Environmental Engineering Reference
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which is a simple combination of Bose Green-functions determined by
(5.2.20), with E q replaced by E q ( T ). Introducing these functions and
the parameters given by (5.2.34), we finally obtain
m ) A q ( T )
B q ( T )
χ xx ( q )= J (1
( ) 2 ,
(5 . 2 . 40 a )
E q ( T )
neglecting third-order terms. A rotation of the coordinate system by
π/ 2 around the z -axis changes the sign of B q ( T ), and hence we have
χ yy ( q )= J (1 − m ) A q ( T )+ B q ( T )
( ) 2 .
(5 . 2 . 40 b )
E q ( T )
These results show that the ratio between the neutron-scattering inten-
sities due to the spin-wave at q , neglecting S zz ( q ), in the two cases
where the scattering vector is perpendicular to the basal y - z plane and
to the x - z plane is
= ±E q ( T )
R q ( T )= S xx ( q )
S yy ( q )
= χ xx ( q , 0)
χ yy ( q , 0)
= A q ( T ) − B q ( T )
A q ( T )+ B q ( T ) .
(5 . 2 . 41)
The measured intensities from Tb, which differ substantially from those
calculated for the Heisenberg ferromagnet, agree well with this expres-
sion, especially if the correction for anisotropic two-ion coupling is taken
into account (Jensen et al. 1975).
In the Heisenberg ferromagnet without rotational anisotropy, corre-
sponding to B q ( T ) = 0, the elementary excitations at low temperatures
are circularly polarized spin waves, in which the local moments precess
in circles around the equilibrium direction. In the presence of anisotropy,
R q ( T ) differs from unity, and the excitations become elliptically polar-
ized spin waves. The eccentricity of the ellipse depends on the wave-
vector of the excited spin wave, and by definition R q ( T ) is the square of
the ratio of the lengths of the principal axes which, at least to the order
in 1 /J which we have considered, is equal to the ratio between the cor-
responding static susceptibility components. So the static anisotropy is
reflected, in a direct way, in the normal modes of the system. The result
(5.2.41) justifies the transformation (5.2.34) by attributing observable
effects to the parameters A q ( T )
B q ( T ), whereas the parameters which
are defined via the Hamiltonian alone, here A q ( T )
±
± B q ( T ), depend on
the particular Bose representation which is employed.
The longitudinal correlation function S zz ( q ), which is neglected
above, contains a diffusive mode at zero frequency, but no well-defined
normal modes of non-zero frequency. There is inelastic scattering, but
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