On Unique Continuation for Non-local Dispersive Models

We consider unique continuation properties of solutions to a family of evolution equations. Our interest is mainly on nonlinear non-local models. This class contains the Benjamin–Ono, the Intermediate Long Wave, the Camassa–Holm, the dispersion generalized Benjamin–Ono and non-local Schrödinger equations as well as their generalizations. We shall review, discuss, expand, and comment on several results. In addition, we shall state some open questions concerning these results and their techniques.


Introduction
In this manuscript we shall study unique continuation properties (UCP) of solutions to some time evolution equations.We are interested in two types of UCP: local ones and asymptotic at infinity.
For local ones we mean the following : if u 1 , u 2 are solutions of the equation which agree in an open set Ω (in the space-time space), then u 1 , u 2 agree in their domain of definition.
Roughly, asymptotic at infinity implies : if u 1 , u 2 are solutions of the equation such that at two different times t 1 , t 2 then u 1 , u 2 are equal in their domain of definition.Here ||| • ||| may represent a weighted norm or an asymptotic behavior at infinity.
For the linear equation one can fix u 2 ≡ 0. In the nonlinear case, a weaker version of these UCP is obtained by assuming that u 2 ≡ 0 is the second solution.In this case, for the nonlinear equation and u 2 ≡ 0, the asymptotic at infinity UCP can be rephrased in the question : what is the strongest possible decay at two different times of a nontrivial solution ?
The "norm" in (1.1) may depend on the time t j , j = 1, 2 and as we will see in some cases one needs three times to achieve the desired result.
The local UCP can be considered in solutions of the associated initial value problem (IVP), initial boundary value problem and mixed problems.In this work, we shall restrict ourselves to the IVP and to the initial periodic boundary value problem (IPBVP).Also, the asymptotic at infinity UCP will be only considered here in solutions of the associated IVP.
It is clear that these UCP should be examined in non-hyperbolic equations.Even in this class, non-hyperbolic models, these UCP may fail.For example, it was proved in [105] that the (generalized Kortewegde Vries) equation possesses traveling waves solution u(x, t) = φ c (x−ct) with c > 0, called compacton, of the form ( We observe that φ c (x − ct) is a classical solution of (1.2) with compact support.Thus, taking u 1 (x, t) = φ c (x−ct) and u 2 (x, t) = φ c (x−ct+4π) one gets a counterexample for our UCP's above.Also, in [4] it was proved that the porous medium equation possesses non-negative compact support (generalized) solutions.
Although our main interest here are non-local nonlinear dispersive problems, we shall first review the known UCP results for the Kortewegde Vries equation.This will allow us to illustrate the difference with the non-local case.Next, we shall consider the Benjamin-Ono equation (section 3), the Intermediate Long Wave equation (section 4), the Camassa-Holm equation (section 4) and related models, the dispersion generalized Benjamin-Ono equation (section 5), and the general non-local Schrödinger equation (section 6).
We observe that the Korteweg-de Vries equation as well as the equations in sections 2-4 are completely integrable models, and the models in sections 3-6 are non-local ones.Except for those in section 6, all the models are one dimensional.
As we shall see below the local UCP results for these nonlocal models are based in stationary arguments.Some of them are classic ones other have been proven recently and are interesting in their own right.

The Korteweg-de Vries equation
In this section we shall study the UCP on solutions to the Kortewegde Vries (KdV) equation.The KdV equation was first derived as a model of propagation of waves on shallow water surfaces [82].The KdV equation was the first equation to be solvable by means of the inverse scattering transform [48].As it was already mentioned we shall use it to illustrate the difference with the non-local case.Thus, we shall examine the associated IVP, i.e.
and that for its k-generalized form (k-gKdV) for which only the cases k = 1, 2 are completely integrable.
