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HAL Id: jpa-00236007

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Submitted on 1 Jan 1959

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Optical Faraday rotation in ferrimagnetic garnets

A.M. Clogston

To cite this version:

A.M. Clogston. Optical Faraday rotation in ferrimagnetic garnets. J. Phys. Radium, 1959, 20 (2-3),

pp.151-154. �10.1051/jphysrad:01959002002-3015100�. �jpa-00236007�

(2)

151

OPTICAL FARADAY ROTATION IN FERRIMAGNETIC GARNETS

By A. M. CLOGSTON,

Bell Telephone Laboratories, Inc., Murray Hill, New Jersey.

Résumé.

2014

Les grenats ferrimagnétiques présentent

une

grande rotation de Faraday optique.

Les transitions dont il s’agit sont interdites, tant par les règles de sélection dues

au

spin que par celles dues à la parité. Une probabilité non-nulle de transition résulte de l’action combinée des

couplages spin-orbite, et des vibrations du réseau. Ceux-ci introduisent dans les états fondamentaux et excités des contributions de parités contraires. Le couplage spin-orbite décompose

ces

états

en

présence d’un champ d’échange

ce

qui produit

une

rotation de Faraday

non

nulle. On calcule le

rapport rotation-absorption et

on

trouve

un

accord satisfaisant avec l’expérience.

Abstract. 2014 The ferrimagnetic garnets exhibit

a

large optical Faraday rotation. The transi- tions involved are both spin and parity forbidden. A non-zero transition probability arises from the combined action of spin-orbit coupling, and lattice vibrations which augment the ground and

excited states with odd-parity angular momentum states. These states are split in the presence of the exchange field by spin-orbit coupling and lead to Faraday rotation. The ratio of rotation to

absorption is calculated and found to give satisfactory agreement with experiment.

PHYSIQUE 20, FÉVRIER 1959,

I. Introduction.

-

Dillon (1957) has recently reported that the ferrimagnetic garnets are suffi- ciently transparent in the visible region of the spectrum so that a considerable amount of light

may be transmitted through thin sections of single crystals. Initial observations of this effect using polarized light vividly revealed the domain struc- ture of the crystals. The contrast between

domains with differently oriented magnetizations

arises from a Faraday rotation of the plane of polarization of a light wave traversing the domain.

Dillon has measured the absorption coefficient and

Faraday rotation as a function of energy in the visible spectrum for a series of ferrimagnetic garnets. He has observed very large rotations,

the origin of which is a matter of fundamental interest. We shall show in this paper that the

Faraday rotation arises from an electric dipole

transition in contrast to the usual magnetic dipole

effect observed with paramagnetic salts of such

ions as Ni++.

II. Energy levels in the crystal field.

-

The

ferrimagnetic garnets have the type form Y3Fe2(FeO4)3, where the yttrium may be replaced by various rare earth ions. The iron ions are trivalent and occur on sites of predominantly

octahedral or tetrahedral symmetry. Trivalent

iron has the ground state electronic con- ration (3d"). The states of this ion in a crystal

field of octahedral symmetry have been discussed at length by Orgel (1955). In Fig. 1, we show an

energy level diagram similar to that presented by Orgel for Mn++ but calculated instead for Fe+++.

On the axis of ordinates are shown the states of the free ion, beginning with the ground state (3d5)6S. Next higher in energy are a series of

quartet states such as (3d5)4 G arising from invert-

ing one spin in the d-shell. Above the quartet

states are series of doublet states also arising

FIG. 1. - Crystal field splitting

of the energy levels of Fe+ + +,

from (3d5) which will not concern us and are not shown. Much higher in energy is a set of sb41es

arising from (3d 4s) and finally a set coming

from (3d4 4p). In the free ion electric dipole tran- sitions between the ground state 68 an4 the

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphysrad:01959002002-3015100

(3)

152

quartet states are highly forbidden by parity and spin considerations. The first electric dipole

allowed transition is to (3d4 4p)sP.

In a crystalline electric field of octahedral sym- metry whose strength is proportional to the para- meter Dq, the quartet energy levels split and move

as shown. A value of Dq between 1 000 and

2 000 seems appropriate to explain the absorption spectra observed in many salts of Mn++ and Fe+++. With such values of Dq, the corresponding

levels for the tetrahedrally coordinated ions are

expected to lie outside the range of interest. Of the states other than quartets, we shall be parti- cularly concerned with the location of (3d4 4p)6 P.

