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(1)

HAL Id: jpa-00234388

https://hal.archives-ouvertes.fr/jpa-00234388

Submitted on 1 Jan 1951

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Magnetic domain patterns

R.M. Bozorth

To cite this version:

(2)

MAGNETIC DOMAIN PATTERNS

By R.

M. BOZORTH,

Bell

Telephone

Laboratories, Murray Hill

(New Jersey).

Sommaire. 2014 La

technique et l’interprétation des diagrammes de poudres magnétiques est briè-vement passée en revue, d’un point de vue historique. Les diagrammes les plus simples observés sont ensuite décrits et expliqués dans la mesure du possible. Dans la troisième Partie, on décrit et discute

de nouveaux diagrammes relatifs : a. à un monocristal dont la direction (1 11) est celle de facile aiman-tation (60 pour 100 Co, 40 pour 100 Ni); b. à un monocristal de cobalt; c. à un alliage polycristallin

fer-silicium et d. à un alliage polycristallin pour aimants permanents (Alnico 5).

JOURNAL PHYSIQUE 12,

19~1,

Brief revievsr. ---

For many decades iron

filings

have been used to

portray

the directions of lines of

magnetic

force in air and to detect flaws or

inho-mogeneitics

in

magnetic

materials. In

193

1 it

occurred to von Hamos and Thiessen

[ 1]

to use

magnetic powder

to detect the local

inhomogeneities

irr

magnetization

that the domain

theory

predicts.

Independently

Bitter

[2] applied

a

suspension

of siderac

(Fe,O,), having particles

about 10-4 cm in

diameter,

to a

polished magnetized

surface and

observed under the

microscope

that the

powder

formed

parallel

lines

regularly spaced

about o. mm

apart

and

approximately perpendicular

to the direction of

magnetization.

The

technique

and

interpretation

of such

patterns

.was then the

subject

of

study

of a number of workers

[3].

The

preparation

of colloid for these studies has been described in some detail

by

Elmore

[4]

who recommends a

suspension

of

magne-tite,

ground

to colloidal

dimensions,

peptized

with

hydrochloric

acid and

protected by

one per cent of soap; an

improvement

on his

technique

has

recently

been

developed

and will be

published

soon.

Elec-trolytic polishing

[4]

overcomes the

objectionable

mechanical

polishing

which disturbs the surfaces. A notable advance was made

by

McKeehan and Elmore

[5]

who first observed a well-defined

pattern

on a

demagnetized single crystal. Figure

i

shows such a

pattern (b)

and also those

patterns

observed when the

magnetization

is directed

(a)

into,

or

(c)

out

of,

the same

portion

of the surface as that shown in

(b).

The

suspension

used for the

experiments

was a true colloid of

Fe,O, particles

small

enough

to show Brownian movement, and a

change

in

magnetization

of the

magnetic specimen

was

accompanied

by

a movement of the lines

immediately

visible to the eye.

More recent

work,

reported

in various articles

by

Williams,

Bozorth and

Shockley [6],

has made visible for the first time the domain boundaries characteristic of unstrained

iron,

and has

improved

considerably

our

knowledge

of the processes of

magnetization. They

used

single crystals

contai-ning

3.8

weight

per cent silicon and

having

surfaces cut

nearly parallel

to

crystallographic

planes.

The

specimens

were annealed and

polished

carefully,

first

mechanically

and then

electrolytically.

After mechanical

polishing

the

powder

pattern

on a surface almost

parallel

to

(100)

is the cc maze »

pattern

of

figure 2 (a),

similar to that of

figure

i.

Fig. I. - n Maze » pattern observed on polished surface of

single crystal of iron; (b) demagnetized, (a) and (c)

magne-tized in opposite directions.

After

electrolytically polishing

and

reapplying

the

powder

to the same area the result is the « tree »

pattern

of

figure

2

(b).

It is evident from this

and other

experiments

that the maze

pattern

is characteristic of a strained surface and that the tree

pattern

shows the domain boundaries of strain-free material.

The directions of

magnetization

in the domains can be determined in several ways,

using techniques

(3)

described in the

original

paper. The result for a

portion

of one tree

pattern

is shown in

figure

2

(c).

