HAL Id: jpa-00208884
https://hal.archives-ouvertes.fr/jpa-00208884
Submitted on 1 Jan 1979
HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.
L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.
FeCl2 in a transverse magnetic field : inequivalent behaviour of the two sublattices at 0 K
J.A. Nasser
To cite this version:
J.A. Nasser. FeCl2 in a transverse magnetic field : inequivalent behaviour of the two sublattices at 0
K. Journal de Physique, 1979, 40 (1), pp.51-56. �10.1051/jphys:0197900400105100�. �jpa-00208884�
FeCl2 in a transverse magnetic field :
inequivalent behaviour of the two sublattices at 0 K
J. A. Nasser
DPh-G/PSRM, CEN Saclay, B.P. N° 2, 91190 Gif sur Yvette, France
(Reçu le 3 janvier 1978, révisé le 10 juillet 1978, accepté le 2 octobre 1978)
Resumé. 2014 Nous étudions à 0 K dans FeCl2
2014un antiferromagnétique uniaxe pour T ~ TN
2014les effets élas-
tiques et magnétiques dus au couplage spin-reseau introduit par le champ cristallin de l’ion Fe2+. A 0 K, en champ perpendiculaire à l’axe de facile aimantation, qui coincide avec l’axe 3 du groupe ponctuel (3 m) des ions fer, les résultats sont les suivants : il s’établit des déformations qui détruisent la symétrie du cristal. Il apparait
une aimantation globale qui a une composante suivant la direction du champ mais aussi une composante suivant l’axe ternaire; ce dernier résultat bien qu’a priori surprenant est conforme aux considerations de symétrie. Par
ailleurs les moments des deux sous-réseaux ne sont plus contenus dans le plan de l’axe et du champ, et ne s’in-
clinent pas également en direction du champ. Enfin, pour un champ de module fixé, les résultats varient avec
la direction du champ dans le plan perpendiculaire à l’axe ternaire.
Abstract.
2014For the uniaxial antiferromagnet FeCl2, we study the elastic and magnetic effects at 0 K due to
the magneto-elastic coupling introduced by the crystal field of the Fe2+ ions. In a magnetic field H perpendicular
to the easy magnetization axis, which is the 3 axis of the point group (3 m) of Fe2+ ions, strains occur destroying
the crystal symmetry and a bulk magnetization appears with components along the field direction and also along
the ternary axis. The presence of the component along the ternary axis is compatible with symmetry considerations.
Also each of the magnetic moments of the two sublattices no longer lies in the plane defined by H and the ternary axis and they do not equally tilt towards the field direction. For H of a given size, the results vary quantitatively
with the direction of H in the plane perpendicular to the ternary axis.
Physics Abstracts
76.80
-75.80
-75-50E - 75.30G
1. Introduction. - The static magnetic properties [ 1 ]
of FeCl2
-an uniaxial antiferromagnet
-as well
as its magnetic excitations [2] have been extensively
studied. But whereas some experiments [3] have clearly shown the importance of the magneto-elastic coupling in this compound, a number of static experi-
mental results obtained either in zero field or with the field parallel to the easy magnetization axis, can be satisfactorily interpreted with a model due to Ôno [4],
which neglects the crystal strains. This arises as under
these experimental conditions the magneto-elastic coupling does not qualitatively modify the results of the model. In a transverse field, however, the
minimization of the free energy can take place through
the introduction of strains which destroy the crystal symmetry giving a magnetic structure which cannot
be predicted within Ôno’s model. For this structure the two sublattices show inequivalent behaviour in the antiferromagnetic phase.
One aspect of this inequivalent behaviour has
already been observed in the Môssbauer spectrum of the Fe 2+ ion [5]. The splitting of the right hand
absorption line into two components as shown on
figure 1, which shows a cos 3 9 dependence, is due to
the fact that the projection on the field direction of the
magnetic moment of one sublattice is not equal to
that of the other sublattice.
The above mentioned magnetic and elastic effects arise from the variations of crystalline field of Fe2 +
with crystal strains. These variations are significative only if the orbital moment is not completely quenched
as in the case for FeC12. The variations disturb the orbital state of Fe2 + which, because of spin-orbit coupling, modifies its spin state.
If Epg and Li (p, q, i = 1, 2, 3) are the respective components, in an orthogonal frame { Oxi }, of the
strain tensor and the orbital moment of the free Fe 21 ion, the development in Gpq of the crystalline field can
be written Y Apqij epq,(Li Lj + Lj LJ. The non-zero
p,4,tj
’
components of the tensor A pqj’ are determined from the point group (3m) of the Fe¥ + ions in the zero field
paramagnetic phase. If one considers the e pq as variational parameters, the development in Gpq is an
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:0197900400105100
52
Fig. 1.
