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Mountain pass type solutions for a generalized Frenkel-Kontorova model
Abstract.
We study a generalized Frenkel-Kontorova model and obtain periodic and heteroclinic mountain pass solutions. Heteroclinic mountain pass solution in the second laminations is new to the generalized Frenkel-Kontorova model. Our proof follows that of Bolotin and Rabinowitz for an Allen-Cahn equation, which is different with heat flow method for finding critical point of Frenkel-Kontorova model in the literature. The proofs depend on suitable choices of functionals and working spaces. We also study the multiplicity of these mountain pass solutions.
Key words and phrases:
Mountain pass solution; periodic solution; heteroclinic solution; Frenkel-Kontorova model2020 Mathematics Subject Classification:
Primary: 49J35; Secondary: 74G22, 74G351. Introduction
In this paper, we study a generalized Frenkel-Kontorova (or FK) model. To introduce the FK model, we need some notations. Let (resp. ), etc. denote the elements of (resp. ) and define . Fix and set . Assume that satisfies (cf. [16]):
-
(S1)
, where is the constant function on ;
-
(S2)
is bounded from below and coercive in the following sence,
-
(S3)
for with , while for ;
-
(S4)
there is some constant such that for all .
For , set
where is defined by with , i.e., the th component is and others . With these local potentials , we can define the formal sum
and its Euler-Lagrange equation
(1.1) |
(1.1) is the equation of our generalized FK moldel.
FK model was first proposed in 1938 ([10]), since then it “has become one of the fundamental and universal tools of low-dimensional nonlinear physics” ([6, p. VII, line 16]). FK model is constituted by a chain of atoms subjected to a periodic potential and is described by the following equation:
Here is -periodic. Equilibrium or stationary state of FK model is a function satisfying
(1.2) |
Our generalized FK model (1.1) is a generalization of (1.2) by setting
and , where . So solutions of (1.1) are also called equilibrium or stationary state of the generalized FK model.
In 1983, Aubry and Le Daeron ([1]) studied minimal solutions of (1.2) and obtained the classification of minimal solutions. Minimal solutions are one of the important classes of equilibrium state. For (1.2), a function is said to be minimal if
(1.3) |
for any with a finite set. Aubry and Le Daeron found that minimal solution did not cross with any of its translation , which led to an oriented homeomorphism map of a circle and then a rotation number. Using rotation number Aubry and Le Daeron made the classification of minimal solutions. Now their results are called Aubry-Mather theory because Mather ([13]) obtained similar results for monotone twist maps of annulus.
After the establishment of Aubry-Mather theory, Moser [15] attempted to generalize this theory to elliptic PDE. He found that for higher dimensional space, minimal solution might cross with its translation. So he posed another property, i.e., without self-intersections on minimal solution. In other words, Moser asked satisfied one and only one of the following inequality holds:
(1.4) |
Moser and then Bangert ([2]) studied a class of elliptic PDE and they obtained similar results of Aubry-Mather theory. Now their results are called Moser-Bangert theory ([17]). Bolotin, Rabinowitz, Stredulinsky ([17, 3, 4, 5]) studied an Allen-Cahn equation, which belonged to the elliptic PDE of Moser and Bangert. They used variational methods to construct more homoclinic and heteroclinic solutions of the Allen-Cahn equation other than Moser and Bangert’s.
In [16, 14, 11], Birkhoff minimizers (corresponding to minimal and without self-intersections solutions in Moser-Bangert theory) have been established and multitransition solutions was constructed in [12]. In this paper, we shall use the methods of [3, 4] to establish a new type of solution, mountain pass solution. Noting that in [16, 14, 11, 12], (1.1) was studied without the assumption (S4) except in [16]. Our results can be seen as a new proof and a refinement of some results of [16] (see also [8, 9]). Note that we only consider the case of rotation vector . In [16], Mountain Pass Theorem was also used to establish critical point. But to prove Mountain Pass Theorem (cf. [16, Lemma 8.6]), Mramor and Rink asked the functional to be a Morse function. If the functional is a Morse function, they obtained a ghost circle which contained a periodic mountain pass solution. When the functional is not a Morse function, using a limiting progress, Mramor and Rink established a ghost circle that contained a stationary solution. If a gap of periodic minimal and Birkhoff solutions is not filled up by minimal solutions, the above stationary solution should be not minimal. The proofs of this paper are more direct than that of [16]. We also establish heteroclinic mountain pass solution in the second laminations (please see [14] for the definition of second laminations) while Mramor and Rink’s result only holds for the “first” lamination.
