Resolvent estimates related with a class of dispersive equations
Hiroyuki Chihara

TL;DR
This paper provides a straightforward proof of resolvent estimates for elliptic Fourier multipliers and applies these results to analyze smoothing effects in certain dispersive equations, focusing on Fourier transform restrictions.
Contribution
It introduces a simple proof technique for resolvent estimates and applies it to dispersive equations, enhancing understanding of smoothing phenomena.
Findings
Resolved resolvent estimates for elliptic Fourier multipliers
Established smoothing estimates for dispersive equations
Analyzed Fourier transform restrictions on cotangent spheres
Abstract
We present a simple proof of the resolvent estimates of elliptic Fourier multipliers on the Euclidean space, and apply them to the analysis of time-global and spatially-local smoothing estimates of a class of dispersive equations. For this purpose we study in detail the properties of the restriction of Fourier transform on the unit cotangent sphere associated with the symbols of multipliers.
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Taxonomy
TopicsAdvanced Mathematical Physics Problems · advanced mathematical theories
Resolvent estimates related with
a class of dispersive equations
Hiroyuki CHIHARA
Mathematical Institute, Tohoku University, Sendai 980-8578, Japan
Abstract.
We present a simple proof of the resolvent estimates of elliptic Fourier multipliers on the Euclidean space, and apply them to the analysis of time-global and spatially-local smoothing estimates of a class of dispersive equations. For this purpose we study in detail the properties of the restriction of Fourier transform on the unit cotangent sphere associated with the symbols of multipliers.
Key words and phrases:
resolvent, dispersive equation, smoothing effect, limiting absorption principle
2000 Mathematics Subject Classification:
Primary 47A10; Secondary 35P25, 47F05
The author was supported by the JSPS Grant-in-Aid for Scientific Research #17540140.
1. Introduction
This paper is concerned with resolvent estimates of elliptic operators on the Euclidean space with constant coefficients. These estimates are equivalent to smoothing properties of solutions to corresponding dispersive evolution equations.
For and , set and . Let be a positively homogeneous function of degree one. Suppose that for . It follows that
[TABLE]
since . Set for some fixed number .
Consider the initial value problem of the form
[TABLE]
where is an unknown function of , and are given functions, , , , , and the operator is defined by
[TABLE]
for an appropriate function . Since is real-valued, the initial value problem (1)-(2) is -well-posed, that is, for any and for any , (1)-(2) possesses a unique solution . Here and denote a usual Lebesgue space and its local space respectively for , and is the set of all -valued continuous functions on . Moreover, the unique solution is explicitly given by
[TABLE]
A typical example of (1) is the Schrödinger evolution equation of a free particle, which is the case . It is well-known that the solution to the free Schrödinger evolution equation on gains extra smoothness in comparison with the initial data and the forcing term. This mathematical phenomenon is called local smoothing effect or local smoothing property. In the last two decades, smoothing properties of solutions to more general dispersive partial differential equations and their applications have been vigorously investigated. See, e.g., [1], [2], [4], [5], [6], [8], [9], [12], [13], [16], [18], [19] and references therein.
In [2] Doi deeply studied the relationship between the behavior of the geodesic flow and the smoothing effect of the Schrödinger evolution equation on complete Riemannian manifolds. Roughly speaking, he proved that the smoothing effect occurs if and only if all the geodesics go to “infinity”. In other words, if there exists a trapped geodesic, then the smoothing effect breaks down. For more general dispersive equations, the smoothing effect depends on the behavior of the Hamilton flow generated by the principal symbol of the equations. Consider dispersive equations with constant coefficients of the form
[TABLE]
where is a real polynomial of order . Let be the principal symbol of . generates the Hamilton flow for . Hoshiro proved that the smoothing effect of solutions to the IVP for (3) occurs if and only if for
[TABLE]
This condition is equivalent to for . See [6] for the detail.
There are some expressions of smoothing estimates. Let and . Throughout this paper, different positive constants are denoted by the same letter . In [16] Sugimoto classified these estimates into three types as follows.