The IVP and IPBVP (as well as other mixed problems) associated to the k-gKdV (2.2) have been extensively analyzed.In particular, their local and global well-posedness, the asymptotic behavior of their solutions, the stability of their special solutions (traveling waves and breathers) among other related topics have attracted great amount of attention, see [90], [114], [79] and references therein.In particular, we recall that the equation (2.2) has traveling wave solutions u(x, t) = φ k (x − t) of the form which belongs to the Schwartz class S(R).
Concerning the local UCP for solution of (2.2) we observe and are also solutions of the k-gKdV equation in the domain R × (t 1 , t 2 ).Similar result applies to the case of the difference u 1 −u 2 of two solutions u 1 , u 2 of the k-gKdV equation.Thus, in the k-gKdV (and in any local model) the local and asymptotic at infinity UCP are related.This is not the case when one considers a non-local model for which the argument in (2.4)-(2.5)does not apply.
In the same regard, as we will see below, in a non-local model the hypothesis in the local UCP can be replaced by the weaker one : if u 1 , u 2 are solutions of the non-local equation such that exist a time t 1 and an open set I in the space variable, such that (i) then This reflects the stationary character of the arguments used in their proofs.
One has that for the KdV equation (or any local model) the condition (i) in (2.6) combined with the equation implies that in (ii).In fact, under the hypothesis (2.6) the local UCP fails for the KdV (or any local model) by just taken t 1 = 0 and appropriate initial data u 1 (x, 0) and u 2 (x, 0).
Concerning the local UCP for the KdV equation we have the following result obtained in [110].
(1) Although the precise definition is not relevant for our discussion here, the type of solutions considered in [110] is quite general.
(2) The proof of Theorem 2.1 in [110] is a consequence of a general Carleman estimate deduced there.It applies to a very general class of solutions to local time evolution equation.The local character of the equation is essential in the argument of the proof.
Next, we consider the asymptotic at infinity UCP for the KdV equation and the k-gKdV equation.In this regard we have: (1) The proof of Theorem 2.3 is based on the inverse scattering method, using the fact that the KdV is a completely integrable model.It cannot be applied to the difference of any two solutions u 1 , u 2 , since it requires to have u 2 ≡ 0.Moreover, it only applies to integrable cases.
(1) The proof of Theorem 2.5 is based on the inverse scattering method.In particular, it needs to assume that u 2 ≡ 0. Similar, result is unknown for any nonlinearities k = 1 of the k-gKdV equation (2.2).
(3) The fact that the decay of the data generates a gain of regularity on the solution was previously observed and studied in [72].
(1) The solution of the associated linear IVP to the k-gKdV in (2.2) is given by the group {V (t) : t ∈ R} where is the Airy function which satisfies the decay estimate + , which explains the exponent 3/2.
(2) The previous remark suggests that the decay of the fundamental solution of the associated linear IVP provides the appropriate weight for the "norm" in the asymptotic at infinity UCP, see . In general, this is not the case.For example, the fundamental solution of the linear Schrödinger equation does not decay.In this case, the weight in (1.1) is related to uncertainty principles for the Fourier transform.In fact, this weight may be different at time t 1 and t 2 , see [37].
(3) For previous results related to Theorem 2.7 see [103] and references therein.
We observe that the decay condition in Theorem 2.7 requires only one side decay at infinity condition.Thus, one may ask if by assuming a decay condition holding at booth of the real line sides this can be relaxed.For example, question : if u 1 , u 2 are appropriate solutions of the k-gKdV equation (2.2) such that does this imply that u 1 ≡ u 2 ?
To conclude this section we recall the so called "soliton resolution conjecture".This affirms, roughly speaking, that for generic initial data the corresponding solution of the k-gKdV will eventually resolve into a radiation component that disperses like a linear solution, plus a localized component that behaves like a soliton or multi-soliton solutions (or breathers).Assuming it, one expects that for large time t to have at most at decay u(x, t) ∼ e ax as x ↑ ∞, since the solitons for the k-gKdV satisfy it, see (2.3).A precise result in this direction seems to be unknown.

