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Original Articles

Solving inverse nodal problem with spectral parameter in boundary conditions

, &
Pages 1790-1801 | Received 09 Nov 2018, Accepted 14 Mar 2019, Published online: 24 Mar 2019

ABSTRACT

In this study, the inverse Sturm-Liouville problem with spectral parameter in boundary conditions on a finite interval is considered. In fact, we use the nodes as input data and compute the approximation of solution of the inverse nodal Sturm-Liouville problem by the first kind Chebyshev polynomials and apply two methods Chebyshev wavelets and Chebyshev interpolation for solving inverse nodal Sturm-Liouville problem. Finally, the results are explained by presenting the numerical example.

AMS SUBJECT CLASSIFICATIONS:

1. Introduction

In this study, we consider the inverse nodal Sturm-Liouville problem with spectral parameter in boundary conditions and use the nodes and the first kind Chebyshev polynomials to calculate the approximate solution. In fact, we apply two methods Chebyshev wavelets and Chebyshev interpolation for solving inverse nodal Sturm-Liouville problem and compare them together by providing the numerical example. Inverse nodal problems have been perused by many authors recently (for example see [Citation1–29]). It seems that McLaughlin [Citation12] was researcher who considered the inverse nodal problems for the first time and got some results about the uniqueness and proved that the potential function in inverse Sturm-Liouville problem can be computed by the nodes.

In [Citation30], Babolian and Fattahzadeh used Chebyshev wavelets method for computing the numerical solution of integral equations by using the first kind Chebyshev polynomials. Also in [Citation31,Citation32], Rashed applied Chebyshev interpolation method to solve the integral-differential and integral equations and showed that the approximate solution of these type equations can be calculated by Chebyshev interpolation method.

In this study, we show that the solution of inverse nodal Sturm-Liouville problem can be the solution of an integral equation and offer Chebyshev wavelets and Chebyshev interpolation methods to obtain the approximation of solution of inverse nodal Sturm-Liouville problem.

Furthermore in all studies on inverse nodal problems, the researchers proved the uniqueness of the potential function by a dense set of nodes. In this study, we show that the approximation of inverse nodal problem solution can be calculated with a finite number of nodes by presenting the numerical example.

We consider the equation (1) y′′+q(x)y=λy,0<x<1,(1) with the boundary conditions (2) U(y):=y(0,λ)hy(0,λ)=0,(2) (3) V(y):=(λH1)y(1,λ)+(λHH2)y(1,λ)=0,(3) where the potential q(x) is a real function and integrable on (0,1), λ=ρ2, λ is the spectral parameter, h,H,H1,H2 are real parameters and r:=HH1H2>0.

In Section 2, we show the asymptotic form of eigenvalues and the nodes of problem (Equation1)–(Equation3) and present the uniqueness theorem for the inverse nodal problem solution. In Section 3, we use Chebyshev wavelets and Chebyshev interpolation methods for approximating the potential q(x) as the solution of inverse Sturm-Liouville problem and illustrate the obtained results by presenting the numerical example in Section 4.

2. Preliminaries

In this section, we produce the asymptotic form of eigenvalues and nodes of the boundary value problem (Equation1)–(Equation3) and present the uniqueness theorem for the inverse nodal problem under the boundary conditions given.

Let λ0<λ1< be the eigenvalues of the problem (Equation1)–(Equation3) and 0<x1n<<xn1n<1, be the nodes of nth eigenfunction. In addition, we denote x0n=0 and xnn=1.

