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Ferromagnetism in Fe-doped Ba6Ge25 chiral clathrate
Yang Li and Joseph H. Ross, Jr.a)
Department of Physics, Texas A&M University, College Station, Texas 77843-4242
͑Received 2 June 2003; accepted 13 August 2003͒
We have synthesized a Ba6Ge25 clathrate, substituting 3 Ge per formula unit by Fe. This chiral
clathrate has Ge sites forming a framework of closed cages and helical tunnel networks. Fe atoms
randomly occupy these sites, and exhibit high-spin magnetic moments. A ferromagnetic transition is
observed with Tcϭ170 K, the highest observed Tc for a magnetic clathrate. However, the magnetic
phase is significantly disordered, and exhibits a transformation to a reentrant spin glass phase. This
system has a number of features in common with other dilute magnetic semiconductors. © 2003
American Institute of Physics. ͓DOI: 10.1063/1.1616658͔
Si, Ge, and Sn clathrates have received increasing atten-
tion over the past few years. These materials have a semi-
conducting framework into which metal atoms can be sub-
stituted, providing a number of possibilities for electronic
materials,1
for example, thermoelectrics,2,3
and
superconductors.4
Ferromagnetism has been observed in Mn-
doped Ge clathrate, with Tcϭ10 K,5
and clathrates having
Eu encapsulated in the cages, with Tc up to 37 K.3
Currently,
there is strong interest in ferromagnetic semiconductors for
spintronic applications,6
and much effort has been devoted to
the magnetic doping of semiconductors using low-
temperature epitaxy.7
Clathrates offer the possibility of semi-
conducting phases containing magnetic atoms at equilibrium,
which might be compatible with conventional substrates.8
Here, we report the synthesis of a stable Fe-doped Ge clath-
rate, and the observation of a ferromagnetic transition with
Tcϭ170 K.
Although several transition metals substitute for Ge in
the type-I clathrate structure,9
attempts at Fe substitution
have failed due to competing Fe–Ge phases. However, we
find that higher temperature synthesis produces an Fe-
containing clathrate of the recently discovered chiral struc-
ture type, Ba6Ge25 .10–12
This clathrate contains an open
Ge–Ge bonded framework, threaded by closed dodecahedral
cages. The material actually forms as Ba6Ge24 , with vacan-
cies occurring preferentially by a Zintl mechanism.12
Our method followed several steps. Elemental mixtures,
with excess Ba, were placed in BN crucibles, sealed under
Ar, and prereacted by rf induction. The resulting mixtures
included type-I clathrates and FeGe2 . Characterization was
by x-ray diffraction ͑Bruker D8 Advance Powder, Cu K␣
radiation͒, and refinement using GSAS software.13
To com-
plete the reaction and eliminate FeGe2 , the mixtures were
arc melted several times in a water-cooled copper crucible.
The ingots were then sealed in quartz ampoules and annealed
at 700 °C for 100 h. By this method we obtained single-
phase or nearly single-phase Ba6Ge25ϪxFex with x up to 3.
However, furnace melting and slower cooling through the
melting point produced a mixture of FeGe2 and clathrate
phases. An x-ray analysis for xϭ3 is shown in Fig. 1. All
observed peaks were indexed according to the cubic space
group P4132 ͑No. 213͒, as previously reported for
Ba6Ge25 .10–12
The lattice constant for xϭ3 is a
ϭ1.45520 nm, slightly larger than reported for Ba6Ge24 (a
ϭ1.45483 nm).12
Energy-dispersive x-ray spectroscopy ͑EDS͒ and elec-
tron diffraction measurements ͑JEOL JEM-2010 electron mi-
croscope, 100 kV͒ for the xϭ3 sample showed that Fe was
indeed incorporated in the clathrate phase. These measure-
ments also showed trace amounts of Ge and FeGe2 to be
present, but below the x-ray detectability limit ͑a few per-
cent͒. Thus, a minor fraction of the Fe atoms are present as
FeGe2 . No other phases were observed. Analysis gave an
average clathrate composition Ba6Ge21.9Fe3.1 for the xϭ3
sample, a Ge:Fe ratio close to the starting composition. The
Fe content per formula unit was 3.1Ϯ1, with variations ob-
served between crystallites, however, the crystallites ap-
peared locally homogeneous, with no apparent clustering.