**TYPE-I : **
Let . Then
[TABLE]
**TYPE-II : **
Suppose . Then
[TABLE]
For TYPE-III, see [8], [16] and [19] for the detail. TYPE-I estimates (4) and (5) were studied by many authors. These inequalities describe time-global and spatially local smoothing effect. TYPE-II estimates (6) and (7), and TYPE-III estimates were first studied by Kato and Yajima in [8]. These inequalities seem to show not only smoothing effect but also integrability of solutions. In [1] the author gave the complete generalization of (4) and (5). More precisely, he proved that if is a real-principal-type homogeneous symbol of degree , that is, is real-valued and satisfies
[TABLE]
then the corresponding TYPE-I estimates hold. Unfortunately, the proof of this generalization in [1] is complicated and not comprehensive. On the other hand, TYPE-II estimates seem to show the integrability of solutions related with low-frequency region also. From a point of view of Fourier analysis, it is very natural to ask whether the curvature effect of the level set of is essential or not.
There are two purposes of this paper. One is to give a simpler proof of the generalization of TYPE-I estimates in [1] for general elliptic symbols. It seems to be very hard to present essentially simpler proof for more general real-principal-type symbols including nonelliptic ones. Another is to consider the influence of the curvature effect of the level set of the elliptic symbol on TYPE-II estimates. More precisely, we will give the complete generalization of TYPE-II estimates (6) and (7), and show that they depend only on and the weight , and are independent of the curvature of the level set of . Our results are the following.
Theorem 1.1**.**
Let .
**TYPE-I: **
Suppose and . Then
[TABLE]
**TYPE-II: **
Suppose . Then
[TABLE]
Theorem 1.1 follows from resolvent estimates.
Theorem 1.2**.**
Let .
**TYPE-I: **
Suppose and . Then
[TABLE]
**TYPE-II: **
Suppose . Then
[TABLE]
To prove Theorem 1.2, we make full use of the estimates of the restriction of Fourier transform on the level set of . Set for . The Fourier transform of is denoted by
[TABLE]
Kuroda first established the restriction estimates related with scattering theory for in [11]. His results played essential roles in [8]. His proof depends on the specificity of . We extend his results as follows.
Lemma 1.3**.**
Let .
**Uniform trace estimates: **
Suppose . Then
[TABLE]
**Hölder continuity: **
Suppose for , and for . Then
[TABLE]
**Low frequency trace estimates: **
Suppose . Then
[TABLE]
To conclude this section, we show how Theorem 1.2 implies Theorem 1.1. In [7] Kato discovered this principle in an abstract operator theoretic setting. We give an elementary Fourier analytic approach below. For an appropriate function , we use the following notation
[TABLE]
Let be the Heaviside function
[TABLE]
Set for short. Using the Fourier transform in the space-time, we have
[TABLE]
Using the above formula and the limiting absorption principle, one can easily show that (12) implies (9), and (13) implies (11). On the other hand, the estimates of are equivalent to
[TABLE]
since
[TABLE]
where or . By the co-area formula (see e.g., [14, Theorem 5.8 in Chapter II]), Hörmander’s observation in [3, Section 14.3] and the estimates (12)-(13), we deduce
[TABLE]
which shows that (12) implies (8), and (13) implies (10).
The organization of this paper is as follows. In Section 2 we prepare some weighted commutator estimates needed later. Section 3 is devoted to proving Lemma 1.3. In Sections 4 and 5 we prove (12) and (13) respectively.
2. Weighted commutator estimates
This section is devoted to preparing weighted commutator estimates used later. Our basic tools are weighted estimates of fractional integrals due to Stein and Weiss.
Theorem 2.1** ([15, Theorem B∗]).**
Suppose , , and . Then
[TABLE]
In particular, if , then
[TABLE]
In this section we show two lemmas. The first one is concerned with the commutator of weights and singular integral operators of order zero.
Lemma 2.2**.**
Let satisfy for and for . Suppose that is homogeneous of degree zero. Then
[TABLE]
Proof.
It suffices to show (19) since
[TABLE]
Since the inverse Fourier transform of is a homogeneous function of degree , we have
[TABLE]
Pick up a positive integer satisfying The mean value theorem gives
[TABLE]
We split our proof into two cases and . When , substituting (22) into (21), we have
[TABLE]
Applying (18) with to (23), we obtain (19) for and . Suppose that . Using (17) with and (18) with , we get
[TABLE]
respectively. Combining (23), (24) and (25), we obtain (19) for and .