The solution of Equation (Equation1) with the initial conditions ϕ(0,λ)=1, ϕ(0,λ)=h, can be written in the following form (see [Citation33,Citation34]) ϕ(x,λ)=cosρx+1ρq1(x)sinρx+12ρ0xq(t)sinρ(x2t)dt+O1ρ2, where q1(x)=h+120xq(t)dt. Integration by parts results 0xq(t)sinρ(x2t)dt=12ρq(x)cosρx+12ρq(0)cosρx, therefore (4) ϕ(x,λ)=cosρx+1ρq1(x)sinρx+O1ρ2.(4) We can write (see [Citation33,Citation34]) (5) Δ(λ):=V(ϕ)=(λH1)ϕ(1,λ)+(λHH2)ϕ(1,λ)=ρ3sinρ+ρ2ωcosρ+ρ2I(ρ),(5) where I(ρ)=1201q(t)cosρ(12t)dt+O1ρ. Using the formula (Equation5), we have (6) ρn=(n1)π+ωnπ+o1n,ω=h+H+1201q(t)dt.(6)

Theorem 2.1

Let the Equation (Equation1) under the initial conditions (7) y(0,λ)=1,y(0,λ)=h,(7) be given. Then, the nodes of problem (Equation1)–(Equation3) and the length of nodes are formulated in the form of (8) xjn=j12n1ωxjnn(n1)π2+q1(xjn)(n1)2π2+O1n3,(8) (9) ljn=1n1ωljnn(n1)π2+12(n1)2π2xjnxj+1nq(t)dt+O1n3,(9) where ω=h+H+1201q(t)dt,q1(xjn)=h+120xjnq(t)dt.

Proof.

We have from (Equation4) ϕ(x,λ)=cosρx+1ρq1(x)sinρx+O1ρ2, where q1(x)=h+120xq(t)dt. Since the nodes {xjn}, n>1, j=1,n1¯, are the zeroes of nth eigenfunction, we can set ϕ(xjn,λn)=0. Thus, cosρnxjn+1ρnq1(xjn)sinρnxjn+O1ρn2=0. Using formula (Equation6), we can write cos(n1)πxjnωxjnnπsin(n1)πxjn+1(n1)πq1(xjn)(sin(n1)πxjn+ωxjnnπcos(n1)πxjn)+O1n2=0. Then cot(n1)πxjnωxjnnπ+1(n1)πq1(xjn)+O1n2=0. Applying Taylor's expansion for the arccot as n, we get xjn=j12n1ωxjnn(n1)π2+q1(xjn)(n1)2π2+O1n3. Also, the nodal length is ljn=xj+1nxjn, therefore ljn=1n1ωljnn(n1)π2+12(n1)2π2xjnxj+1nq(t)dt+O1n3. Also see [Citation21,Citation22].

Theorem 2.2

The potential q1201q and the parameters h and (H2λH)/(λH1) are uniquely ascertained by any dense subset of the nodes in (0,1).

Proof.

Similar to the process used to prove the uniqueness theorem in [Citation6,Citation28], this theorem can be proved easily.

Corollary 2.3

The potential function q of the boundary value problem (Equation1)–(Equation3) is uniquely ascertained by a dense set of the nodes and the constant ω=h+H+1201q(t)dt.

Proof.

Similar to [Citation6,Citation13,Citation14], we consider two Sturm-Liouville problems (Equation1)–(Equation3) with the potential functions q, q~ and the nodal points xjn, x~jn as xjn=x~jn, j=1,n1¯, n>1. In addition, we suppose that ω=ω~. Then, using formula (Equation6), we have ρn=ρ~n and consequently λn=λ~n. Also, according to Theorem 2.2, we have (H2λnH)/(λnH1)=(H~2λnH~)/(λnH~1), thus, Hλn2+(H2+HH~1)λnH~1H2=H~λn2+λn(H~2+H~H1)H1H~2. Then, we can write H=H~,H2H~2=H1H~1=K,H2+HH~1=H~2+H~H1. By choosing K=1, the above relations are stablished and then we obtain H1=H1~,H2=H2~. Since ω=ω~, H=H~ and according to Theorem 2.2, h=h~, then we have 01q=01q~ and consequently by using Theorem 2.2, we get q=q~ almost everywhere on (0,1).

3. Numerical solution of the inverse nodal problem

In this section, we consider the inverse nodal problem below.

