytope.

Moreover, we will assume throughout the paper that the forcing term satisfies the following two hypotheses:

H1)

;

H2)

there exists such that is -Lipschitz continuous (with respect to the metric ) for a.e. .

Remark 2.1.

Assumption H1) can be weakened and replaced by

H1)’

for every , .

Indeed under the weaker assumption H1)’, all the arguments and the estimates presented throughout the paper continue to work in any time interval , with some of the constants involved possibly depending on . In the same way, if one restricts our study to the evolution of sets with compact boundary, then one could assume that is only locally bounded in space. We assume H1) instead of H1)’ to simplify the presentation.

In all that follows by the expression “admissible forcing term” we will mean a forcing term satisfying H1) and H2) above.

We are now ready to provide a suitable distributional formulation of the curvature flow Equation 1.1.

Definition 2.2.

Let be a closed set. Let be a closed set in and for each denote . We say that is a superflow of Equation 1.1 with initial datum if the following hold:

(a)

Initial condition: .

(b)

Left continuity: as for all .

(c)

If for some , then for all .

(d)

Differential inequality: Set , and

Then there exists such that the inequality

holds in the distributional sense in for a suitable such that a.e., is a Radon measure in , and for every .

We say that , an open set in , is a subflow of Equation 1.1 with initial datum if is a superflow of Equation 1.1 with replaced by and with initial datum .

Finally, we say that , a closed set in , is a solution of Equation 1.1 with initial datum if it is a superflow and if is a subflow, both with initial datum , assuming in addition that both and coincide with the closure of their interior.

In Subsection 4.2 we will prove the existence of solutions satisfying Equation 2.5 with . In our definition, “super”flow refers to the fact that the distance function may grow faster than the distance to a solution of the mean curvature flow, which corresponds to a set shrinking also faster than expected with Equation 1.1.

Remark 2.3.

Notice that the closedness of yields that is lower semicontinuous. Indeed, if , with , we can choose with . Then, since any limit point of is in , one deduces . On the other hand, condition (b) implies that is left-continuous. Moreover, by condition (d) of Definition 2.2, the distributional derivative is a Radon measure in , so that is locally a function with bounded variation; using the fact that the distance functions are uniformly Lipschitz, we can deduce that for any , converges locally uniformly in as to some function with in , while converges locally uniformly to as (cf. Reference 22, Lemma 2.4).

Remark 2.4.

Notice that the initial condition for subflows may be rewritten as . In particular, if is a solution according to the previous definition, then .

We now introduce the corresponding notion of sub- and supersolution to the level set flow associated with Equation 1.1.

Definition 2.5 (Level set subsolutions and supersolutions).

Let be a uniformly continuous function on . We will say that a lower semicontinuous function is a supersolution to the level set flow corresponding to Equation 1.1 (level set supersolution for short), with initial datum , if and if for a.e. the closed sublevel set is a superflow of Equation 1.1 in the sense of Definition 2.2, with initial datum .

We will say that an upper semicontinuous function is a subsolution to the level set flow corresponding to Equation 1.1 (level set subsolution for short), with initial datum , if  is a level set supersolution in the previous sense, with initial datum and with replaced by .

Finally, we will say that a continuous function is a solution to the level set flow corresponding to Equation 1.1 if it is both a level set subsolution and supersolution.

2.3. The comparison principle

In this subsection we establish a comparison principle between sub- and superflows as defined in the previous subsection. A first technical result is a (uniform) left-continuity estimate for the distance function to a superflow.

Lemma 2.6.

Let be a superflow in the sense of Definition 2.2, and the associated distance function. Then, there exist depending on such that for any and any ,

and (for any with )

Proof.

The proof follows the lines of the proof of Reference 22, Lemma 3.2 up to minor changes that we will briefly describe in the following. By definition of a superflow we have

wherever . Consider with . For , let and define

We have that , while, in , is in time, the singular part is nonnegative (as the singular part is nonnegative thanks to Equation 2.5 and the assumption on ), and the absolutely continuous part satisfies

As , we obtain that is a supersolution of the -total variation flow starting from , and we can reproduce the proof of Reference 22, Lemma 3.2: we find that there exists a constant such that for as long as this bound ensures that , which is as long as

Now we prove that for any

Indeed, as long as Equation 2.8 holds true we have

On the other hand, for later times the left-hand side of Equation 2.9 is (always) nonnegative and the right-hand side becomes nonpositive. Notice that Equation 2.9 can be rewritten as

and since this holds for any and does not depend on the particular value of , it holds in fact for any and we denote this point simply by in the sequel.

Since , we deduce that for any ,

Inequality Equation 2.6 follows by Taylor expansion, while Equation 2.7 is in fact equivalent to Equation 2.6, up to a change of constants.

We can now show the following important comparison result.

Theorem 2.7.

