Environmental Engineering Reference
In-Depth Information
where
σ
α
=
σ
α
(
q
) is the relative magnetization at the wave-vector
q
.
Introducing this into the free-energy expression, and utilizing the condi-
tion that
i
cos(
q
·
R
i
+
ϕ
)=0,if
q
is not a reciprocal lattice vector,
we find
J
2
F
0
)
/N
=
4
σ
α
f
=(
F
−
α
{
2
A
α
−J
(
q
)
}
J
4
αβ
+
8
σ
α
σ
β
,
B
αβ
{
2+cos2(
ϕ
α
−
ϕ
β
)
}
(2
.
1
.
24)
if 4
q
is different from a reciprocal lattice vector.
The coecients of
the second power are thus
=1
/χ
αα
(
q
,σ
=0),where
the susceptibility is evaluated at zero magnetization. As long as all the
second-order coecients are positive, at any value of
q
, the free energy
is at its minimum when
σ
α
= 0, i.e. the system is paramagnetic. The
smallest of these coecients are those at
q
=
Q
,where
∝{
2
A
α
−J
(
q
)
}
(
q
)hasits
maximum. In the heavy rare earths, with the exception of Gd,
Q
is
non-zero and is directed along the
c
-axis. Depending on the sign of
B
2
, the magnetic structures occurring in the heavy rare earths may be
divided into two classes, which we will discuss in turn.
J
2.1.3 Transversely ordered phases
When
B
2
>
0, as in Tb, Dy, and Ho, the two basal-plane components
of
χ
(
Q
) both diverge at the same critical temperature
T
N
.Usingthe
approximate high-temperature value (2.1.20) for the susceptibility, we
find that 1
/χ
ξξ
(
Q
,σ
=0)=1
/χ
ηη
(
Q
,
0) = 2
A
ξ
−J
(
Q
) vanishes at the
temperature determined by
(
Q
)
1+
5
)
B
2
/k
B
T
N
.
k
B
T
N
3
−
2
)(
J
+
2
J
(
J
+1)
J
(
J
(2
.
1
.
25)
Below
T
N
,both
σ
ξ
and
σ
η
are generally non-zero at the wave-vector
Q
,
and the free energy
f
, given by (2.1.24) with
σ
ζ
= 0, is minimized when
σ
ξ
(
Q
)=
σ
η
(
Q
)=
σ
Q
,and
σ
Q
=
J
1
/
2
(
Q
)
2
A
ξ
4
J
2
B
ξξ
−
π
2
,
;
ϕ
ξ
− ϕ
η
=
±
(2
.
1
.
26
a
)
corresponding to the helical ordering:
J
iξ
=
Jσ
Q
cos (
Q
·
R
i
+
ϕ
)
(2
.
1
.
26
b
)
J
iη
=
±
Jσ
Q
sin (
Q
·
R
i
+
ϕ
)
.
The length of the angular-momentum vector is
Jσ
Q
, independent of the
site considered. There are two energetically-degenerate configurations,
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