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In mathematics and its applications, a classical Sturm–Liouville equation, named after Jacques Charles François Sturm (1803–1855) and Joseph Liouville (1809–1882), is a real second-order linear differential equation of the form where y is a function of the free variable x. Here the functions p(x) > 0 has a continuous derivative, q(x), and w(x) > 0 are specified at the outset, and in the simplest of cases are continuous on the finite closed interval [a,b]. In addition, the function y is typically required to satisfy some boundary conditions at a and b. The function w(x), which is sometimes called r(x), is called the "weight" or "density" function. The value of λ is not specified in the equation; finding the values of λ for which there exists a non-trivial solution of (1) satisfying the boundary conditions is part of the problem called the Sturm–Liouville problem (S L). Such values of λ when they exist are called the eigenvalues of the boundary value problem defined by (1) and the prescribed set of boundary conditions. The corresponding solutions (for such a λ) are the eigenfunctions of this problem. Under normal assumptions on the coefficient functions p(x), q(x), and w(x) above, they induce a Hermitian differential operator in some function space defined by boundary conditions. The resulting theory of the existence and asymptotic behavior of the eigenvalues, the corresponding qualitative theory of the eigenfunctions and their completeness in a suitable function space became known as Sturm–Liouville theory. This theory is important in applied mathematics, where S–L problems occur very commonly, particularly when dealing with linear partial differential equations that are separable.
Under the assumptions that the S–L problem is regular, that is, p(x)^{−1} > 0, q(x), and w(x) > 0 are real-valued integrable functions over the finite interval [a, b], with separated boundary conditions of the form
[math]\displaystyle{ y(a)\cos \alpha - p(a)y^\prime (a)\sin \alpha = 0, }[/math] |
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[math]\displaystyle{ y(b)\cos \beta - p(b)y^\prime (b)\sin \beta = 0, }[/math] |
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the main tenet of Sturm–Liouville theory states that:
Note that, unless p(x) is continuously differentiable and q(x), w(x) are continuous, the equation has to be understood in a weak sense.
The differential equation (1) is said to be in Sturm–Liouville form or self-adjoint form. All second-order linear ordinary differential equations can be recast in the form on the left-hand side of (1) by multiplying both sides of the equation by an appropriate integrating factor (although the same is not true of second-order partial differential equations, or if y is a vector.)
The Bessel equation:
can be written in Sturm–Liouville form as
The Legendre equation,
can easily be put into Sturm–Liouville form, since D(1 − x^{2}) = −2x, so, the Legendre equation is equivalent to
Less simple is such a differential equation as
Divide throughout by x^{3}:
Multiplying throughout by an integrating factor of
gives
which can be easily put into Sturm–Liouville form since
so the differential equation is equivalent to
In general, given a differential equation
dividing by P(x), multiplying through by the integrating factor
and then collecting gives the Sturm–Liouville form.
The map
can be viewed as a linear operator mapping a function u to another function Lu. We may study this linear operator in the context of functional analysis. In fact, equation (1) can be written as
This is precisely the eigenvalue problem; that is, we are trying to find the eigenvalues λ_{1}, λ_{2}, λ_{3}, ... and the corresponding eigenvectors u_{1}, u_{2}, u_{3}, ... of the L operator. The proper setting for this problem is the Hilbert space L^{2}([a, b],w(x) dx) with scalar product
In this space L is defined on sufficiently smooth functions which satisfy the above boundary conditions. Moreover, L gives rise to a self-adjoint operator. This can be seen formally by using integration by parts twice, where the boundary terms vanish by virtue of the boundary conditions. It then follows that the eigenvalues of a Sturm–Liouville operator are real and that eigenfunctions of L corresponding to different eigenvalues are orthogonal. However, this operator is unbounded and hence existence of an orthonormal basis of eigenfunctions is not evident. To overcome this problem one looks at the resolvent
where z is chosen to be some real number which is not an eigenvalue. Then, computing the resolvent amounts to solving the inhomogeneous equation, which can be done using the variation of parameters formula. This shows that the resolvent is an integral operator with a continuous symmetric kernel (the Green's function of the problem). As a consequence of the Arzelà–Ascoli theorem this integral operator is compact and existence of a sequence of eigenvalues α_{n} which converge to 0 and eigenfunctions which form an orthonormal basis follows from the spectral theorem for compact operators. Finally, note that [math]\displaystyle{ (L-z)^{-1} u = \alpha u }[/math] is equivalent to [math]\displaystyle{ L u = (z+\alpha^{-1}) u }[/math].
If the interval is unbounded, or if the coefficients have singularities at the boundary points, one calls L singular. In this case the spectrum does no longer consist of eigenvalues alone and can contain a continuous component. There is still an associated eigenfunction expansion (similar to Fourier series versus Fourier transform). This is important in quantum mechanics, since the one-dimensional Schrödinger equation is a special case of a S–L equation.
We wish to find a function u(x) which solves the following Sturm–Liouville problem:
[math]\displaystyle{ L u = \frac{d^2u}{dx^2} = \lambda u }[/math] |
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where the unknowns are λ and u(x). As above, we must add boundary conditions, we take for example
Observe that if k is any integer, then the function
is a solution with eigenvalue λ = −k^{2}. We know that the solutions of a S–L problem form an orthogonal basis, and we know from Fourier series that this set of sinusoidal functions is an orthogonal basis. Since orthogonal bases are always maximal (by definition) we conclude that the S–L problem in this case has no other eigenvectors.
Given the preceding, let us now solve the inhomogeneous problem
with the same boundary conditions. In this case, we must write f(x) = x in a Fourier series. The reader may check, either by integrating ∫exp(ikx)x dx or by consulting a table of Fourier transforms, that we thus obtain
This particular Fourier series is troublesome because of its poor convergence properties. It is not clear a priori whether the series converges pointwise. Because of Fourier analysis, since the Fourier coefficients are "square-summable", the Fourier series converges in L^{2} which is all we need for this particular theory to function. We mention for the interested reader that in this case we may rely on a result which says that Fourier's series converges at every point of differentiability, and at jump points (the function x, considered as a periodic function, has a jump at π) converges to the average of the left and right limits (see convergence of Fourier series).
Therefore, by using formula (4), we obtain that the solution is
In this case, we could have found the answer using antidifferentiation. This technique yields u = (x^{3} − π^{2}x)/6, whose Fourier series agrees with the solution we found. The antidifferentiation technique is no longer useful in most cases when the differential equation is in many variables.
Suppose we are interested in the modes of vibration of a thin membrane, held in a rectangular frame, 0 < x < L_{1}, 0 < y < L_{2}. We know the equation of motion for the vertical membrane's displacement, W(x, y, t) is given by the wave equation:
The equation is separable (substituting W = X(x) × Y(y) × T(t)), and the normal mode solutions that have harmonic time dependence and satisfy the boundary conditions W = 0 at x = 0, L_{1} and y = 0, L_{2} are given by
where m and n are non-zero integers, A_{mn} is an arbitrary constant and
Since the eigenfunctions W_{mn} form a basis, an arbitrary initial displacement can be decomposed into a sum of these modes, which each vibrate at their individual frequencies [math]\displaystyle{ \omega_{mn} }[/math]. Infinite sums are also valid, as long as they converge.