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Submitted on 1 Jan 1982
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Magnetic properties of the ternary oxide glasses,
Li2O-B2 O3-Fe2O3 from 57Fe Mössbauer spectroscopy
J.P. Sanchez, J.M. Friedt
To cite this version:
1707
Magnetic
properties
of the
ternary
oxide
glasses,
Li2O-B2O3-Fe2O3
from
57Fe
Mössbauer
spectroscopy
J. P. Sanchez and J. M. Friedt
Centre de Recherches Nucléaires, 67037
Strasbourg
Cedex, France(Reçu le 13 avril 1982, révisé le 2 juillet, accepté le 22 juillet 1982)
Résumé. 2014 L’état de valence et la coordination du fer ont été établis par
spectroscopie
Mössbauer de 57Fe dans lesoxydes
ternaires amorphes,Li2O-B2O3-Fe2O3.
Dans la gamme de concentrations étudiée (~ 8,4 at%
Fe), les ionsFe3+ sont tétra- et
hexacoordinés ;
la faibleproportion
( 15%)
d’ionsFe2+,
observée dans certains échantillons,est liée aux conditions de
préparation.
Lespropriétés magnétiques
de ces verres, établies en combinant des mesuresmacroscopiques (susceptibilité dynamique
etaimantation)
et locales(spectroscopie Mössbauer),
sont déterminéespar la concentration des ions fer. A faible concentration
(~
3 at %) de fer, des ions Fe 3+ isolés coexistent avec despetits agrégats (2
à 3 atomes)antiferromagnétiques.
Pour des teneurs en ferplus
élevées (3,8 à 8,4 at%),
les verresprésentent
une transitionmictomagnétique
conduisant à un ordrespéromagnétique.
Dans un échantillon étudiéen détail (5,8 at
%
Fe), la variation de latempérature
degel (Tf)
avec lafréquence
de mesure obéit à une loi deFulcher.
Abstract. 2014 57Fe Mössbauer spectroscopy has been combined with bulk magnetic measurements to determine
the valence state and coordination of iron as well as the
magnetic properties
of the ternary oxideglasses,
Li2O-B2O3-Fe2O3.
In allinvestigated glasses
(~ 8.4 at % Fe), the Fe3+ ions coexist in tetrahedral and octahedralcoordina-tions ; the presence of Fe2+ ions ( 15
%),
which is observed in someglasses,
is related topreparation
conditions. Themagnetic
properties
of theglasses
aregoverned
by
the iron content. At low iron concentration ( 3 at%),
isolated Fe3+ ions coexist with
antiferromagnetic
dimers and trimers. Atlarge
iron content (3.8 to 8.4 at%)
theglasses
undergo
amictomagnetic
transition to asperomagnetic
ordered state. Thefreezing
temperature(Tf),
which isfrequency dependent,
is found to follow a Fulcher law in onesample
(5.8 at%
Fe)investigated
in detail.J.
Physique
43(1982)
1707-1716 NOVEMBRE 1982, ClassificationPhysics
Abstracts 61.40D - 75.50K - 76.80 1. Introduction. - Considerableexperimental
and theoretical work has been devotedrecently
to the structural[1, 2]
andmagnetic properties [3, 4]
ofdisordered
systems.
Theconcept
ofspin glass
ormictomagnetism [5],
corresponding
to the randomfreezing
ofspins
via aprogressive blocking
of themagnetization
of clusters or via a collectivephase
transition,
has been extended from dilutedmagnetic
alloys
CuMn,
AuFe,
etc...[6])
torandomly
dilutedcrystalline
solids such asEuxSr 1 - xS [7]
orEuxGd1 - xS
[8]’ and
toamorphous compounds
withpredominantly
antiferromagnetic
interactions[9].
The
present report
concerns the latter class ofmaterials. The
properties
of theternary
oxideglasses,
L’20-B203-Fe2o3,
are inferredby combining
bulk(ac-susceptibility, magnetization)
and local(17 Fe
Mossbauer
spectroscopy)
measurements. In apre-vious paper on the
Ba0-B203-Fe203
glass
systems
[10]
it has been shown that the
magnetic properties
aregoverned by
the Fe concentration.Here,
moreatten-tion is devoted to the dilute concentration range, where isolated
Fe3 +
ions coexist with smallmagnetic
clus-ters, and to the intermediate concentration range, where the
glasses
exhibit amictomagnetic
transitionowing
totopological
disorder and frustration effects. The nature of the transition isinvestigated
in detail for onesample (5.8
at% Fe) by following
thedepen-dence of the
freezing
temperature
on the time window(0.5
to10-8
s)
of themeasuring technique.