The high energy and extended orbits of this state make the crystal field approximation inadequate.

The model that we adopt requires that this state

be actually depressed to the neighborhood of 20,000 cm-’.

III. Effect of exchange coupling and spin-oibit

interaction.

-

We now recognize that the ferri- magnetic garnets. will have strong exchange forces acting upon the individual ions. We shall concern

ourselves principally with the lowest energy state 4T1(4G), derived from 4G. This state is an

orbital triplet and therefore has a total degeneracy

of 12. In the strong exchange field, this dege-

neracy is partly removed as shown in Fig. 2. In

FIG. 2.

-

Effect of exchange field

on

energy levels.

the notation adopted here, 4A, 4B and 4C are the

orbital components of 4Tl and a subscript will

denote the spin state. The ground state is also split in the exchange field as shown in Fig. 2. We

limit our considerations to very low temperatures

and suppose only the lowest spin state is occupied.

Let us now consider the effect of spin-orbit coupl-

ing on this array of states. We find that the

states mix in the following groups :

We shall be particularly concerned with the states derived from 685/2 and 4A3/2 which become respectively,

where W is the separation between 6S5/2 and 4A3/2,

,

and b =V5N aocp. Here, x is the spin-orbit coupl- ing parameter,

and

We can ca’Iculate b - 150 cm-1. The quantities Nocp and NOCF are respectively the fractional amount of 4P and 4F mixed with 4G to form 4 Tl (4 G). The coupling between and 4Tl(4G) arises only because 4TI(4G) has an admix-

ture of 4P. This admixture takes place only for

the states of symmetry Tl.

IV. Magnetic dipole transitions.

-

We now consider the strength of magretic dipole transitions between the ground state (1) and the excited mani-

fold 4Tx(4G). These transitions involve the matrix elements of (L + 2S), which will exist between the

ground state and the state formed from (683/2 4B3/2 4A1i2), and have the order of magni-

tude 4 g b/W where is the Bohr magneton. The f

value for this transition will then be

which we calculate to be about 10-9. The observ- ed oscillator strengths, on the other hand are

about 10-4. We thus eliminate magnetic dipole

transitions as the source of the observed absorp-

tions and rotations.

V. Electric dipole transitions.

-

Electric dipole

transitions between the ground state (1) and excited

state (2) are forbidden by parity since all the states involved are constructed from 3d orbitals. To obtain an allowed transition, we adopt a model in

which these states are augmented by a portion of a

state arising from the configuration (3d4 4p)..It is possible that this model is over simplified and that a

better theory must consider charge transfer states

(4)

involving electrons associated with the oxygen

ligands. The desired admixture can be brought

about if the Fe+++ does not lie at a center of sym-

metry or if the symmetry is destroyed by lattice

vibrations. In the ferrimagnetic garnets, the Fe+++ is symmetrically surrounded by 0- ions.

We need consider then only the effect of lattice vibrations. Vibrations of particular symmetries

can introduce an additional potential energy for the electrons of the central ion of the form

(ax + by + cz) which is effective in bringing

about the required mixing. There are two pro-

cesses which will take place : (1) the mixing of (3d5)6S5l2 with (3d4 4p)6 P5/2; and (2) the mixing

of (3d5)4A3/2 with (3d4 4p)4D3/2 and (3d4 4p)4F3/2.

Both of these processes will contribute to the

strength of the absorption line ; but we shall simplify the discussion here by considering only

the first case. It may be noted, however, that

process (1) contributes line strength only to tran-

sitions involving 4TJ. Transitions involving 4T2

must arise from process (2).

The state 6P is 18 fold degenerate and will split

in the exchange field as shown in Fig. 2, where again we will consider only the lowest state 6 PS/2.

The remaining degeneracy of this state is split by spin-orbit coupling into three states characterized

by orbital angular momentum 1, 0 and - 1 which

we shall designate as 6P5/2(1), 6P5/2(0), 6P5/2(- 1)

and assign energies A -r- u, A, and A - u respec- tively. We now calculate thelfollowing matrix

components,

,

v -

ground state and excited state wave functions

become

Using these wave functions, we may calculate the

following

--

matrix components of the dipole

~

moment P.

where M = (6Ps/2(1)IPxI68s/2) = el, is the matrix

component for electric dipole transition from 685/2

to 6P5/2.

