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Magnetic domain patterns
R.M. Bozorth
To cite this version:
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 toportray
the directions of lines ofmagnetic
force in air and to detect flaws orinho-mogeneitics
inmagnetic
materials. In193
1 itoccurred to von Hamos and Thiessen
[ 1]
to usemagnetic powder
to detect the localinhomogeneities
irrmagnetization
that the domaintheory
predicts.
Independently
Bitter[2] applied
asuspension
of siderac
(Fe,O,), having particles
about 10-4 cm indiameter,
to apolished magnetized
surface andobserved under the
microscope
that thepowder
formedparallel
linesregularly spaced
about o. mmapart
andapproximately perpendicular
to the direction ofmagnetization.
The
technique
andinterpretation
of suchpatterns
.was then thesubject
ofstudy
of a number of workers[3].
Thepreparation
of colloid for these studies has been described in some detailby
Elmore[4]
who recommends asuspension
ofmagne-tite,
ground
to colloidaldimensions,
peptized
withhydrochloric
acid andprotected by
one per cent of soap; animprovement
on histechnique
hasrecently
beendeveloped
and will bepublished
soon.Elec-trolytic polishing
[4]
overcomes theobjectionable
mechanicalpolishing
which disturbs the surfaces. A notable advance was madeby
McKeehan and Elmore[5]
who first observed a well-definedpattern
on ademagnetized single crystal. Figure
ishows such a
pattern (b)
and also thosepatterns
observed when the
magnetization
is directed(a)
into,
or(c)
outof,
the sameportion
of the surface as that shown in(b).
Thesuspension
used for theexperiments
was a true colloid ofFe,O, particles
smallenough
to show Brownian movement, and achange
inmagnetization
of themagnetic specimen
wasaccompanied
by
a movement of the linesimmediately
visible to the eye.More recent
work,
reported
in various articlesby
Williams,
Bozorth andShockley [6],
has made visible for the first time the domain boundaries characteristic of unstrainediron,
and hasimproved
considerably
ourknowledge
of the processes ofmagnetization. They
usedsingle crystals
contai-ning
3.8weight
per cent silicon andhaving
surfaces cutnearly parallel
tocrystallographic
planes.
Thespecimens
were annealed andpolished
carefully,
firstmechanically
and thenelectrolytically.
After mechanicalpolishing
thepowder
pattern
on a surface almostparallel
to(100)
is the cc maze »pattern
offigure 2 (a),
similar to that offigure
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
andreapplying
thepowder
to the same area the result is the « tree »pattern
offigure
2(b).
It is evident from thisand other
experiments
that the mazepattern
is characteristic of a strained surface and that the treepattern
shows the domain boundaries of strain-free material.The directions of
magnetization
in the domains can be determined in several ways,using techniques
described in the
original
paper. The result for aportion
of one treepattern
is shown infigure
2(c).
The local
magnetization
inunmagnetized
materialis
always parallel
to one of thecrystal
axes, and theboundaries
separate
domainsmagnetized
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 domainboundaries
takes
place
uponapplication
of field or stress. Theeffect of uniform tension is shown in
figure
3. In this material tension increases themagnetization
in the direction of the
tension,
and the mechanismby
which this isaccomplished
is hereapparent :
domains orientedparallel
to the axis of tension areenlarged
by displacement
of domainboundaries,
at the expense
of
domains oriented atright
angles,
so that the latter domainsdisappear
almostentirely
when the tension issufficiently large.
With release of tension theoriginal
kind of treepattern
forms,
cause the return of the
powder
lines to the sameplaces
after
they
have been disturbedtemporarily by
field or uniform stress.When the surfaces are not
parallel
ornearly
parallel
tosimple crystallographic
planes,
thepatterns
arelikely
to be morecomplicated. 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 suchpatterns.
Although
thesimple
patterns
are wellunderstood,
it has notyet
beenpossible
to understand in detail the more elaborate ones. It isbelieved, however,
that the basicprinciples
thatapply
to thesimple
ones are alsoapplicable
to the morecomplex
ones. Theseprinciples
are discussed below.Experiments
on cobalt have also been instructive.Bitter
[7]
observed twotypes
ofpatterns
onpoly-crystalline
material and Elmore[8], working
withsingle crystals,
found thehexagonal
lace-likepatterns
on surfaces
parallel
to thehexagonal
planes (o01 )
perpendicular
to thecrystal
axis,
and thestraight
linepatterns
onprism planes,
as shown in theproperties
ofcobalt,
known to have a direction of easymagnetization parallel
to thecrystal
axis. The domains are thenexpected
to belong
in thedirection of the axis and
packed together
like a bundle of needles(or sheets).