The local

magnetization

in

unmagnetized

material

is

always parallel

to one of the

crystal

axes, and the

boundaries

separate

domains

magnetized

at goo or at 180° to each other.

Fig. 2. - Maze and a tree » patterns, (a) and (b), observed on the same portion of a single crystal after mechanical

and eliectrolytic polishing, respectively. Directions of magnetization in the tree pattern are shown at (c).

Fig. 3. - Effect of increasing tension (a) to (d), on the tree

pattern. In (fi tension has been released.

Visible

movement of domain

boundaries

takes

place

upon

application

of field or stress. The

effect of uniform tension is shown in

figure

3. In this material tension increases the

magnetization

in the direction of the

tension,

and the mechanism

by

which this is

accomplished

is here

apparent :

domains oriented

parallel

to the axis of tension are

enlarged

by displacement

of domain

boundaries,

at the expense

of

domains oriented at

right

angles,

so that the latter domains

disappear

almost

entirely

when the tension is

sufficiently large.

With release of tension the

original

kind of tree

pattern

forms,

(4)

cause the return of the

powder

lines to the same

places

after

they

have been disturbed

temporarily by

field or uniform stress.

When the surfaces are not

parallel

or

nearly

parallel

to

simple crystallographic

planes,

the

patterns

are

likely

to be more

complicated. Figure

4

Fig. 4. -

Complicated patterns observed on (1 10) and (i I i) planes.

Fig. 5. -° Patterns on cobalt surfaces cut parallel and perpendicular to the hexagonal axis.

shows two

examples

of such

patterns.

Although

the

simple

patterns

are well

understood,

it has not

yet

been

possible

to understand in detail the more elaborate ones. It is

believed, however,

that the basic

principles

that

apply

to the

simple

ones are also

applicable

to the more

complex

ones. These

principles

are discussed below.

Experiments

on cobalt have also been instructive.

Bitter

[7]

observed two

types

of

patterns

on

poly-crystalline

material and Elmore

[8], working

with

single crystals,

found the

hexagonal

lace-like

patterns

on surfaces

parallel

to the

hexagonal

planes (o01 )

perpendicular

to the

crystal

axis,

and the

straight

line

patterns

on

prism planes,

as shown in the

(5)

properties

of

cobalt,

known to have a direction of easy

magnetization parallel

to the

crystal

axis. The domains are then

expected

to be

long

in the

direction of the axis and

packed together

like a bundle of needles

(or sheets).

The boundaries of such domains thus

correspond

to the

patterns.

Moving pictures

of the

patterns

taken with

slowly

changing

field

strength

show sudden

displacements

of the boundaries

corresponding

to

jumps

much

larger

than those

usually

attributed to the Bark-hausen effect.

Germer

[9]

has measured the

strength

of

magnetic

fields close to the surface of an

unmagnetized

cobalt

crystal

and found that near a

hexagonal

face it is of the order of 104 Oe and falls off with distance from the surface so that it is

relatively

weak at mm. The fields near

prism

faces

are weaker and fall off more

slowly

with

distance,

in the way that

they

would

expect

if the domains are needlelike as assumed.

The domain structure around cavities and inclu-sions was

investigated theoretically by

Néel

[10]

before any direct observations were made. Obser-vations of a number of

crystal

surfaces under the

microscope

showed the presence of an occasional hole that had formed

accidentally during

freezing

or

etching

or

polishing

of the

crystal.

The

patterns

around two holes in

(100)

surfaces are shown in

(a)

and

(b)

of

figure

6. The structure observed was almost identical with that

predicted

by

N6el,

and can be

interpreted

with the

help

of

figure

6

(c).

Briefly,

the energy is lowered

by

the formation of

«

spikes o

which

help

the

magnetic poles

to

spread

out over a

larger

area.

Fig. 6. - N6el spikes a around holes in a crystal surface, and their interpretation.

The

interpretation

of the various structures can

be carried out in terms of

energies

of associated

with domain

walls,

magnetic

poles (magnetostatic

energy), crystal

anisotropy,

strain and the inter-action of the

magnetization

with the field if any be

present.

The

theory

has been summarized

recently

by

Kittel

[11].

In the next section the

simpler

types

of structure will be discussed on this basis. The

following

section describes the

appli-cation of the

powder

pattern

technique

to various

problems,

and the new conclusions that can be drawn from the various

experiments

will be

pointed

out.