Equations (8) and (9) allow us to make a rough

estimate of the oscillator strength of the electric

dipole transitions. If /0 is the strength of the

transition from 6S to 6 P we find

We estimate occc* as follows : a motion that

moves an Fe+++ ion a distance d toward one of its 6 surrounding 0- ions creates a value of

oc

given by

,

where a is the (Fe+++

-

0=) distance. X-ray

data (Geller, 1957) indicate that, at room tempe-

rature the root mean square value of (dIa) is

about 1/10. This would indicate that

cc

- 5 Dq.

Since not all the vibrations will be as effective as

the one taken above, we estimate roughly loci r-J 1 000 cm-1. The most interesting absorp-

tion peak in Dillon’s measurements occurs at W = 16,000 cm-1. We assume further that the

very strong absorption edge beginning a 20,000 cm-1 is to be associated with direct tran- sitions to the 6P level. Accordingly we chose

A

=

20,000 cm-1. We further estimate roughly

that f o = 1/3. Using these values we obtain

f r-J 10-5. This is within an order of magnitude

of the measured values.

VI. Faraday rotation.

-

It is clear from equa- tions (8) and (9) that the transition probabilities

for right and left hand circularly polarized waves

are different and that a rotation of the plane of polarization will therefore occur. If it is assumed that the excited level is broadened by vibrations

and has a Gaussian line shape, it may be shown that the rotation will exhibit a dispersion shaped

curve with a maximum value in radians/cm given

by

where 3W is the root mean square width of the

line, N is the number of ions per cubic centimeter and Sois the dielectric constant of the crystal. The absorption coefficient at the center of the line is

similarly found to be,

The ratio r/6, becomes simply

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154

If we assume, as before, that W = 16,000 cm-’

and A = 20,000 cm-1, and in addition assume

Jgo = 2.5 and u = 100 cm-1, we find that

ria

=

.013. Using the experimental data give by Dillon, the ratio is found to be .008. This order of magnitude agreement is evidence for the

correctness of the proposed mechanism.

VII. Acknowledgements.

-

The author would like to acknowledge many informative discussions of the questions treated here with C. J. Ballhausen,

A. D. Liehr and J. F. Dillon.

REFERENCES DILLON (J. F.), Bull. Phys. Soc., 1957, 2, 238.

GELLER (S.), J. Phys. Chem. Solids, 1957, 3, 30.

ORGEL (L. E.), J. Chem. Phys., 1955, 23,1004.

DISCUSSION

Mr. Smit.

-

1) What about the temperature dependence of the Faraday rotation ?

2) In BaFe12019, in which also Faraday rotation

of visible light has been observed by C. Kooy of the Philips Laboratories (5 000°/cm) many of the ions

are not a centre of symmetry for the crystalline

field. Do you expect that in that case the Faraday

rotation should be extra strong ?

3) If the ground state has a residual angular

momentum, a much simpler theory gives Faraday

rotation. Should this give a greatly différent

result ?

Mr. Clogston. -1) The Faraday rotation is only slightly dependent on the temperature. The absorption lines narrow by about a factor of two

between room temperature and liquidjhelium tem-

peratures.

2) This depends of course on the degree of asymmetry. 1 would certainly expect increased coupling to the odd parity states if there does not exist a center of symmetry.

3) 1 would expect rather différent results, but I

have not considered any such case in detail.

Mr. Suhl.

-

The question whether the ground

state has appreciable orbital angular momentum is

connected with the question of the extent to which

the presence of a magnetic axis prevents the usual quenching of angular momentum. Has Mr. Smit considered this problem ?

Mr. Prof. Kittel.

-

What can be said about the role of the Verwey charge transfer process is causing optical absorption in the visible region of the spectrum ? Have any experiments been carried

out in which Fe++ is deliberately introduced into into a structure otherwise Fe+++.

Mr. Clogston.

-

It has been our experience that

the magnetic garnets which are very nearly stochio-

metric are much more transparent than crystals

where the Verwey processes can occur. We have

not tried to observe the effects of changing the

valence state of the iron ions.

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