Motion by mean curvature from Glauber-Kawasaki dynamics
Tadahisa Funaki, Kenkichi Tsunoda

TL;DR
This paper derives the motion by mean curvature for particle system interfaces under a specific scaling of Glauber-Kawasaki dynamics, extending hydrodynamic limits to include interface evolution in particle systems.
Contribution
It introduces a new scaling regime where Glauber dynamics is sped up slower than Kawasaki dynamics, leading to a derivation of mean curvature motion from particle systems.
Findings
Derived motion by mean curvature from Glauber-Kawasaki dynamics.
Extended hydrodynamic limits to interface evolution.
Connected particle system behavior with geometric interface motion.
Abstract
We study the hydrodynamic scaling limit for the Glauber-Kawasaki dynamics. It is known that, if the Kawasaki part is speeded up in a diffusive space-time scaling, one can derive the Allen-Cahn equation which is a kind of the reaction-diffusion equation in the limit. This paper concerns the scaling that the Glauber part, which governs the creation and annihilation of particles, is also speeded up but slower than the Kawasaki part. Under such scaling, we derive directly from the particle system the motion by mean curvature for the interfaces separating sparse and dense regions of particles as a combination of the hydrodynamic and sharp interface limits.
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Motion by mean curvature from Glauber-Kawasaki dynamics
Tadahisa Funaki and Kenkichi Tsunoda
Abstract
We study the hydrodynamic scaling limit for the Glauber-Kawasaki dynamics. It is known that, if the Kawasaki part is speeded up in a diffusive space-time scaling, one can derive the Allen-Cahn equation which is a kind of the reaction-diffusion equation in the limit. This paper concerns the scaling that the Glauber part, which governs the creation and annihilation of particles, is also speeded up but slower than the Kawasaki part. Under such scaling, we derive directly from the particle system the motion by mean curvature for the interfaces separating sparse and dense regions of particles as a combination of the hydrodynamic and sharp interface limits.
†† 1) Department of Mathematics, School of Fundamental Science and Engineering, Waseda University, 3-4-1 Okubo, Shinjuku-ku, Tokyo 169-8555, Japan. e-mail: [email protected]
2) Department of Mathematics, Osaka University, 1-1, Machikaneyama-cho, Toyonaka, Osaka 560-0043, Japan. e-mail: [email protected]†† Keywords: Hydrodynamic limit, Motion by mean curvature, Glauber-Kawasaki dynamics, Allen-Cahn equation, Sharp interface limit.†† Abbreviated title running head: MMC from Glauber-Kawasaki dynamics†† 2010MSC: Primary 60K35 ; Secondary 82C22, 74A50.†† The author1) is supported in part by JSPS KAKENHI, Grant-in-Aid for Scientific Researches (S) 16H06338, (A) 18H03672, 17H01093, 17H01097 and (B) 16KT0024, 26287014. The author2) is supported in part by JSPS KAKENHI, Grant-in-Aid for Early-Career Scientists 18K13426.
1 Introduction
In this paper, we consider the Glauber-Kawasaki dynamics, that is the simple exclusion process with an additional effect of creation and annihilation of particles, on a -dimensional periodic square lattice of size with and study its hydrodynamic behavior. We introduce the diffusive space-time scaling for the Kawasaki part. Namely, the time scale of particles performing random walks with exclusion rule is speeded up by . It is known that, if the time scale of the Glauber part stays at , one can derive the reaction-diffusion equation in the limit as .
This paper discusses the scaling under which the Glauber part is also speeded up by the factor , which is at the mesoscopic level. More precisely, we take such as satisfying , and shows that the system exhibits the phase separation. In other words, if we choose the rates of creation and annihilation in a proper way, then microscopically the whole region is separated into two regions occupied by different phases called sparse and dense phases, and the macroscopic interface separating these two phases evolves according to the motion by mean curvature.
