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STRUCTURAL AND MAGNETIC PROPERTIES OF AMORPHOUS BaO-Fe2O3-B2O3 SYSTEM

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HAL Id: jpa-00218637

https://hal.archives-ouvertes.fr/jpa-00218637

Submitted on 1 Jan 1979

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STRUCTURAL AND MAGNETIC PROPERTIES OF AMORPHOUS BaO-Fe2O3-B2O3 SYSTEM

Y. Syono, A. Ito

To cite this version:

Y. Syono, A. Ito. STRUCTURAL AND MAGNETIC PROPERTIES OF AMORPHOUS BaO-Fe2O3-B2O3 SYSTEM. Journal de Physique Colloques, 1979, 40 (C2), pp.C2-115-C2-117.

�10.1051/jphyscol:1979239�. �jpa-00218637�

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JOURNAL DE PHYSIQUE Colloque C2, suppldment au

n o

3, Tome 40, mars 1979, page C2-115

STRUCTURAL

AND

MAGNETIC

PROPERTIES

OF AMORPHOUS Ba0-Fe203-B203 SYSTEM Y. Syono and A.

to*

The Research I n s t i t u t e for Iron, Steel and Other MetaZs, Tohoku University, Sendai 980, Japan

I Department of Physics, Ochcmomizu University, Otsuka, Bunkyo-ku, Tokyo 112, Japan

R6sumd.- Des verres homogsnes du type BaO-Fen03 (39-63 mo1.X FezOs) avec B203 en petite quantitd ant 6tL obtenus par trempe B partir de 1'Qtat liquide. L'Ltude Miissbauer montre que le verre comporte essentiellement des mailles tetragdriques de ~ e ~ + 0 1 , et qu'il existe un ordre antiferr~rnagngti~ue 2 courte distance 1 basse tempgrature.

Abstract.- Homogeneous glasses of the iron-rich Ba0-Fe203 system (39-63 mol.% FezO3) with a small amount of B2O3 are prepared by splat cooling method. ~Xssbauer study reveals that the glass mainly consists of tetrahedral network of Fe3+04 and a short range antiferromagnetic order is formed at low temperatures.

Amorphous specimens of the iron-rich BaO-Fe2Os system with a small amount of B203 were prepared by splat cooling method with the aid of laser melting technique /I/. Gssbauer spectrum was measured from room temperature to 4.2 K and analyzed using an elec- tronic computer. Mzssbauer parameters determined are summarized in table I. The glasses presently prepared areclassified into two groups with the FezOs/BaO ratio greater and smaller than I.

around Fe3+ ions in the glass is supposed to be very similar to that in the crystalline Ba0.Fen03 in ~ c h Fe3+ ions occupy only tetrahedral sites 121. A rela- tively large quadrupole splitting, AE, is observed in the glass. The width of the spectrum is 0.47 mm/s, only twice as broad as that of the innermost peak of iron, 0.23 mm/s, corroborating rather uniform tetra- hedral environment around ~ e ions in the glass. ~ +

The temperature variation of Mbsbauer spectra

Table I : Mzssbauer parameters of amorphous Ba0-Fe203-Bz03 system

Specimen

!

Composition, mol%: 61, mm/s I AE, mm/s

i

Hint,kOe

;

r TN, K

:Fe203 BaO B2O3:Fe3+(t) Fe3+(o) " ~ e ~ + " :Fe3+(t) ~e~+(o) " ~ e ~ + " :Fe3+(t) ~e~+(o)

:

I 1 I I I

1 I 1 I I I

I I I I I I

- - -

I

:

F e - 2 : 3 9 57 4 i 0 . 2 3

- :

0.84 I I

I I 1 1 I I

m i

F e - 4 : 3 9 48 13i0.24

- -

:0.97

- - :

450

- :

70

%:

Fe- 9

:

54 37 9

:

0.35 0.37 0.51

:

0.92 0.41 1.56

:

I

h I I

1 I 1 I

4 I

Fe-10 54 39 7

:

0.32 0.38 0.53

:

0.93 0.42 1.62

:

460 500 I :I00

1 I I I I

:

Fe-11

:

58 38 4

:

0.29 0.38 0.50

:

0.92 0.32 1.66

:

I I

I I I I I I

:

Fe-14

:

63 32 5

:

0.43 0.45 0.55

:

0.86 0.37 1.55

:

450 490

:

140

.--L--,---L---L---I---L---J

i i I I

<;BaO,Fe203

:

50 50

- :

0.2

- - :

0.25

- -

i47.2'

-

i880/2/

1 I 1 1

k:~a0.2~e203

:

67 33

- :

0.21 0.41

-

i0.23 0.08

-

:486 516+ :945/3/

I I I I

6 and AE are at room temperature.-%efferred to iron metal.- Hint is at 4.2 K.- 'values at room temperature.