But we point out that in [16], the authors obtained non-minimal solution for rotation vector such that the Aubry-Mather set had gap, provided that ghost circle was not consists of minimizers. In [8, 9], the authors showed that there was some critical point in the gap of ground states of some FK model for any rotation vector such that gap (in the “first” lamination) condition held. Our result does not cover these cases and we limit ourselves in the case that . We also prove the multiplicity of mountain pass solutions which is new to this generalized FK model. Other FK type models (cf. [8, 9] and references there in) may be studied using the method of the present paper and will be considered in the future.
This paper is organized as follows. We introduce some definitions and lemmas in Section 2. In Section 3, periodic mountain pass solution is established and it is proved that there are infinitely many solutions of this type. Heteroclinic mountain pass solution is considered and the multiplicity is studied in Section 4. In Appendix A, we present the detailed proofs of some properties of Section 3. A heat flow method for proving the existence of mountain pass solution is also included in Appendix A.
2. Preliminary
We review some definitions and some lemmas of [16, 14, 11, 12]. Assume satisfies (S1)-(S3) in this section. For functions , means for all , and similarly one define etc. The following lemmas provide important comparison results.
Lemma 2.1 (cf. [14, Lemma 2.6]).
For and an arbitrary finite set , we have
Lemma 2.2 (cf. [11, (3.1)]).
If satisfies for fixed , then there is a subsequence of converging pointwise.
Lemma 2.3 (cf. [14, Lemma 2.5]; [16, Lemma 4.5]).
Assume that and are solutions of (1.1) and . Then either or .
A function is said to have bounded action if there exists , such that for all with (cf. [14, p. 1525, line -3], [11, p. 1112, line -8]).
Lemma 2.4 (cf. [14, Lemma 2.4], [11, Lemma 2.11]).
Assume have bounded action with bounded constant . Then there exists a constant such that for any finite set ,
Here the closure of a set is defined by .
Definition 2.5.
-
•
(cf. [16, Definition 2.3]) A function is said to be minimal for potentials (or for potential ) if for every finite subset and every with support, denoted by , included in ,
where the support of is and interior of is .
- •
For , let
If , we use to replace Similarly for , one define , which consists of functions that is periodic in with periods .
2.1. Periodic minimal and Birkhoff solutions
For , define , and . It was proved in [11] that was ordered and consisted of minimal and Birkhoff solutions of (1.1). Replacing by and minimizing the corresponding functional, we do not obtain more periodic solutions, as stated in the following.
For , let
and . For , define
(2.1) |
The following lemma was proved in [11] by Moser’s method (cf. [15], see also [17, Proposition 2.2]).
Lemma 2.6 (cf. [11, Proposition 3.1]).
Let and Then Moreover, and .
Suppose that constitutes a lamination, or in other words, there is a gap in , i.e.,
() |
Here adjacent means there does not exist such that . In [11], heteroclinic minimal and Birkhoff solutions are constructed under condition ().
2.2. Heteroclinic minimal and Birkhoff solutions in
To construct heteroclinic minimal and Birkhoff solutions, assume that () holds. Let . Set . For , define , then it was proved in [11, Proposition 3.2] that for some . Thus we can define
(2.2) |
and we have (by [11, Lemma 3.3])
(2.3) |
Set
For , as was proved in [11, Proposition 3.4], if , then
In other words, becomes in the definition of . Set
Then, as was proved in [11], is attained and
is an ordered set and consists of heteroclinic minimal and Birkhoff solutions of (1.1). Moreover, we have
Lemma 2.7 (cf. [12, Proposition 2.13]).
Suppose () holds and with . If satisfies (1.1) for (resp. ), then as (resp. as , where and or .
Similar to Section 2.1, varying the periods of function in cannot produce more minimal and Birkhoff solution. To see this, for let
Set
(2.4) |
For , define
and
Similar to (2.2) is well-defined and it satisfies
Lemma 2.8 (cf. [11, Proposition 3.4]).
For , if ,
Remark 2.9.