Interpretation

of

simple

patterns.

-- The

simple

domain

patterns

that were first understood may be listed as follows :

Plate

pattern,

(100) plane;

Tree

pattern

on surfaces

nearly

parallel

to

(1oo);

Neel "

spikes "

around

cavities;

Line

pattern

on cobalt

parallel

to

[oo .

r

] axis.

Others,

interpreted

more

recently,

are referred to in the third

part

of this paper.

Plate Pattern. - A

typical

«

plate»

pattern,

with domains of

closure,

is shown in

figure

7. This is a stable

configuration

in zero

applied

field,

for reasons illustrated in

figure

8. In the

possible

single

domain

(a),

the

poles

at the end

give

rise to

magnetostatic

energy

equal

to In

(b)

this is reduced

considerably by

the introduction of the

wall,

with which is associated some energy. In

(c)

the

poles

are eliminated

completely

but there is some strain energy associated with the magne-tostriction of the domains of

closure,

the material

of which does not fit into the space it would occupy if

unmagnetized.

In

(d)

the energy of

magnetostric-tive strain is reduced

further,

and the wall energy is increased.

The various

energies

may be evaluated and the

(6)

Fig. 7. -- ~ Plate » pattern with domains of closure, on the (100) surface of an iron-silicon crystal.

Fig. 8. - Theoretical domain

structures illustrating the

energies associated with magnetic poles, domain walls and

magnetostriction.

strain

energy

is

ergs per cm8 of the volume of the domains of closure.

Young’s

modulus

[12]

in the direction

is x 1012 ergs :

cm2,

the saturation

magnetostriction [13]

in this direction is

and the domain wall energy about i erg per cm2

of wall. For one cm3 of a

crystal

slab

composed

of domains L cm

long

and D cm wide the volume of domains of closure is

D

and the wall

( 2 L ) area is

The sum of the

energies

is then

per cm3 of

crystal,

which is a minimum for

or 0.08 for silicon iron. In the

crystal

of

figure

7, L = 0.22 cm and the calculated and observed values of D are o.03 and

o.o5cm,

respectively.

The

agreement

is

good,

considering

the

approximations

made.

When a field is

applied

the thickness of the domains diminishes. The

theory

has been worked out

by

Néel

[14],

and confirmed

by

the data of Bates and

Neale [15J.

This will not be considered further here. Tree Pattern. - This was the first of the

(7)

complicated

patterns

shown to be in accord with our

present

ideas of domain

theory

[6].

This

pattern

is observed when the surface of an iron

crystal

(positive anisotropy constant)

is

slightly

inclined

(at

angle 0)

to the

(100) crystallographic planes,

and its

explanation

can be understood

qualitatively

by

reference to

figure

9. In the

plate-like

domains

Fig, 9. - Explanation of the tree pattern.

that compose most of the

crystal

the

magnetization

is

parallel

to the

crystal planes,

and therefore the

lines of

magnetic

flux will cut the surface at an

angle

and

produce

a

density

of

magnetic poles

of ±

1s

sin 0 on alternate

strips

of width W. There will then be a

magnetostatic

energy

proportional

to W sin2 0 per unit area. This energy is reduced

by

formation of the tree

patterns

even

though

the wall energy is added. The branches

transport

flux accross the « trunks » of the treees and as

they taper

this flux is distributed as

magnetic

poles

over the domain wall

separating

the branch from the

underlying

domain. A minimum energy

theory

has been worked out

[6],

and this

explains

the dimensions of the branches and their variation with 0 within a factor of about 2. When the

angle

0 becomes

larger

the branches lie closer

together,

as shown in

flgure

I o, and then

overlap

so that the trunk of the tree becomes

completely

hidden.

«

Spikes

». - N6el’s theoretical

investi-gations

of the domain structure around cavities

and

conclusions,

as well as the

previous

work of Kersten

[16], prompted

an

investigation

of the

powder

patterns

in areas where visible cavities occured in

crystal

surfaces. Two

patterns

observed in

(IOO)

surfaces have

already

been shown in

figure

6 and

they

have the form

predicted

by

Néel on

purely

theoretical

grounds.