1.1 Known result on hydrodynamic limit
Before introducing our model, we explain a classical result on the hydrodynamic limit for the Glauber-Kawasaki dynamics in a different scaling from ours. Let be the -dimensional square lattice of size with periodic boundary condition. The configuration space is denoted by and its element is described by . In this subsection, we discuss the dynamics with the generator given by , where
[TABLE]
for a function on . The configurations and are defined from as
[TABLE]
The flip rate in the Glauber part is a nonnegative local function on (regarded as that on for large enough), and is the translation acting on or defined by or . In fact, has the following form:
[TABLE]
where and represent the rates of creation and annihilation of a particle at , respectively, and both are local functions which do not depend on the occupation variable .
Let be the Markov process on generated by . The macroscopically scaled empirical measure on , that is with the periodic boundary, associated with a configuration is defined by
[TABLE]
Then, it is known that the empirical measure converges to as in probability (multiplying a test function on ) if this holds at . Here, is a unique weak solution of the reaction-diffusion equation
[TABLE]
with the given initial value , is the Lebesgue measure on and
[TABLE]
where is the Bernoulli measure on with mean . This was shown by De Masi et al. [7]; see also [12] and [13] for further developments in the Glauber-Kawasaki dynamics. We use the same letter for functions on and the reaction term defined by (1.4), but these should be clearly distinguished.
From (1.1), the reaction term can be rewritten as
[TABLE]
if are given as the finite sum of the form:
[TABLE]
with some constants . Note that are equal to (1.5) with replaced by . We give an example of the flip rate and the corresponding reaction term determined by (1.4).
Example 1.1**.**
Consider in (1.1) of the form
[TABLE]
with and such that three points are different. Then,
[TABLE]
In particular, under a suitable choice of six constants , one can have
[TABLE]
with some , satisfying ; see the example in Section 8 of [13] with given in -dimensional setting. Namely, is bistable with stable points and unstable point , and satisfies the balance condition .
For the reaction term of the form (1.8), the equation (1.3) considered on instead of admits a traveling wave solution which connects two different stable points , and its speed is [math] due to the balance condition. The traveling wave solution with speed [math] is called a standing wave. See Section 4.2 for details.
1.2 Our model and main result
The model we concern in this paper is the Glauber-Kawasaki dynamics on with the generator with another scaling parameter . The parameter depends on as and tends to as .
If we fix so as to be independent of , then, as we saw in Section 1.1, we obtain the reaction-diffusion equation for in the hydrodynamic limit:
[TABLE]
The partial differential equation (PDE) (1.9) with the large reaction term , which is bistable and satisfies the balance condition as in Example 1.1, is called the Allen-Cahn equation. It is known that as the Allen-Cahn equation leads to the motion by mean curvature; see Section 4. Our goal is to derive it directly from the particle system.
For our main theorem, we assume the following five conditions on the creation and annihilation rates and the mean , of the initial distribution of our process.
- (A1)
have the form (1.6) with , both of which have at least one positive components, and three points are different.
- (A2)
The corresponding defined by (1.4) or equivalently by (1.7) is bistable, that is, has exactly three zeros and , hold, and it satisfies the balance condition .
- (A3)
is increasing and is decreasing in under the partial order defined by for , where are defined by (1.6) with replaced by .
- (A4)
\|\nabla^{N}u^{N}(0,x)\|\leq C_{0}K\,\big{(}\!=C_{0}K(N)\big{)} for some , where with the unit vectors of the direction and stands for the standard Euclidean norm of .
- (A5)
defined by (2.5) from satisfies the bound (4.3) at .
The condition (A5) implies that a smooth hypersurface in without boundary exists and converges to weakly in as , see (4.7) taking . We denote for a closed hypersurface which separates into two disjoint regions,
[TABLE]
It is known that a smooth family of closed hypersurfaces in , which starts from and evolves being governed by the motion by mean curvature (4.1), exists until some time ; recall and see the beginning of Section 4 for details. Note that the sides of in (1.10) with is kept under the time evolution and determined continuously from those of . We need the smoothness of to construct super and sub solutions of the discretized hydrodynamic equation in Theorem 4.6.
Let be the distribution of on and let be the Bernoulli measure on with mean . Recall that is the mean of under for each . Our another condition with is the following.
- (A6)δ
The relative entropy at defined by (2.4) behaves as as with some and satisfies .
The main result of this paper is now stated as follows. Recall that is defined by (1.2).