Let be a superflow with initial datum , and let be a subflow with initial datum in the sense of Definition 2.2. Assume that . Then,

where is as in Equation 2.5 for both and .

Proof.

Let and be the maximal existence time for and . For all we have that either or is empty. For all such ’s the conclusion clearly holds true.

Thus, we may assume without loss of generality that and we consider the case . By iteration (thanks to the left-continuity of ) it is clearly enough to show the conclusion of the theorem for a time interval for some .

Let us fix . We denote by and the fields appearing in the definition of superflow (see Definition 2.2), corresponding to and , respectively. Consider the set

We now set

with to be chosen later. By our assumptions . Moreover, since by construction

it follows from Lemma 2.6 that there exists such that

Relying again on Lemma 2.6 and arguing similarly we also have (for a possibly smaller )

and

where

Since is Lipschitz continuous in space and is a measure wherever is positive, it follows that (and in turn ) is a function in and its distributional time derivative has the form⁠Footnote4

4

With a slight abuse of notation, in the jump part at we denote by what should be the Hausdorff measure on the hyperplane .

where is the (countable) set of times where jumps and is the diffuse part of the derivative. It turns out that (see Remark 2.3) for each . Moreover, since the positive part of is absolutely continuous with respect to the Lebesgue measure (cf. Definition 2.2(d)), Equation 2.5 entails

in . Using the chain rule (see for instance Reference 5), in we have

An analogous formula holds for . Recalling that and belong to it follows that

in the sense of measures in provided that we have chosen (cf. Equation 2.11 and the conditions in Definition 2.2(d))

Note also that a.e. in

Fix and set and . By Equation 2.10 we have

Using as before the chain rule for functions, recalling Equation 2.13 and the fact that the jump parts of and are nonnegative, in we have

where in the last inequality we have used Equation 2.13. Choose a cut-off function such that and on . For every we set . Using Equation 2.15 and Equation 2.16, we have

where we have also used the inequality , which follows from Equation 2.14 and the convexity and symmetry of . By Hölder’s inequality and using the explicit expression of and , we get

for some constant depending only on the -norms of and and on . Since at , a simple ODE argument then yields

for all . Observing that and as , we conclude that , and in turn in . In particular, by Equation 2.12, we have shown that in . In turn, this easily implies that for (see the end of the proof of Reference 22, Theorem 3.3). This concludes the proof of the theorem.

The previous theorem easily yields a comparison principle also between level set subsolutions and supersolutions.

Theorem 2.8.

Let , be uniformly continuous functions on and let , be respectively a level set subsolution with initial datum and a level set supersolution with initial datum , in the sense of Definition 2.5. If , then .

Proof.

Recall that by Definition 2.5 there exists a null set such that for all the sets and are respectively a subflow with initial datum and a superflow with initial datum , in the sense of Definition 2.2. Fix now and choose , with , . Since , we have

where the last inequality follows from the uniform continuity of . Thus, by Theorem 2.7, for all ,

Letting , with , we conclude that for all , which is clearly equivalent to .

2.4. Distributional versus viscosity solutions

We show here that in the smooth cases, the notion of solution in Definition 2.2 coincides with the definition of standard viscosity solutions for geometric motions, as for instance proposed in Reference 12.

Lemma 2.9.

Assume , and assume that is continuous also with respect to the time variable. Let be a superflow in the sense of Definition 2.2. Then, is a viscosity supersolution of

in , and in fact in whenever , where is the extinction time of introduced in Definition 2.2.

A converse statement is also true; see Reference 20Reference 22.

Proof.

We follow the proof of a similar statement in Reference 22, Appendix. Let be a smooth test function and assume has a (strict) local minimum at , . In other words, we can assume that near , , while . We can also assume that the latter quantity is (i.e., ), since if it is zero, then we trivially deduce that while .

If , thanks to Reference 10, Prop. 2.2 we can assume that also the spatial Hessian (and then , ). As usual, if we assume that and choose , we observe that near , and, for close enough to and close enough to ,

Hence, one has that near (for ), for some

It follows that for such , , where is a neighborhood of . For small enough we deduce that does not meet , in other words for constant depending only on . It then follows from Lemma 2.6, and more precisely from Equation 2.6, that (provided , where is as in Lemma 2.6)

which is positive if is close enough to , a contradiction. Hence .

If, on the other hand, , then we can introduce the set , and we have that is a smooth set near for close to , which contains , with a contact at . We then let , which is at least near (as are ) and is touching from below at all the points for small.

Assume that

at . Then, by continuity, we can find small and a neighborhood of in where

Possibly reducing and using (cf. Remark 2.3) the left-continuity of , since , we can also assume that in .

We choose then small enough so that is such that , and for small we define . Then has a unique strict minimum point at in . Moreover if is small enough, by continuity, we still have that

in .