The boundaries of such domains thuscorrespond
to thepatterns.
Moving pictures
of thepatterns
taken withslowly
changing
fieldstrength
show suddendisplacements
of the boundariescorresponding
tojumps
muchlarger
than thoseusually
attributed to the Bark-hausen effect.Germer
[9]
has measured thestrength
ofmagnetic
fields close to the surface of anunmagnetized
cobaltcrystal
and found that near ahexagonal
face it is of the order of 104 Oe and falls off with distance from the surface so that it isrelatively
weak at mm. The fields nearprism
facesare weaker and fall off more
slowly
withdistance,
in the way thatthey
wouldexpect
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 ofcrystal
surfaces under themicroscope
showed the presence of an occasional hole that had formedaccidentally during
freezing
oretching
orpolishing
of thecrystal.
Thepatterns
around two holes in(100)
surfaces are shown in(a)
and(b)
offigure
6. The structure observed was almost identical with thatpredicted
by
N6el,
and can beinterpreted
with thehelp
offigure
6(c).
Briefly,
the energy is loweredby
the formation of«
spikes o
whichhelp
themagnetic poles
tospread
out over alarger
area.Fig. 6. - N6el spikes a around holes in a crystal surface, and their interpretation.
The
interpretation
of the various structures canbe carried out in terms of
energies
of associatedwith domain
walls,
magnetic
poles (magnetostatic
energy), crystal
anisotropy,
strain and the inter-action of themagnetization
with the field if any bepresent.
Thetheory
has been summarizedrecently
by
Kittel[11].
In the next section thesimpler
types
of structure will be discussed on this basis. Thefollowing
section describes theappli-cation of the
powder
pattern
technique
to variousproblems,
and the new conclusions that can be drawn from the variousexperiments
will bepointed
out.Interpretation
ofsimple
patterns.
-- Thesimple
domainpatterns
that were first understood may be listed as follows :Plate
pattern,
(100) plane;
Tree
pattern
on surfacesnearly
parallel
to(1oo);
Neel "
spikes "
aroundcavities;
Line
pattern
on cobaltparallel
to[oo .
r] axis.
Others,
interpreted
morerecently,
are referred to in the thirdpart
of this paper.Plate Pattern. - A
typical
«plate»
pattern,
with domains of
closure,
is shown infigure
7. This is a stableconfiguration
in zeroapplied
field,
for reasons illustrated in
figure
8. In thepossible
single
domain(a),
thepoles
at the endgive
rise tomagnetostatic
energyequal
to In(b)
this is reducedconsiderably by
the introduction of thewall,
with which is associated some energy. In(c)
thepoles
are eliminatedcompletely
but there is some strain energy associated with the magne-tostriction of the domains ofclosure,
the materialof which does not fit into the space it would occupy if
unmagnetized.
In(d)
the energy ofmagnetostric-tive strain is reduced
further,
and the wall energy is increased.The various
energies
may be evaluated and theFig. 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
isergs per cm8 of the volume of the domains of closure.
Young’s
modulus[12]
in the directionis x 1012 ergs :
cm2,
the saturationmagnetostriction [13]
in this direction isand the domain wall energy about i erg per cm2
of wall. For one cm3 of a
crystal
slabcomposed
of domains L cmlong
and D cm wide the volume of domains of closure isD
and the wall( 2 L ) area is
The sum of the
energies
is thenper cm3 of
crystal,
which is a minimum foror 0.08 for silicon iron. In the
crystal
offigure
7, L = 0.22 cm and the calculated and observed values of D are o.03 ando.o5cm,
respectively.
Theagreement
isgood,
considering
theapproximations
made.When a field is
applied
the thickness of the domains diminishes. Thetheory
has been worked outby
Néel[14],
and confirmedby
the data of Bates andNeale [15J.
This will not be considered further here. Tree Pattern. - This was the first of thecomplicated
patterns
shown to be in accord with ourpresent
ideas of domaintheory
[6].
Thispattern
is observed when the surface of an ironcrystal
(positive anisotropy constant)
isslightly
inclined(at
angle 0)
to the(100) crystallographic planes,
and itsexplanation
can be understoodqualitatively
by
reference tofigure
9. In theplate-like
domainsFig, 9. - Explanation of the tree pattern.
that compose most of the
crystal
themagnetization
isparallel
to thecrystal planes,
and therefore thelines of
magnetic
flux will cut the surface at anangle
andproduce
adensity
ofmagnetic poles
of ±1s
sin 0 on alternatestrips
of width W. There will then be amagnetostatic
energyproportional
to W sin2 0 per unit area. This energy is reducedby
formation of the treepatterns
eventhough
the wall energy is added. The branchestransport
flux accross the « trunks » of the treees and asthey taper
this flux is distributed asmagnetic
poles
over the domain wallseparating
the branch from theunderlying
domain. A minimum energytheory
has been worked out[6],
and thisexplains
the dimensions of the branches and their variation with 0 within a factor of about 2. When theangle
0 becomeslarger
the branches lie closertogether,
as shown inflgure
I o, and thenoverlap
so that the trunk of the tree becomes
completely
hidden.