Theorem 1.1**.**
Assume the six conditions (A1)–(A6)δ with small enough chosen depending on . Then, we have
[TABLE]
for every and , where or denote the integrals on of with respect to the measures or , respectively.
The proof of Theorem 1.1 consists of two parts, that is, the probabilistic part in Sections 2 and 3, and the PDE part in Section 4. In the probabilistic part, we apply the relative entropy method of Jara and Menezes [24], [25], which is in a sense a combination of the methods due to Guo et al. [22] and Yau [31]. In the PDE part, we show the convergence of solutions of the discretized hydrodynamic equation (2.2) with the limit governed by the motion by mean curvature. More precise rate of convergence in (1.11) is given in Remark 3.1.
We give some explanation for our conditions. If we take in Example 1.1, we have , and has the form (1.8) with , , and so that the conditions (A1)–(A3) are satisfied. For simplicity, we discuss in this paper of the form (1.6) only, however one can generalize our result to more general given as in (1.5). The corresponding may have several zeros, but we may restrict our arguments in the PDE part to a subinterval of , on which the conditions (A2) and (A3) are satisfied. The entropy condition in (A6)δ is satisfied, for example, if and holds for some .
In the probabilistic part, we only need the following condition weaker than (A5).
- (A7)
for some .
For convenience, we take such that by making smaller and larger if necessary; see the comments given below Theorem 4.1. The condition (A7) with this choice of is called (A7)′. Under this choice of , the condition (A3) can be weakened and it is sufficient if it holds for . The conditions (A1), (A4), (A6)δ, (A7) are used in the probabilistic part, while (A2), (A3), (A5) are used in the PDE part. To be precise, (A2), (A3) are used also in the probabilistic part but in a less important way; see the comments below Theorem 2.1.
The derivation of the motion by mean curvature and the related problems of pattern formation in interacting particle systems were discussed by Spohn [29] rather heuristically, and by De Masi et al. [11], Katsoulakis and Souganidis [27], Giacomin [21] for Glauber-Kawasaki dynamics. De Masi et al. [9], [10], Katsoulakis and Souganidis [28] studied Glauber dynamics with Kac type long range mean field interaction. Related problems are discussed by Caputo et al. [3], [4]. Similar idea is used in Hernández et al. [23] to derive the fast diffusion equation from zero-range processes. Bertini et al. [2] discussed from the viewpoint of large deviation functionals.
In particular, the results of [27] are close to ours. They consider the Glauber-Kawasaki dynamics with generator under the spatial scaling , where should satisfy the condition with some . If we write as in our case, the generator becomes so that plays a role similar to our . They analyze the limit of correlation functions.
On the other hand, our analysis makes it possible to study the limit of the empirical measures, which is more natural in the study of the hydrodynamic limit, under a milder assumption on the initial distribution . Moreover, we believe that our relative entropy method has an advantage to work for a wide class of models in parallel. Furthermore, this method is applicable to study the fast-reaction limit for two-component Kawasaki dynamics, which leads to the two-phase Stefan problem, see [8].
Finally, we make a brief comment on the case that is unbalanced: . For such , the proper time scale is shorter and turns out to be , so that the equation (1.9) is rescaled as
[TABLE]
It is known that this equation exhibits a different behavior in the sharp interface limit as , see p. 95 of [16]. The present paper does not discuss this case.
2 Relative entropy method
We start the probabilistic part by formulating Theorem 2.1. This gives an estimate on the relative entropy of our system with respect to the local equilibria and implies the weak law of large numbers (2.6) as its consequence. We compute the time derivative of the relative entropy to give the proof of Theorem 2.1. In Sections 2 and 3, it is unnecessary to assume , so that we discuss for all including .
2.1 The entropy estimate
From (1.1), the flip rate of the Glauber part has the form
[TABLE]
where with of the form (1.5). Let be the solution of the discretized hydrodynamic equation:
[TABLE]
where is defined by
[TABLE]
for and
[TABLE]
Note that are given by (1.5) with replaced by and is the Bernoulli measure with non-constant mean . In the following, we assume that have the form (1.6) and, in this case, we have
[TABLE]
Let and be two probability measures on . We define the relative entropy of with respect to by
[TABLE]
if is absolutely continuous with respect to , , otherwise. Let be the distribution of on and let be the Bernoulli measure on with mean . The following result plays an essential role to prove Theorem 1.1.