Suppose and . Using elementary interpolation and (22), we deduce
[TABLE]
Substituting (26) into (21), we have
[TABLE]
Using (18) with , we have
[TABLE]
Here we remark that and for . Using (17) with and , we deduce
[TABLE]
Combining (27), (28), (29), and (30), we obtain (19) for . This completes the proof. ∎
The second lemma in this section is concerned with commutator estimates between weights and fractional differentiations in frequency space of .
Lemma 2.3**.**
Let , and let satisfy for and for . Set and . Then
[TABLE]
Proof.
First we remark that the Fourier transform of is homogeneous of degree . We split our proof into four cases: Case 1 (, ), Case 2 (, ), Case 3 (, ) and Case 4 (, ).
Case 1. Suppose and . Note that . We compare with . We evaluate
[TABLE]
The mean value theorem gives
[TABLE]
Since ,
[TABLE]
Since is homogeneous of degree zero,
[TABLE]
where . Combining (33), (34) and (35), we have
[TABLE]
Substituting (36) into (32), we deduce
[TABLE]
Using (17) with and (18) with , we deduce
[TABLE]
Similarly, using (17) with and (18) with , we deduce
[TABLE]
Applying (38) and (39) to (37), we obtain (31) for and .
Case 2. Suppose and . Note that . We evaluate
[TABLE]
Using factorization and the mean value theorem, we deduce
[TABLE]
Then we have
[TABLE]
Applying (42) to (40), we deduce
[TABLE]
Applying (17) with and (18) with to (43), we deduce
[TABLE]
which is desired.
Case 3. Suppose and . Since
[TABLE]
using (18) with , we obtain
[TABLE]
Case 4. Suppose and . A simple computation gives
[TABLE]
Using the results of Case 1, we deduce
[TABLE]
[TABLE]
where . Using (19) with , we have
[TABLE]
Applying (17) with to (47), we have
[TABLE]
Then we get
[TABLE]
Combining (44), (45) and (48), we obtain (31) for and . This completes the proof. ∎
3. Restriction estimates
In this section we prove Lemma 1.3.
Proof of uniform trace estimates (14).
We split into finite numbers of small surfaces given by graphs of functions as follows. Since , for , and is compact, there exist finite numbers of closed sets and points () such that
[TABLE]
Fix . Using an appropriate rotation in , we may assume . Set
[TABLE]
[TABLE]
The homogeneity of implies that for
[TABLE]
Since is positively homogeneous of degree one and (49), -direction is transversal to the small surface . Since , the implicit function theorem shows that there exists a homogeneous function of degree zero such that
[TABLE]
provided that is sufficiently small. Since for , we deduce
[TABLE]
Set for short. The uniqueness of the implicit function on implies that
[TABLE]
Now we evaluate . Set for short. Note that
[TABLE]
Then we have for any
[TABLE]
Let be the surface element on . Using (51), the one-dimensional Sobolev embedding (See, e.g., [17, Chapter 4]) and the Plancherel formula, we deduce
[TABLE]
Summing up the above estimates on up to , we obtain (14). ∎
Proof of Hölder continuity (15).
In view of (14), it suffices to show (15) only for . Fix . The Sobolev embedding theorem shows that
[TABLE]
where for . Note that for . Integrating (52) over and using (19), we deduce
[TABLE]
This completes the proof. ∎
Proof of low frequency trace estimates (16).
In view of (14), it suffices to show the case . Suppose () or (). Using (15), we deduce
[TABLE]
Consider the case (). Set for short. Applying (53) with “” to , we deduce
[TABLE]
Using (18) with , we have
[TABLE]
Using (19) with and and (17) with , we deduce
[TABLE]
Combining (54), (55) and (56), we obtain (16) for . This completes the proof. ∎
4. Smoothing estimates
In this section we prove the resolvent estimates (12). Obviously, it suffices to show (12) for . Let be a real-valued symbol. We remark that for
[TABLE]
Hence, it suffices to show (12) for . In view of (20) for , the proof of (12) is reduced to the following.
Lemma 4.1**.**
Let . Suppose and . Then,
[TABLE]
Proof.
