In mathematics, a Green's function is a type of function used to solve inhomogeneous differential equations subject to boundary conditions. Technically, a Green's function of a linear operator L acting on distributions over a manifold M, at a point x0, is any solution of (Lf)(x) = δ(x − x0), where δ is the Dirac delta function. If the kernel of L is nontrivial, then the Green's function is not unique. However, in practice, some combination of symmetry, boundary conditions and/or other externally imposed criteria would give us a unique Green's function. Also, please note that Green's functions in general are distributions, not necessarily proper functions.
Not every operator L admits a Green's function. A Green's function can also be thought of as a one-sided inverse of L.
Green's functions are also a useful tool in condensed matter theory, where they allow the resolution of the diffusion equation - and in quantum mechanics, where the Green's function of the Hamiltonian is a key concept, with important links to the concept of density of states. The Green's functions used in those two domains are highly similar, due to the analogy in the mathematical structure of the diffusion equation and Schrödinger equation.
The Green's function was named after British mathematician George Green, who first developed the concept in the 1830s.
Convolving with a Green's function gives solutions to inhomogeneous differential-integral equations, most commonly a Sturm-Liouville problem. If g is the Green's function of an operator L, then the solution for f of the equation Lf = h is given by
This can be thought of as an expansion of h according to a Dirac delta function basis (projecting h over δ(x − s)) and a superposition of the solution on each projection. Such an integral is known as a Fredholm integral equation, the study of which constitutes Fredholm theory.
The primary use of Green's functions in mathematics is to solve inhomogeneous boundary value problems. In particle physics, Green's functions are also usually used as propagators in Feynman diagrams (and the phrase "Green's function" is often used for any correlation function).
Let be the Sturm-Liouville operator, a linear differential operator of the form
Let be a continuous function in . We shall also suppose that the problem
Then there is one and only one solution u(x) which satisfies
and it is given by
where g(x,s) is Green's function and satisfies the following demands:
If a differential operator L admits a set of eigenvectors (i.e. a set of functions and scalars such that ) that are complete, then we can construct a Green's function from these eigenvectors and eigenvalues.
By complete, we mean that the set of functions : satisfies the following completeness relation:
We can prove the following:
Now consider acting on this on each side with the operator L. We'll end up with the completeness relation, which was assumed true.
The general study of the Green's function written in the above form, and its relationship to the function spaces formed by the eigenvectors, is known as Fredholm theory.
Green's functions for linear differential operators involving the laplacian may be readily put to use using the second of Green's identities.
To derive Green's theorem, begin with the divergence theorem (otherwise known as Gauss's law):
Let and substitute into Gauss' law. Compute and apply the chain rule for the operator:
Plugging this into the divergence theorem, we arrive at Green's theorem:
Suppose that our linear differential operator L is the laplacian, , and that we have a Green's function G for the laplacian. The defining property of the Green's function still holds:
Let in Green's theorem. We get:
Using this expression, we can solve Laplace's equation or Poisson's equation , subject to either Neumann or Dirichlet boundary conditions. In other words, we can solve for everywhere inside a volume where either (1) the value of is specified on the bounding surface of the volume (Dirichlet boundary conditions), or (2) the normal derivative of is specified on the bounding surface.
Suppose we're interested in solving for inside the region. Then the integral
This form expresses the well-known property of harmonic functions, that if the value or normal derivative is known on a bounding surface, then the value of the function inside the volume is known everywhere.
In electrostatics, we interpret as the electric potential, as electric charge density, and the normal derivative as the normal component of the electric field.
If we're interested in solving a Dirichlet boundary value problem, we choose our Green's function such that vanishes when either x or x' is on the bounding surface; conversely, if we're interested in solving a Neumann boundary value problem, we choose our Green's function such that its normal derivative vanishes on the bounding surface. Thus we are left with only one of the two terms in the surface integral.
With no boundary conditions, the Green's function for the Laplacian is:
Supposing that our bounding surface goes out to infinity, and plugging in this expression for the Green's function, we arrive at the familiar expression for electric potential in terms of electric charge density:
Given the problem
Find Green's function.
First step: From demand-2 we see that
Summarize the results:
Second step: Now we shall determine a(s) and b(s).
Using demand-1 we get
Check that this automatically satisfies demand-5.
So our Green's function for this problem is:
where the +(-) signifies the retarded (advanced) Green's function.
Then the density of one particle states at energy E is written as
Greensche Funktion | Fonction de Green | グリーン関数 | Функция Грина
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"Green's function".
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