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Accordingly, the slow spatial variations require the substitution
in (15), where
may be viewed as a variational parameter, the whole spatial variation
being transferred upon the new Fermi wavevector
; a similar
substitution
holds for the
electron density (14), and it is worth noting that such substitutions
are valid over those space regions where
and
are
comparable in magnitude; such substitutions are corrected by the quantal
effects of the Hartree equations, as discussed above, as due to the abrupt
spatial variations of the self-consistent potential and the electron density
in the neighbourhood of the ionic cores. A linearized version[1] is
thereby obtained for the Thomas-Fermi scheme, which consists in
 |
(17) |
according to (14) and (15), where the Thomas-Fermi screening
wavevector
has been introduced through
 |
(18) |
it will be taken as the variational parameter; the Bohr radius
Å is used as length unit and the atomic unit
eV is also used for energy. Poisson's equation (7) reads now
 |
(19) |
and its solution provides the self-consistent field
. It is worth
noting that the quasi-classical description and the quasi-classical
equilibrium equation (15) are valid for slow spatial variations,
requiring thus the linearized Thomas-Fermi scheme; the usual ''
''-Thomas-Fermi model, where
, would be inappropriate
for the slightly inhomogeneous electron liquid; the ''
''-Thomas-Fermi
model holds in the classical limit of the quantal mechanics, which is often
called the ''quasi-classical approximation''.[2]
[4]
Two-cluster aggregation
|
In order to estimate the effect of the quantal corrections, as
arising from those spatial regions of abrupt variations, the variational
parameter
given by (18) (associated with the
electron density) may be compared with the average Fermi wavevector
 |
(20) |
where
 |
(21) |
is the total charge; it is worth noting here the electric neutrality of the
aggregate, as obtained from Poisson's equation (7), for instance; such
a comparison can also be made between the variational parameter
and the
average parameter
, obtained through (18) with
replaced by
.
Next: Energy
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