The case of the Benjamin-Ono equation
Next, we shall consider the Benjamin-Ono (BO) equation where H denotes the Hilbert transform The BO equation was first deduced in [7] and [100] as a model for long internal gravity waves in deep stratified fluids.Later, it was shown to be a completely integrable system [2].We recall that the BO equation possesses traveling wave solutions (solitons) u(x, t) = φ(x − t) of the form which is smooth but it exhibits a very mild decay in comparison with that of the k-gKdV (2.2) described in (2.3).The well-posedness of the IVP and the IPBVP for the BO equation and its generalized k-form k-gBO equation, i.e.
has been broadly studied, we refer to [109] for a survey of these results.
Next, we shall introduce the following notation: The known asymptotic at infinity UCP for the BO equation are embedded in the following well-posedness result in weighted spaces Z s,r : [45] after [66]- [67]).Let u ∈ C([0, T ] : H 5 (R)) be the solution of the IVP for the BO equation (3.1) with data u 0 .
( (2) The proof of Theorem 3.1 is based on weighted energy estimates and relies on several inequalities for the Hilbert transform H.Among them the so called where 1/p+1/p = 1.In particular, |x| α ∈ A p if and only if α ∈ (−1, p−1).It was shown in [62] that the Hilbert transform H is bounded in L p (wdx) if and only if w satisfies (3.7).Moreover, it was established in [102] that in the case p = 2 the operator norm is a multiple of c 2 (w) in (3.7).The proof uses these results although not in their strongest versions.Also, the proof of Theorem 3.1 relies on commutator estimates for the Hilbert transform H, mainly the following : for The case k + m = 1 corresponds to the Calderón commutator estimate [18].The general case of (3.8) was deduced in [5].For a different proof see [30].
(3) The result in Theorem 3.1 is due to the connection between the dispersive relation (modeling by an operator with non-smooth symbol) and the nonlinearity of the BO equation (3.1).In particular, one can see that if u 0 ∈ Ż5,4 with xu 0 (x)dx = 0, then the solution U (t)u 0 (x) of the associated linear IVP However, for the same data u 0 one has that the corresponding solution u(x, t) of the BO equation (4) The value of t * in (3.6) can be motivated by the identity d dt (using the second conservation, i.e. the L 2 -norm of the real solution) which describes the time evolution of the first momentum of the solution.Hence, So assuming that one looks for the times where the average of the first momentum of the solution vanishes, i.e. for t such that which under the assumption (3.9) has a unique solution t = t * given by the formula in (3.6).
(5) Theorem 3.1 leaves open the question of a UCP at infinity involving only two different times by strengthening the hypothesis on the decay.More precisely, can one find r > 4 such that if u ∈ C([−T, T ] : Żs,7/2 − ), s 1, is a solution of the BO equation (3.1) satisfying that there exist t 1 , t 2 ∈ [−T, T ], t 1 = t 2 such that u(t j ) ∈ Żs,r , j = 1, 2, then u ≡ 0?
In [42] it was proved that this is not possible at least for r < 11/2.Next, we consider the local UCP for solutions of the IVP associated to the k-gBO equation (3.4).In this regard we have the following result: be strong solutions of k-gBO equation (3.4).If there exist an open interval I ⊂ R and t 1 ∈ (0, T ) such that (1) It is surprising that a period of more than 30 years separated the local UC result for the k-gKdV (2.2) (Theorem 2.1) and that for the k-gBO (3.4) (Theorem 3.3).Specially, since many results first established for the KdV equation have been studied in the BO equation, see [90].Maybe, this is due to the difference in their proof arguments.More concretely, the classical approach in [110], [68], [34], [35], among others, is based on Carleman estimates which cannot be extended to non-local models.For these ones, it seems that simpler but very specific stationary arguments are needed.Some of them have just recently been established.(2) Theorem 3.3 extends to a pair of solutions u 1 , u 2 of the Burgers-Hilbert (BH) equation see [9], [63].