The glass with Fe203/~a0 < 1 is proved to have a rather simple structure. Figure 1 (upper curve) shows the Mijssbauer spectrum of the specimen Fe-2 measured at room temperature. The spectrum is fitted by a single doublet with the Lorentzian profile by the least square method. The value of the isomer shift, 6 = 0.23 mm/s, indicates that the glass isform- ed by tetrahedral network of Fe3+o4. The structure

of the specimen, Fe-4, is shown in figure 2. At 4 . 2 ~ a well resolved hyperfine sextet is observed. The internal field, Hint, is estimated to be 450 kOe, as expected for Fe3+ ions in tetrahedral environments.

The spectrum is very nearly SYmetric, revealing an apparent disappearance of quadrupole shift in the magnetically ordered state, in spite of the large quadrupole splitting observed in the room temperature

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyscol:1979239

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JOURNAL DE PHYSIQUE

spectrum. 39F+O348BaO.l 3B20, (Fe- 4 )

I

I I I I I I I I I I I

Room Temp.

I I I I I

~ e ~ + ( t )

I [-

Fig. 1 : Demonstration of comput?er curve fitting for paramagnetic spectra of the glasses measured at room temperature.

Upper curve : Fe-2 (FezOsIBa 0 < 1).

Lower curve : Fe- 14 (FezOg/BaO > 1 )

.

- -

The distribution of the internal field is supposed to be narrow, when the quadrupole broadening effect is taken into consideration

111.

The temperature de- pendence of the internal field approximately follows a Brillouin function with S = 512, yielding a magne- tic ordering temperature of 70 K. This value is by an order of magnitude smaller than the Ndel tempe- rature of the corresponding crystalline phase, Ba0.Fe203 121. This decrease is attributed to weak- enedsuperexchange interaction due to randomness of

2 6 -

-

0 Z

-

i2!

4

bond angles in the glass.

The iron-rich glass (Fez03/Ba0 > 1) shows com-

39Fe203.578;10.4Bz03

-

~ e ~ * ( 1 ) (Fe-2) -

' I

'FC'"

~e";lo) y*...

... . . .,. .

- -

I

!

!

I I 63Fe203 I .328a0.5B26 ( F ~ - 1 4 ~ )

plex paramagnetic spectra at room temperature. An example of computer curve fitting is demonstrated in figure 1 (lower curve). In the analysis, the width of each line is fixed to be 0.47 mm/s, the same as that obtained for the spectrum of Fe-2. The spectrum is successfully explained by superposition of two doublets due to tetrahedral and octahedral Fe3+ ions plus an additional weak doublet which is tentatively assigned to be due to "Fez+" ions. The glass struc- ture of this group seems to correspond to the Ba0.2Fez03 crystal hydrothermally synthesized 131, in which ~ e ions are equally distributed among ~ + the tetrahedral and octahedral site. The hyperfine spectrum at low temperatures is also interpreted to

2 1 0 1 2 3

VELOCITY (mmls)

hts T=40K

...

I&- . .;..:.. .; .. .,;:

?.

. . . .,:. . . .

'

. . . '

;

. . .

;

. . . . .

:-' ' .

- . . .

. . . .

>,

-....

...

...

Fig. 2 : Temperature variation of Gssbauer spectra of the glass, Fe-4(hfs : hyperfine spectrum

-

pms : paramagnetic spectrum).

consist of two sextets with the internal field of 450 and 500 kOe, corresponding to the tetrahedral and octahedral Fe3+ ions respectively. The magnetic ordering temperature determined from temperature variation of the internal field is only 140 K in the most iron-rich specimen

111.

Preliminary magnetic measurements reveal that the magnetic susceptibility shows a broad maximum around the magnetic ordering temperature, obeying Curie-Weiss law in higher temperatures. No evidence for superparamagnetic behavior is found in harmony with MEssbauer measurements. Summarizing, the magne- tic ordering achieved in the present amorphous sys- tem is of the short range antiferromagnetism, simi- lar to that found in FePOb by neutron diffraction 141.

Acknowledgments.- The authors are indebted to Mr.0.

Horie and Dr. K. Okamura for their collaboration in the early stage of this work. Their thanks are due to Professors Y. Nakagawa and S. Yajima for warm encouragements. They are grateful to Professor Y.

Matsui who kindly wrote and offered the computer program. The computer analysis was done at the Com- puter Center, Tohoku University.

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References

/ I

/

Horie, O., Syono, Y., Nakagawa, Y., Ito, A., Okamura,

K. and Yajima, S., Solid State Commun.

2

(1978) 423.

121 Do-Dinh, C., Bertaut, E.F. and Chappert, J., J. Phy- sique

2

(1969) 566.

/3/ Okamoto, S., Sekizawa, H. and Okamoto, S.I., J. Phys.

Chem. Solids

2

(1975) 591.

/4/ Wedgwood, F.A. and Wright, A.C., J. Non-Cryst. Solids 21 (1976) 95.

-

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