Similar to Lemma 2.6, we have
Lemma 2.10 (cf. [11, Proposition 3.20]).
Let and . Then Moreover, , and .
3. Mountain pass solutions in the gap of
Assume that satisfies (S1)-(S4) in this and the following two sections. We establish periodic mountain pass solution of (1.1) in this section. Firstly we introduce the working space and the corresponding functional. For , set
It is easy to see that is a Banach space. Define as in Section 2.1 and assume that () holds. For , set . Then since , and
(3.1) |
where is the Fréchet derivative of . If , then
hold for all . Hence by the periodicities of and , is a solution of (1.1).
3.1. Periodic mountain pass solution
Consider the semiflow , which is defined by
(3.2) |
Set , then for any . For ,
(3.3) |
where is the constant in (S4) and are constants depending only on . By Cauchy-Lipschitz-Picard Theorem (please see e.g., [7, Theorem 7.3]), is well-defined and is in . For , we have the following comparison result.
Proposition 3.1.
Assume . If and , then for all .
The proof of Proposition 3.1 follows from [16, Theorem 6.2] with slight modifications. For the reader’s convenience, we provide the proof of Proposition 3.1 in Appendix A. Result similar to Proposition 3.1 also appears in [9]. In [9], one need a “transitive” condition ([9, p. 2414, line 7]). In our settings, (S3) ensures this condition.
As in [4], we choose a subset of to prove the deformation lemma. Set
It is easy to see that is a compact set with respect to the norm , as shown in the following proposition.
Proposition 3.2.
is compact with respect to the norm .
Proof.
Assume . By the definition of , we only need to prove that is compact with respect to pointwise convergence, which follows from Lemma 2.2. ∎
Remark 3.3.
Proposition 3.2 will be used in the proof of deformation lemma (please see Lemma 3.4 (v) below). In the proof of [3, Proposition 3.6], Bolotin and Rabinowitz obtained “compactness” by verifying the corresponding functional satisfied Palais-Smale condition. In our settings, the compactness condition is directly obtained.
We have the following deformation lemma.
Lemma 3.4.
In [16, Lemma 8.6], the authors established Mountain Pass Theorem by imposing a condition that the functional was a Morse function. This condition is used to prove a similar property of Lemma 3.4 (v). We prove Lemma 3.4 in Appendix A. Now set
and
Proposition 3.5.
.
Proof.
By Lemma 2.6, for any ,
(3.4) |
So . Suppose, by contradiction, . Then there exist and such that
(3.5) |
and
(3.6) |
(3.7) |
Since , a compact set by Proposition 3.2, has a subsequence (still denoted by ) which converges in to . Since is continuous on , by (3.4) and (3.7),
Then . Hence or . But by (3.6),
a contradiction. So . ∎
Theorem 3.6.
is a critical value of on with a corresponding critical point satisfying and is a solution of (1.1).
Proof.
Suppose, by contradiction, . Lemma 3.4 (v) implies that there exists such that
(3.8) |
By the definition of , there is an satisfying
Then by Lemma 3.4 (i) and (iii), we have . But by (3.8),
which is impossible by the definition of . Thus and is a critical value with a corresponding critical point , so . Since is a solution of (1.1), by Lemma 2.3, . ∎
Remark 3.7.
As in [4], we prove that is indeed a mountain pass critical value as follows. Set
and
So is a classical mountain pass critical value. We have:
Proposition 3.8.
.
Proof.
Remark 3.9.
There is another candidate of solution, the maximum of on , in the gap of .
Proposition 3.10.
Proof.
Remark 3.11.
If such that , then choose such that hold for all . The argument in Proposition 3.10 shows that .
If obtained in Proposition 3.10 is a solution of (1.1), then by Lemma 2.3, . Conversely, if , by Proposition 3.10, is a solution of (1.1). Unfortunately, we do not know whether obtained in Proposition 3.10 is a solution of (1.1) for general .
But for , we see , thus is a solution of (1.1). In fact, as one can easily see, is same to the mountain pass solution of Theorem 3.6.
For , may be coincide with and it may not give more solutions. To see this, we examine the classical Frenkel-Kontorova model.
Example.
Let and , . Set
Then is attained at () and is attained at (). Assume the gap pair is and . So and is attained at () and is attained at ().