(3) It also applies to solutions of the IPBVP associated to the k-gBO equation (3.4).In this case the Hilbert transform is defined as It will be clear from the proof of Theorem 3.3 sketched below that this can be generalized in the following form: , and u(x, t 1 ) = P n (x), x ∈ I, where Q (k+1)n−1 and P n are polynomials with real coefficients of degree at most (k + 1)n − 1 and n, respectively, then Next, we shall sketch the proof of Theorem 3.3.
Proof of Theorem 3.3.We need the following consequence of Schwarz reflection principle in complex analysis.
Using Proposition 3.6 we get: By standard approximation, the same result holds assuming that f ∈ H s (R), s ∈ R. Thus, defining is continuous and has an analytic extension F (x + iy) on y > 0. Hence, using Proposition 3.6 one proves Lemma 3.7.
To conclude the proof of Theorem 3.3 we define which satisfies the equation By the hypothesis and the equation one has that w(x, t 1 ) = H∂ 2 x w(x, t 1 ) = 0, x ∈ I. Thus, Lemma 3.7 yields the result.

The intermediate Long Wave equation
The Intermediate Long Wave (ILW) equation can be written as where u = u(x, t) is a real-valued function, δ > 0 and Also, L δ is a multiplier operator with symbol The ILW equation describes long internal gravity waves in a stratified fluid with finite depth given by the parameter δ, see [84] and [71].Moreover, it was shown in [80]- [81] that is formally a completely integrable model as the KdV, the CH and the BO equations, see also [70].The ILW equation has traveling waves solutions (solitons) where a ∈ (0, π/δ) solves the equation aδ cot(aδ) = 1 − cδ, see [71].
Regarding the IVP associated to the ILW equation (4.1) it was proven in [1] that solutions of the ILW equation converge, as δ → ∞ (deep-water limit), to solutions of the IVP associated to the BO equation with the same initial data.Also, it was established in [1] that if u δ (x, t) denotes a solution of the ILW equation (4.1), then converges, as δ → 0 (shallow-water limit), to a solution of the KdV equation with the same initial data.
With respect to well-posedness of the IVP associated to ILW equation we refer to [109] and references therein.
We do not know any result concerning the asymptotic at infinity UCP for the ILW equation, even in the case where the second solution u 2 ≡ 0.
In [77] the local UCP results for the BO equation were extended to the ILW equation : As in the case of BO equation one has the following extension of the second part of Theorem 4.1: be a strong solutions of ILW equation (4.1).If there exist an open interval I ⊂ R and t 1 ∈ (0, T ) such that where Q 2n−1 and P n are polynomials with real coefficients of degree at most 2n − 1 and n respectively, then Next, we shall sketch the proof of Theorem 4.1.
Proof of Theorem 4.1.First, we shall have the following result related to that in Proposition 3.6: Thus, F ∈ L 1 (R) with appropriate exponential decay.Therefore F (x) has an analytic extension to the strip D 2δ = {z = x + iy ∈ C : 0 < y < 2δ}.This completes the proof.

The Camassa-Holm equation and related models
This section is mainly concerned with the Camassa-Holm (CH) equation (5.1)The CH equation (5.1) was first explicitly written in [43] a work on hereditary symmetries.Later, it was explicitly derived as a physical model for shallow water waves in [19], where its solutions were also investigated.It has also appeared as a model in nonlinear dispersive waves in hyper-elastic rods [29].
The CH equation has special traveling waves solutions (solitons) called peakons (5. 2) The multi-peakon solutions exhibit the "elastic" collision property that reflects their soliton character.
It is convenient to rewrite the CH equation as 3) The IVP as well as the IPBVP associated to the equation (5.3) has been considerably examined.