Theorem 2.1**.**
We assume the conditions (A1)–(A4) and (A7)′**. Then, if (A6)δ holds with small enough , we have
[TABLE]
as . The constant depends on .
Note that the condition (A7)′, i.e. (A7) with an additional condition on the choice of , combined with the comparison theorem implies that the solution of the discretized hydrodynamic equation (2.2) satisfies that for all and ; see the comments given below Theorem 4.1. The conditions (A2) and (A3) are used only to show this bound for .
2.2 Consequence of Theorem 2.1
We define the macroscopic function associated with the microscopic function as a step function
[TABLE]
where is the box with center and side length . Then the entropy inequality (see Proposition A1.8.2 of [26] or Section 3.2.3 of [17])
[TABLE]
combined with Theorem 2.1 and Proposition 2.2 stated below shows that
[TABLE]
for every , where
[TABLE]
Proposition 2.2**.**
There exists such that
[TABLE]
Proof.
Set and observe
[TABLE]
as . Then, we have
[TABLE]
for every , where we used the elementary inequality to obtain the second inequality. By the independence of under , the expectations inside the last braces can be written as
[TABLE]
where and . Applying the Taylor’s formula at , we see
[TABLE]
for . Thus we obtain
[TABLE]
for sufficiently small. This shows the conclusion. ∎
2.3 Time derivative of the relative entropy
For a function on and a measure on , set
[TABLE]
where
[TABLE]
Take a family of probability measures on differentiable in and a probability measure on as a reference measure, and set . Assume that these measures have full supports in . We denote the adjoint of an operator on by in general. Then we have the following proposition called Yau’s inequality; see Theorem 4.2 of [17] or Lemma A.1 of [25] for the proof.
Proposition 2.3**.**
[TABLE]
where stands for the constant function , .
We apply Proposition 2.3 with to prove Theorem 2.1.
2.4 Computation of
We compute the integrand of the second term in the right hand side of (2.8). Similar computations are made in the proofs of Lemma 3.1 of [20], Appendix A.3 of [25] and Lemmas 4.4–4.6 of [17]. We introduce the centered variable and the normalized centered variable of under the Bernoulli measure with mean as follows:
[TABLE]
where , . We first compute the contribution of the Kawasaki part.
Lemma 2.4**.**
Let be a Bernoulli measure on with mean . Then, we have
[TABLE]
where .
Proof.
Take a test function on and compute
[TABLE]
where denotes the indicator function of a set . To obtain the second line, we have applied the change of variables , and then the identity
[TABLE]
and finally the symmetry in and . Since one can rewrite as , we have
[TABLE]
However, the sum of the last term vanishes, while the sum of the second and third terms is computed by exchanging the role of and in the third term and in the end we obtain
[TABLE]
The right hand side in (2.10) can be further rewritten as
[TABLE]
by computing the coefficient of in (2.10) as
[TABLE]
which gives by taking the sum in . Finally, the first term in (2.11) can be symmetrized in and and we obtain (2.9). ∎
The following lemma is for the Glauber part. Recall that the flip rate is given by (2.1) with of the form (1.5) in general.
Lemma 2.5**.**
The Bernoulli measure is the same as in Lemma 2.4. Then, we have
[TABLE]
where is given by (2.3) and
[TABLE]
with a finite sum in with and some local functions of for each . In particular, if have the form (1.6), we have
[TABLE]
where are shift-invariant bounded functions of defined by
[TABLE]
respectively.
Proof.
The first identity in (2.12) is shown by computing for a test function and applying the change of variables as in the proof of Lemma 2.4; note that
[TABLE]
To see the second identity in (2.12), we recall (1.5) and note that
[TABLE]
for . Therefore, we have
[TABLE]
Since the last term is equal to , this shows the second identity with
[TABLE]
In particular, for of the form (1.6), we have
[TABLE]
This leads to the desired formula (2.13). ∎
We have the following lemma for the last term in (2.8).