2.ExperimentaL
- Theamorphous samples
wereprepared by rapid quenching using
the roller techni-que as described in detail elsewhere[11].
The finalcompositions
of theternary
oxides were checkedby
standard chemicalanalysis.
Thenon-crystalline
natureof the
products
was establishedby X-ray
andelec-tron diffraction as well as
by
transmission electronmicroscopy. Dc-magnetic
data will bereported
indetail
by
Chaumont and Bernier in aforthcoming
paper [ 12].
Ac-susceptibility
measurements wereperformed
atthe C.R.T.B.T.
(Grenoble) using
a mutual inductancebridge operating
between 17 Hz and 11 kHz[13].
The "Fe
Mossbauer measurements wereperform-ed as a function of
temperature
between 1.4 and 295 Kagainst
a57Co/Rh
source. Someexperiments
werecarried out in a
longitudinal
externalmagnetic
fieldup to 80 k0e
provided by
asuperconducting
coil.Absorbers
containing
about 5mg/cm2
of natural iron were used. The Mossbauerspectra
werecomputer
analysed
as described in detail in apreceding
paper[10].
3.
Experimental
results. -57Fe
Mossbauer data
are
reported
for theternary
oxideglasses,
L’20-B203-Fe2o3,
of nominalcompositions given
in table I. Table I. - Nominalcompositions
of
the ternary oxideglasses, Li20-B203-Fe203’ investigated
in this work.Complementary ac-susceptibility
measurements asa function of
temperature
andfrequency
arereported
for one
specific sample
e(5.8
at%
Fe),
in which themictomagnetic
transition is established in detail.3. 1 M6SSBAUER MEASUREMENTS. - At 77
K the
samples
b,
c andf,
withrespectively
1.8,
3.0 and 6.9Fig. 1. - Mossbauer
spectra of samples b (1.8 at
%
Fe)and h (8.4
at %
Fe) at 77 K. The full curvescorrespond
to a fitassuming Lorentzian
lineshapes
(see text).Table II. -
Mössbauer data at 77 K
of
the ternary oxideglasses, Li20-B203-Fe203’ bjs
is the isomershift
versusiron metal at RT.
AL
andWL
representrespectively
thequadrupole splitting
and the resonance widthassuming
Lorentzian
lineshapes.
P is thefractional
spectral
areaof
iron in agiven
coordination and(or)
valence state. x is1709
at
%
Fe, present
twoslightly asymmetric
Mossbauer lines(Fig. 1).
Assuming
Lorentzianlineshapes,
thespectra
aresatisfactorily analysed
as asuperposition
of two broadened
quadrupole
doublets with different isomer shifts andquadrupole splittings characterizing
Fe3 +
ions in both octahedral(Oh)
and tetrahedral(Td)
coordinations(Table II).
By
contrast, the Mossbauerspectra
ofsamples
d,
e, g and h withrespectively
3.8, 5.8,
7.6 and 8.4 at%
Fepresent
at 77 K a third resonance line at about 2.1mm/s
superposed
upon theprevious
two main resonances(Fig.
1).
Thespectra
aredecomposed
into threesym-metrical broadened
doublets, indicating
the presence ofFe3 +
ions,
bothoctahedrally
andtetrahedrally
coordinated,
and of a small amount ofFe 21
ions(Fig.
1,
TableII).
The observation ofFe2 +
ions in theseglasses
is related topreparation
conditions rather than tocompositional
or other effects.The Mossbauer spectrum of
sample
a(0.6
at%
Fe)
reveals at 77 K
(Fig.
2)
asuperposition
of a centraldoublet and of a
magnetic hyperfine
structure(see
below).
At 4.2
K, except
forsample
c(3.0
at% Fe),
theMossbauer spectra of all
samples
understudy
reveala fraction of the iron ions
experiencing
amagnetic
hyperfine
field.However,
two classes of behaviourFig. 2. -
Temperature
dependence
of the Mossbauerspec-tra of sample a (0.6 at % Fe).