In [88] and [104] strong local well-posedness of the IVP associated to (5.10) was established in the classical Sobolev space However, one observes that peakon solutions, described in (5.2) (case k = 0), do not belong to these spaces.In fact, one has that for any where for s ∈ R and p ∈ [1, ∞) with H s,2 (R) = H s (R), see [90].However, where W 1,∞ (R) denotes the space of Lipschitz functions.
In [26] it was proved that if u 0 ∈ H 1 (R) with u 0 −∂ 2 x u 0 ∈ M + (R) (the set of positive Radon measures with bounded total variation), then the IVP for the CH equation ( 5.3) has a unique solution is uniformly bounded.In [116] the existence of a H 1 -global weak solution for the IVP for the CH equation (5.1) for data u 0 ∈ H 1 (R) was established.
In [23] and [24] (see also [88]) conditions on the data u 0 ∈ H 3 (R) were derived to guarantee that the corresponding local solution u ∈ C([0, T ] : H 3 (R)) of the IVP associated to the CH equation (5.3) blows up in finite time, i.e.
which corresponds to the breaking of waves.
Formally, one has that H 1 -solutions of the CH equation (5.3) satisfy the conservation law so that the H 1 -norm of the solutions constructed in [92] (see Theorem 5.5 below) remains invariant within the existence interval.
In [14] and [15] the existence and uniqueness, respectively, of a H 1 global solution for the CH equation (5.1) was established.
For other well-posedness results we refer to [53], [54] and references therein.
(1) The conclusion of Theorem 5.1 still holds with the decay in (5.7)-(5.8)assumed for x ↓ −∞.(2) Roughly, Theorem 5.1 affirms that a non-trivial solution of the CH equation can decay faster at two times than peakon (soliton) solution (5.2).This is not the case of the k-gKdV equation, k-gBO equation and the dgBO equation (section 6).In view of the soliton resolution conjecture this should be the case for very large values of the time t, see the comments at the end of the section 2.
The next result shows that Theorem 5.1 is optimal: 58]).Assume that for some T > 0 and s > 3/2, is a strong solution of the IVP associated to the CH equation (5.3).If for some θ ∈ (0, 1), u 0 (x) = u(x, 0) satisfies ).Given u 0 ∈ H 1 (R) ∩ W 1,∞ (R) ≡ X there exist T = T ( u 0 X ) > 0 and a unique solution u = u(x, t) of the IVP associated to the CH equation for some universal constant C > 0.
Moreover, given R > 0, the map u 0 → u, taking the data to the solution, is continuous from the ball {u 0 ∈ X : The periodic version of this theorem was previously established in [31].
The CH equation (5.3) is a member of the b-family of equations : For b = 2 one gets the CH equation and for b = 3 one obtains the Degasperis-Procesi (DP) equation [32], the only bi-hamiltonian and integrable models in this family, see [38], [32].
Remark 5.6.The results in Theorem 5.1 and Theorem 5.3 extend directly to all the members in the b-family, see [57].The same applies to Theorem 5.5, and its periodic version in [31].
Concerning the local UCP for solutions of the IVP for the CH equation (5.3), in fact for all b-equations in (5.9), we have: Theorem 5.7 ([91]).Let u = u(x, t) be the solution of the IVP for an equation in (5.9) provided by Theorem 5.5 (see Remark 5.6).If there exist an open interval I ⊂ R and a time t 1 ∈ [0, T ] such that u(x, t 1 ) = ∂ t u(x, t 1 ) = 0, x ∈ I, then u ≡ 0.

In particular, if there exists an open set
The result in Theorem 5.7 extends to solution of the IPBVP : 91]).Let u = u(x, t) be the local solution of the IPBVP for an equation in (5.9) found in [31], (see Remark 5.6 (ii)).If there exist an open interval I ⊂ S and a time In particular, if there exists an open set Remark 5.9.