Lemma 2.6**.**
Recalling that , , is Bernoulli, we have
[TABLE]
where .
Proof.
The proof is straightforward. In fact, we have by definition
[TABLE]
and therefore,
[TABLE]
This shows the conclusion. ∎
The results obtained in Lemmas 2.4, 2.5 and 2.6 are summarized in the following corollary. Note that the discretized hydrodynamic equation (2.2) exactly cancels the first order term in . Therefore only quadratic or higher order terms in survive. We denote the solution of (2.2) simply by .
Corollary 2.7**.**
We have
[TABLE]
where . In particular, when are given by (1.6), omitting to write the dependence on , this is equal to
[TABLE]
where stands for , and and are defined similarly.
3 Proof of Theorem 2.1
We prove in this section Theorem 2.1. In view of Proposition 2.3 and Corollary 2.7, our goal is to estimate the following expectation under by the Dirichlet form and the relative entropy itself, where and , :
[TABLE]
Note that the condition (A7)′ implies that appearing in the definition of is bounded; see the comments given below Theorem 4.1. From the condition (A4) combined with Proposition 4.3 stated below, the first term in (3.1) can be treated similarly to the second, but with the front factor replaced by ; see Section 3.3 for details.
3.1 Replacement by local sample average
Recall that we assume have the form (1.6) by the condition (A1) so that has the form (2.13). With this in mind, recall the definition of defined in (2.15):
[TABLE]
where is defined in Corollary 2.7. The first step is to replace by its local sample average defined by
[TABLE]
where
[TABLE]
for functions and . Since will be smaller than , one can regard as a subset of . The reason that we consider both and is to make defined by (3.4) satisfy the condition for any .
Proposition 3.1**.**
We assume the conditions of Theorem 2.1 and write and by omitting . For small enough, we choose when and when . Then, the cost of this replacement is estimated as
[TABLE]
for every with some when and the last is replaced by when .
The first step for the proof of this proposition is the flow lemma for the telescopic sum. We call a flow on a finite graph connecting two probability measures and on if and hold for all . We define a cost of a flow by
[TABLE]
The following lemma has been proved in Appendix G of [25].
Lemma 3.2** (Flow lemma).**
For each , let be the uniform distribution on and set . Then, there exists a flow on connecting the Dirac measure and such that with some constant , independent of , where
[TABLE]
The flow stated in Lemma 3.2 is constructed step by step as follows. For each , we first construct a flow connecting and such that with some . Then we can obtain the flow connecting and by simply summing up : . It is not difficult to see that the cost of is bounded by . Finally, we define the flow connecting and by
[TABLE]
whose cost is bounded by ; see [25] for more details.
Recall defined in Lemma 3.2 and note that can be regarded as a probability distribution on . Set , then we have
[TABLE]
and similarly . Therefore,
[TABLE]
where is defined in Lemma 3.2 and . Note that supp. Let be a flow given in Lemma 3.2. Accordingly, since is a flow connecting and , one can rewrite
[TABLE]
For the last line, we introduced the change of variables for the sum in . Thus, we have shown
[TABLE]
where
[TABLE]
Note that satisfies for any . Indeed, in (3.4), only if or , namely, or , but these are not in due to the condition (A1) for .
Another lemma we use is the integration by parts formula under the Bernoulli measure with a spatially dependent mean. We will apply this formula for the function .
Lemma 3.3** (Integration by parts).**
Let and assume holds for with some . Let be a function satisfying for any . Then, for a probability density with respect to , we have
[TABLE]
and the error term is bounded as
[TABLE]
with some , where .
Proof.
First we write
[TABLE]
Then, by the change of variables and noting the invariance of under this change, we have
[TABLE]
To replace the last by , we observe
[TABLE]
with
[TABLE]
By the condition on , this error is bounded as
[TABLE]
These computations are summarized as
[TABLE]
For the second term denoted by , applying the change of variables again, we have
[TABLE]
since and . This completes the proof. ∎
We apply Lemma 3.3 to given in (3.3). However, in (3.3) depends on which varies in space. We need to estimate the error caused by this spatial dependence.
