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Mössbauer studies of NaFes2 : magnetic hyperfine fields and covalency in MFeS2 compounds (m=Na, k, Rb, Cs)
C.A. Taft
To cite this version:
C.A. Taft. Mössbauer studies of NaFes2 : magnetic hyperfine fields and covalency in MFeS2 compounds (m=Na, k, Rb, Cs). Journal de Physique, 1977, 38 (9), pp.1161-1162.
�10.1051/jphys:019770038090116100�. �jpa-00208682�
1161
MÖSSBAUER STUDIES OF NaFeS2 : MAGNETIC HYPERFINE FIELDS AND COVALENCY IN MFeS2 COMPOUNDS (M=Na, K, Rb, Cs) (*)
C. A. TAFT
Centro Brasileiro de
Pesquisas Fisicas,
Av. WenceslauBraz, 71,
Rio deJaneiro,
Brasil(Reçu
le 2 novembre1976,
révisé le 5 mai1977, accepté
le 23 mai1977)
Résumé. 2014 L’étude Mössbauer de NaFeS2, de la température ambiante à celle de l’hélium liquide,
révèle la présence d’ordre magnétique en dessous de 77 K. Le champ hyperfin à 4,2 K est de 270 kOe.
Les paramètres hyperfins du fer dans NaFeS2 indiquent la
configuration
à spin fort de Fe3+(6S5/2),
Nous montrons que les valeurs réduites du champ hyperfin dans NaFeS2 comme dans les composés MFeS2 (M=K, Rb, Cs) peuvent se corréler à l’aide de notions simples : champ hyperfin transféré
par les électrons 4s,
électronégativité
des cations.Abstract. 2014 Mössbauer studies of NaFeS2 from room temperature down to liquid helium tem- perature indicate a magnetic
ordering
below 77 K. The magnitude of the hyperfine field is 270 kOe at 4.2 K. The measuredhyperfine
parameters characterize iron in NaFeS2 to be in thehigh
spin Fe3+6S5/2
configuration. We show that in NaFeS2 2014 as in the other MFeS2 compounds (M=K, Rb, Cs) - the reduced values of hyperfine fields (150-270 kOe) can be correlated with simple concepts such as transferred hyperfine fields via 4s contribution and cationic electronegativity.LE JOURNAL DE PHYSIQUE TOME 38, SEPTEMBRE 1977,
Classification Physics Abstracts
76.80
1. Introduction. - In our
previous
work we report- ed on Mossbauer studies ofcovalency
effects in alcali-dithioferratesAFeS2 (A=K, Rb, Cs).
Theseeffects cause a
large
reduction of the observedmagnetic hyperfine
fields from theexpected
ionic value[1, 2].
In this work I report on Mossbauer studies of
NaFeS2
in thetemperature
range (300-4.4K)
indi-cating
also alarge
deviation of the measuredmagnetic
field from the ionic value.
It is
interesting
to note that themagnitude
of themagnetic
field in the alcali-dithioferrate series can be correlated with acovalency
scale based on 4s contri- bution and cationicelectronegativity.
2.
Experimental.
- Thesamples
wereinvestigated using
a 1024 multichannelanalyser, operating
in themultiscaler mode to a
velocity
transducer of the Kankeleittype.
The source was a 10 mCi of" Co
in a Pd matrixhaving
a width of 0.28mm/s
measuredagainst
a natural iron absorber. The gamma rays weredetected with a thin Nal
(Tl)
scintillator mounted in aphoto-multiplier
tube. Theliquid
helium measu-rement was taken with both source and absorber in
liquid
helium. The low temperature measurementswere recorded
using
an Elscint cryostat withtempe-
(*) This paper was presented at the International Conference
on the Applications of the Mossbauer Effect, Corfu (Greece) 1976.
rature controller. The
temperature stability
was± 2 °C. The
samples
wereprepared by fusing
ironpowder
with sodium carbonate andsulphur
andleaching
the coldproduct
in water.3. Results and discussion. -
Figure
1 shows thetransmission
spectra
ofNaFeS2
at several tempera-tures. From 300 K down. to 77 K a
quadrupole
doublet with a temperature
independent splitting
of0.58
mm/s
is observed. The roomtemperature
isomer shift value is 0.36mm/s (w.r.t. Fe).