(1) Others UCP for the IPBVP for the b-equations in (5.9) have been obtained in [13] and [12].(2) From the above results, one has that for the CH equation (5.3) (and for all the members in the b-family (5.9)) both local and asymptotic at infinity UCP's are known only in the case where the solution u 2 ≡ 0. Therefore, the UCP result for two arbitrary solutions u 1 , u 2 remains open.
Next, we shall sketch the proof of Theorem 5.7 and remark that the proof for Theorem 5.8 is similar, see [91].
Proof of Theorem 5.7.We observe that formally Thus, from the hypothesis b 2 and from the equation Thus, defining and which yields the desired result.
Remark 5.10.One can ask if the result in Theorem 5.7 still hold under the assumption and for some open interval I ⊂ R ∂ t u(x, t 1 ) = 0 and u(x, t 1 ) = k 0 , x ∈ I (see Theorem 3.5).
In the case b = 0 in (5.9) the previous proof provides the result.However, for other values of the parameter b ∈ (0, 3], in particular for the CH and DP equations, the result is unknown. Finally, we consider the generalized form of the CH (gCH) equation (5.10) or its formally equivalent form (5.11) In [86] a systematic study on the existence and properties of traveling wave solutions for the gCH was provided.The definition in [86] for traveling waves solutions of the gCH equation is equivalent to the following one: Definition 5.11.
A function φ(x−ct) is a traveling wave solution of the gCH equation if (i) φ ∈ H 1 loc (R) and (ii) φ satisfies, in the weak sense, the equation (5.12) Remark 5.12.
(1) One sees that if φ(x) is a traveling wave solution of (5.10), then −φ(−x) is red also a traveling wave solution of (5.10) with −k instead of k.
Following [86] and restricting to the setting c > 0 and φ ∞ > m, with lim one has : peakons exist if and only if k = m.In this case c = φ ∞ .
The cuspons with decay, i.e. φ is a weak solution of (5.12), smooth on R − {a}, having a cusp at a ∈ R The stumpons with decay, i.e. φ is a continuous weak solution of (5.12) such that there exist a, b, d ∈ R with a < b, d > 0, such that increasing in (−∞, a), decreasing in (a, ∞), satisfying (5.13), (inserting the interval [a, b] at the cusp of a cuspon).Remark 5.13.
(1) The argument given above for the proof of Theorem 5.7 shows that if m > 0 a (positive) stumpon with decay can only exists if k ≤ 0. Similarly, if m < 0 then one needs to have k ≥ 0, see Remark 5.12.In the case, m = 0 one needs k = 0.
From the existence result of stumpons in [86] this case provides a counter-example of the question stated in Remark 5.10 for the gCH equation in (5.10) with k = 0. Thus, this question for the CH equation in (5.3) remains open.
(2) Similarly, by taking m = 0 and two stumpon solutions with common maximum realized at intervals I 1 and one gets a negative answer to the local UCP for two arbitrary (weak) solutions of the gCH with k = 0, see Remarks 5.9 (2) and 5.12.

The dispersion generalized Benjamin-Ono equation
Next, we shall consider the dispersion generalized Benjamin-Ono (dgBO) equation where D α x = (−∂ 2 x ) α/2 .One has that in (6.1) α = 2 corresponds to the KdV equation, α = 1 to the BO equation, α = 0 to the inviscid Burgers' equation (after a change of frame), and α = −1 to the so called Hilbert-Burgers equation.Also, we recall that only in the cases α ∈ {1, 2} the model is completely integrable.
For α ∈ [1, 2] the dgBO equation possess traveling waves solutions In the case α ∈ (1, 2) the existence (up to symmetry of the equation) of the traveling wave was established in [117], and the uniqueness in [41].
Remark 6.2.Roughly speaking, we observe that Theorem 6.1 with α = 1 corresponds to Theorem 3.1, and that the gain in decay due to the stronger dispersion, i.e. α ∈ (1, 2) is consistent with the result in (6.2) obtained in [74].
The next result regards local UCP for solutions of (6.1).
