The Green's function is expressed in the usual cite-centered
angular momentum expansion
For layered systems we apply a 2D-Fourier transform [13]:
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(3) |
The calculation of the Green's function requires a matrix inversion. To
simplify the formulas we drop all angular momentum and cite indices. Equation
4 can be easily transformed to:
Due to the exponential decrease of the screened structure constants, the
coupling can be limited to few neighbouring shells, so that the 2D Fourier
transform of the reference Green's function has the structure of a band matrix
coupling only neighbouring layers. Therefore, one can simplify the matrix
by grouping several atomic layers into so-called principal
layers [14,15], the coupling of which is limited to the
first nearest principal layers only. Assuming a system of identical repulsive
potentials in a lattice, the reference Green's function has the form:
For the case of a finite slab system the has a finite rank, is band
diagonal and has the form of eq. 7, while
is
diagonal in the cite index and in the principal layer representation
eq.4 has the form of the Dyson equation for a linear chain with
nearest neighbour coupling only. For such systems, the diagonal blocks of the
real system Greenīs function
, which are required to obtain the charge
density,
can be
calculated [16], [17] with efford that scales linear with the
number of principal layers in the slab
. This
-scaling behaviour is one
of the main advantages of the screened KKR approach.
The band diagonal form of the Green's function allows us to treat also
semiinfinite systems. In this case we need to invert an infinite matrix. We
can divide the system in three regions: an intermediate region (I), embedded
into two (unperturbed) semi-infinite left (L) and right (R) halfspaces. The
regions R and L are characterized by bulk potentials, so that the new
selfconsistency process affects only the potentials of the region I.
Using an inversion-by-partitioning
tequnique it is easy to see that, embedding region I into the semiinfinite L
and R host media would only affect the and
blocks of the
Green's function matrix. This embedding information is included in the surface
Green's function
(left halfspace),
(right
halfspace) which we obtain using an iterative procedure, the so called
decimation method, as described in ref [14,15].
Usually 5-6 iterations are enough, to obtain well converged
surface Green's functions.
Only a few
points (i.e. close to Van Hove singularities)
require additional effort.