Inverse nodal problem. Given the nodes {xjn}, construct the potential q(x).

Since the nodes {xjn}, are the zeroes of the nth eigenfunction ϕ(x,λn), then, we can write ϕ(xjn,λn)=0,j=1,n1¯,n>1. Thus, using (Equation4), we get (10) 0xjnq(t)dt2ρncotρnxjn2h.(10) The equation mentioned above is the first kind Fredholm integral equation. To calculate the solution of inverse problem, it is sufficient that we get the solution of integral equation mentioned above. We approximate the potential q by the first kind Chebyshev polynomials as the basic functions and convert the integral equation (10) to the system of linear equations. For approximating the potential q, we use two methods Chebyshev wavelets and Chebyshev interpolation.

3.1. Chebyshev wavelets method

Consider following Chebyshev wavelets on the interval [0,1) as [Citation30] ψl,m(t)=2k/2T~m(2kt2l+1),l12k1t<l2k1,0,otherwise, where T~m(t)=1π,m=0,2πTm(t),m>0, and m=0,1,,M1, l=1,2,,2k1, k can be any positive integer and the functions Tm(t) are the first kind Chebyshev polynomials of degree m on the interval [1,1] gotten by the recursive formula below: T0(t)=1,T1(t)=t,Tm+1(t)=2tTm(t)Tm1(t),m=1,2,. A function f(t) on the interval [0,1) is expressed as f(t)l=12k1m=0M1cl,mψl,m(t)=CTψ(t), where C=[c10,c11,,c1(M1),c20,,c2(M1),,c2k10,,c2k1(M1)]T,Ψ(t)=[ψ10(t),,ψ1(M1)(t),ψ20(t),,ψ2(M1)(t),,×ψ2k10(t),,ψ2k1(M1)(t)]T. We approximate the potential q(t) by Chebyshev wavelets and have (11) q(t)l=12k1m=0M1cl,mψl,m(t).(11) Substituting (Equation11) into (Equation10), we obtain l=12k1m=0M1cl,m0xjnψl,m(t)dt2ρncotρnxjn2h,n>1,j=1,n1¯. Now, Let the nodal points {xjn}, be given. The solution of inverse nodal problem can be calculated by using the steps below:

  1. Choose k, M. Then set n=2k1M+1.

  2. Compute the unknown vector C by applying the linear system below: AC=B, where A=a101a111a1(M1)1a201a2(M1)1a2k101a2k1(M1)1a102a112a1M1a202a2(M1)2a2k102a2k1(M1)2.........a10ma11ma1(M1)ma20ma2(M1)ma2k10ma2k1(M1)m where al,mj=0xjnψl,m(t)dt,l=1,2k1¯,m=0,M1¯,n=2k1M+1,j=1,n1¯,m=2k1M, and B=2ρncotρnx1n2h2ρncotρnx2n2h...2ρncotρnxn1n2h,C=[c10,c11,,c1(M1),c20,,c2(M1),,c2k10,,c2k1(M1)]T.

  3. Find the approximate values q(ti), i=1,m¯ by using the following formula [q(ti)]=CTΦ, where ti=2i12kM,i=1,2,,2k1M, and Φ=ψ12m,ψ32m,,ψ2m12m,m=2k1M.

3.2. Chebyshev interpolation method

By using Chebyshev interpolation technique for the function q(t), one can show [Citation31,Citation32] that (12) q(t)i=0Nqili,N(t),t(0,1),(12) where li,N(t)=2δiNk=0N′′Tk(2t1)coskiπN,δi=0.5i=0,N,10<i<N, and the numbers qi, i=0,N¯ exist the values of potential function q(t) in the points ti=(cos(iπ/N)+1)/2 which are the extrema of TN(2t1). In addition, ′′ is the sum of all terms except the first and last two sentences so that the sum of half of the two sentences is considered.