The chiral clathrate structure ͑Fig. 1͒ has Ba situated in
open channels as well as closed cages. In the Ge25 frame-
work, two of the six distinct sites have three Ge–Ge bonds,
the others having four. By contrast, type I and II clathrates
have only four-bonded Ge sites in approximately tetrahedral
bonding configurations, and closed cages. In our x-ray analy-
sis we placed Fe predominantly on three of the six sites,
similar to the occupation parameters for In-doped Ge25
a͒
Electronic mail: jhross@tamu.edu
FIG. 1. X-ray refinement for Ba6Ge22Fe3 . Upper curve: data and fit, with
difference plot below. Ticks show peaks indexed according to the chiral
clathrate structure. Inset: unit cell with Ge–Fe framework, showing dis-
torted dodecahedral cage at the lower left. Three-bonded sites are larger
circles.
APPLIED PHYSICS LETTERS VOLUME 83, NUMBER 14 6 OCTOBER 2003
28680003-6951/2003/83(14)/2868/3/$20.00 © 2003 American Institute of Physics
Downloaded 01 Oct 2003 to 165.91.253.39. Redistribution subject to AIP license or copyright, see http://ojps.aip.org/aplo/aplcr.jsp
clathrate,12
and the refinement gave a composition
Ba6Ge21.8Fe3.0 , in excellent agreement with the EDS result
(Ba6Ge21.9Fe3.1). However, since the Fe and Ge x-ray struc-
ture factors are similar, we found that Fe could be redistrib-
uted among framework sites to give a similar composition
and nearly identical goodness of fit (R values: Rwpϭ0.077
and Rpϭ0.053). The specific Fe locations, therefore, are un-
certain, although it is clear that they are distributed in the
clathrate framework.
Magnetic measurements were made on a Ba6Ge22Fe3
sample using a superconducting quantum interference device
magnetometer ͑Quantum Design MPMS-XL͒. Zero-field-
cooled ͑ZFC͒ magnetization was measured on warming in
fixed field, while field-cooled ͑FC͒ magnetization was mea-
sured versus decreasing temperature in constant field. Figure
2 shows data for 0.1 T applied field. The high-temperature
behavior was fit to a Curie–Weiss law
␹ϭ
C
TϪTc
ϩ␹dia ,
where ␹dia denotes a diamagnetic background. The value C
ϭ5.6ϫ10Ϫ5
K m3
/kg indicates an effective moment peff
ϭ5.5 ␮B per Fe, close to the free-ion value, 5.9 ␮B , for
high-spin Fe (peffϭg͓J(Jϩ1)͔1/2
). Tc obtained from the fit is
180 K. The diamagnetic term, ␹diaϭϪ8.2ϫ10Ϫ8
m3
/kg, is
large and may be an overestimation due to rounding of the
transition. Some distribution of Tc seems likely because of
the observed Fe concentration distribution. However, low
temperature magnetization measurements agree with the Cu-
rie fit; Tcϭ170 K is estimated from a modified Arrott plot
͑inset to Fig. 3͒.
A divergence of ␹FC and ␹ZFC starts near 170 K, and
becomes much more pronounced below 110 K ͑Fig. 2͒. The
remanence was also measured, warming the sample after re-
moval of the field, and found to decrease with temperature,
and vanish near 110 K. The magnetization at 2 K ͑Fig. 3͒ is
polarized to 0.75 ␮B per Fe in a small field. However, full
saturation is not reached even at 7 T, where the magnetiza-
tion corresponds to 1 ␮B per Fe. This value is considerably
lower than expected, given the value peffϭ5.5 ␮B obtained
from the Curie fit. This suggests a canted or noncollinear
spin configuration.
The observed magnetic behavior cannot be due to the
small amount of FeGe2 , which has a spiral spin structure
below 289 K, becoming commensurate at 263 K.14
These do
not correspond to the observed transitions, and the observed
moments clearly could not result from inclusions of this
phase at the few percent level.
To further understand the magnetic behavior, in-phase
(␹Ј) and out-of-phase (␹Љ) ac susceptibilities were mea-
sured under a 0.6 mT ac field, with the results shown in Fig.