If there exist an open interval I ⊂ R and t 1 ∈ (0, T ) such that In particular, if Remark 6.4.The condition on s in Theorem 6.3 is not optimal.
As in the case of the k-gBO equation (3.4) and the ILW equation (4.1) we have as a consequence of Theorem 6.3 and its proof: Theorem 6.5.Let n ∈ Z + and be a strong solution of dgBO equation (6.1).If there exist an open interval I ⊂ R and t 1 ∈ (0, T ) such that ∂ t u 1 (x, t 1 ) = Q 2n−1 (x), and u(x, t 1 ) = P n (x), x ∈ I, where Q 2n−1 and P n are polynomial with real coefficients of degree at most 2n − 1 and n, respectively, then, The main idea to prove Theorem 6.3 and Theorem 6.5 is to apply the following result found in [50], (see results in [39], [40], [106], [118]).
(1) Notice that the case n = 1 and a = 1/2 in Theorem 6.6 corresponds to Lemma 3.7.(2) Theorem 6.6 still holds if one replaces (6.3) by the following hypothesis : there exist polynomials P n , Q k of degree n, k, respectively, such that (3) Theorem 6.6 tells us that a fractional porous medium equation of the form cannot have compact support solutions.
The proof of Theorem 6.6 is a consequence of the characterization of the fractional power of the Laplacian found in [16] : then for α ∈ (0, 2) there exists c > 0 such that Once, Theorem 6.6 is available the proof of Theorem 6.3 follows the argument given in the proof of Theorem 3.3.
Motivated by Theorem 6.6 and using an argument found in [111] the following result was established in [78]: )

The general fractional Schrödinger equation
In this section we shall consider fractional Schrödinger (GFDS) equations of the form where (i) when m = 0, W = P = 0, it was used in [85] to describe particles in a class of Levi stochastic processes, (ii) when m > 0, W = P = 0, it was derived as a generalized semi-relativistic (Schrödinger) equation, see [87] and references therein, (iii) when m = 0, α = 1, V = W = 0, and P (u, ū) = ±|u| α u, α > 0, it is known as the half-wave equation, see [6], [49] and references therein, (iv) when m = 1, V = P = 0, F (|z|) = |z| 2 the model arises in gravitational collapse, see [33], [47] and references therein, (v) when m = 0, V = W = 0 and it was deduced in [65] in the study the long-time behavior of solutions to the water waves equations in R 2 , where (−∂ 2 x ) 1/2 modeling the dispersion relation of the linearized gravity water waves equations for one-dimensional interfaces.
The well-posedness of the IVP associated to some equations of the type in (7.1) has motivated several works, we refer to [87], [11], [20], [21], [61], [83] and references therein.Here, in order to simplify the exposition, we will assume that the IVP associated to the equation (7.1) is locally well-posed in H s (R n ) for s ≥ s * = s * (α, n, V, W, F, P ).Concerning local UCP for the IVP associated to the equation (7.1) with m > 0, we have the following result: be two solutions of the IVP associated to the GFDS equation (7.1) with W ≡ 0. If there exist an open set D ⊂ R n and then In particular, if with Ω open, then u 1 ≡ u 2 .(2) For the general form of the GFDS equation (7.1), i.e.W = 0, the result in (1) still holds if u 2 (x, t) = 0 for (x, t) ∈ R n × [0, T ].
(1) In the case V ≡ W ≡ 0 the appropriate versions of Theorem 3.5, Theorem 4.2, and Theorem 6.5 still hold for the IVP associated to the equation (7.1).
(2) The proofs of Theorem 7.1 and Theorem 7.2 are based on the results in Theorem 6.8 and Theorem 6.6, respectively (see [78]).
Finally, we briefly discuss the asymptotic UCP for solution of the IVP associated to the equation (7.1).This question is largely open, even in the case when the operator modeling the dispersion L m relation is local, i.e. α ∈ 2Z + and m ≥ 0.