Lemma 3.4**.**
(1)* Assume that and satisfy the same conditions as in Lemma 3.3. Then, we have*
[TABLE]
and the error term is bounded as
[TABLE]
*with some .
(2) In particular, for defined in (3.4), we have*
[TABLE]
and
[TABLE]
Proof.
By the definition of , we have
[TABLE]
For , we have
[TABLE]
On the other hand, can be rewritten as
[TABLE]
For , one can apply Lemma 3.3 to obtain
[TABLE]
Finally for , observe that
[TABLE]
Therefore, we obtain (1). Since for any , taking and changing the sign of both sides, (2) is immediate from (1). ∎
We can estimate the first term in the right hand side of (3.5) by the Dirichlet form of the Kawasaki part and obtain the next lemma.
Lemma 3.5**.**
Let satisfy the condition in Lemma 3.3 with . Then, for every , we have
[TABLE]
with some , where
[TABLE]
is a piece of the Dirichlet form corresponding to the Kawasaki part considered on the bond and the error term is given by Lemma 3.4.
Proof.
For simplicity, we write for . By decomposing f(\eta^{x,y})-f(\eta)=\big{(}\sqrt{f(\eta^{x,y})}+\sqrt{f(\eta)}\big{)}\big{(}\sqrt{f(\eta^{x,y})}-\sqrt{f(\eta)}\big{)}, the first term in the right hand side of (3.5) is bounded by
[TABLE]
for every . Applying the change of variables , the second term of the last expression is equal to and bounded by
[TABLE]
This shows the conclusion. ∎
We now give the proof of Proposition 3.1.
Proof of Proposition 3.1.
By Lemma 3.5, choosing with , we have
[TABLE]
For , since from the condition (A4) combined with Proposition 4.3 stated below, estimating , we have
[TABLE]
Thus, estimating for the second term of (3.6) (though this term has a better constant , the same term with arises from ), we obtain
[TABLE]
We assume without loss of generality that is an integer and that for notational simplicity. Then, for the second term of the right hand side in (3.7), we first decompose the sum as regarding . Note that the random variables are independent for each . Recall that . Then, applying the entropy inequality, we have
[TABLE]
Now we apply the concentration inequality (see Appendix B of [24]) for the last term:
Lemma 3.6** (Concentration inequality).**
Let be independent random variables with values in the intervals . Set and . Then, for every , we have
[TABLE]
In fact, since is a weighted sum of independent random variables, from this lemma, we have
[TABLE]
for every , where is a universal constant and is the variance of . On the other hand, it follows from the flow lemma that . Therefore, we have
[TABLE]
Thus, taking , we have shown
[TABLE]
with some . For small enough, choose when and when . Then, recalling in the condition (A6)δ, when , we have
[TABLE]
which shows (3.2). When ,
[TABLE]
This shows the conclusion for and the proof of Proposition 3.1 is complete. ∎
3.2 Estimate on
The next step is to estimate the integral . We assume the same conditions as in Proposition 3.1 and therefore Theorem 2.1. We again decompose the sum as and then, noting the -dependence of , use the entropy inequality, the elementary inequality and the concentration inequality to show
[TABLE]
for with small enough. Roughly saying, by the central limit theorem, both and behave as in law for large , respectively, where denotes a Gaussian random variable with mean [math] and variance . This effect is controlled by the concentration inequality. When , we chose so that we obtain
[TABLE]
When , we chose so that we obtain (3.11) with replaced by .
3.3 Estimates on three other terms
Two terms and defined in (2.15) can be treated exactly in a same way as and we have similar results to Proposition 3.1 and (3.11) for these two terms.
The term requires more careful study. As we pointed out at the beginning of this section, the condition (A4) combined with Proposition 4.3 shows that
[TABLE]
Therefore, the front factor behaves like instead of . Noting this, for the replacement of with , we have a similar bound (3.8) with replaced by . However, since , one can absorb even by the factor with as in (3.9) and (3.10) (with replaced by ). Thus, the bound (3.2) in Proposition 3.1 holds also for in place of .
