Environmental Engineering Reference
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obtain
4 χ + ( ω )+ χ o
+ ( ω ) =
S z
0
χ xx ( ω )= χ yy ( ω )= 1
( ) 2 ,
(3 . 5 . 24 a )
2
and
4 χ + ( ω )
+ ( ω ) =
S z
ihω
0
χ yx ( ω )= i
χ xy ( ω )=
χ o
( ) 2 . (3 . 5 . 24 b )
2
We note here that χ xy ( ω )and χ xy ( ω ), obtained by replacing ω by
ω + i and letting
0 + , are both purely imaginary. Of the remaining
components in χ o ( ω ), only χ zz ( ω ) is non-zero, and it comprises only an
elastic contribution
χ zz ( ω )= β ( δS z ) 2 δ ω 0 ,
( δS z ) 2
( S z ) 2
S z
2
0 . (3 . 5 . 25)
with
0
Because χ o
2
( xy )-matrix equation and a scalar equation for the zz -component. In-
verting the ( xy )-part of the matrix
±z ( ω ) = 0, the RPA equation (3.5.8) factorizes into a 2
×
χ o ( ω )
{
1
J
( q )
}
, we find
χ o ( ω )
χ xx ( ω )
−|
|J
( q )
χ xx ( q )=
2 ( q ) ,
χ o ( ω )
1
−{
χ xx ( ω )+ χ yy ( ω )
}J
( q )+
|
|J
where the determinant is
S z
0
χ o ( ω )
= χ xx ( ω ) χ yy ( ω )
χ xy ( ω ) χ yx ( ω )=
|
|
( ) 2 .
2
By a straightforward manipulation, this leads to
E q
S z
0
χ xx ( q )=
( ) 2 ,
(3 . 5 . 26 a )
( E q ) 2
with
E q =∆
S z
S z
0 J
( q )=
0 {J
( 0 )
−J
( q )
}
.
(3 . 5 . 26 b )
The same result is obtained for χ yy ( q ). We note that (3 . 5 . 26 a ) should
be interpreted as
.
1
1
E q + + ih
χ xx ( q )= 2
S z
0
lim
0 +
ih +
E q
This result is nearly the same as that deduced before, eqns (3.4.10-
11), except that the RPA expectation-value
S z
is replaced by its MF
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