On the other hand,
In the gap of , there is one locally maximum point , and there are two mountain pass critical points and but no other locally maximum point exists. Please see Figure 1 for the graph of .

3.2. Multiplicity of periodic mountain pass solutions
We shall prove that varying will produce more periodic mountain pass solutions. This is different with periodic minimal and Birkhoff solutions (cf. Section 2.1, Lemma 2.6). Toward this end, for , assume . By Theorem 3.6, there exists such that is a mountain pass solution. Since , . It is possible that . But we shall show this cannot happen for infinite many . First we have
Proposition 3.12.
There is a constant , independent of , such that
Proof.
To estimate we need to construct a suitable . To do so, we first define the following for .
If is even, set
For , set
Lastly set
and for . Extend as a -periodic function on .
If is odd, then is even and thus is well-defined for and by the previous paragraph. Now define for and . Let for and then extend as a -periodic function on .
For the above , set
(3.11) |
Letting gives . Notice that for , , on for at most two points, and for any , is monotone nondecreasing in . Thus we have
for some independent of . Hence for , . Enlarging if necessary shows that hold for all , thus Proposition 3.12 is proved. ∎
Now we prove the multiplicity of periodic mountain pass solutions.
Theorem 3.13.
The set is infinite.
Proof.
If is replaced by , similar arguments of this section give more periodic mountain pass solutions. What happens if we change the coordinate systems ? we learn from [11, Lemma 5.4] that if with and the vectors are linearly independent, then we do not obtain more periodic minimal and Birkhoff solutions. Different with minimal and Birkhoff solutions, changing coordinate systems produces more periodic mountain pass solutions. To see this, for simplicity set , , and for . Set . Denote by the set of critical points of on in the coordinate sysetems . Let be the critical point that are -periodic in and -periodic in . Assume . Notice that by Proposition 3.12 and Theorem 3.13 there are infinitely many functions of this type. We have:
Proposition 3.14.
.
Proof.
Suppose, by contradiction, for some . Since , there is some such that
(3.12) |
Certain classes of sets which consist of solutions of (1.1) attracts researchers’ attention. When the elements in the set have good order property, the set becomes a foliation or lamination. With the periodic mountain pass solutions in hand, one may wonder: is there a possibility that the periodic mountain pass solutions constitute a foliation or lamination? Unfortunately, the answer is “negative”. (In fact, we construct some periodic solutions that are cross. These periodic solutions are suspected to be mountain pass type. Please see Remark 3.21 below.) To this end, we need the following definition.
Definition 3.15.
We say touches from below (resp. above) if (resp. ), and there exists such that . We say intersects if there are , such that .
Set
and
Then . Similar to Theorem 3.6, is a critical value of with a corresponding critical point in . By Proposition 3.1 and Lemma 3.4, , where is defined as in (3.2). For , set . For , define
where satisfying and is a solution of (1.1). By the periodicity of and , means
-
(a)
, or
-
(b)
touches from below, or
-
(c)
.
For , (a) will not hold. We need the following lemma.
Lemma 3.17.
For , either or touches from below.
Proof.
For , and then . We have the following three cases.
-
(1)
Assume . Then and we are throuth.
-
(2)
Assume touches from below. Then and we are throuth.
-
(3)
Assume . Then .
-
(a)
If , then so is , contradicting the definition of .
-
(b)
If touches from below, then so is .
-
(a)
Thus either or touches from below. ∎
Since is continous, is attained. Similar results hold for . Moreover, have the following monotone property.
Proposition 3.18.
Assume .
-
(1)
If for all , then the map (resp. ) is monotone nondecreasing (monotone non-increasing).
-
(2)
Assume there is some such that . If such is unique, then for all . If for and is the maximal interval owning this property, then and .
Proof.
Remark 3.19.
We suspect that in the case (1) of Proposition 3.18, either is strictly increasing or for some . To support this, suppose .
-
•
If touches from below, then . Indeed, by Proposition 3.1, for . In particular, . If then , a contradiction.
-
•
If , then . Indeed, suppose, by contradiction . Then by Lemma 3.17, either or touches from below. Both cases contradict .
But we do not know if there are such that touches from below and .
Theorem 3.20.
Proof.