4. The higher-temperature data could be fit to a Curie law
with Tcϭ180 K, in accord with the dc results. ␹Ј exhibits a
strong rise below 200 K, corresponding to the ferromagnetic
transition. However, below a maximum, ␹Ј decreases at
lower temperatures and becomes frequency dependent, while
␹Љ also becomes frequency dependent. The frequency depen-
dence, combined with the decrease of ZFC vs FC magneti-
zation below 110 K, are characteristic of reentrant spin glass
systems.15,16
We conclude that the transition near 170 K is
ferromagnetic, while the 110 K irreversibility point corre-
sponds to a spin-glass freezing transition.
Frequency dependent ␹ac is found in spin glasses, while
for ordinary ferromagnets the time scale is much too small,
even for the critical slowing down region near Tc .15,16
Canted ferromagnets with a low-temperature antiferromag-
FIG. 2. Ba6Ge22Fe3 ZFC, FC, and remanent magnetization vs temperature,
with Hϭ0.1 T. Insets at right: FC data at high temperatures, dashed curve
showing a Curie–Weiss fit.
FIG. 3. M –H hysteresis at 2 K, with the low-field region expanded at the
right. Left inset: modified Arrott plot of M vs H, with ␥ϭ1.0 and ␤
ϭ0.45.
FIG. 4. Ac susceptibility vs temperature, measured in zero dc field. Fre-
quency increases from top to bottom as shown, for both ␹Ј and ␹Љ.
2869Appl. Phys. Lett., Vol. 83, No. 14, 6 October 2003 Y. Li and J. H. Ross, Jr.
Downloaded 01 Oct 2003 to 165.91.253.39. Redistribution subject to AIP license or copyright, see http://ojps.aip.org/aplo/aplcr.jsp
netism have exhibited ac behavior similar to that of a reen-
trant spin glass,17
however, ␹Љ in that case shows only an
increase with frequency, and no shift in canting transition
temperature. The variation of ␹Љ peak position, Tp , per de-
cade of frequency, ͓dTp /d(log f )/Tp͔, is 0.042 for
Ba6Ge22Fe3 , which is in the range of values observed for
spin glasses, 0.004–0.08.16
Spin-glass reentrance is attributed to the freezing of
transverse degrees of freedom in a ferromagnet containing
disorder.18
Alternatively, a cluster-glass mechanism has been
argued,19
and it is clear that ferromagnetic clusters and con-
siderable disorder in the ferromagnetic state20
do play a role
in real materials. However, a cluster glass alone does not
explain the present data, particularly the low-temperature
saturation. A remanence increase on cooling in the glassy
state is also typical of such spin glasses.21
Fe occupancy of framework sites is below the percola-
tion threshold, even for second-neighbor bonds, so it is likely
that the mechanism for magnetic ordering is conduction–
electron mediation, as in diluted magnetic semiconductors.
For comparison, in (Ga1ϪxMnx)As, Mn carries about 5 ␮B ,
and Tc scales linearly with small values of x, reaching Tc
ϭ110 K for xϭ0.05.7
The present system is quite similar in
Tc vs x. Band-structure calculations22
indicate a gap below
the Fermi level in Ba6Ge25 , which may quite possibly be the
EF location in the Zintl composition Ba6Ge24 . The Zintl
concept23
involves valence counting to give a closed-shell
bonding configuration. Assuming valence 3 for Fe,
Ba6Ge21(3/4)Fe3 is also a Zintl phase, and very close to the
average composition found here. Thus, it seems likely that
EF is near a band edge in this material, and the semiconduc-
tor model is appropriate.
There is considerable interest in the effects of disorder
on the magnetic behavior of magnetic semiconductors;24–26
the conduction–electron mediated interaction provides frus-
tration, giving a noncollinear ordered state.24
For the case of
͑Ga,Mn͒N, the ground state appears to be a spin glass with
no ferromagnetism.27
Here, we observe a ferromagnetic tran-
sition and spin-glass state in the same material.
In summary, a Ba6Ge22Fe3 clathrate was synthesized,
exhibiting a ferromagnetic Tcϭ170 K. Below 110 K, a tran-
sition to a reentrant spin glass was evidenced by the onset of
frequency-dependent ac susceptibility and a characteristic
field-dependent magnetization.
This work was supported by the Robert A. Welch Foun-
dation, Grant No. A-1526, and by the National Science
Foundation, Grant No. DMR-0103455.