The

energetics

of this kind of

pattern,

as

already

reported [6]

is as follows.

The

magnetostatic (or

demagnetization)

energy

associated with a hole

[see

(1)

of

f g.

6

(c)]

around

which there is no domain structure, is

No

being

the

demagnetizing

factor,

"Yo

the volume of the hole and

Is

the saturation

magnetization

of the material around the hole. If domains are formed as in

(2), poles

are not

present

at the

edges

of the

cavity

but are distributed

along

the domain boundaries as indicated. In this case there will be

Fig. I o. -

Dependence of the tree pattern on the angle between

the surface and the (1oo) planes.

energies

associated both with the

demagnetization

(a

volume

effect)

and with the domain walls

(area

effect) :

N

being

the

demagnetizing

factor of the volume V enclosed

by

the domain

boundaries,

the energy per unit area of wall and A the total wall area. Assume a

spherical

hole of diameter d and a domain

(8)

of this

ellipse

is

and the volume and surface are

easily

calculable. The

magnetostatic

energy is then

a factor

of ’

being

included to take account of

25 °

the

permeability

of the domains

themselves,

and the wall energy is

Using

the

appropriate

numerical values d=o.oo1 cm,

Is

=

1580,

ew = 1.5

ergs :

cm2,

the calculated

value of I for which

Ed

-~- is a minimum is o.1 o cm and the ratio

of j is

then

approximately

100. The

observed

ratio

for the domain of

figure

6

{b)

is about 50, smaller

by

a factor of 2. This is a

satis-factory

agreement

in view of the

simplifications

used.

Moving

Boundaries. -

Simple

geometry

has been observed in at least two

experiments

on the move-ment of domain boundaries

accompanying

a

change

of

magnetization

with

changing

applied

field.

Williams and

Shockley

[6]

observed a

simple

struc-ture in a hollow

rectangle

with sides

parallel

to

[100]

directions,

and

they

have described

[17]

some

experiments

on the movement of such a

boundary

with slow and

rapid changes

in

magnetic

field.

Fig. I I. - Effect of Néel «"spikes » on the movement of a Bloch wall.

Spikes

such as those

just

described have an

impor-tant effect on the movement of

large

domain

walls,

as noted

by

Williams and

Shockley [ 6]

and illustrated

(9)

Fig. 2. - Movement of a well during magnetization parallel to a [on] ] direction in a (100) plane.

(10)

is consumed in

forming

the additional wall. This

mechanism seems to be

important

in the

inter-pretation

of

hysteresis

loss and coercive force and is discussed

by

Shockley

and Williams in an

accom-panying

paper.

A

moving boundary composed

of a number of

segments

of

straight

lines is observed in a

(100)

plane

when

magnetized parallel

to a

[001]

direction

(fig. 12).

The boundaries that move are between domains

magnetized antiparallel

to each other

( 1 8 0 ° wall).

Patterns. - Cobalt-nickel

crystal.

- The

geometry

of

patterns

on the materials of cubic

symmetry

already

examined is

closely

connected with the fact that their directions of easy

magnetiza-tion are

[100].

Heretofore no

simple

patterns

have been

reported

on

crystals,

like

nickel,

in which the directions of easy

magnetization

are

[111].

It seemed

probable

that the failure to observe

patterns

in such

crystals

was connected with the fact their

crystal anisotropy

was too small

(for

nickel the

anisotropy

constant K is 60 ooo as

compared

Fig. 14. - Effect of

magnetization on the pattern on the cobalt-nickel crystal.

with 280 ooo for iron

containing

several per cent

of

silicon). Consequently

a

crystal

of a cobalt-nickel

alloy containing

60 per cent cobalt and

having

a constant of about 200 ooo

according

to Shih

[18],

has been

prepared by

slow

cooling

of the melt as described

by

Walker,

Williams and Bozorth

[19].

The surface of the

crystal

was cut

parallel

to a

(0 1 1)

plane

so that

4

of the 8 directions of easy magne-tization were

parallel

to the surface. The

pattern

and its

interpretation

are shown in

figure

13.

All of the

theoretically expected angles

between

adjacent

domains -

180°,

109°, 71°

-

are observed. It is also noticed that the domain structure is smaller than that observed on iron-silicon

crystals.