These parametersare
typical
for iron in thehigh spin Fe3+ 6S5J2
confi-guration [1-4].
At 4.4 K thespectrum
wasadditionally split by
astrong magnetic hyperfine
interaction and themagnitude
of thehyperfine
field wasI Hhf
= 270 k0152( ±
5kOe).
Thesign
ofHhf
isassumed to be
negative
as this isusually
the casein
Fe3+ high-spin compounds.
Electric field
gradient (EFG)
calculations[1, 2]
in this series of
compounds
indicatednegligible
valuesof asymmetry parameter
(q).
In the present case ofa small
quadrupole
interactionsuperimposed
on alarge magnetic hyperfine
interaction in theabsorber,
the observation of an
unchanged quadrupole split- ting (1)
indicates that the main axis of the EFG coin- (’) (= shift of the inner lines pairs versus the outermost linesof the six-line pattern). ,
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:019770038090116100
1162
FIG. 1. - Absorption spectra for NaFeS2 at various temperatures.
cides with the axis of the
magnetic hyperfine
field.In this case a
negative sign
of the EFG can besimply
derived.
The
magnitude
of the internal field inNaFeS2 (270 k0e)
which is assumed to be the saturationfield,
is
unusually
small for a ferric ion. There are appa-rently
considerablecovalency
effects fromneigh- boring spins.
Molecular orbital calculationssuggest
that there should be a linearrelationship
betweenthe covalent induced
hyperfine
field and thecharge
transfer to the 4s state.
Assuming
such a relation-ship
we can write[1]
where Hionic = - 630 kOe is the ionic field and
H4s
= + 1 348 kG is the averagehyperfine
fielddue to one 4s electron and
Q4,
is the number of 4s electrons at theFe3 +
ionoriginating
from thecovalent
ligands.
From theModified
WWJ Plot[1]
one obtains
Q4s
= 0.22. This estimateyields Hhf
= - 330k0e,
which is areasonably good
esti-mate.
Various attempts have been made to correlate the extensive Mossbauer data with available
electronega- tivity
scales[5].
In this isostructural seriesMFeS2 (M=Na, K, Rb, Cs)
in which the cation M is theonly varying element,
it appears reasonable toattempt
such a correlation. Theincreasing electronegativity
of the cation will decrease the 4s electron
density
atthe Fe nucleus and hence reduce the
proposed
trans-ferred
hyperfine
fields. One would thusexpect
thecompounds
with thelarger electronegativity
valuesto be more
ionic, i.e.,
havelarger
values ofhyperfine
fields. The fields measured at 4.4 K are considered
as saturation values
(for
Na andCsFeS2)
and asnegative.
Infigure 2,
I haveplotted
the measuredFIG. 2. - Magnetic hyperfine fields in MFeS2 (M = K, Rb, Cs, Na)
vs cationic (M) electronegativity.
values of
magnetic
field vs cationicelectronegati- vity [6, 7],
whichsuggests
that the cationic electrone-gativity
iseffectively
agood covalency parameter
in this series ofcompounds.
Acknowledgments.
- I amgrateful
to OEA andCNPq (Brasil)
for financialsupport.
References
[1] TAFT, C. A., RAJ, D. and DANON, J., J. Physique Colloq. 35 (1974) C 6-241.
[2] TAFT, C. A., RAJ, D. and DANON, J., J. Phys. & Chem. Solids 36
(1975)283.
[3] TAFT, C. A., RAJ, D. and DANON, J., Phys. Stat. Sol. 64 (1974)
111.
[4] TAFT, C. A., Proceedings of the International Conference on
Mössbauer Spectroscopy, Cracow, Poland (1975).
[5] GONSER, U., Ed. Mössbauer Spectroscopy (Springer-Verlag,
Berlin Heidelberg, New York) 1967.
[6] PRITCHARD, H. O. and SKINNER, H. H., Chem. Rev. 55 (1955)
745.
[7] PAULING, L., The Nature of the Chemical Bond (Cornell Univ.
Press, 3rd Ed., New York) 1960.