Fig. 3. -
4.2 K Mossbauer spectra of
Li20-B203-Fe203
glasses
at different iron concentrations (lower concentration range,samples
a,b).
can be
distinguished, according
to the ironconcen-tration range. At iron content x 3.0 at
%,
the fraction of iron ionsshowing
amagnetic
hyperfine
structure decreases with
increasing
ironconcentra-tion ;
theopposite
trend is observed for x > 3.0 at%
(Figs.
3 and4).
The former behaviour is characteristic for
para-magnetic
relaxation effects. In addition to the above mentioned concentrationdependence,
thisattribu-tion is further
supported
from thetemperature
dependence
of thespectra,
which reveal aprogres-sive
broadening
andcollapse
of the« magnetic»
lines(see
Fig.
2 at 77 and 295K).
The concentration andtemperature
dependences correspond
tospin-spin
andspin-lattice coupling
relaxation mechanismsrespectively. By
reference tocomputed
relaxation lineshapes,
thetemperature dependence (Fig.
2)
actually
indicates a distribution of relaxation rates, which isprobably
connected toinhomogeneity
of themagnetic
environment of theFe3 +
ions,
asalready
inferred from thequadrupole
interaction distribution.Micro-crystalline heterogeneities (e.g. precipitated
ferritesetc)
in theproportion
which would be indicatedby
the Mossbauer data are ruled out from electronmicroscopy
and bulkmagnetization
results.In the
larger
Fe concentration range(x
> 3.0at
%),
the iron concentrationdependence
of the 4.2 K Mossbauerspectra (Fig.
4)
shows an increasein resolution of the
magnetic hyperfine
structurewith
increasing
x. Detailedtemperature dependence
Fig.
4. - 4.2 K Mossbauerspectra of
Li,O-B,O,-Fe2o3 glasses
at different iron concentrations (upper concentration range, samples c to h).indicates that the
magnetic hyperfine
structure setsin at 7 ± 0.5 K
(Fig. 5).
Themagnetic hyperfine
splitting
increases and the lines become less broadened when thetemperature
decreases.Magnetic
saturation is achieved at 1.4 Konly
for the more concentratedsample
h(8.4
at%)
for whichmagnetic broadening
occurs at 14 + 2 K.
For this
sample
h(8.4
at%
Fe),
the saturated magne-ticspectrum
(1.4
K)
isanalysed
in thehypothesis
ofan «
amorphous » magnetic
structure,using
afitting
procedure
described in detail in[10] (Fig. 6) :
a"
random orientation is assumed for the
angle
0bet-ween electric field
gradient
andhyperfine
fieldprin-cipal
axes. Thisresults,
to firstorder,
in asymmetrical
magnetic spectrum.
The effects of the aboveangular
distribution and of the distribution of
quadrupole
splitting
arerepresented by
a uniformbroadening
ofall the
magnetic
components given
from aperturba-tion calculation as
[10, 14] :
where
WL is
the linewidth observed in theparama-gnetic
state(77 K)
and6Wo
= - A,
with
dbeing
-,,15-the
quadrupole splitting
deduced from thepara-magnetic
data. The distribution function of thehyperfine
field is then fitteddirectly
from the data.The average fields and the standard deviations for both the
octahedrally
andtetrahedrally
coordinatedFe3 +
ions are collected in table III. It should be noticed that the averagehyperfine
fields,
are lower than those measured in
crystalline
iron-basedoxides
(e.g. Fe3 +(Oh)=
537.5k0e,
Fe3+(Td)=521
kOe inLiFe508
at 4.2K)
or than that(530 kOe)
deter-mined for isolated
Fe3 +
ions under alarge
external field at 4.2 K(see
below).
3.2 SUSCEPTIBILITY MEASUREMENTS. -
Preli-minary
dc-susceptibility
andmagnetization
measure-ments have been
reported by
Chaumont et al.[1,1].
A more detailed account of their work will bepu-blished
[12].
The main features of their data aresummarized here.
Reciprocal susceptibilities,
x -1,
of theglasses
understudy
follow a Curie-Weiss law above somecharacteristic
temperature
TD
(e.g.