«
Spikes
». - N6el’s theoreticalinvesti-gations
of the domain structure around cavitiesand
conclusions,
as well as theprevious
work of Kersten[16], prompted
aninvestigation
of thepowder
patterns
in areas where visible cavities occured incrystal
surfaces. Twopatterns
observed in(IOO)
surfaces havealready
been shown infigure
6 andthey
have the formpredicted
by
Néel onpurely
theoreticalgrounds.
The
energetics
of this kind ofpattern,
asalready
reported [6]
is as follows.The
magnetostatic (or
demagnetization)
energyassociated with a hole
[see
(1)
off g.
6(c)]
aroundwhich there is no domain structure, is
No
being
thedemagnetizing
factor,
"Yo
the volume of the hole andIs
the saturationmagnetization
of the material around the hole. If domains are formed as in(2), poles
are notpresent
at theedges
of thecavity
but are distributedalong
the domain boundaries as indicated. In this case there will beFig. I o. -
Dependence of the tree pattern on the angle between
the surface and the (1oo) planes.
energies
associated both with thedemagnetization
(a
volumeeffect)
and with the domain walls(area
effect) :
N
being
thedemagnetizing
factor of the volume V enclosedby
the domainboundaries,
the energy per unit area of wall and A the total wall area. Assume aspherical
hole of diameter d and a domainof this
ellipse
isand the volume and surface are
easily
calculable. Themagnetostatic
energy is thena factor
of ’
being
included to take account of25 °
the
permeability
of the domainsthemselves,
and the wall energy isUsing
theappropriate
numerical values d=o.oo1 cm,Is
=1580,
ew = 1.5
ergs :cm2,
the calculatedvalue of I for which
Ed
-~- is a minimum is o.1 o cm and the ratioof j is
thenapproximately
100. Theobserved
ratio
for the domain offigure
6{b)
is about 50, smallerby
a factor of 2. This is asatis-factory
agreement
in view of thesimplifications
used.Moving
Boundaries. -Simple
geometry
has been observed in at least twoexperiments
on the move-ment of domain boundariesaccompanying
achange
ofmagnetization
withchanging
applied
field.Williams and
Shockley
[6]
observed asimple
struc-ture in a hollowrectangle
with sidesparallel
to[100]
directions,
andthey
have described[17]
someexperiments
on the movement of such aboundary
with slow andrapid changes
inmagnetic
field.Fig. I I. - Effect of Néel «"spikes » on the movement of a Bloch wall.
Spikes
such as thosejust
described have animpor-tant effect on the movement of
large
domainwalls,
as noted
by
Williams andShockley [ 6]
and illustratedFig. 2. - Movement of a well during magnetization parallel to a [on] ] direction in a (100) plane.
is consumed in
forming
the additional wall. Thismechanism seems to be
important
in theinter-pretation
ofhysteresis
loss and coercive force and is discussedby
Shockley
and Williams in anaccom-panying
paper.A
moving boundary composed
of a number ofsegments
ofstraight
lines is observed in a(100)
plane
whenmagnetized parallel
to a[001]
direction(fig. 12).
The boundaries that move are between domainsmagnetized antiparallel
to each other( 1 8 0 ° wall).
Patterns. - Cobalt-nickel
crystal.
- Thegeometry
ofpatterns
on the materials of cubicsymmetry
already
examined isclosely
connected with the fact that their directions of easymagnetiza-tion are
[100].
Heretofore nosimple
patterns
have beenreported
oncrystals,
likenickel,
in which the directions of easymagnetization
are[111].
It seemedprobable
that the failure to observepatterns
in suchcrystals
was connected with the fact theircrystal anisotropy
was too small(for
nickel theanisotropy
constant K is 60 ooo ascompared
Fig. 14. - Effect of
magnetization on the pattern on the cobalt-nickel crystal.
with 280 ooo for iron
containing
several per centof
silicon). Consequently
acrystal
of a cobalt-nickelalloy containing
60 per cent cobalt andhaving
a constant of about 200 oooaccording
to Shih[18],
has beenprepared by
slowcooling
of the melt as describedby
Walker,
Williams and Bozorth[19].