On the other hand, (3.11) should be modified as
[TABLE]
Note that (3.12) holds with instead of in an averaged sense in as we will see in Lemma 4.4. But this is not enough to improve (3.13) with to .
3.4 Completion of the proof of Theorem 2.1
Finally, from Proposition 2.3, Proposition 3.1 (for ) and (3.11) (for ), (3.13) (for ), choosing small enough such that , we obtain
[TABLE]
with some () when and () when . Thus, Gronwall’s inequality shows
[TABLE]
Noting with and from in the condition (A6)δ, this concludes the proof of Theorem 2.1, if we choose small enough.
Remark 3.1**.**
The above argument actually implies for some . From Theorem 4.1, the probability in the left hand side of (1.11) is bounded above by for sufficiently large, recall defined below (2.6). On the other hand, from the proof of Proposition 2.2, there exists a constant , which depends only on , such that . These estimates together with the entropy inequality show that
[TABLE]
for sufficiently large. This gives the rate of convergence in the limit (1.11).
4 Motion by mean curvature from Glauber-Kawasaki dynamics
The rest is to study the asymptotic behavior as of the solution of the discretized hydrodynamic equation (2.2), which appears in (2.6). We also give a few estimates on which were already used in Section 3.
Theorem 4.1 formulated below is purely a PDE type result, which establishes the sharp interface limit for and leads to the motion by mean curvature. Recall that we assume . A smooth family of closed hypersurfaces in is called the motion by mean curvature flow starting from , if it satisfies
[TABLE]
where is the inward normal velocity of and is the mean curvature of multiplied by . It is known that if is a smooth hypersurface without boundary, then there exists a unique smooth solution of (4.1) starting from on with some ; cf. Theorem 2.1 of [5] and see Section 4 of [16] for related references. In fact, by using the local coordinate for in a tubular neighborhood of where is the signed distance from to and is the projection of on , is expressed as a graph over and represented by , , , and the equation (4.1) for can be rewritten as a quasilinear parabolic equation for . A standard theory of quasilinear parabolic equations shows the existence and uniqueness of smooth local solution in . We cite [1] as an expository reference for the definitions of mean curvature, motion by mean curvature flow and Allen-Cahn equation. As we mentioned above, Section 4 of [16] also gives a brief review of these topics.
The limiting behavior of as is given by the following theorem. Recall that the solution is extended as a step function on as in (2.5).
Theorem 4.1**.**
Under the conditions (A2), (A3) and (A5), for and , converges as to defined by (1.10) from the hypersurface in moving according to the motion by mean curvature (4.1).
Combining the probabilistic result (2.6) with this PDE type result, we have proved that converges to in probability when multiplied by a test function . This completes the proof of our main Theorem 1.1.
Under the condition (A7)′, especially with chosen as , by the comparison theorem (Proposition 4.5 below) for the discretized hydrodynamic equation (2.2) and noting that, if (or ), the solution of (2.2) increases in toward (or decreases to ) by the condition (A2), the condition implies the same for . In particular, this shows with some for all and .
4.1 Estimates on the solutions of the discretized hydrodynamic equation
We give estimates on the gradients of the solutions of the discretized hydrodynamic equation (2.2). These were used to estimate the contribution of the first term in (3.1) and also in (3.6) as we already mentioned. Let be the discrete heat kernel corresponding to on . Then, we have the following global estimate in .
Lemma 4.2**.**
There exist such that
[TABLE]
where and stands for the standard Euclidean norm of as we defined before.
Proof.
Let be the heat kernel corresponding to the discrete Laplacian on . Then, we have the estimate
[TABLE]
with some constants , independent of and , where . For example, see (1.4) in Theorem 1.1 of [6] which discusses more general case with random coefficients; see also [30]. Then, since
[TABLE]
the conclusion follows. ∎
We have the following -estimate on the gradients of .
Proposition 4.3**.**
For the solution of (2.2), we have the estimate
[TABLE]
if holds.
Proof.
From Duhamel’s formula, we have
[TABLE]
By noting is bounded and applying Lemma 4.2, we obtain the conclusion. ∎
It is expected that behaves as near the interface by the scaling property (see Section 4.2 of [17] and also as Theorem 4.6 below suggests) and decays rapidly in far from the interface where would be almost flat. In this sense, the estimate obtained in Proposition 4.3 may not be the best possible. In a weak sense, one can prove the behavior (instead of ) for as in the next lemma.