By Proposition 3.12 and its proof, for there are and such that
By Proposition 3.5, . Then for large ,
(3.14) |
Since are monotone, we have
Lemma 3.4 (iv) shows that there are a and a sequence as such that
and is a solution of (1.1). Note that by (3.14) and Lemma 3.4 (ii),
(3.15) |
thus and then . We claim that intersects . Noticing that are solutions of (1.1), if does not intersect , then by Lemma 2.3 either (i) or (ii) . If (i) holds, by the definition of , there is some , such that . But by the periodicity of and , for large enough,
a contradiction. If (ii) is satisfied, by the definition of , there exists such that . But
for large , again a contradiction. Thus Theorem 3.20 is proved by setting . ∎
Remark 3.21.
Since obtained by Theorem 3.20 are lying in the gap of , by Lemma 2.2 we can extract a subsequence converging to a function such that is a solution of (1.1).
Corollary 3.22.
Proof.
Since , either or .
- (1)
-
(2)
Now assume . By Lemma 2.7, there are satisfying
(3.16) -
(a)
If , then is a homoclinic solution.
-
(b)
Otherwise suppose and assume there is no subsequence of converging to homoclinic solution. Without loss of generality, set and . Then is a heteroclinic solution. In this case, it is interesting that we can construct another solution of (1.1). Indeed, for , by (3.16) there exists satisfying
(3.17) Since pointwise as , there is a such that for ,
Thus we have and provided sufficiently small. But noticing that is -periodic in , we obtain
and with . Hence there is a such that
(3.18) Let . Then proceeding as for , we have that pointwise for some satisfying and . If , then similar to (1), is a new solution which is different with since . So we assume . We claim
(3.19) Suppose (3.19) holds for the moment. Then (3.18) implies
(3.20) Hence applying Lemma 2.7 shows that
Since we assume there is no subsequence of converging to homoclinic solution, so is a heteroclinic solution from to .
-
(a)
4. Mountain pass solutions in the gap of
We construct heteroclinic mountain pass solution in this section. The difference is that the sum in the definition of of (2.1) involves only finite many terms, but in this section a new functional, , will be a sum of infinitely many terms. Suppose that () and () hold. For , set
(4.1) |
Obviously is a Banach space with norm . In fact, this norm is on .
Remark 4.1.
The norm will be used in a similar result of Lemma 3.4 (v) of the deformation lemma. In the proof of Lemma 3.4 (v), can be replaced by equivalent norm since there are only finite many terms. But for infinitely many term in the definition of , cannot be replaced by any more. Noticing that to show is , one need the norm , which cannot be replaced by . Please see the proof of Proposition 4.3.
For , define
where is defined in Section 2.2. For simplicity, set and . Since implies for some , we have and
Thus by Lemma 2.8 and Remark 2.9,
is well-defined and if , then
(4.3) |
Since we use a modified Mountain Pass Theorem to show the existence of critical point, the functional should be well-defined from to and be . Fortunately, this is the case, as the following two propositions show.
Proposition 4.2.
For any , and thus (4.3) holds.
Proof.
Proposition 4.3.
We have . If , i.e., is a critical point of , then is a solution of (1.1).
Proof.
Firstly, we prove that is Gateaux differentiable. For , and ,
Since , . Thus we have
(4.5) |
Now following Section 3, let us define semiflow as follows:
Set . Similar proof of (3.3) shows that for some . The proof of is easier (cf. (4.6)). So is well-defined and is in . Moreover, a new version of Proposition 3.1 is obtained.
Set
Note that if and ,
(4.7) |
In other words, .
Proposition 4.4.
is compact with respect to the norm .
Proof.
Set
Hence one have new versions of Lemma 3.4, Proposition 3.5 and Theorem 3.6. Thus we obtain a mountain pass critical point and then a heteroclinic mountain pass solution satisfying for any . Next we study the multiplicity of heteroclinic mountain pass solutions. It sufficies to prove a silimlar result of Proposition 3.12. To this end, for each , let .
Set
Then is a mountain pass critical value of on with a corresponding mountain pass critical point such that with and is a solution of (1.1). We have:
Proposition 4.5.
There is a constant , independent of , such that
Proof.