Let us consider some particular cases.First, we fix α = 2 and m = 0, so (L m ) α/2 = −∆.In this setting, for the associated linear problem with V ≡ W ≡ P ≡ 0 the asymptotic UCP can be re-phrased in terms of uncertainty principles for the Fourier transform.For example, the L 2 version of Hardy uncertainty principle [56] found in [28] can be stated as: This result can be reformulated in terms of the free Schrödinger group {e it∆ : t ∈ R} : We observe that in this case the weight at time t = 0 and t = T may be different.This is a general fact exploited in several works, see [37] and references therein.
In [36], the result in (7.7), except for the case T /αβ = 1/4, was enlarged for solutions u(x, t) of the equation with the complex valued potential V = V (x, t) satisfying the decay assumption lim Moreover, in [36] an example of a complex valued potential V (x, t) verifying (7.8) for which the corresponding solution u(x, t) ≡ 0 holds that u(x, 0) e |x| 2 /β 2 , u(x, T ) e |x| 2 /α 2 ∈ L 2 (R n ) with T /αβ = 1/4, was given.This affirms that the result is sharp.
We do not know a result as that in (7.12) with a weaker weight that the Gaussian e |x| 2 /4 at time t = 0 and t = 1.Also, we do not know a solution of the equation (7.11) which has a stronger decay that u 1 (x, t) = e it ϕ(x) for t ∈ [0, 1], see (7.13).
Returning to the general equation in (7.1) one observes that for m = 0 the symbol of the dispersive operator is non-smooth.Therefore, from the discussed results of the BO equation one expect the strongest possible decay of the solution to be weaker than that for the case m > 0 where the symbol is smooth.Also, the form of the Hartree integrand should play an essential role in the strongest possible decay of the solution.
Finally, we have some comments concerning the product rule for fractional derivatives.Theorem 6.6 tells us that the pointwise inequality involving the fractional Riesz potential D = (−∆) In this regard the following pointwise estimate was established in [27] : Theorem 7.4 ([27]).Let a ∈ (0, 2) and any f ∈ C ∞ 0 (R n ).Then the following inequality holds: For a generalization of Theorem 7.4 we refer to [17].From Theorem 6.6 and Theorem 7.4 one has : with D a (f 2 ) non-vanishing in any open subset of (supp(f )) c .

( 6 )
One sees that the UCP in Theorem 3.1 assumes that the second solution u 2 ≡ 0. A result for asymptotic at infinity UCP involving two arbitrary solutions u 1 , u 2 of the IVP for the BO equation remains open.(7) The results (1)-(3) in Theorem 3.1 extend to solutions of the IVP associated to the k-gBO equation in (3.4).However, part (4) and (5) (modified version) hold for solutions of the IVP associated to the k-gBO equation in (3.4) when k is odd.
be a strong solution of k-gBO equation (3.4).If there exist an open interval I ⊂ R and t 1 ∈ (0, T ) such that

Proposition 3 . 6 .
Let I ⊆ R be an open interval, b ∈ (0, ∞] and be strong solutions of ILW equation (4.1).If there exist an open interval then |u(x, t)|, |∂ x u(x, t)| = O(e −θx ), as x ↑ ∞, uniformly in the time interval [0, T ].Remark 5.4.(1) We observe the UCP in Theorem 5.1 is restricted to the case where u 2 ≡ 0. A result of this kind for two arbitrary solutions u 1 , u 2 of the CH equation (5.3) is unknown.(2) In [92] Theorem 5.1 and Theorem 5.3 were extended to the solutions of the CH equation (5.3) obtained in the following class which contains the peakons solutions (5.2): Theorem 5.5 ([92]

V
= V (x, t) representing the potential energy, W = W (|x|) the Hartree integrand, and P (z, z) the nonlinearity with P (0, 0) = 0.Concrete examples of the model in (7.1) arise in several different contexts, for example: