
TL;DR
This paper extends Ambarzumyan type theorems to Sturm--Liouville dynamic equations on time scales, providing conditions under which the potential function is uniquely determined by spectral data.
Contribution
It introduces new Ambarzumyan type results for Sturm--Liouville problems on arbitrary time scales, unifying discrete and continuous cases.
Findings
Established conditions for potential uniqueness on time scales.
Unified continuous and discrete spectral theory results.
Extended classical theorems to dynamic equations on time scales.
Abstract
In this paper, we consider a Sturm--Liouville dynamic equation with Robin boundary conditions on time scale and investigate the conditions which guarantee that the potential function is specified.
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Ambarzumyan Type Theorems on a Time Scale
A. Sinan Ozkan Department of Mathematics, Faculty of Science, Cumhuriyet University 58140
Sivas, TURKEY [email protected]
Abstract.
In this paper, we consider a Sturm–Liouville dynamic equation with Robin boundary conditions on time scale and investigate the conditions which guarantee that the potential function is specified.
Key words and phrases:
Ambarzumyan Theorem, Time scale, Sturm-Liouville equation; inverse problem; dynamic equations.
2000 Mathematics Subject Classification:
31B20, 39A12, 34B24
1.
Introduction
Time scale theory was introduced by Hilger in order to unify continuous and discrete analysis [16]. From then on this approach has received a lot of attention and has applied quickly to various area in mathematics. Sturm–Liouville theory on time scales was studied first by Erbe and Hilger [11] in 1993. Some important results on the properties of eigenvalues and eigenfunctions of a Sturm–Liouville problem on time scales were given in various publications (see e.g. [2], [3], [4], [8]-[10], [12], [14]-[22] and the references therein).
Inverse spectral problems consist in recovering the coefficients of an operator from their spectral characteristics. Althouhgh there are vast literature for inverse Sturm–Liouville problems on a continuous interval, there are no study on the general time scales. For Sturm-Liouville operator on a continuous interval, the study which starts inverse spectral theory, was published by Ambarzumyan [1] in 1929. He prove that: if is continuous function on and the eigenvalues of the problem
[TABLE]
are given as then
Freiling and Yurko [13] generalized this result as implies
The goal of this paper to prove an Ambarzumyan type theorem on a general time scale and to apply it on the a special time scale. In our main result, Theorem 1, we generalize the results of Freiling and Yurko for Sturm-Liouville operator with more general boundary conditions on a time scale.
2. Preliminaries and Main Results
If is a closed subset of it called as a time scale. The jump operators , and graininess operator on are defined as follow:
[TABLE]
A point of is called as left-dense, left-scattered, right-dense, right-scattered and isolated if , , , and respectively.
A function is called rd-continuous on if it is continuous at all right-dense points and has left-sided limits at all left-dense points in . The set of rd-continuous functions on is denoted by or .
Put \mathbb{T}^{k}:=\left\{\begin{array}[]{cc}\mathbb{T}-\{\sup\mathbb{T}\}\text{,}&\sup\mathbb{T}\text{ is left-scattered}\\ \mathbb{T}\text{,}&\text{the other cases}\end{array}\right.,
Let Suppose that for given any there exist a neighborhood such that
[TABLE]
for all then, is called differentiable at . We call the delta derivative of at A function defined as for all is called an antiderivative of on . In this case the Cauchy integral of is defined by
[TABLE]
Some important relations whose proofs appear in [6], chapter1 will be needed. We collect them in the following lemma.
Lemma 1**.**
*Let , be two functions and
i) lf exists, then is continuous at ;
ii) if is right-scattered and is continuous at , then is differentiable at and where
iii) if exists, then
iv) if , exist and is defined, then and if , then ;
v) if , then it has an antiderivative on ;
vi) if consists of only isolated points and with then
vii) if for all and then *
Throughout this paper we assume that is a bounded time scale, and . Consider the boundary value problem generated by the Sturm–Liouville dynamic equation
[TABLE]
subject to the boundary conditions
[TABLE]
where is real valued continiuous function on , and is the spectral parameter. Additionally, we assume that , and
Definition 1**.**
The values of the parameter for which the equation (1) has nonzero solutions satisfy (2) and (3), are called eigenvalues and the corresponding nontrivial solutions are called eigenfunctions.
It is proven in [6] that all eigenvalues of the problem (1)-(3) are real numbers.
Definition 2**.**
A solution of (1) is said to have a zero at if , and it has a node between and if . A generalized zero of is then defined as a zero or a node.
Lemma 2** ([2]).**
The eigenvalues of (1)-(3) may be arranged as and an eigenfunction corresponding to has exactly generalized zeros in the open interval .
Lemma 3**.**
If is an eigenfunction of the problem (1)-(3) then and
Proof.
It is clear from Lemma 1 that and . We claim that and . Otherwise, from (2) and (3) or hold, then by the uniqueness theorem of the solution of initial value problems is identically vanish which contradicts that it is the eigenfunction. Therefore the proof is completed from the assumption
Theorem 1**.**
Let be the first eigenvalue of (1)-(3). If
[TABLE]
then
Proof.
Let be the corresponding eigenfunction to From eq(1) and Lemma 2 we can write on
[TABLE]
It is from the relation
[TABLE]
that
[TABLE]
From Lemma 3 we can integration of both sides from to . Therefore the following equality is obtained
[TABLE]
It can be seen from Lemma 2 and our hypothesis that the right side of the last equality is negative and the left side is non-negative. Thus and so is constant. Substituting is constant into equation (1), it is concluded that .
Corollary 1**.**
The first eigenvalue of the problem is then,
This corollary is a generalization of the results of Freiling and Yurko [13] onto the time scale.
Corollary 2**.**
Under the hypothesis ; if , then the problem
[TABLE]
has at least one negative eigenvalue.
We conclude this paper with specializing our first result for a particular time scale which consists of only isolated points.
Remark 1**.**
Consider the time scale
[TABLE]
and the following problem
[TABLE]
If the first eigenvalue of the problem satisfy then
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] V.A. Ambarzumyan, Über eine Frage der Eigenwerttheorie, Z. Phys. 53 (1929), pp. 690–695.
- 2[2] R.P. Agarwal, M. Bohner, and P.J.Y. Wong, Sturm-Liouville eigenvalue problems on time scales, Appl. Math. Comput. 99 (1999), pp. 153–166.
- 3[3] P. Amster, P. De Na´poli, and J.P. Pinasco, Eigenvalue distribution of second-order dynamic equations on time scales considered as fractals, J. Math. Anal. Appl. 343 (2008), pp. 573–584.
- 4[4] P. Amster, P. De Na´poli, and J.P. Pinasco, Detailed asymptotic of eigenvalues on time scales, J. Differ. Equ. Appl. 15 (2009), pp. 225–231.
- 5[5] F. Atkinson, Discrete and Continuous Boundary Problems, Academic Press, New York, 1964.
- 6[6] M. Bohner and A. Peterson, Dynamic Equations on Time Scales, Birkha¨user, Boston, MA, 2001.
- 7[7] M. Bohner and A. Peterson (eds.), Advances in Dynamic Equations on Time Scales, Birkha¨user, Boston, MA, 2003.
- 8[8] F.A. Davidson and B.P. Rynne, Global bifurcation on time scales, J. Math. Anal. Appl. 267 (2002), pp. 345–360.
