Hydrodynamic limit for the Ginzburg-Landau $\nabla\phi$ interface model with non-convex potential
Jean-Dominique Deuschel, Takao Nishikawa, Yvon Vignaud

TL;DR
This paper extends the hydrodynamic limit analysis of the Ginzburg-Landau $ abla ext{phi}$ interface model to non-convex potentials, addressing challenges in identifying equilibrium states and establishing uniform variance estimates.
Contribution
It proves the equivalence between stationarity and the Gibbs property for non-convex potentials and completes the characterization of equilibrium states at high temperature.
Findings
Established the equivalence between stationarity and Gibbs property.
Completed the identification of equilibrium states in high temperature regime.
Derived uniform variance estimates for extremal Gibbs measures.
Abstract
Hydrodynamic limit for the Ginzburg-Landau interface model was established in [Nishikawa, 2003] under the Dirichlet boundary conditions. This paper studies the similar problem, but with non-convex potentials. Because of the lack of strict convexity, a lot of difficulties arise, especially, on the identification of equilibrium states. We give a proof of the equivalence between the stationarity and the Gibbs property under quite general settings, and as its conclusion, we complete the identification of equilibrium states under the high temparature regime in [Deuschel and Cotar, 2008]. We also establish some uniform estimates for variances of extremal Gibbs measures under quite general settings.
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsStochastic processes and statistical mechanics · Theoretical and Computational Physics · Material Dynamics and Properties
\RCS
Hydrodynamic limit for the Ginzburg-Landau interface model with non-convex potential
Jean-Dominique Deuschel and Takao Nishikawa and Yvon Vignaud
J.-D.Deuschel: Institut für Mathematik, Technische Universität Berlin, Berlin, Germany
E-mail address: [email protected]
T. Nishikawa: Department of Mathematics, College of Science and Technology, Nihon University, Tokyo, Japan
E-mail address: [email protected]
Y. Vignaud: Lycée Jean Jaurès, Argenteuil, France
Abstract.
Hydrodynamic limit for the Ginzburg-Landau interface model was established in [12] under the Dirichlet boundary conditions. This paper studies the similar problem, but with non-convex potentials. Because of the lack of strict convexity, a lot of difficulties arise, especially, on the identification of equilibrium states. We give a proof of the equivalence between the stationarity and the Gibbs property under quite general settings, and as its conclusion, we complete the identification of equilibrium states under the high temparature regime in [2]. We also establish some uniform estimates for variances of extremal Gibbs measures under quite general settings.
1. Introduction
We consider the large scale hydrodynamic behavior of the the Ginzburg-Landau interface model. This is an effective interface model, describing the stochastic dynamic of the separation of two distinct phases.
The position of the interface is described by height variables measured from a fixed -dimensional discrete hyperplane . Here, we will take when we consider the system on a discretized torus with the periodic boundary condition, or when we consider the system on the domain with Dirichlet boundary condition. is a microscopic domain corresponding to a given macroscopic domain which is bounded and has a smooth boundary. See Section 2 for the precise definition.
The corresponding Hamiltonian on for given height variable is of the form
[TABLE]
with a symmetric function . The Langevin equation associated with is given by
[TABLE]
where in the drift term is defined by
[TABLE]
and is a family of independent copies of the one dimensional standard Brownian motion.
The aim of this paper investigate and identify the hydrodynamic limit of at diffusive scaling, that is, for time while for space. In the case of a strictly convex potential for which there exist two constants such that
[TABLE]
the hydrodynamic limit has been established for periodic lattice in [7] and for discretized domain with Dirichlet boundary conditions in [12]. In particular, the corresponding macroscopic motion is identified as the solution of the nonlinear partial differential equation
[TABLE]
where the surface tension is defined via thermodynamic limit.
In these results, the condition (1.1) plays an essential role in the analysis for the stochastic dynamics , especially, in the identification of equilibrium states and the establishment of the strict convexity of . The our aim in this paper is to prove the hydrodynamic limit without the strict convexity assumption (1.1), see Assumptions 2.1, 2.2 and 2.3 for details.
Our motivation comes from recent results in [2] and [3] where both strict convexity of the surface tension and identification of the extremal gradient Gibbs measures hold, for non-convex potential at sufficiently high temperature.