Then we continue as in Reference 22, Appendix: given nonincreasing, convex, vanishing on , and positive on , we introduce for small enough. We then show that, thanks to Equation 2.5, for ,

as we have assumed in . This is in contradiction with

and it follows that Equation 2.18 cannot hold: one must have

at . Since this equation is geometric and the level set is , which is the level of (near ), we also deduce that at the same point,

so that is a supersolution of Equation 2.17.

3. Minimizing movements

As in Reference 22, in order to build solutions to our geometric evolution problem, we implement a variant of the Almgren-Taylor-Wang Reference 3 minimizing movements scheme Equation 1.4 (in short the ATW scheme) introduced in Reference 18Reference 19. In Section 3.2 we adapt this construction to take into account the forcing term, as in Reference 24. We start by presenting some preliminary properties of the incremental problem.

3.1. The incremental problem

Given with and , let denote the Radon measure associated with the linear functional

see Reference 9. We recall the following result.

Proposition 3.1.

Let , , and . There exist a field and a unique function such that the pair satisfies

Moreover, for any and with ,

and for every the set solves the minimization problem

If and if , are the corresponding solutions to Equation 3.1 (with replaced by and , respectively), then .

Finally if in addition is Lipschitz with for some norm , then the unique solution of Equation 3.1 is also Lipschitz and satisfies a.e. in . As a consequence, Equation 3.1 is equivalent to

Proof.

See Reference 18, Theorem 2, Reference 1, Theorem 3.3.

The comparison property in the previous proposition has the following “local” version, which results from the geometric character of Equation 3.1.

Lemma 3.2.

Let , be Lipschitz functions and let , , be solutions to Equation 3.1 with replaced by . Assume also that for some ,

Then, a.e.

Proof.

Let us set for and observe that

Writing Equation 3.1 for and subtracting the equations we get

Let be a smooth, increasing, nonnegative function with support in , let , and let . First notice that

since it can be easily checked that in . Thus, from Equation 3.5 we deduce that

Notice that the last integral in this equation is nonpositive, since by Equation 3.3, the set is contained (up to a negligible set) in . Hence, using also that thanks to Equation 3.4, we deduce

Letting we obtain

so that

where . Replacing now with , , assuming , we obtain

as we have assumed . It follows that a.e., which is the thesis of the lemma.

Remark 3.3.

The result remains true if , , are not assumed to be Lipschitz. This is because again, in this case, the pairing is nonnegative, which may be shown for instance by first approximating the functions with Lipschitz functions.

We conclude this subsection with the following useful computation, proved in Reference 18, p. 1576.

Lemma 3.4.

Let and let be the solution to Equation 3.2, with , where . Then is given by

as long as .

3.2. The ATW scheme

Let , , and satisfy all the assumptions stated in Subsection 2.2. Set

Let be closed. Fix a time-step and set . We then inductively define (for all ) according to the following procedure: if , , then let satisfy

and set .⁠Footnote5 If either or , then set . We denote by the first discrete time such that , if such a time exists; otherwise we set . Analogously, we denote by the first discrete time such that , if such a time exists; otherwise we set .

5

Choosing might provide a different (smaller) solution, which would enjoy exactly the same properties as the one we (arbitrarily) chose.

Remark 3.5.

In the following, when changing mobilities, forcing terms, and initial data, we will sometimes write in place of in order to highlight the dependence of the scheme on , , and . More generally, given any closed set , will denote the th minimizing movements starting from with mobility , forcing term and time-step , as described by the algorithm above.

Remark 3.6 (Monotonicity of the scheme).

From the comparison property stated in Proposition 3.1 it easily follows that if are closed sets, then (with the notation introduced in the previous remark) for all . In addition, note that for all . Thus, if , then we may apply Lemma 5.2 below with , , and with the Euclidean norm to deduce that for all .

The assumption that the sets are at positive distance is necessary, otherwise one could only conclude, for instance, that the smallest solution of the ATW scheme from is in the complement of any solution from , etc.

We now study the space regularity of the functions constructed above. In the following computations, given any function and , we denote . Then, the function satisfies

where in the last inequality we also used the Lipschitz-continuity of . By the comparison property stated in Proposition 3.1 we deduce that . By the arbitrariness of , we get , and in turn

We are now in a position to define the discrete-in-time evolutions constructed via minimizing movements. Precisely, we set

where stands for the integer part.

We conclude this subsection with the following remark.

Remark 3.7 (Discrete comparison principle).

Remark 3.6 now reads as follows: if are closed sets and if we denote by and the discrete evolutions with initial datum and , respectively, then for all . Analogously, if , is defined with a forcing , and is defined with the forcing , then for all .