Lemma 4.4**.**
We have
[TABLE]
Proof.
By multiplying u_{x}(t)\,\big{(}=u^{N}(t,x)\big{)} to the both sides of (2.2) and taking the sum in , we have
[TABLE]
Here, we have used the bound . Since , we have the conclusion. ∎
4.2 Proof of Theorem 4.1
For the proof of Theorem 4.1, we rely on the comparison argument for the discretized hydrodynamic equation (2.2); cf. [14], Proposition 4.1 of [15], Lemma 2.2 of [18] and Lemma 4.3 of [19].
Assume that has the following property: If satisfies (i.e., for all ) and for some , then holds. Note that given in (2.3) with of the form (1.6) has this property, since is increasing and is decreasing in in this partial order by the condition (A3).
Proposition 4.5**.**
Let be super and sub solutions of
[TABLE]
Namely, satisfies (4.2) with “”, while satisfies it with “” instead of the equality. If , then holds for all . In particular, one can take the solution of (4.2) as or .
Proof.
Assume that and hold at some . Since are super and sub solutions of (4.2), we have
[TABLE]
On the other hand, noting that
[TABLE]
and that by the assumption, we have . This shows that can not exceed for all . ∎
For with sufficiently small, one can find a traveling wave solution , which is increasing in and its speed by solving an ordinary differential equation:
[TABLE]
where are two stable solutions of . Note that and . The solution is unique up to a translation and one can choose satisfying ; see [5], p.1288. Note also that the traveling wave solution is associated with the one-dimensional version of the reaction-diffusion equation and not with the discrete equation (4.2). Indeed, solves the equation
[TABLE]
which is a one-dimensional version of (1.3) or (1.9) with considered on the whole line in place of with replaced by and connecting two stable solutions at .
Let be the motion of smooth hypersurfaces in determined by (4.1). Let be the signed distance function from to , and similarly to [5], p.1289, let be a smooth modification of such that
[TABLE]
where is taken such that is smooth in the domain . We define two functions by
[TABLE]
Applying Proposition 4.5 and repeating computations of Lemma 3.4 in [5], we have the following theorem for defined by (2.5) from the solution of (2.2). The functions describe the sharp transition of and change their values quickly from one side to the other crossing the interface to the normal direction.
Theorem 4.6**.**
We assume the conditions (A2), (A3) and (A5), in particular is smooth and the following inequality (4.3) holds at . The condition on can be relaxed and we assume for . Then, taking large enough, there exists such that
[TABLE]
holds for every , , and .
Proof.
Let us show that
[TABLE]
for every with some . We decompose
[TABLE]
The term can be treated as in [5], from the bottom of p.1291 to p.1293. Note that in their paper corresponds to here, and they treated the case with a non-local term, which we don’t have. Since we can extend in the definition of super and sub solutions in their paper to (i.e., we can take instead of ) for every , we briefly repeat their argument by adjusting it to our setting. The case with noise term is discussed by [14], pp.412-413.
In fact, can be decomposed as
[TABLE]
where
[TABLE]
by just writing instead of (i.e., here ) in [5], p.1292 noting that , and in our setting. Repeating their arguments, one can show that, if is large enough compared with , hold for some , and since . Therefore, we obtain
[TABLE]
For the rest in (4.4), since and so that are smooth in , we have
[TABLE]
The first one follows from Taylor expansion for up to the third order term, while the second one follows by taking the expansion up to the first order term. Therefore, if , these terms stay bounded in and are absorbed by estimated in (4.6) with chosen large enough. Thus, we obtain . The lower bound by is shown similarly. ∎
Theorem 4.1 readily follows from Theorem 4.6 by noting that we have from the definitions of ,
[TABLE]
for and .
Remark 4.1**.**
The choice in the definition of the super and sub solutions is the best. In fact, in stead of , if we take with , then we may consider but this diverges so that also must diverge. On the other hand, if , as the above proof shows, we don’t have a good control.
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