In the case of the dynamics on the torus , the limit follows quite simply from additional estimates. However, for the dynamics on the discretized domain with the Dirichlet boundary condition, the derivation is much harder, since we can not use the relative entropy and entropy production. The main step then is to characterize the set of stationary measures for the gradient field associated with the infinite system of SDEs, which is essentially used in order to establish local equilibrium as in [12] without using the relative entropy and the entropy production.
In case of strictly convex , the structure of the translation invariant stationary measures is completely identified by [7], its proof relying the assumption (1.1). To complete our proof of the hydrodynamic limit in the non-convex case, we need to identify the class of translation invariant stationary measures as the class of Gibbs distributions.
This subject has been intensively studied in the literature, cf. [9] for stochastic Ising models, [10] for the diffusion process on the infinite dimensional torus , [5] for the diffusion process on , [13] for the diffusion process on the infinite product with a Riemannian manifold with positive curvature. In this paper we show the similar result, adapting the argument of [5] to gradient Gibbs distributions. The main challenge here is the lack of ellipticity of the gradient dynamic, see Section 3 and 5 for details.
An alternative derivation of the hydrodynamic limit for the Ginzburg-Landau model based on a two scale argument has been proposed by [8] and [6]. Unlike our proof, relying on the assumption on the uniqueness of the extremal gradient Gibbs distribution, the two scale argument uses logarithmic Sobolev inequalities. However, this approach seems restricted to the one-dimensional case in [8], respectively strict convexity assumption for the potential (1.1) in [6].
Before closing this section, let us give briefly the organization of this paper. In Section 2, we formulate our problem more precisely, and state the main result. In Section 3, we present some properties of translation invariant stationary measures, especially, the relationship between stationarity and the Gibbs property, and some uniform estimates for their variances. Note that results in this section hold under the quite general Assumption 2.1. In Section 4, after establishing a priori bounds for stochastic dynamics and summarize properties of the surface tension, we derive the macroscopic equation from the stochastic dynamics. Here, we rely quite explicitly on the further Assumptions 2.2 and 2.3. In Section 5, we give a proof of Theorem 3.1, presented at Section 3.
2. Model and main result
2.1. Model
Let be a bounded domain in with a Lipschitz boundary. For convenience, let contain the origin of . Let be the discretized microscopic domain corresponding to in the sense that
[TABLE]
where stands for the hypercube in with center and side length , that is,
[TABLE]
On we consider the dynamics governed by the following stochastic differential equations (SDEs)
[TABLE]
with the boundary condition
[TABLE]
with some and initial data , where for and , or more generally for and . The height variable in (2.2) is defined by
[TABLE]
for every , where is a function belonging to . We note that the function describes the macroscopic boundary condition and the height variable describes the microscopic one.
We make the following assumption on the interaction potential :
Assumption 2.1*.*
The function has the following representation:
[TABLE]
where functions are symmetric functions and satisfy
- (1)
There exist constants such that
[TABLE] 2. (2)
There exists a constant such that
[TABLE]
Example 2.1*.*
If a function is symmetric and satisfies
[TABLE]
for some and , then the function admits the decomposition as in Assumption 2.1. Indeed, we can take as follows:
[TABLE]
with . Letting , that is,
[TABLE]
we can easily see that and they fulfill conditions (1) and (2) in Assumption 2.1.
Further assumptions dealing with the strict convexity of the surface tension and the characterization of extremal gradient Gibbs measures are stated below, see Assumptions 2.2 and 2.3 for details.
We regard (2.1) as the model describing the motion of microscopic interfaces and introduce the macroscopic height variable as follows:
[TABLE]
where being the solution of (2.1) with (2.2).
2.2. Notations
Before stating the detail of our main result, we need to introduce several notations. Note that we will follow the same manner as in [7] and [12].
Let be the set of all directed bonds in . We write and for . We denote the bond by again if it doesn’t cause any confusion. For every subset of , we denote the set of all directed bonds included and touching by and , respectively. That is,
[TABLE]
For , the gradient is defined by
[TABLE]
Now, let be the family of all gradient fields which satisfy the plaquette condition (2.1) in [7], i.e., . Let be the set of all such that
[TABLE]
We denote equipped with the norm . We introduce the dynamics governed by the SDEs
[TABLE]
where is the family of independent one dimensional Brownian motions. Since the coefficients are Lipschitz continuous in , this equation has the unique strong solution in for every . Note that defined from the solution of the SDE (2.1) on satisfies (2.4) for and boundary conditions for when letting for .