The surface of thecrystal
was cutparallel
to a(0 1 1)
plane
so that4
of the 8 directions of easy magne-tization wereparallel
to the surface. Thepattern
and itsinterpretation
are shown infigure
13.All of the
theoretically expected angles
betweenadjacent
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 morecompli-cated
pattern
that may beexpected
in a structurehaving
8 instead of 6 directions of easymagnetiza-tion and
having
nogoo
boundaries.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
ofcomplicated
geometry,
resolves itself inhigh
fields to a series of lines atright angles
to the direction of theapplied
field,
the direction ofmagnetization
alternating
inadjacent
domains between the two[111]
]
directions oriented mostnearly
to the direction of the field. The boundariesare between domains in which the directions of
magnetization
differby
i ogo.
Cobalt. -
are
reproduced
here15)
becauseinteresting
regularities
are observed in thepattern.
Thespecimen,
cut with a surfaceparallel
to a(I 00)
plane,
ismagnetized
parallel
to the surface in the direction of thehexagonal
axis[001].
Infigure
15, b isunmagnetized
while a and c aremagnetized
inopposite
directions. Thedisplacements
of alternate lines inopposite
directions shows that the boun-daries move so that more material ismagnetized
parallel
to the field and lessantiparallel
to it. Carefulcomparison
of a and c shows also that the lines which moveupwards
in one move down-wards in the other so thatimperfections
that appear in a thinner domain in a are in a thicker domain in c.In
figure
16 the contrast betweenneighboring
domains is enhanced
by
applying
a small normal field. Thespecimen
surface isslightly
inclined to thehexagonal
axis, so themagnetic poles
on thesurface are
alternately
north and southpoles
in successive domains. The verticle field enhances thepole
strength
on half of the domains andneu-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 commercialsilicon-iron sheet material used for transformer cores the
separate
crystals
arealigned
with their[ 100]
axesapproximately parallel
to thelong
dimension of the sheet. Apowder photograph
of such material1 ~),
takenby
H. J.Williams,
shows that domainFig. 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 inadjacent crystals
are almostparallel,
and one believes that thecrystals
must also benearly aligned
in 3-dimensional space so that theplatelike
domains of the twocrystals
willjoin
together
along planes
of contact that go below the surface observed. Thealignment
insome of the
crystals
isobviously
too poor for domainsto cross
crystal
boundaries.Alnicos. - In a recent
study
of the mechanism in Alnico 5(5 1
per centFe, 2l~
per centCo, 14
per cent Ni 8 per centAl,
3 per centCu)
heat treated in amagnetic
field,
Nesbitt has observedpowder pattern
thathelp
inunderstanding
the nature of this maetrial. In a series ofexperiments
aspecimen
was heatedto 1300° C and cooled at the « normal » rate
of 20 C : s to 8ooo C and then
quenched
in oil. Amagnetic
field waspresent
fromgooo
C to roomtemperature.
Examinationby
thepowder technique
shows the existence oflong
domains,
about 0.02 mm inwidth,
aligned approximately parallel
to the fieldpresent
during
the heat treatment.They
cut acrosscrystal
boundaries with no substantialchange
in direction(see fig.
18)
and show that themagnetization
iseverywhere parallel
orantiparallel
to the field used
during
heat treatment. In this material themagnetization
isobviously
notparallel
to the easy
crystallographic
direction nearest to theFig. 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 measurementparallel
to theheat-treating
field,
domain boundaries are observed to moveIg).
Thehysteresis loop
Fig. 20. - Rotation of
magnetization of domains in Alnico V when magnetized at right angles to field present during heat treatment.
field is
applied
atright angles
to theheat-treating
field thepowder
patterns
show domain rotation withoutboundary displacement (see
f g. 20).
This is inagreement
with the form of themagnetization
curve, which rises almost
linearly
to saturation at about4oo
to450
Oe.These
experiments
show thatlarge
domainshaving
astrongly preferred
orientation exist when the material isprepared
in the manner described. When the material is cooled at the normal rate totemperatures
lower than 8ooo C the domains are muchsmaller,
and when the material isaged
at 6ooo C no domain has so far been detected in theunmagnetized
condition.Recently
Nesbitt has observed their formation upon theapplication
of a field to materialgiven
the usual Alnico 5treat-ment-cooling
in a field andaging.
The coercive force of thequenched specimen having large
domains is 15Oe,
that of thespecimen having
smaller domains is 35o, while that of the materialgiven
the usual Alnico 5 treatment is 600.The manner in which the
preferred
direction ofmagnetization
is fixed in the structure is notyet
known,
but it ispossible
that it is connected withthe atomic
ordering
that exists in thesealloys,
as shownby X-rays.