3.3. Evolution of -Wulff shapes

We start paving the way for the convergence analysis of the scheme by deriving some estimates on the minimizing movements starting from a Wulff shape. We consider as initial set the -Wulff shape for . First, thanks to Lemma 3.4 (with ) (cf. also Reference 18, Appendix B, Eq. (39)), the solution of Equation 3.1 with is given by , where

Observe then that there exist two positive constants such that

and in particular

Thus, for any we have

Denoting by the solution to Equation 3.2, with defined above, then Lemma 3.4 yields

provided that (here and in the following denotes a positive constant that depends only on the dimension and may change from line to line). Notice that for

Taking into account Equation 3.13, we may apply the comparison principle stated in Proposition 3.1 to infer that if and , then

provided that . Since

and setting for

by iteration we deduce that

for all and .

In particular, there exist a constant depending only on , , and the dimension , and depending also on , such that for any and for all

3.4. Density estimates and barriers

In this section we collect some preliminary estimates on the incremental problem that will be crucial for the stability properties established in Section 5.1. The following density lemma and the subsequent corollary show that the solution to the incremental problem starting from a closed set cannot be too “thin” in . The main point is that the estimate turns out to be independent of and ; see also Lemma 1.3 and Remark 1.4 in Reference 44. We observe that there exist positive constants , such that

Lemma 3.8.

Let be a closed set, let , and let with for some . Let be a solution to

for all positive . Then, there exist depending only on and , and depending on and , with the following property: if is such that for all and with , then

Proof.

We adapt to our context a classical argument from the regularity theory of the (quasi)minimizers of the perimeter Reference 44, Lemma 1.3, Remark 1.4. As mentioned before, the main point is to use the fact that the Wulff shapes lie outside to deduce that the constants are independent of and . Let and be as in the statement. Fix such that . For all , set . For a.e. , we have:⁠Footnote6

6

We use here that is even, otherwise the constant in the formula should be replaced by , where is such that ; see also Remark 6.3.

with the outer normal vector to . Using also the fact that

(since in ), by minimality of in Equation 3.18 we find

The above inequality and the (anisotropic; see for instance Reference 32) isoperimetric inequality yield

where we have used that . We observe also that (using and the coarea formula)

so that for a.e. , . Using that for all , the inequality Equation 3.19 implies in turn that

If we obtain, integrating the above inequality on ,

where we have used Equation 3.17 for the last inequality. The thesis follows.

Remark 3.9.

The same argument shows that a similar but -dependent density estimate holds inside .

We introduce the following notation: for any set , for any norm , and for we denote

and we will omit in the notation if is the Euclidean norm. We also recall the notation introduced in Remark 3.5 to denote the th minimizing movement starting from , with mobility , forcing term and time-step .

Corollary 3.10.

Let and be an admissible forcing term and a mobility, respectively, and let . Denote by the corresponding (single) minimizing movement starting from (see Section 3.2 and Remark 3.5). Let and be the constants provided by Lemma 3.8 for . If and with , then

Proof.

Recall that , where solves

Thus, by virtue of Proposition 3.1, setting for , we have that solves Equation 3.18 with . Since belongs to the interior of and , from Lemma 3.8 we deduce that

The thesis follows by monotone convergence by letting .

Lemma 3.11.

Let be a convex set and let . Then,

where depends only on the dimension .

Proof.

Notice that is convex for all positive , so that is a convex set contained in , and

Therefore, thanks to the coarea formula,

The next lemma provides a crucial estimate on the “expansion” of any closed set under a single minimizing movement, provided that satisfies a uniform exterior Wulff shape condition. The result is achieved by combining a barrier argument with the density estimate established in Corollary 3.10.

Lemma 3.12.

For any , , , there exists depending on the previous constants, on the anisotropy , and the dimension , and there exists depending on the same quantities but , with the following property: let be a mobility satisfying

and let be an admissible forcing term with . Then for any closed set such that , where is a family of (closed) -Wulff shapes of radius , and for all , we have .

Proof.

First notice that Equation 3.22 is equivalent to Hence, recalling Equation 3.16, there exists a constant depending only on , ( in Equation 3.16), and , such that

for all . By Lemma 3.11 it follows that for a possibly different constant depending only on , , and , we have

for all .

Observe now that there exists depending only on , such that

where stands for the cube of side centered at . Let be the constant provided by Corollary 3.10, and let be the constant provided by the covering Lemma 3.13 below, corresponding to the constant in Equation 3.24, , and . Set , where is the constant in Equation 3.23, and note that for we have

Let be such that for some , and assume by contradiction that . Without loss of generality we may assume .

By taking smaller if needed, we can also assume that and for all , where is the radius provided by Corollary 3.10. Thus, recalling also Equation 3.24, for , applying Lemma 3.13 below (with ) to the family

which by assumption on and covers , we find a finite subfamily

of elements such that

By scaling back we obtain

Note now that by the comparison principle (see Remark 3.6)

Thus, using also Equation 3.23, Equation 3.25, and Equation 3.26 we deduce that