Since we define Gibbs measures on by Dobrushin-Lanford-Ruelle (DLR, for short) equation, we the finite volume Gibbs measure in advance. For a finite set and fixed , we define the affine space by
[TABLE]
We define the finite volume Gibbs measure on by
[TABLE]
where is the Lebesgue measure on and is the normalizing constant.
Let be the set of all probability measures on and let be those satisfying for each . The measure is sometimes called tempered. Let be the family of translation invariant, tempered Gibbs measures introduced by [7], namely, the family of satisfying the Dobrushin-Lanford-Ruelle equation
[TABLE]
where is the -algebra generated by . Note that the dynamics given by (2.4) is reversible under . We denote the family of with ergodicity under spatial shifts by .
2.3. Assumptions on Gibbs measures and the surface tension
In order to derive the hydrodynamic limit, we will assume both uniqueness of the extremal gradient Gibbs distributions and strict convexity of the surface tension. These assumption are always satisfied under (1.1), cf. see [4] and [7], or for non-convex potential at sufficiently high temperature, cf. [2] and [3]. On the other hand, at critical temperature, Biskup and Kotecký give an example of gradient Gibbs measures with two different extremal states, cf. [1]. The derivation of the corresponding hydrodynamic limit in this case is very challenging open problem.
More precisely, let be the periodic lattice and be the set of all directed bonds in . With , we consider the finite volume Gibbs measure on by
[TABLE]
where is Lebesgue measure on , is the normalizing constant and is defined by for with and . We denote the law of by .
Assumption 2.2*.*
For each there exists a unique extremal such that
[TABLE]
Furthermore, it can be obtained as the weak limit of the periodic Gibbs as .
Under Assumption 2.2, the sequence defined by
[TABLE]
has a limit. We thus define the (normalized) surface tension surface tension by
[TABLE]
Moreover, we can show the following thermodynamic identities between the surface tension and ergodic Gibbs measures:
[TABLE]
which will be shown in Section 4.2. They play an essential role in the derivation of the hydrodynamic limit.
Further we need some technical assumption on the regularity of which are well known in the strictly convex case (1.1), cf. [7] or in the high temperature regime [2].
Assumption 2.3*.*
The surface tension is and is Lipschitz continuous. Furthermore, is strictly convex in the following sense: there exist two constants satisfying
[TABLE]
Remark 2.1*.*
Note that the convexity of the surface tension, alternatively defined in terms of fixed boundary conditions has been established in [11] under very general conditions. Moreover, the strict convexity (i.e. lower bound in (2.9) with ) is not essential for the hydrodynamic limit since an approximation of could be implemented as in [7].
The following example shows that our Assumptions 2.2 and 2.3 hold in the high temperature regime:
Example 2.2*.*
We introduce a positive parameter corresponding to the inverse temperature, that is, the potential takes the form
[TABLE]
where the symmetric functions satisfy
[TABLE]
for some and for some . Then for , (independent of !) of the form
[TABLE]
both Assumptions 2.2 and 2.3 are satisfied when , see [2] and its arXiv version (arXiv:0807.2621v1 [math.PR]).
2.4. Main Result
The main result in this paper is the following:
Theorem 2.1**.**
We assume Assumptions 2.1, 2.2 and 2.3. Furthermore, we assume that there exists satisfying the following:
- (1)
The function has a compact support in . 2. (2)
The sequence of initial data for (2.1) satisfies
[TABLE]
where is the macroscopic height variable corresponding to .
Then, for every , converges in as to which is the unique weak solution of the partial differential equation (PDE)
[TABLE]
where . Here, the function is the surface tension. More precisely, for every ,
[TABLE]
holds.
3. Stationary measures and estimate for variance
In this section, we mainly discuss properties of stationary measures of (2.4) while working on the general assumption, Assumption 2.1. We believe that the results of this section are relevant beyond the derivation of the hydrodynamic limit.
3.1. Generator of (2.4) and stationary measures
We at first note that the infinitesimal generator of (2.4) is given by
[TABLE]
where
[TABLE]
To keep notation simple, we sometimes denote by if it doesn’t cause any confusion.