100 K forsample
h with 8.4 at% Fe)
and show anegative
curvaturebelow this
temperature.
The latter feature indicatesCurie-1711
Fig. 5.
- Temperature dependence
of the M6ssbauerspectra of sample e (5.8 at
%
Fe) around themagnetic
transition.0
Fig. 6. -
Mossbauer spectrum of sample h (8.4 at % Fe) at 1.4 K. The full curve corresponds to a fit as discussed in the text.
Table III. -
Hyperfine
interaction datafrom
theanalysis of
the Mössbauer spectrumof sample
h(8.4
at
% Fe)
at 1.4 K.Hhf
and a arerespectively
themean value and the standard deviation
of
the Gaussiandistribution
of
thehyperfine field.
6 is assumed to be the samefor
the tetrahedral and octahedralhyperfine
field
distributions. Othersymbols
aredefined
as inTable II.
* The random orientation of the
angle B
between theEFG and Hb axes is taken into account
by introducing
an uniform
broadening
of the lines andsetting
thequadru-pole splitting
L1equal
to zero (see text).Weiss constants,
CM,
are ingeneral
significantly
lower than the free ionFe3 +
value(Ct
=4.38); they
increase with
decreasing
Feconcentration,
reaching
C,
for the less concentratedsamples
(
0.6 at% Fe).
The modulus of
0p
decreases(from
115 K tozero)
with
decreasing
iron content. In none of thesamples
does
x -1
show aminimum;
absence of remanenceeffects is observed within the
investigated
tempera-ture range, i.e. above 4.2 K.
Magnetization (per
at gFe)
decreases withincreas-ing
iron content and does not saturate even for theless-concentrated iron
sample (up
to 150 kOe at4.2
K).
Forinstance,
forsample
e(5.8
at%)
themagnetization
at 4.2 K(20 kOe),
which amounts to2 100
emu/at
g Fe,
is far below theFe3 +
free-ion saturation value of 27 924emu/at
g Fe. At 4.2K,
theM(H)
curve of this samesample
(e)
shows aslight
curvature
except
in the low fieldregion
(
5kOe)
where a very weakferrimagnetic
component
(LiFe508
crystallites)
saturates. Theshape
is similar to those found inamorphous
manganese aluminosilicates[16].
Theac-susceptibility
ofsample
e(5.8
at%)
exhibitsa somewhat broad cusp below 4.2 K which is fre-quency
dependent;
it takesplace
attemperatures
of3.25,
3.35 and 3.45 K forrespective measuring
fre-quencies
of17.3,
197.6 and 2 103 Hz(Fig. 7).
This cusp defines thespin freezing temperature Tf.
In thefrequency
range accessible toac-susceptibility
T f
varies
linearly
withlog
v; theslope
of the relative shift ofTf
against
decimallogarithm
offrequency,
is an order of
magnitude larger
than in the canonicalmetallic
spin glass
CuMn[17].
Note that the assump-tion of an Arrhenius law for thefrequency
dependence
of
Tf
T -1 - -
k
In v
leads tounphysical
valuesf
fFig.
7. -Ac-susceptibility
ofsample
e (5.8 at%
Fe) as a function of temperature for various measuringfrequencies.
for both the characteristic
frequency
and the activation energy
(Ea/k ~
270K).
4.
Magnetic
properties
of theternary
oxideglasses :
Li2O-B2O3-Fe2O3.
-Combining
thepresent
M6ss-bauer andac-susceptibility
data with results fromdc-susceptibility
andmagnetization
measurements[11,
12],
it appears that theinvestigated
iron-based oxideglasses
exhibit two distinct classes ofmagnetic
behaviour,
according
to the concentration range of themagnetic
iron ions. Theboundary
between thetwo
regimes
lies in the range 3.0-3.8 at%
Fe. 4.1 UPPER CONCENTRATION RANGE. - Considerfirst
sample
e(5.8 at % Fe)
which isrepresentative
of this concentration range. Above 7 ± 0.5
K,
the Mossbauerspectra present
quadrupole
doubletsrevealing
«paramagnetic »
behaviour(Fig.
5).
Below7 K the doublet smears out and
develops
progressi-vely
into amagnetic lineshape (Fig. 5).