It suffices to show (58) for and . For the sake of convenience, set with and . Using the Plancherel formula and the co-area formula, we have
[TABLE]
Applying (14) to the imaginary part of (59), we obtain
[TABLE]
According to , we split the evaluation of the real part of (59) into three cases: Case 1 (), Case 2 () and Case 3 ().
Case 1. Suppose . Set . Using (18) with , we deduce
[TABLE]
Case 2. Suppose . We split the real part of (59) into three parts according to the size of as follows.
[TABLE]
It is easy to deal with and . In fact, since for , and for , we have
[TABLE]
for . In the same way as (61), we can obtain
[TABLE]
The estimate of is delicate. Since
[TABLE]
for , we have
[TABLE]
Applying (14) and (15) to , we deduce
[TABLE]
where . The mean value theorem shows that for
[TABLE]
Substituting (67) into (66), we have
[TABLE]
for . Substituting (68) into (65), we get
[TABLE]
Combining (62), (63) and (69), we obtain (58) for and .
Case 3. Suppose . Case 3 is slightly different from Case 2. We split the real part of (59) into four parts as follows.
[TABLE]
It is easy to evaluate , and . Since for , and for ,
[TABLE]
for and . Hence, we deduce
[TABLE]
Since for , we can get
[TABLE]
in the same way as (61).
is also delicate. Since
[TABLE]
we have
[TABLE]
Here we remark that for
[TABLE]
Hence (67) is valid also for and , and (68) also holds for and . Thus, we can deduce
[TABLE]
Combining (70), (71), (72) and (73), we obtain (58) for and . This completes the proof. ∎
5. Low frequency estimates
In this section we prove (13). In view of (57), it suffices to show (13) only for . We first show the estimates essentially related with the low frequency part.
Lemma 5.1**.**
Let . Suppose . Then
[TABLE]
Proof.
In view of (57), we have only to show (74) for . Set for and . In the same way as (59), we have
[TABLE]
First we evaluate the imaginary part of (75). Pick up . Using (16), we deduce
[TABLE]
Here we remark that . Using (17) with and , we have
[TABLE]
Substituting (77) into (76), we obtain
[TABLE]
Next we consider the real part of (75)
[TABLE]
When , set . Using (18) with , we deduce
[TABLE]
for and .
For , we split (79) into three parts
[TABLE]
It is easy to handle and . In fact, since for and for ,
[TABLE]
for . Hence we can obtain
[TABLE]
for in the same way as (80).
We need to deal with carefully. Pick up . Using (64), we have
[TABLE]
[TABLE]
In the same way as (67), we have
[TABLE]
for . In the computation of (76) and (77), we have obtained
[TABLE]
Using (85) and (86), we obtain
[TABLE]
for . Set for short. We remark that (20) and (77) show that for any
[TABLE]
Applying (15), (16), (88) and (67) to , we deduce
[TABLE]
for . Combining (84), (87) and (89), we have
[TABLE]
for . Substituting (90) into (83), we have
[TABLE]
for . Combining (78), (80) and (91), we obtain (74). ∎
Finally, we complete the proof of (13).
Proof of (13).
We make a little use of the elementary theory of pseudodifferential operators freely. See, e.g., [10]. Pick up satisfying
[TABLE]
We split into two parts
[TABLE]
[TABLE]
Here we remark that and are smooth functions on whose derivatives of any order are all bounded. Using (92), (74) and (12), we deduce that
[TABLE]
Since () are -bounded operators, we obtain (13). ∎
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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- 2[2] S.-I. Doi, Smoothing effects of Schrödinger evolution groups on Riemannian manifolds , Duke Math. J. 82 (1996), 679–706.
- 3[3] L. Hörmander, “The analysis of linear partial differential operators II”, Springer-Verlag, 1983.
- 4[4] T. Hoshiro, On weighted L 2 superscript 𝐿 2 L^{2} -estimates of solutions to wave equation , J. Anal. Math. 72 (1997), 127–140.
- 5[5] T. Hoshiro, Mourre’s method and smoothing properties of dispersive equations , Comm. Math. Phys. 202 (1999), 255–265.
- 6[6] T. Hoshiro, Decay and regularity for dispersive equations with constant coefficients , J. Anal. Math. 91 (2003), 211–230.
- 7[7] T. Kato, Wave operators and similarity for some non-selfadjoint operators , Math. Ann. 1965/1966 , 258–279.
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