Environmental Engineering Reference
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that the trace of the Hamiltonian (2.1.1) vanishes, and hence that the
denominator in (2.1.11) is Tr
=(2 J +1) N . For the second-order
{
1
}
term in the numerator, we find
Tr J J H = δ ij B 2 Tr J J O 2 ( J i ) −J
( ij )Tr J J J i · J j
= δ ij δ αβ B 2 Tr J [3 J iz
J ( J +1)]
( ij )Tr J J ,
δ αβ J
utilizing that J J is a linear combination of second- and lower-rank
tensors for i = j , and a product of first-rank tensors for i
= j .When
α = z (or ζ ), we may readily calculate the first trace, using
m 4 =
1
15
J ( J + 1)(2 J + 1)(3 J 2 +3 J
1) .
The traces with α = x or α = y must be equal, and using this equality
in the case α = x , for instance, we may replace J x
in the trace by
1
2 ( J x + J y )
1
1
2 J z . As the constant term multiplied by
2 J ( J +1)
3 J z
3 J z
J ( J + 1) does not contribute (as Tr
{
J ( J +1)
}
= 0), the
trace with α = x or y is equal to
1 / 2 times that with α = z . Only the
single-ion terms contribute to the trace when i = j (
( ii ) is assumed to
be zero), and of these only the lowest-rank term B 2 appears, to leading
order. The two-ion coupling only occurs in the trace, and hence in
χ αβ ( ij ), when i
J
= j , and this contribution may be straightforwardly
calculated. To second order in β , the off-diagonal terms are zero, whereas
J ( J +1) β 1
) β
χ αα ( ij )= δ ij 3
5
2
)( J + 2
1) B 2 ( J
(3 δ αζ
+ 3
J ( J +1) β 2
J
( ij ) .
Introducing the Fourier transform of the two-ion coupling,
( q )=
j
( ij ) e −i q · ( R i R j ) ,
J
J
(2 . 1 . 13)
we find that, to the order considered, the inverse of the q -dependent
susceptibility may be written
2 )( J + 2 )
5 J ( J +1)
1
3 k B T
1) 6( J
B 2 −J
1 αα ( q )=
J ( J +1) +(3 δ αζ
( q )+
O
(1 /T ) .
(2 . 1 . 14)
The inverse susceptibility in the high-temperature limit thus increases
linearly with the temperature, with a slope inversely proportional to the
square of the effective paramagnetic moment (
1 / 2 ). The
susceptibilities determined experimentally by magnetization measure-
∝{
J ( J +1)
}
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