In thepre-sence of an intense external field
(40
and 80kOe)
at4.2
K,
thespectral
resolution issignificantly
enhanced and thespectral
splitting
increases(Fig. 8).
Several
explanations
may be considered in orderto account for this behaviour.
Superparamagnetic
effects canhardly
beinvoked; indeed,
neitherelec-tron
microscopy
normagnetization
data indicatethe presence of
superparamagnetic particles.
More-over, the Mossbauer
spectra
do not present thetem-perature
dependence
characteristic forsuperpara-magnets
i.e. afully
developed magnetic
spectrum
coexisting
with aparamagnetic
doublet over a widetemperature
range[18].
Also,
magnetic
fieldsatura-tion,
which should beeasily
achieved for smallinde-pendent magnetic particles
even in arelatively
smallexternal
field,
is not observed.Paramagnetic
relaxationeffects,
corresponding
toFig.
8. -Applied
fielddependence
of the Mossbauerspec-tra of
sample
e (5.8at %
Fe) at 4.2 K (external fieldparallel
to y-raypropagation
axis).spin flipping
of individualFe3 +
ions,
arereasonably
ruled out
from
the relative narrowness of thetempe-rature range where these effects would occur
(compare
figures
2 and5)
and from thetemperature
dependence
of thespectral
shape (by
reference to establishedexamples
andcalculations).
The observed
temperature
and external fielddepen-dences of the Mossbauer
spectra
ofsample
e,along
with theac-susceptibility
cusp, rather suggest amictomagnetic
transition[5].
Over atemperature
range below
T f,
the Mossbauerspectral shapes
canbe
reproduced qualitatively by
aspherical
relaxationmodel
[8,
19,
20],
whenassuming
some distributionof relaxation rate. This latter
assumption
isneces-sary in
particular
torepresent
theapparent
persis-tence of the
paramagnetic
doublet,
while aunique
isotropic
relaxation rate wouldimply
a fastsmearing
out of these
peaks [8,
19,
20].
The alternativeexpla-nation of
temperature
dependent exchange
field distribution cannot bedefinitively
ruled out from thepresent
results. Notice that theproposed
interpre-tation is consistent with the one demonstrated inanother established concentrated
spin glass
system,
i.e.Eu1-xGdxS,
where a narrowfrequency
1713
The
mictomagnetic
transition is understood interms of a
progressive
freezing
of theisotropic
fluc-tuations of
magnetization
of clusters[5,
8,
21].
Con-trary to the
original
model of Tholence and Tournier[21],
which assumed the existence ofessentially
independent
magnetic
clouds(clusters),
the external fielddependence
of the Mossbauerspectra
indicatesstrong interactions among the clusters via
dipolar
and/or
exchange
interactions.Indeed,
verylarge
fields arerequired
to block the relaxation andsatu-ration is not even reached at 80 kOe. The same
conclusion is ascertained from the
frequency
depen-dence of thefreezing
temperature Tf [22-25]. Defining
the Mossbauerfreezing
temperature
as thetempe-rature of appearance of the
wings coexisting
with thequadrupole
doublet(Fig. 5),
thefrequency
dependence
ofTf
can be extended from the lac rangeto
10’ Hz,
i.e. the characteristicfrequency
of57 Fe
Mossbauerspectroscopy.
An Arrheniusplot,
T f 1
vs. In
v,
shows a curvature,indicating
that such a lawcannot represent the
frequency dependence.
A betterdescription
of thefrequency dependence
ofT f
is achievedby using
a Fulcherlaw,
where
To
is aphenomenological parameter
whichtakes into account the interactions among the clusters
[22-25].
Theplot
ofTf
vs.1/(ln
v - Invo)
is linearwith a characteristic
frequency
vo =109
Hz(Fig. 9).
The interaction energy,
To,
and the activation energy,Ea/k,
are 2.7 and 9.9 Krespectively.
These values arecomparable
to those obtained in manganese and cobalt aluminosilicateglasses [23].
At
temperatures
well belowT f
themagnetization
fluctuation isfrozen,
resulting
into a static «amor-phous »
type
Mossbauerspectrum
as found forsample
h at 1.4 K(Fig.
6).