This difference in size may be due to the more

compli-cated

pattern

that may be

expected

in a structure

having

8 instead of 6 directions of easy

magnetiza-tion and

having

no

goo

boundaries.

(11)

Fig. I5. --- Patterns on the (roo) surface of cobalt; a. positive

field, b.

zerolfield, c. negative field, parallel to the axis.

Fig. 16. - Pattern

on cobalt (100) surface, with small field applied normal to the surface.

structure,

originally

of

complicated

geometry,

resolves itself in

high

fields to a series of lines at

right angles

to the direction of the

applied

field,

the direction of

magnetization

alternating

in

adjacent

domains between the two

[111]

]

directions oriented most

nearly

to the direction of the field. The boundaries

are between domains in which the directions of

magnetization

differ

by

i ogo.

Cobalt. -

(12)

are

reproduced

here

15)

because

interesting

regularities

are observed in the

pattern.

The

specimen,

cut with a surface

parallel

to a

(I 00)

plane,

is

magnetized

parallel

to the surface in the direction of the

hexagonal

axis

[001].

In

figure

15, b is

unmagnetized

while a and c are

magnetized

in

opposite

directions. The

displacements

of alternate lines in

opposite

directions shows that the boun-daries move so that more material is

magnetized

parallel

to the field and less

antiparallel

to it. Careful

comparison

of a and c shows also that the lines which move

upwards

in one move down-wards in the other so that

imperfections

that appear in a thinner domain in a are in a thicker domain in c.

In

figure

16 the contrast between

neighboring

domains is enhanced

by

applying

a small normal field. The

specimen

surface is

slightly

inclined to the

hexagonal

axis, so the

magnetic poles

on the

surface are

alternately

north and south

poles

in successive domains. The verticle field enhances the

pole

strength

on half of the domains and

neu-tralizes the

poles

on the other domains, so that the colloid is attracted in the one kind and not in the other.

Polycrystalline

material. - In some commercial

silicon-iron sheet material used for transformer cores the

separate

crystals

are

aligned

with their

[ 100]

axes

approximately parallel

to the

long

dimension of the sheet. A

powder photograph

of such material

1 ~),

taken

by

H. J.

Williams,

shows that domain

Fig. 17. - Pattern on

polycristalline iron-silicon alloy, showing that domains sometimes cross grain boundaries.

boundaries often cross

crystal

boundaries. This occurs when the

[100]

directions in

adjacent crystals

are almost

parallel,

and one believes that the

crystals

must also be

nearly aligned

in 3-dimensional space so that the

platelike

domains of the two

crystals

will

join

together

along planes

of contact that go below the surface observed. The

alignment

in

some of the

crystals

is

obviously

too poor for domains

to cross

crystal

boundaries.

Alnicos. - In a recent

study

of the mechanism in Alnico 5

(5 1

per cent

Fe, 2l~

per cent

Co, 14

per cent Ni 8 per cent

Al,

3 per cent

Cu)

heat treated in a

magnetic

field,

Nesbitt has observed

powder pattern

that

help

in

understanding

the nature of this maetrial. In a series of

experiments

a

specimen

was heated

to 1300° C and cooled at the « normal » rate

of 20 C : s to 8ooo C and then

quenched

in oil. A

magnetic

field was

present

from

gooo

C to room

temperature.

Examination

by

the

powder technique

shows the existence of

long

domains,

about 0.02 mm in

width,

aligned approximately parallel

to the field

present

during

the heat treatment.

They

cut across

crystal

boundaries with no substantial

change

in direction

(see fig.

18)

and show that the

magnetization

is

everywhere parallel

or

antiparallel

to the field used

during

heat treatment. In this material the

magnetization

is

obviously

not

parallel

to the easy

crystallographic

direction nearest to the

(13)

Fig. 18. - Pattern

on Alnico V : domains crossing crystal boundaries.

Fig. 19. - Movement of domain boundaries during magnetization of Alnico V.

When a field is

applied

for measurement

parallel

to the

heat-treating

field,

domain boundaries are observed to move

Ig).

The

hysteresis loop

(14)

Fig. 20. - Rotation of

magnetization of domains in Alnico V when magnetized at right angles to field present during heat treatment.

field is

applied

at

right angles

to the

heat-treating

field the

powder

patterns

show domain rotation without

boundary displacement (see

f g. 20).

