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Double hysteresis loops in ferromagnetic crystals

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HAL Id: jpa-00236031

https://hal.archives-ouvertes.fr/jpa-00236031

Submitted on 1 Jan 1959

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Double hysteresis loops in ferromagnetic crystals

A.A. Hirsch

To cite this version:

A.A. Hirsch. Double hysteresis loops in ferromagnetic crystals. J. Phys. Radium, 1959, 20 (2-3),

pp.262-263. �10.1051/jphysrad:01959002002-3026200�. �jpa-00236031�

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262

DOUBLE HYSTERESIS LOOPS IN FERROMAGNETIC CRYSTALS

By A. A. HIRSCH,

Department of Physics, Technion-Israel Institute of Technology, Haifa, Israel.

Résumé.

2014

Un monodomaine présentant une anisotropie mixte magnéto-cristalline et uni- axiale peut donner une courbe d’aimantation composée de deux boucles asymétriques reliées par

un segment, le long duquel l’aimantation est réversible. Le processus d’aimantation irréversible

commence à partir d’un champ critique. Ce cycle double pourrait être une explication possible du

mécanisme d’aimantation des matériaux ayant des cycles étirés, comme les Perminvars.

Abstract.

2014

A single domain with mixed magnetocrystalline and uniaxial anisotropies can

show a magnetization curve composed of two asymmetric loops connected by a section over which

the magnetization is reversible. The irreversible process starts at acritical field. The double

loop could be a possible explanation for the mechanism of magnetization in materials with con-

tricted loops as Perminvars.

LE JOURNAL DE PHYSIQUE ET LE RADIUM TOME 20, FÉVRIER-MARS 1959,

Single ferromagnetic domains of cubic structure may show double hysteresis loops [1, 2]. The

transition of the ordinary hysteresis loop into

the double loop depens on :

1° the magnitude of the magnetic uniaxial ani- sotropy and its direction with respect to that of the magnetic field and to that of the crystallogra- phics axes ;

20 the ratio of the constants of uniaxial aniso-

tropy and magnetocrystalline anisotropy.

The magnetization in the direction of the magne- tic field, I, is obtained by minimising the free

energy of the crystal. For a prolate spheroidal

domain whose polar axis lies along the [100] direc- tion, the values of 1 are given by the following expressions :

for a magnetic field, H, in a [001] direct ion.

where Ii is the magnetocrystalline constant.

Ta is the spontaneous magnetization and Na, Nb

are the demagnetization coefficients along the polar

and equatorial axes. A rectangular magnetization loop can be derived from these relations for a posi-

tive K. The shape of this loop changes with changing value of the factor F. For F = 0.5 the

loop becomes -double. In case of a negative K,

the magnetization loop is ordinary and its coercive force is equal to zero for F == - 0.5.

When the magnetic field lies along the polar

axis of the domain, the magnetization loop is rectangular for .K > 0 and its coercive force increases with increasing factor F.

Two double hystérésis loops of a crystal with

a positive K are illustrated in figure 1 for F - 0.5

and F =1.

FIG. 1.

Thé inverse slope of the magnetization curve for

low-fields and small values of f is given hy

where f = I/Is. This portion of the curve corres-

ponds to stable equilibrium directions of the magne- tization vector.

For large values of f and low-fields (at a crystal

field which corresponds to a sharply increasing magnetization), the inverse slope of magnetization

curve is expressed by

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphysrad:01959002002-3026200

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263

This portion of the curve shows non-stable equilibruim directions of Is.

Fm. 2.

Fic.3.

The condition dHO,,,, dI = 0 leads to the following

relation for thé ;critical field :

It is supposed that the theory of the double

hysteresis loop can be applied for analysis of the magnetization curves of single-crystal cobalt fer- rite which are measured by Foner and Artman [3].

The magnetocrystalline anisotropy constant deriv-

ed from equation (2) and (4) is of the same order

of magnitude as calculated by these investigators.

Figure 2 shows the magnetization curve of a crystal with"a negative K for F .- - 0. 5.

A composite magnetization loop of two domains with magnetocrystalline constants of différent

signs is shown’in figure 3 (F1 - 0.5, F2 - - 0.5

and K1 = - K2). Loops of simila.r shape have

been measured by several investigators in Per-

minvar. The mechanism of the magnetization of

a double loop can give also a possible explanation

for the magnetic behaviour of this material.

REFERENCES’

[1] HIRSCH (A. A.), Bull. Res. Couns. Israel, 1957, 6 A, 276.

[2] HIRSCH (A. A.), Bull. Res. Couns. Israel, 1958, 7 F, in print.

[3] FONER (S.) and ARTMAN (J. O.), J. Appl. Physics, 1958, 29, 443.

DISCUSSION

Mr. Artman and Foner.

--

VGe would like to

point out that a single domain analysis does not applyto our problem. As discussed by us in detail

at this çonference, in order to explain our results it

is essential that a multi-domain structure exist.

Mr. Hirsch.

-

In multi-domain materials

having some ordered domain arrangement it is possible to have a magnetization process which

occur only by domain rotation. when the external

magnetic field lies in a direction perpendicular

to the walls of the domains, the magnetization is

rotational.

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