In summary,
although
thedynamics
involved atthe
mictomagnetic
transition cannot be elucidatedunambiguously
from thepresent
results,
it isqualita-tively argued
thatfreezing
takesplace
atTf
via aFig. 9. -
Frequency
dependence
of Tfor
sample e (5.8 at% Fe) using a Fulcher law. To and
Ea/k
are deduced from the plot of Tfvs. 1/(In vo - In
v) with vo = 109 s-1.spherical
relaxation mechanism. The fluctuations ofmagnetization
of individual clusters arestrongly
coupled.
This is deduced from thefrequency
depen-dence ofTf
and from therelatively
narrow range ofrelaxation rates.
Indeed,
in the presence of suchinteractions between
clusters,
the relaxation ratewill be less
dependent
on cluster size than for instance in a truesuperparamagnet.
The
temperature
dependence
of the Mossbauerspectra
of the othersamples belonging
to thelarge
concentrationregime
(3.8
to 8.4 at%)
has beeninvestigated
in less detail. It appears that thefreezing
temperature
isapproximately proportional
to the iron atomic fraction. The increase ofTf
is also evident from the evolution of thespectral
shape
at 4.2 K with ironconcentration,
which reveals anincreasing
fraction of
magnetic component (Fig. 4).
The reduction of saturation
hyperfine
field in the ordered(speromagnetic)
state ascompared
to theextrapolated paramagnetic
value(evaluated
from the external fieldmeasurements)
or to the value incomparable crystalline compounds
cannot be attri-buted tochanging covalency
effects[26]
in view of the similarbjs.
Morereasonably,
one may invokelargely
differentsupertransferred
anddipolar
contri-butions to thehyperfine
field inamorphous
materialsas a consequence of
positional
disorder.Alternatively,
zero-point spin
deviationsmight
beresponsible
forHh f
and moment reduction[26],
as established forFig. 10. - Mossbauer
crystalline
one-dimensionalantiferromagnets [27].
However,
the existence ofspin
waves in frustratedamorphous magnets
is still debated[28].
The frustration
implied by
the combination ofnegative superexchange
interactions and oftopolo-gical
disorder leads well belowTf
to a newtype
ofmagnetic
order(speromagnetism) :
thespins
arefrozen in random directions and
antiferromagnetic
correlationsextend,
at the most, over a few inter-atomic distances[29]. Speromagnetic
structure is proven at 4.2 K for thepresent
glasses
by investigating
themagnetic polarization
inducedby
an externalfield. For
sample
h(8.4
at%), application
at 4.2 K of a field of 80 kOe has no effect on the averagelinepositions
while minorchanges
affect the relative line areas and linewidths(Fig. 10).
Both effects revealnegligible
momentpolarization
evenby
suchlarge
external fields in accordance with the
strong
negative
exchange
revealedby
thelarge
value of thepara-magnetic
Curietemperature,
i.e.0p
= - 115 K forsample
h(8.4
at% Fe).
Theslight (5 %)
decrease oflinewidth is attributed to the
quenching
of relaxationpersisting
at 4.2 K in the absence of external field. This conclusion is consistent with thetemperature
dependence
in the absence offield,
which showsbetween 4.2 and 1.4 K a
slight
increase of the outerline
intensity (Figs.
4, 6).
Also,
the deducedmagnetic
ordering
agrees with the small value of the inducedmagnetization (a
few%
of theoreticalFe3 +
saturationvalue)
and with the absence of saturation at fieldsas
large
as 150 k0e[11, 12].
4.2 LOWER CONCENTRATION RANGE. - A
quite
differentmagnetic
behaviour is observed for the lower concentration range(Figs.
2 and3). Sample
c(3.0
at%)
shows aquadrupole
doublet down to 4.2K,
while at the same
temperature
amagnetic hyperfine
structure
component
coexists with aquadrupole
doublet in
samples
a and b(with respectively
0.6 and 1.8 at%).
The fraction of themagnetically split
component
increases withdecreasing
ironconcen-tration
(Fig. 3).