We can see that the Gibbs property implies reversibility under (2.4), and therefore stationarity, see Proposition 3.1 in [7] for details. We note that the same argument as in [7] is applicable in quite general setting, including ours. In Theorem 2.1 of [7], the equivalence of the Gibbs property and stationarity is shown using (1.1), here we show this result using another approach.
Theorem 3.1**.**
We assume Assumption 2.1. If is invariant under spatial shift and a stationary measure corresponding to , i.e.,
[TABLE]
*then is a Gibbs measure, i.e., (2.5) holds. *
Since the proof of Theorem 3.1 is slightly long, we postpone the proof until the end of this paper, see Section 5.
3.2. Uniform bound for the variance for stationary measures
If the potential is a strictly convex function satisfying (1.1), we then get the uniform bound for the variance for Gibbs measures as a direct consequence of the Brascamp-Lieb inequality. See [4] for details. Our next result based on dynamical approach shows that the variance remains bounded in the tilt for general potentials under Assumption 2.1.
Theorem 3.2**.**
We assume Assumption 2.1. Let be the family of stationary measures for the gradient field (2.4) which are tempered, translation invariant and ergodic under spatial shift. The variance of under are bounded from above by a constant independent of , that is,
[TABLE]
holds.
Proof.
We shall show the desired bound by arranging the argument of the proof of Proposition 2.1 of [7]. We fix and we define the vector by
[TABLE]
Let be the solution of SDEs (2.4) with initial distribution . Introducing by
[TABLE]
and
[TABLE]
where is an arbitrary chain connecting [math] to , we then obtain that solves the SDEs
[TABLE]
Our calculation will be based on the energy estimate for introduced above.
Let and . For a deterministic with
[TABLE]
we obtain
[TABLE]
with a martingale by Itô’s formula. Performing summation-by-parts, we get
[TABLE]
We thus have
[TABLE]
where and are defined by
[TABLE]
From now on, we shall give bounds for expectations of and separately.
We at first give a estimate for the expectation of . Here, the same argument as the proof of (2.14) in [7] can be applied. That is, from ergodicity and temperedness of , we have
[TABLE]
and this implies that
[TABLE]
We therefore obtain that for every there exists such that
[TABLE]
holds for every .
We shall next calculate and its expectation. From Assumption 2.1, can be calculated as follows:
[TABLE]
Using Schwarz’s inequality, we obtain the following estimate for the second term :
[TABLE]
for arbitrary . If holds, we then have
[TABLE]
by taking . Note that the estimate (3.5) trivially holds when . Summarizing above and taking expectation, we obtain
[TABLE]
Here, we have used
[TABLE]
which follows from the definition of and . From the relationship , the stationarity of and the definition of , we have
[TABLE]
Since is translation invariant, we also have
[TABLE]
with a constant . Applying above, we finally conclude
[TABLE]
We next calculate the expected value of . Putting by
[TABLE]
we have
[TABLE]
from the definition of . We shall thus calculate instead of . Using Schwarz’s inequality, we obtain
[TABLE]
for an arbitrary , where and are define by
[TABLE]
For , since is Lipschitz continuous, there exists a constant such that
[TABLE]
by using the translation invariance of . For , let us use a similar argument to the proof of (2.12) in [7]. Taking , we have
[TABLE]
for every . For the term , the calculations runs quite parallel to the argument in [7] and we can obtain that for every there exists such that
[TABLE]
holds for every . Let us give a bound for the term . Using Itô’s formula, we obtain
[TABLE]
and therefore we get
[TABLE]
Similarly to (3.4), we obtain that for every there exists such that
[TABLE]
holds for every . We also obtain
[TABLE]
by a simple calculation. We shall estimate the term . We note that
[TABLE]
where
[TABLE]
Here, we have used
[TABLE]
which follows from the definition of and the symmetry of . We therefore obtain
[TABLE]
Summarizing above, we conclude the following: for every there exists such that
[TABLE]
for every and with a constant . Note that the constant does not depend on while may depend on . Combining (3.7) with (3.8) and (3.9), we get the following bound for :
[TABLE]
for every and large enough.
