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Mössbauer studies of NaFes2 : magnetic hyperfine fields and covalency in MFeS2 compounds (m=Na, k, Rb, Cs)

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Submitted on 1 Jan 1977

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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�

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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. Wenceslau

Braz, 71,

Rio de

Janeiro,

Brasil

(Reçu

le 2 novembre

1976,

révisé le 5 mai

1977, accepté

le 23 mai

1977)

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 measured

hyperfine

parameters characterize iron in NaFeS2 to be in the

high

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 of

covalency

effects in alcali-dithioferrates

AFeS2 (A=K, Rb, Cs).

These

effects cause a

large

reduction of the observed

magnetic hyperfine

fields from the

expected

ionic value

[1, 2].

In this work I report on Mossbauer studies of

NaFeS2

in the

temperature

range (300-4.4

K)

indi-

cating

also a

large

deviation of the measured

magnetic

field from the ionic value.

It is

interesting

to note that the

magnitude

of the

magnetic

field in the alcali-dithioferrate series can be correlated with a

covalency

scale based on 4s contri- bution and cationic

electronegativity.

2.

Experimental.

- The

samples

were

investigated using

a 1024 multichannel

analyser, operating

in the

multiscaler mode to a

velocity

transducer of the Kankeleit

type.

The source was a 10 mCi of

" Co

in a Pd matrix

having

a width of 0.28

mm/s

measured

against

a natural iron absorber. The gamma rays were

detected with a thin Nal

(Tl)

scintillator mounted in a

photo-multiplier

tube. The

liquid

helium measu-

rement was taken with both source and absorber in

liquid

helium. The low temperature measurements

were recorded

using

an Elscint cryostat with

tempe-

(*) 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

were

prepared by fusing

iron

powder

with sodium carbonate and

sulphur

and

leaching

the cold

product

in water.

3. Results and discussion. -

Figure

1 shows the

transmission

spectra

of

NaFeS2

at several tempera-

tures. From 300 K down. to 77 K a

quadrupole

doublet with a temperature

independent splitting

of

0.58

mm/s

is observed. The room

temperature

isomer shift value is 0.36

mm/s (w.r.t. Fe).

These parameters

are

typical

for iron in the

high spin Fe3+ 6S5J2

confi-

guration [1-4].

At 4.4 K the

spectrum

was

additionally split by

a

strong magnetic hyperfine

interaction and the

magnitude

of the

hyperfine

field was

I Hhf

= 270 k0152

( ±

5

kOe).

The

sign

of

Hhf

is

assumed to be

negative

as this is

usually

the case

in

Fe3+ high-spin compounds.

Electric field

gradient (EFG)

calculations

[1, 2]

in this series of

compounds

indicated

negligible

values

of asymmetry parameter

(q).

In the present case of

a small

quadrupole

interaction

superimposed

on a

large magnetic hyperfine

interaction in the

absorber,

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 lines

of the six-line pattern). ,

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphys:019770038090116100

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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 be

simply

derived.

The

magnitude

of the internal field in

NaFeS2 (270 k0e)

which is assumed to be the saturation

field,

is

unusually

small for a ferric ion. There are appa-

rently

considerable

covalency

effects from

neigh- boring spins.

Molecular orbital calculations

suggest

that there should be a linear

relationship

between

the covalent induced

hyperfine

field and the

charge

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 average

hyperfine

field

due to one 4s electron and

Q4,

is the number of 4s electrons at the

Fe3 +

ion

originating

from the

covalent

ligands.

From the

Modified

WWJ Plot

[1]

one obtains

Q4s

= 0.22. This estimate

yields Hhf

= - 330

k0e,

which is a

reasonably good

esti-

mate.

Various attempts have been made to correlate the extensive Mossbauer data with available

electronega- tivity

scales

[5].

In this isostructural series

MFeS2 (M=Na, K, Rb, Cs)

in which the cation M is the

only varying element,

it appears reasonable to

attempt

such a correlation. The

increasing electronegativity

of the cation will decrease the 4s electron

density

at

the Fe nucleus and hence reduce the

proposed

trans-

ferred

hyperfine

fields. One would thus

expect

the

compounds

with the

larger electronegativity

values

to be more

ionic, i.e.,

have

larger

values of

hyperfine

fields. The fields measured at 4.4 K are considered

as saturation values

(for

Na and

CsFeS2)

and as

negative.

In

figure 2,

I have

plotted

the measured

FIG. 2. - Magnetic hyperfine fields in MFeS2 (M = K, Rb, Cs, Na)

vs cationic (M) electronegativity.

values of

magnetic

field vs cationic

electronegati- vity [6, 7],

which

suggests

that the cationic electrone-

gativity

is

effectively

a

good covalency parameter

in this series of

compounds.

Acknowledgments.

- I am

grateful

to OEA and

CNPq (Brasil)

for financial

support.

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.

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