For , let , then
Set where is defined in (3.11). To prove Proposition 4.5, it suffices to show that
(4.8) |
holds for some independent of . Note
for any . For any , let
By the construction of , consists of at most two regions, say () of the form with . Therefore
(4.9) |
Then
(4.10) |
Then by (4.9), the cardinality of
is at most a finite number, denoted by , independent of , where
Proceeding as in Theorem 3.13 we obtain infinitely many heteroclinic mountain pass solutions. When we want to go further as in Section 3 to see that heteroclinic mountain pass solutions do not constitute a foliation or laminaion, we encounter more difficulties. For instance, in the definition of , means either touches from below or . But for unbounded domain , besides the above two possibilities, may lead to and
(4.12) |
Notice that (4.12) always holds since as . Thus if one want to show a result similar to Theorem 3.20, one need a new idea to exclude the third possibility in the proof of Theorem 3.20.
Remark 4.6.
We can obtain another heteroclinic mountain pass solution lying in the gap of (please see [11] for the definition) and we can construct more heteroclinic mountain pass solutions by the methods of Sections 3 and 4 for higher dimension (cf. [11, Section 5]). Thus in the gap of the second laminations (in the sense of [14]) we have heteroclinic mountain pass solutions.
Remark 4.7.
Throughout this paper, only the minimal and Birkhoff solutions corresponding to rotation vector are considered (for the definition of rotation vector, please see [11]). One can generalize the above results to minimal and Birkhoff solutions corresponding to rotation vector and obtain corresponding mountain pass solutions.
Appendix A Appendix
In this appendix, we prove Proposition 3.1, Lemma 3.4 and Theorem 3.6 of Sections 3. First is the proof of Proposition 3.1, which follows [16, Theorem 6.2] with slight modifications.
Proof of Proposition 3.1. Define . So , and satisfies the following linear ODE:
Similar calculation of (3.3) implies is Lipschitz. By (S3)-(S4), there is an such that the operators are positive: implies .
Note moreover that both the and the are uniformly bounded operators, whence the ODEs and define well-posed initial value problems. More importantly, solves if and only if solves . We will now prove that for every and every , . Then, obviously, as well, which then completes the proof of Proposition 3.1.
To prove the claim on , we solve the initial value problem for by Picard iteration, that is we write
where the are defined inductively by
Observe that the positivity of implies that the are positive as well. Because and , we can therefore estimate, for any with ,
(A.1) | ||||
Now choose a such that and recall that . Then from (A.1) it follows that if , then for all , .
To generalize to the case that , let us choose a sequence of lattice points such that and . Then, by induction, for any . Thus, if and , then . ∎
Next we prove Lemma 3.4.
Proof of Lemma 3.4. (i). Suppose . Then is a solution of (1.1), thus for all . So is a solution of the initial problem:
By the uniqueness of the solution of the above initial problem, .
(iv). By (A.2) and Lemma 2.6, is non-increasing with a lower bound . So has a limit as . Since
we have
for some sequence . Since , a compact set by Proposition 3.2, there is a such that in along a subsequence of . Note that is continuous, thus
which implies
i.e., is a solution of (1.1).
(v). Firstly we claim that: there exists a constant such that if , then
(A.3) |
Here is the dual space of the Banach space and . Indeed, if the claim fails then for any , there are satisfying
as . But since , a compact set by Proposition 3.2, we may assume that as and . Thus , which contradicts . So (A.3) holds.
Now we prove (v). Suppose, by contradiction, that there is a such that , then for all . Since
(A.4) |
we have
contrary to the existence of . Here the third equality follows from (A.2) and the first inequality follows from (A.3)-(A.4). ∎
Now a heat flow method is used to give the following (cf. [5, Proposition 2.12]):
Another proof of Theorem 3.6. For , let . Set , then for any , . We claim that:
there is a satisfying for all . |
Indeed, for any there exists such that . We can extract a subsequence of , say converging to some as . If for some , then for large . Then enlarging if necessary such that , by Lemma 3.4 (ii), , which is a contradiction. Thus the claim holds.
By Lemma 3.4 (iv), there is a subsequence of converging to some such that is a solution of (1.1) and
By Proposition 3.2, letting (up to a subsequence) completes the proof of Theorem 3.6. ∎
Acknowledgments
The author wishes to express his gratitude to Professor Zhi-Qiang Wang (Utah State University) for helpful discussion and for giving me a lot of encouragement. The author is supported by the Fundamental Research Funds for the Central Universities (no. 34000-31610274).
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