Inserting (3.4), (3.6) and (3.10) into the expectation of (3.2) divided by , we obtain
[TABLE]
for every and large enough. Here, taking and recalling the definition of and , we obtain
[TABLE]
with constants . We emphasize that constants appearing on (3.11) does not depend on . Choosing large enough such that
[TABLE]
we conclude the desired bound. ∎
Remark 3.1*.*
The argument in the proof of Theorem 3.2 can be applied also to the finite volume Gibbs measures defined in Section 2.3. Under Assumption 2.1, the variance of under are bounded from above by a constant independent of and , that is,
[TABLE]
holds. The above implies that the sequence is tight for given and every limit point is a tempered, translation invariant Gibbs measure.
4. The proof of Theorem 2.1
In this section, we shall complete our main result, Theorem 2.1. To do so, we at first summarize properties of the surface tension . The estimate established in the previous sections will play a key role in the proofs. After that, we finish the proof of Theorem 2.1.
4.1. A priori bounds for the macroscopic height variable
We shall derive the bound corresponding to Proposition 4.1 in [12]. Once we have Proposition 4.1 and Theorem 3.1 in Section 3, we can follow the argument of [12] assuming that the limit of the initial datum is smooth enough.
Proposition 4.1**.**
There exists a constant depending and such that
[TABLE]
where is defined by for .
Proof.
Using Itô’s formula, we have
[TABLE]
where is a martingale. Performing the summation-by-parts at the second term in the right hand side, we obtain
[TABLE]
Here, we have used the boundary condition for and . For the main part , we have
[TABLE]
from the strict convexity of . Next, we have for
[TABLE]
where the constant is defined by
[TABLE]
Finally, for , we have
[TABLE]
for an arbitrary . Choosing , we have
[TABLE]
Summarizing above, we get
[TABLE]
Taking the expectation, we obtain the conclusion.∎
4.2. Surface tension and thermodynamic identities
In this subsection, we verify several properties of surface tension . Note that in view of our estimate of the variance, Theorem 3.2, we easily can get the identity (2.7) following the argument of [7]. The proof of the second equality (2.8) is more delicate, since, in view of the missing higher moment estimate, we cannot apply immediately apply the argument of [7].
Proposition 4.2**.**
For every translation-invariant, ergodic Gibbs measure , we have
[TABLE]
Proof.
Let and we denote simply by . We define by for . We at first note that
[TABLE]
holds by the summation-by-parts. Since we have
[TABLE]
from the DLR equation and the integration-by-parts, we obtain
[TABLE]
On the other hand, we have
[TABLE]
and therefore we obtain
[TABLE]
Since we have
[TABLE]
by translation-invariance of and also have
[TABLE]
by translation-invariance of and the identity (2.7), we obtain the conclusion once we have
[TABLE]
By Schwarz’s inequality, we have
[TABLE]
for an arbitrary . Let us estimate the first term in the right hand side. Let us take arbitrarily. We can then take such that (3.9) with holds for every . Choosing as , we obtain
[TABLE]
which shows (4.1) since is bounded uniformly in . ∎
Finally, we shall establish similar decomposition for as in Section 3.3 of [12]. Applying the arguments there, we can obtain the uniform -bound with and the oscillation inequality for the discrete version of (2.11).
Proposition 4.3**.**
There exist a -valued function and a matrix-valued function satisfying
[TABLE]
such that the identity
[TABLE]
holds.
Proof.
We at first recall the relationship between the surface tension and the Gibbs measures:
[TABLE]
where is the ergodic Gibbs measure with mean . Using and in Assumption 2.1, we shall take as
[TABLE]
and as
[TABLE]
It is easy to verify (4.3) and (4.2) with and defined above by using Assumption 2.1. Furthermore, the property is an immediate consequence of Theorem 3.2 and Schwarz’s inequality. ∎
4.3. Derivation of the macroscopic equation
We shall at first summarize the properties satisfied by the solution for the discretized PDE introduced in Section 3.1 of [12]. Since we have assumed the strict convexity of at Assumption 2.3, we obtain a priori bounds for in and , see Proposition 3.1, Corollary 3.2 in [12]. Furthermore, since we have (4.3), we obtain the uniform bound of in and the oscillation inequality, see Propositions 3.3 and 3.4 in [12].
We next verify the coupled local equilibrium. Applying Theorem 3.1, Proposition 4.1 and the bound for stated above, we see that Proposition 4.2 in [12] is still valid. Summarizing above, we obtain that the arguments in Section 4.4 works completely, and we can finally conclude Theorem 2.1.