This is in

agreement

with the form of the

magnetization

curve, which rises almost

linearly

to saturation at about

4oo

to

450

Oe.

These

experiments

show that

large

domains

having

a

strongly preferred

orientation exist when the material is

prepared

in the manner described. When the material is cooled at the normal rate to

temperatures

lower than 8ooo C the domains are much

smaller,

and when the material is

aged

at 6ooo C no domain has so far been detected in the

unmagnetized

condition.

Recently

Nesbitt has observed their formation upon the

application

of a field to material

given

the usual Alnico 5

treat-ment-cooling

in a field and

aging.

The coercive force of the

quenched specimen having large

domains is 15

Oe,

that of the

specimen having

smaller domains is 35o, while that of the material

given

the usual Alnico 5 treatment is 600.

The manner in which the

preferred

direction of

magnetization

is fixed in the structure is not

yet

known,

but it is

possible

that it is connected with

the atomic

ordering

that exists in these

alloys,

as shown

by X-rays.

I am indebted to Messrs H. J. Williams and E. A. Nesbitt for several of the

photographs

repro-duced in this

article,

and to Mr J. C. Walker for assistance with the

experimental

work,

especially

in the

preparation

of the

single crystals

of the cobalt-nickel

alloy.

Remarque

de M. Bates. - I

congratulate

Dr Bozorth on his beautiful

pictures

on alnico V. I

myself

have tried on and off for four years to obtain

tem, but without success. Was the

crystal

sur-face

prepared

in a

special

way or was the

dry powder

technique

used ?

Question

de M.

Epetboin.

- Le monocristal de

cobalt at-t-il subi au

pr6alable

un

polissage

elec-trolytique ?

Au

sujet

des difficult6s rencontr6es par M. le Prof.

Bates,

je

me souvients que dans notre laboratoire M. Amine a obtenu deux

aspects

diff6-rents de la surface

polie

d’un

alnico,

suivant que l’on utilisait un bain a base d’acide

phosphorique

à chaud

(8oo C)

ou d’acide

perchlorique-anhydride

(15)

Réponse

de M. Bates. -- We have done

some

experiments

on

electrolytic

polishing

and have devised a

bridge

circuit for

controling

it. This is to be described in a

forthcoming

paper in Journ. Scient. Instr.

Remarque

de M. Sucksmith. - I would like to

obtain a three dimensional

picture

of a domain in

cobalt,

which should be

simple

on account of the

single

easy direction of the

magnetization.

What is the reason for

assuming

that

they

are « needles » or « sheets » since the

right

hand

picture

of the

figure

5

suggests

that

they

are rods whose cross section is that of a

hexagonal

cluster

Remarque

de M.

Shockley.

-- It

may be

appro-priate

to

point

out that in

figure

17

presented by

Dr Bozorth there appear domains of closure which can be understood in terms of the

relationship

between the

crystal grain

boundary

and

crystal

axes. The

diagram

pre-sented here

(fig. 21 )

repre-sents a

grain boundary

ABC which is

symmetrical

between the two

crystals

for the

segment

BC. For Fig. 21. - Domain structure the

segment

BC,

domains

near a grain boundary. can form

along

easy di-rections with no free

poles generated

on the

boundary.

Between

points

A and

B, however,

there will be

magnetic poles.

The

magnetostatic

energy of these

poles

may be reduced

by

introducing

reentrant

spike

domain which reduce the

density

on the

grain boundary.

The effect of one such

spike

is shown in the

diagram;

in

figure 17

of Bozorth’s

aticle,

a number of such

spikes

are

present.

The

generation

of such

spikes

are

frequently

observed to be discontinuous and

consequently

irreversible. This

suggests

that in

polycristalline

material an

appreciable

contribution to the coercive force and

hysteresis

may be made

by

discontinuities in the

pattern

of domain

walls,

a process

quite

similar to that discussed

by

N6el.

A une

question

de M.

Guillaud,

M. Bates

répond.

-The field

applied perpendicular

to the surface was not measured

exactly;

but it was of the order of 13o Oe.

