The Green's function method [1] [2]
The Green's function may be used in conjunction with Green's theorem to construct solutions for problems that are governed by
ordinary or partial differential equations.
Integral equation for the field at 
Here the specific position is
and the general coordinate position is
in 3D. ==
A typical physical sciences problem may be written as
Here
is the source,
is the particular solution called the field.
The quantity
is the Dirac delta function.
The problem is set up in a volume
bounded by a surface
There may be boundary conditions, that is to say, prescribed values of
or its derivatives on
the boundary
. The
indicates adjoint meaning that this is the operator
and its respective Green's function allow the expression to be written as an exact divergence.
General form
We write the more general form of Green's theorem making use of these definitions as
where the integrand of the volume integral is an exact divergence
and the left hand side follows from an application of the divergence theorem.
Integral equation for the field, non-self adjoint operator
Substituting from the equalities above
applying the sifting property of the delta function, and rearranging terms, we have
Self adjoint case
The situation where the operator
is called the self-adjoint case.
We leave the
, but note that there is an explicit form for the right hand side
Here
is the normal derivative which is the directional derivative
in the direction normal to the surface
Integral equation for the field, self adjoint operator
Substituting from the equalities above
applying the sifting property of the delta function, and rearranging terms, we have the integral equation of the
field
This result is an integral equation for the field observed at the specific position
,
written in the form of an integral equation. The boundary
may have specific values
of
and/or
or may be sent to infinity, if
an unbounded medium is desired. In the latter case, the boundary conditions are replaced with a radiation condition.
Aki and Richards (2002)[3] uses the term
representation theorem for such a result.
References
- ↑ Bleistein, N. (1984). Mathematical methods for wave phenomena. Academic Press.
- ↑ Bleistein, N., J. K. Cohen, & J. W. Stockwell Jr., (2001). Mathematics of multidimensional seismic imaging, migration, and inversion. Springer Verlag.
- ↑ Aki, K., & Richards, P. G. (2002). Quantitative seismology (Vol. 1).
External links
find literature about Green's function method
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