5. Proof of Theorem 3.1
Our proof follows the argument of [5] however special care is required in view of the non ellipticity of the generator .
5.1. Generator and Dirichlet form
In this section, we mainly discuss properties of stationary measures of (2.4) while working on the general assumption, Assumption 2.1.
Since the calculation is based on the generator and the Dirichlet form, we shall introduce them before starting discussion.
We recall that the infinitesimal generator of (2.4) is given by
[TABLE]
where
[TABLE]
We also recall that we sometimes denote by for simplicity.
We also introduce the finite version of (5.1). We at first introduce the state space for that. We define for a finite set by
[TABLE]
Note that introduced in Section 2.2 and are state spaces for the dynamics with the boundary condition given by and free boundary condition, respectively. For a finite set we define the differential operator and by
[TABLE]
and
[TABLE]
respectively. Here, is the operator defined by
[TABLE]
The former is the generator associated to the dynamics on for given , which is governed by SDEs
[TABLE]
The dynamics is reversible under the finite volume Gibbs measure introduced in Section 2.2. The latter is the generator associated to governed by SDEs
[TABLE]
on , which corresponds to the dynamics (2.4) with free boundary condition. The character “” in notions means free boundary condition. Here, and are defined by
[TABLE]
for . Note that is also reversible and the reversible measure is
[TABLE]
on , where is the Lebesgue measure on and is the normalizing constant. The Dirichlet form associated to is given by
[TABLE]
which plays a key role in the proof of the main theorem in this section, Theorem 3.1.
5.2. Proof of Theorem 3.1
In this subsection, let us complete the proof of Theorem 3.1, which is based on the method of [5]. Main tool is the integration-by-parts formula for and entropy production rate. For the computation, we introduce a small lemma:
Lemma 5.1**.**
Let be a finite subset of .
- (1)
Let be a probability density on . Then, the image measure of by the discrete gradient is nothing but the Lebesgue measure on . 2. (2)
If is the form , then
[TABLE]
holds. Especially, if is -measurable, we have
[TABLE]
Proof.
It is easy to see that
[TABLE]
for every and bounded , which indicates that the integral
[TABLE]
does not depend in the choice of a probability density . Now, we check that the image measure has uniformity in . For , there exists the such that and
[TABLE]
holds. For a bounded function , we have
[TABLE]
which shows the first assertion.
For , we obtain
[TABLE]
which shows the second assertion. ∎
Let us start to prove Theorem 3.1. We at first introduce by
[TABLE]
where
[TABLE]
For we define by
[TABLE]
where is the height variable satisfying and . Note that is uniquely determined by and . We also define by
[TABLE]
Applying Lemma 5.1, we can easily verify that is probability density on . Let . Since , we have
[TABLE]
Multiplying whose support is in , and integrating in by the uniform measure on , we obtain
[TABLE]
Applying Lemma 5.1, the right hand side is calculated as follows:
[TABLE]
where is the measure on defined by
[TABLE]
with a probability density on . Here, we have used the relationship
[TABLE]
for by the symmetry of . Noting
[TABLE]
we obtain that the right hand side of (5.4) is computed as follows:
[TABLE]
We shall first calculate . Performing integration-by-parts in , we have
[TABLE]
Noting that integrands of and the first term in the right hand side of (5.5) are function of , each integral does not depend on the choice of by Lemma 5.1 and therefore the second term does not also. On the other hand, since the second term converges to zero if taking the limit with , we conclude that the second term must be zero.
Let us choose as
[TABLE]
with some bounded smooth function and
[TABLE]
Noting
[TABLE]
we have
[TABLE]
Next, we shall compute . Performing the integration-by-parts in again, we have
[TABLE]
Summarizing (5.4), (5.7) and above, we obtain
[TABLE]
if we take as in (5.6), where is defined by
[TABLE]
We note that if we can take , the left hand side coincides with the entropy production rate, that is,
[TABLE]
holds, where is the probability density with respect to given by
[TABLE]
In this case, we simply denote by . Before continuing the discussion for , we shall verify the integrability of integrands in (5.9) with .
Lemma 5.2**.**
For every , the integral (5.9) is finite if .
Proof.