Asalready
discussed,
thisconcen-tration
dependence, along
with thetemperature
dependence
observed for eachsample (Fig. 2),
cha-racterize the occurrence ofparamagnetic
relaxationeffects. The coexistence of slow- and fast
relaxing
Fe3 +
ions reveals a non-statistical distribution ofthese ions within the
glass
matrix. Thehyperfine
field at 4.2 Kcorresponding
to the ±5/2
state ofthe slow
relaxing
Fe3 +
ions amounts to 520 kOe.Application
of alarge longitudinal magnetic
field(up
to 80kOe)
onsample
c(3.0
at%)
reveals amagne-tic
splitting
for a fraction of theFe3+
ions(Fig. 11).
The field
dependence
of the outer lines(c)
follows aBrillouin law
(S
=5/2, p
= 5JlB)’
indicating
thatthis
component
arises from isolatedFe3 +
ions. The saturation value ofHh f equals -
530 kOe. The centralpart
of thespectra
(a)
does notsplit
andmerely corresponds
to theapplied
field.Thus,
thiscomponent is attributed to
antiferromagnetically
Fig.
11. -Applied
field(longitudinal) dependence
of theMossbauer spectra of
sample
c(3.0
at% Fe)
at 4.2 K. Thebar
diagram
refers to the threesubspectra corresponding
to isolated Fe3 + ions (c),
antiferromagnetically coupled
dimers (a) and
larger
iron clusters(b).
coupled
dimers which as a whole behave asnon-magnetic.
The lines(b),
between the outer set andthe central
portion
of thespectra, correspond
to aneffective field of - 250 kOe and are
tentatively
assigned
toantiferromagnetically coupled
trimers[30].
The above discussion is consistent with the observed
reduction of Curie constant for this
composition
(CM
= 3.43 vs. free ion value of4.38).
Theproportion
of
coupled
clusters decreases withdecreasing
Feconcentration,
withmainly
isolatedFe3 +
ions atx = 0.6 at
%.
5. Structural
properties
of theternary
oxideglasses :
L’20-B203-Fe2o3’
- Theinfor-1715
mation available from the Mossbauer data is the coordination and valence state of the iron ions. This
type
of information isgenerally
obtainedby
compar-ing
the measured isomer shifts(or
hyperfine fields)
to those established in
crystalline compounds [31].
Thebjs
allows astraightforward
attribution tohigh
spin
ferric or ferrous ions and can alsogenerally
provide
their coordination. Forinstance,
thebls
(at
77K)
of 4-coordinatedFe3 +
ions falls in the range from 0.26 to 0.43mm/s (vs.
iron atRT)
whilebjs
for 6-coordinatedFe3 +
ions is in the range from 0.38 to 0.63mm/s [32].
From the 77 K Mossbauer data of the
present
glasses (Table II),
it is concluded thatFe3 +
ions arepresent
in both tetrahedral and octahedral coordi-nations. This is also confirmed fromcrystallization
study [12],
which initiates with the formation ofLiFe508
where theFe3 +
ionspresent
both coordi-nations. The 4-coordinatedFe3 +
ionsexperience
alarger
electric fieldgradient
than the 6-coordinatedones. Both the average isomer shift and
quadrupole
splitting
of theFe3 +
ions increase withdecreasing
Li20
content(Tables
I andII)
asalready reported
by
Raman et al.[33].
These authors account for thisbehaviour in terms of a
change
of coordination fromtetrahedral to octahedral with
decreasing Li20
con-tent.
However,
thisexplanation
is inconsistent with thepresent
results which show that theLi20
pro-portion
does not affect theFe 3’(O,)/Fe 3 ’ (Td)
ratio.Combining
the two sets ofdata,
it issuggested
that theglasses including
Li as a cation differstructurally
from those with other(Na, K)
alkali cations. This conclusion issupported by
the monotonous decrease of averageðlS
as a function ofLi20 proportion
reported by
Raman et al.[33],
while forNa20
orK20 glass
modifiers asharp anomaly
is observedfor
6js
at aspecific
alkali oxide concentration.The effect of
Li20
addition on the structuralevo-lution of the borate network has been
investigated
in detail from"B
nuclearmagnetic
resonance inB203-Li20 glasses by Bray
and his coworkers[34].