I am indebted to Messrs H. J. Williams and E. A. Nesbitt for several of the
photographs
repro-duced in thisarticle,
and to Mr J. C. Walker for assistance with theexperimental
work,
especially
in the
preparation
of thesingle crystals
of the cobalt-nickelalloy.
Remarque
de M. Bates. - Icongratulate
Dr Bozorth on his beautiful
pictures
on alnico V. Imyself
have tried on and off for four years to obtaintem, but without success. Was the
crystal
sur-faceprepared
in aspecial
way or was thedry powder
technique
used ?Question
de M.Epetboin.
- Le monocristal decobalt at-t-il subi au
pr6alable
unpolissage
elec-trolytique ?
Ausujet
des difficult6s rencontr6es par M. le Prof.Bates,
je
me souvients que dans notre laboratoire M. Amine a obtenu deuxaspects
diff6-rents de la surfacepolie
d’unalnico,
suivant que l’on utilisait un bain a base d’acidephosphorique
à chaud(8oo C)
ou d’acideperchlorique-anhydride
Réponse
de M. Bates. -- We have donesome
experiments
onelectrolytic
polishing
and have devised abridge
circuit forcontroling
it. This is to be described in aforthcoming
paper in Journ. Scient. Instr.Remarque
de M. Sucksmith. - I would like toobtain a three dimensional
picture
of a domain incobalt,
which should besimple
on account of thesingle
easy direction of themagnetization.
What is the reason for
assuming
thatthey
are « needles » or « sheets » since theright
handpicture
of the
figure
5suggests
thatthey
are rods whose cross section is that of ahexagonal
clusterRemarque
de M.Shockley.
-- Itmay be
appro-priate
topoint
out that infigure
17presented by
Dr Bozorth there appear domains of closure which can be understood in terms of therelationship
between thecrystal grain
boundary
andcrystal
axes. Thediagram
pre-sented here(fig. 21 )
repre-sents agrain boundary
ABC which issymmetrical
between the twocrystals
for thesegment
BC. For Fig. 21. - Domain structure thesegment
BC,
domainsnear a grain boundary. can form
along
easy di-rections with no freepoles generated
on theboundary.
Betweenpoints
A andB, however,
there will be
magnetic poles.
Themagnetostatic
energy of these
poles
may be reducedby
introducing
reentrantspike
domain which reduce thedensity
on thegrain boundary.
The effect of one suchspike
is shown in thediagram;
infigure 17
of Bozorth’saticle,
a number of suchspikes
arepresent.
Thegeneration
of suchspikes
arefrequently
observed to be discontinuous andconsequently
irreversible. Thissuggests
that inpolycristalline
material anappreciable
contribution to the coercive force andhysteresis
may be madeby
discontinuities in thepattern
of domainwalls,
a processquite
similar to that discussedby
N6el.A une
question
de M.Guillaud,
M. Batesrépond.
-The field
applied perpendicular
to the surface was not measuredexactly;
but it was of the order of 13o Oe.Remarque
de M. Hoselitz. - Thepowder
patterns
shown
by
Dr Bozorth to occur on Alnico V whenquenched
from 8ooo C can beexplained
without any additionalassumptions
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 thefully
heat treated condition have shown that themagneti-sation energy can be
represented by
a cubic term and a uniaxial termprobably acting
in one of the[100]
directions. The order ofmagnitude
of these energy are up to I o ergs : cc. In thequenched
material describedby
DrBozorth,
these values may beconsiderably
smaller and I cannot comment on thisparticular
case.However,
as mentionedby
DrBozorth,
similarpowder
patterns
are observedby
Nesbitt in thefully
heat treatedmaterial,
butonly
inrelatively
high
fields.If a field of about 5oo Oe is
applied
in the pre-ferred direction ofmagnetisation,
the field energy termHJS
becomes of the same order ofmagnitude
as themagnetic
anisotropy
term estimated in ourexperiments,
and it isconsequently
likely
that at fieldsof this
magnitude,
the actual field direction will become the direction of themagnetisation.
Hence it can be understood that no unidirectional domains are observedby powder
patterns
until fields of about the coercive force areapplied,
when most domains will be veryhearly aligned
with the field direction andconsequently
many domains boundaries will havedisappeared.
Thuslarge
unidirectional domains boundaries will exist in this condition.Demande de M. Bauer. - Serait-il
possible
de faire cesexp6riences
pour des corps dont lepoint
de Curie est voisin de latemperature
ordinaire et de voir comment les domaineschangent
avec latemperature ?
Reponse n6gative
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