We at first note that
[TABLE]
By the definition of , we have for
[TABLE]
and
[TABLE]
Here, we have used
[TABLE]
On the other hand, we have for
[TABLE]
and
[TABLE]
We conclude that is square-integrable.
Next, let us verify that is also square-integrable. Note that
[TABLE]
and
[TABLE]
for some from Lipschitz continuity of . It is easy to see that the first term is finite by using temperedness of . We can obtain that the second term is also finite since we have
[TABLE]
and
[TABLE]
by the definition of . ∎
Using , we can now bound the right hand side of (5.8):
Lemma 5.3**.**
Assume that the function satisfies for every . We then have bounds for and in (5.8) as follows:
[TABLE]
with some constants independent in and , where is defined by
[TABLE]
Proof.
We at first obtain
[TABLE]
by the assumption on . We therefore get
[TABLE]
for some constant , which shows (5.13). We note that is equal to zero if is not on the boundary of . Also for (5.14), we obtain
[TABLE]
for some constant by applying (5.11) and (5.12) again. ∎
Summarizing above and applying Schwarz’s inequality, we obtain
[TABLE]
By taking limit to with keeping and applying Fatou’s lemma.
[TABLE]
Here, using Jensen’s inequality and shift-invariance and temperedness of , we get
[TABLE]
with a constant independent of and , and therefore get
[TABLE]
Summarizing (5.15) and (5.16), we get
[TABLE]
We note that the left hand side of (5.17) coincides with the entropy production rate, that is, the identity
[TABLE]
holds, where the probability measure on is defined by . We note that the core of Dirichlet form is the family of smooth -measurable functions.
For , let us take by
[TABLE]
where . Because boxes appearing above are disjoint, we get
[TABLE]
On the other hand, we have
[TABLE]
where the right hand side is the entropy production rate defined by
[TABLE]
for a finite and on or with large enough. Repeating the argument as in the proof of Lemma 4.2 in [7], we obtain the Gibbsian property of .
Aknowledgement
The first author thanks RIMS at Kyoto University and The University of Tokyo for the kind hospitality and the financial support. The second author was partially supported by the grant for scientific research by College of Science and Technology, Nihon University.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] M. Biskup and R. Kotecký, Phase coexistence of gradient Gibbs states , Probab. Theory Related Fields 139 (2007), no. 1-2, 1–39. MR 2322690 (2008 d:82024)
- 2[2] C. Cotar and J.-D. Deuschel, Decay of covariances, uniqueness of ergodic component and scaling limit for a class of ∇ ϕ ∇ italic-ϕ \nabla\phi systems with non-convex potential , Ann. Inst. Henri Poincaré Probab. Stat. 48 (2012), no. 3, 819–853. MR 2976565
- 3[3] C. Cotar, J.-D. Deuschel, and S. Müller, Strict convexity of the free energy for a class of non-convex gradient models , Commun. Math. Phys. 286 (2009), 359–376.
- 4[4] J.-D. Deuschel, G. Giacomin, and D. Ioffe, Large deviations and concentration properties for ∇ φ ∇ 𝜑 \nabla\varphi interface models , Probab. Theory Relat. Fields 117 (2000), 49–111.
- 5[5] J. Fritz, Stationary measures of stochastic gradient systems, infinite lattice models , Z. Wahrsch. Verw. Gebiete 59 (1982), no. 4, 479–490. MR MR 656511 (83j:60108)
- 6[6] T. Funaki, Hydrodynamic limit for the ∇ φ ∇ 𝜑 \nabla\varphi interface model via two-scale approach , Probability in Complex Physical Systems: In Honour of Erwin Bolthausen and Jürgen Gärtner, Springer Proceedings in Mathematics, vol. 11, Springer, Heidelberg, 2012.
- 7[7] T. Funaki and H. Spohn, Motion by mean curvature from the Ginzburg-Landau ∇ ϕ ∇ italic-ϕ \nabla\phi interface model , Commun. Math. Phys. 185 (1997), 1–36.
- 8[8] N. Grunewald, F. Otto, C. Villani, and M.G. Westdickenberg, A two-scale approach to logarithmic Sobolev inequalities and the hydrodynamic limit , Ann. Inst. Henri Poincaré Probab. Stat. 45 (2009), no. 2, 302–351. MR 2521405 (2010 c:60293)