Remarque

de M. Hoselitz. - The

powder

patterns

shown

by

Dr Bozorth to occur on Alnico V when

quenched

from 8ooo C can be

explained

without any additional

assumptions

from our views

(HOSELITZ

and

MCCAIG,

Nature,

1949,

164,

p.

581;

Proc.

Phys.

Soc.,

I go9,

B,

62,

p.

163). Magnetostriction

and other measurements on this material in the

fully

heat treated condition have shown that the

magneti-sation energy can be

represented by

a cubic term and a uniaxial term

probably acting

in one of the

[100]

directions. The order of

magnitude

of these energy are up to I o ergs : cc. In the

quenched

material described

by

Dr

Bozorth,

these values may be

considerably

smaller and I cannot comment on this

particular

case.

However,

as mentioned

by

Dr

Bozorth,

similar

powder

patterns

are observed

by

Nesbitt in the

fully

heat treated

material,

but

only

in

relatively

high

fields.

If a field of about 5oo Oe is

applied

in the pre-ferred direction of

magnetisation,

the field energy term

HJS

becomes of the same order of

magnitude

as the

magnetic

anisotropy

term estimated in our

experiments,

and it is

consequently

likely

that at fields

of this

magnitude,

the actual field direction will become the direction of the

magnetisation.

Hence it can be understood that no unidirectional domains are observed

by powder

patterns

until fields of about the coercive force are

applied,

when most domains will be very

hearly aligned

with the field direction and

consequently

many domains boundaries will have

disappeared.

Thus

large

unidirectional domains boundaries will exist in this condition.

Demande de M. Bauer. - Serait-il

possible

de faire ces

exp6riences

pour des corps dont le

point

de Curie est voisin de la

temperature

ordinaire et de voir comment les domaines

changent

avec la

temperature ?

Reponse n6gative

de MM. Bozorth et Bates. REFERENCES.

[1] HAMOS L. v. and THIESSEN P. A. - Z. Physik, 1931,

71, 442.

[2] BITTER F. 2014 Phys. Rev., 1931, 38, 1903.

[3] KAYA S.2014 Z. Physik, 1934, 89, 796, and 1934, 90, 551.

- SIXTUS K. J. -

Phys. Rev., 1937, 51, 870. -SOLLER T. 2014 Z. Physik, 1937, 106, 485. - ELMORE W. C. and Mc KEEHAN L. W. - Tr. Amer. Inst. Min. Met. Engrs, 1936, 120, 236.

[4] ELMORE W. C. 2014 Phys.

Rev., 1938, 54, 1092, and 1942, 62, 486.

[5] Mc KEEHAN L. W. and ELMORE W. C. - Phys. Rev., 1934, 46, 226.

[6] WILLIAMS H. J. -

Phys. Rev., 1946, 70, 106 and

subse-quent brief reports. - WILLIAMS H.

J., BOZORTH

R. M. and SHOCKLEY W.- Phys. Rev., 1949, 75, 155. -WILLIAMS H. J. and SHOCKLEY W. - Phys. Rev., 1949, 75, 178.

[7] BITTER F. 2014 Phys. Rev., 1932, 41, 507.

[8] ELMORE W. C. 2014 Phys. Rev., 1938, 53, 757.

[9]

GERMER L. H. 2014 Phys. Rev., 1942, 62, 295. [10] NÉEL L. - Cahiers de Physique, 1944, 25, 21.

[11]

KITTEL C. 2014 Rev. Mod.

Physics, 1949, 21, 541.

[12]

BENFORD F. G. - Metal Progr., 1946, 46, 94.

[13] CARR W. J. - Private Communication.

[14] NÉEL L. - J. Physique Rad., 1944, (8), 5, 241.

[15] BATES L. F. and NEALE F. E. -

Physica, 1949, 15, 220. [16] KERSTEN M. - Physik. Z., 1943, 44, 63.

[17] WILLIAMS H. J. and SHOCKLEY W. - Phys. Rev., 1950, 80, ooo.

[18] SHIH J. W. - Phys. Rev., 1936, 50, 376.

[19] WALKER J. G., WILLIAMS H. J. and BOZORTH R. M. 2014

Rev. Sci. Instruments, 1949, 20, 947. [20] HOSFLITZ K. and Mc CAIG M. -

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