-Môssbauer spectrum of Fe2+ at 4.2 K and H = 60 k0e;
qJ is the angle defined in figure 2.
operator which can be decomposed into two parts,
one having 3m symmetry, and the other, l5w, with a
lower symmetry. ôw is certainly smaller than the operator of trigonal symmetry and also smaller than the spin-lattice coupling operator due to the exchange
interaction. Nevertheless it is bw which is responsible
for the effects studied here. The operator with 3m
symmetry (as well as the development in Ep9 of exchange integrals) can cause the appearance of strains which however cannot lower the crystal symmetry and can lead to the appearance of magnetic
effects qualitatively similar to those contained in Ôno’s model.
The importance in FeCl2 of spin-lattice coupling
associated with the strain variation of crystal field parameters was initially described by G. Laurence and
D. Petitgrand [6] following Laurence’s thermal con-
ductivity measurements in FeCl2 [2] (G. Laurence 1971). Subsequent theoretical [7] and experimental [8]
studies have examined the consequences of this spin-
lattice coupling on the magnetic excitations in FeC12.
We predict here the influence of this coupling on the
static properties of FeC12.
In this study we consider ôw to be a perturbation to
be added to Ôno’s model at 0 K. One can verify that
our results agree with symmetry considerations.
2. âw as a perturbation of the rigid crystal model.
-Figure 2 represents the antiferromagnetic structure of FeCl2 at 0 K in zero field. The easy magnetization axis
is the ternary axis. In the Oxyz frame, Oz is parallel
to the ternary axis and Ox is contained in a mirror
plane.
In Ôno’s model this structure is explained by taking
into account crystalline field, spin-orbit coupling, ferromagnetic exchange between the Fe2 + ions con-
tained in the same plane perpendicular to the temary axis and the antiferromagnetic exchange between
Fig. 2.
-Antiferromagnetic order of FeCl2 at 0 K and H = 0.
the Fe2 + ions contained in two successive planes perpendicular to the ternary axis. Starting from the
fundamental level of the free Fe2 + ion (L = 2, S = 2),
these interactions are treated as successively decreasing perturbations.
After diagonalizing the crystalline field and the
spin-orbit coupling, one can consider the fundamental level of each ion as a triplet in which there exists an
axial anisotropy term. If one introduces a fictitious
spin s, s = 1, the anisotropy term can be written
-
D(si - 1).
If one uses a two-sublattice molecular field approxi-
mation and taking into account bw and the Zeeman effect in a transverse field, the fundamental level of each ion can be obtained by diagonalizing the Hamil-
tonian JCa within the triplet, where :
Jcx, the Hamiltonian used by Ôno, can be written :
with a = 1, 2 and fl = 2, 1 ; 1 and 2 are the indices of the two sublattices. In this expression : sx, sy, sz
are the components of s in Ox, Oy, Oz. xa, ya, z’ are
the mean values of sx, sy, Sz in the sublattice a ; they are
the solutions of the molecular field equations. Jlll II
and J, _L characterize the ferromagnetic interaction.
H is the modulus of the transverse field H ; (Ox, H) = Q. y. is the Bohr magneton and g1. a
spectroscopic term (gl = 3.22).
bw can be written in terms of the components Lx,
Ly, Lz of the free Fe2 + ion orbital momentum L :
The expression for bw is limited to second order in
Lx, Ly, LZ.
If bw is treated as a perturbation compared with Jea, xa, Ya and z§ can be written :
where bxa, bya and bza are zero if ôw is neglected.
2.1 RESULTS NEGLECTING bw.
-For H smaller than the critical field He ( ~ 130 k0e) of the antiferro-
magnetic saturated paramagnetic transition, the compound is in an antiferromagnetic phase. The magnetic moments of the two sublattices are confined in the plane defined by Oz and H and are equally
inclined with respect to the field. Furthermore the
projection of each sublattice moment on the field direction is independent of cp. This situation is des- cribed by the following relations :
z and x being only dependent on H ; we choose z > 0.
We can finally prove the following results :
-
Jc1 and Je2 have the same eigenvalues which depend only upon H. We call them Ek with k = I, II,
III in increasing order.
-
The normalized eigenvectors 1 03C81/k > associated
with the eigenvalue Ek of Jc1 can be written :
where Âkl Uk and vk are real and where ms = ± 1, 0 >
are the eigenvectors of sz and S2. We obtain 03C8k2
by permuting À,k and vk.
-