Substituting (Equation12) into (Equation10) with n1, we have i=0Nqi2δiNk=0N′′0xjnTk(2t1)dtcoskiπN2ρncotρnxjn2h,n>1. Denote g(xjn)=2ρncotρnxjn2h, n>1, and Ik(xjn)=0xjnTk(2t1)dt,R(ti,xjn)=2δiNk=0N′′Ik(xjn)coskiπN. Using the above formulas, we have i=0NR(ti,xjn)qig(xjn),n>1. Now, Let the nodal points {xjn}, be given. Then, the solution of inverse nodal problem can be calculated by using the following steps:

  1. Choose n and set N=n2.

  2. Find the coefficients qi, i=0,N¯ by the linear system below: Aqˆ=B, where qˆ=[q0q1qN]T, A=R(t0,x1n)R(t1,x1n)...R(tN,x1n)R(t0,x2n)R(t1,x2n)...R(tN,x2n)............R(t0,xn1n)R(t1,xn1n)...R(tN,xn1n)=1Nk=0N′′Ik(x1n)2Nk=0N′′Ik(x1n)coskπN...1Nk=0N′′(1)kIk(x1n)1Nk=0N′′Ik(x2n)2Nk=0N′′Ik(x2n)coskπN...1Nk=0N′′(1)kIk(x2n)............1Nk=0N′′Ik(xn1n)2Nk=0N′′Ik(xn1n)coskπN...1Nk=0N′′(1)kIk(xn1n),where Ik(xmn)=0xmnTk(2t1)dt. Moreover B=g(x1n)g(x2n)...g(xn1n)=2ρncotρnx1n2h2ρncotρnx2n2h...2ρncotρnxn1n2h.

  3. Calculate the potential function q by using the formula (Equation12).

4. Numerical example

In this section, we use the methods presented in this study to solve inverse nodal problem (Equation1)–(Equation3) and provide a numerical example to show the accuracy of presented methods. The calculations associated with the example presented in this section are performed using Matlab software program.

Example 4.1

Consider the potential q(x)=sin(3πx) and h=H=1. The numerical values of nodes xjn, n=13, j=1,12¯ can be computed by the formula (Equation8) seen in Table . Now, we suppose that the nodes given in Table  are the input data and q is the unknown function in inverse nodal problem. We get the approximation of potential q as the solution of inverse nodal problem by using Chebyshev wavelet method and Chebyshev interpolation method. The results gotten in this example with k=M=3 and n=13 are seen in Table  where q and q~ denote the exact and approximate solutions, respectively. In Table , It is clear that Chebyshev interpolation method compared with Chebyshev wavelet method is more accurate. Finally, we draw the numerical approximation obtained with k=4, M=7 and n=57 and exact solution by using Chebyshev wavelet method shown in Figure . It is seen that for large n, wavelet Chebyshev method is a good method for solving the inverse nodal Sturm-Liouville problems.

Figure 1. Approximate and exact solutions of inverse nodal problem using Chebyshev wavelet method in Example 4.1 with n=57: (***) for the exact solution and (- - -) for the approximate solution.

Figure 1. Approximate and exact solutions of inverse nodal problem using Chebyshev wavelet method in Example 4.1 with n=57: (***) for the exact solution and (- - -) for the approximate solution.

Table 1. Numerical values of nodes xjn in Example 4.1 with n=13.

Table 2. Absolute error of exact and approximate solutions in Example 4.1.

5. Conclusion

In this study, we propounded Sturm-Liouville equation with boundary conditions included spectral parameter. We applied the relationship between the inverse nodal Sturm-Liouville problem and Fredholm integral equation of the first kind and computed the approximate solution of associated inverse problem by Chebyshev wavelet and Chebyshev interpolation methods for the first time. By preparing the numerical example, we showed that both methods were good methods for solving the inverse nodal problems of this form but Chebyshev interpolation method was more accurate compared with Chebyshev wavelet method. Furthermore, in provided example, it could be found that the approximation of potential q was computed with a finite number of nodes.

Disclosure statement

No potential conflict of interest was reported by the authors.

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