For a molar ratio R of alkali oxide to boron oxide smaller than0.5,
they
observe in addition toB03
units a
growing
fraction of boron atoms in tetrahedral coordination(B04 units)
forincreasing
Li20
content.For 0.5 R
1, i.e.,
the concentration range of interesthere,
theproportion
of bothsymmetrical
B03
andB04
units decreases whereas a fraction ofasymmetric B03
units(with
one or twonon-bridging
oxygens)
grows with R. It has beenrecently argued
that the decrease of bothbls
and thequadrupole
splitting
ofFe3+
ions withincreasing
alkali oxidecontent
might
be connected with the formation ofnon-bridging
oxygens in theneighbourhood
of these ions[35]. However,
furtherinvestigations
are neededto confirm such a
proposal
and noarguments
canbe inferred from the
present
results tosupport
thishypothesis.
It is felt that nostrictly significant
infor-mation can be inferred from thepresent
results withrespect to the
glass
former orglass
modifierproperty
of the iron atoms in the considered
glasses.
Suchtype
ofinvestigation
wouldrequire
a detailedinves-tigation
of the iron coordinationdependence
on theratio of alkali to boron elements and on the
iron
concentration
respectively.
Moreover,
theB203
glas-ses
might
notrepresent
the best choice for such studies since the coordinationgeometry
of boronalready changes
fromtriangular
to tetrahedral inbinary
alkali oxide-boron oxideglasses.
A distribution of
quadrupole splittings,
deduced from the Lorentzianlinebroadenings,
is observed in all of theinvestigated samples.
As discussedexten-sively
previously,
this is attributed to fluctuations around average values ofbonding angles
anddis-tances within
nearly
constant structural units (octa-hedra andtetrahedra) [10].
Relevant information about the
heterogeneity
of the iron distribution within theglass
host is inferred from the localmagnetic
data revealedby
Mossbauerspectroscopy.
The observation in the lower Fe concentration range of smallmagnetic
clusters(dimers
andtrimers) coexisting
with isolatedFe3 +
ions agrees with earlierreports [10, 30]
and turns out torepresent
a common feature for iron-based oxideglasses. According
tosusceptibility
data(Curie
cons-tant),
theFe3 +
ions occurpredominantly
as isolatedspecies
in the lower iron concentrationglass (0.6
at
%) [11, 12].
However,
theinhomogeneous
para-magnetic
relaxation behaviour observed for thissample
indicates that theFe3 +
ions are notrandomly
distributed in the
glass
matrix. 6. Conclusion. -The valence and coordination of the iron ions in
L’20-B203-Fe2o3
glasses (
8.4at
% Fe)
have been determinedby
57Fe
Mossbauerspectroscopy.
TheFe3+
ions occur in bothtetra-hedral and octatetra-hedral
coordinations;
the presence ofFe2 +
ions,
in someglasses,
corresponds
determi-nantly
toequilibrium
conditions in thepreparation
process.The
magnetic properties,
ascertained fromcombin-ed bulk
(ac-susceptibility, magnetization)
and local(Mossbauer)
measurements, are determinedprima-rily by
the iron content in theglasses.
At low iron concentration( 3
at%)
Mossbauer studies in external fields demonstrate the coexistence ofmagnetic
clusters on the atomic scale with isolatedFe3 +
ions. At 0.6 at%
Fe,
theFe3 +
ions occurmainly
as isolatedions; however,
they
are distributednon-statistically
in the
glass.
In the upper concentration range
(3.8
to 8.4 at%),
the
glasses present
amictomagnetic
transition atTf
as characterized from Mossbauer and
ac-susceptibi-lity
measurements. Thetemperature
Tf
increasesmonotonously
with the iron concentration.Strong
interactions among the clusters are evidencedthrough
the
frequency dependence
ofTf
which follows arandom arrangement,
resulting
in asperomagnetic
structure.
Although
atemperature dependent
distri-bution of
exchange
interaction or distribution oftransition
temperatures
via chemicalheterogeneities
cannot be ruled out
definitively
frompresent
results,
it is
suggested
that,
similar toEu,
_xGdxS,
themicto-magnetic
transitions atT f
proceed
via aprogressive
freezing
of random fluctuations of cluster magnetiza-tion.However,
one should notice that the abovebasic
ambiguity
about the actual nature of thespin
glass
transition affects most of theexisting
experi-mental results and affords a
particularly challenging
question.
Acknowledgments.
- We thank C. Chaumont andJ. C. Bernier for
providing
thesamples
and for communication of theirdc-susceptibility
and magne-tization data.References
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