1
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G. Cordier and P. Woll, J. Less-Common Met. 169, 291 ͑1991͒.
10
W. Carrillo-Cabrera, J. Curda, H. G. von Schnering, S. Paschen, and Y.
Grin, Z. Kristallogr. 215, 207 ͑2000͒.
11
H. Fukuoka, K. Iwai, and S. Yamanaka, J. Solid State Chem. 151, 117
͑2000͒.
12
S.-J. Kim, S. Hu, C. Uher, T. Hogan, B. Huang, J. D. Corbett, and M. G.
Kanatzidis, J. Solid State Chem. 153, 321 ͑2000͒.
13
A. C. Larson and R. B. von Dreele, Technical Report No. LAUR 86-748,
Los Alamos National Laboratory ͑2000͒.
14
L. M. Corliss, J. M. Hastings, W. Kunnmann, R. Thomas, J. Zhuang, R.
Butera, and D. Mukamel, Phys. Rev. B 31, 4337 ͑1985͒.
15
K. Binder and A. P. Young, Rev. Mod. Phys. 58, 801 ͑1986͒.
16
J. A. Mydosh, Spin Glasses: An Experimental Introduction ͑Taylor and
Francis, London, 1993͒.
17
S. Mukherjee, R. Ranganathan, and S. B. Roy, Phys. Rev. B 50, 1084
͑1994͒.
18
M. Gabay and G. Toulouse, Phys. Rev. Lett. 47, 201 ͑1981͒.
19
L. D. Rakers and P. A. Beck, Phys. Rev. B 36, 8622 ͑1987͒.
20
W. Bao, S. Raymond, S. M. Shapiro, K. Motoya, B. Fa˚k, and R. W. Erwin,
Phys. Rev. Lett. 82, 4711 ͑1999͒.
21
C. M. Wynn, M. A. Gıˆrt¸u, J. Zhang, J. S. Miller, and A. J. Epstein, Phys.
Rev. B 58, 8508 ͑1998͒.
22
I. Zerec, A. Yaresko, P. Thalmeier, and Y. Grin, Phys. Rev. B 66, 045115
͑2002͒.
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M. Kauzlarich ͑VCH, New York, 1996͒.
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J. Schliemann and A. H. MacDonald, Phys. Rev. Lett. 88, 137201 ͑2002͒.
25
G. Zara´nd and B. Janko´, Phys. Rev. Lett. 89, 047201 ͑2002͒.
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S. Dhar, O. Brandt, A. Trampert, K. J. Friedland, Y. J. Sun, and K. H.
Ploog, Phys. Rev. B 67, 165205 ͑2003͒.
2870 Appl. Phys. Lett., Vol. 83, No. 14, 6 October 2003 Y. Li and J. H. Ross, Jr.
Downloaded 01 Oct 2003 to 165.91.253.39. Redistribution subject to AIP license or copyright, see http://ojps.aip.org/aplo/aplcr.jsp

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Ferromagnetism in Fe-doped Ba6Ge25 Chiral Clathrate

  • 1. Ferromagnetism in Fe-doped Ba6Ge25 chiral clathrate Yang Li and Joseph H. Ross, Jr.a) Department of Physics, Texas A&M University, College Station, Texas 77843-4242 ͑Received 2 June 2003; accepted 13 August 2003͒ We have synthesized a Ba6Ge25 clathrate, substituting 3 Ge per formula unit by Fe. This chiral clathrate has Ge sites forming a framework of closed cages and helical tunnel networks. Fe atoms randomly occupy these sites, and exhibit high-spin magnetic moments. A ferromagnetic transition is observed with Tcϭ170 K, the highest observed Tc for a magnetic clathrate. However, the magnetic phase is significantly disordered, and exhibits a transformation to a reentrant spin glass phase. This system has a number of features in common with other dilute magnetic semiconductors. © 2003 American Institute of Physics. ͓DOI: 10.1063/1.1616658͔ Si, Ge, and Sn clathrates have received increasing atten- tion over the past few years. These materials have a semi- conducting framework into which metal atoms can be sub- stituted, providing a number of possibilities for electronic materials,1 for example, thermoelectrics,2,3 and superconductors.4 Ferromagnetism has been observed in Mn- doped Ge clathrate, with Tcϭ10 K,5 and clathrates having Eu encapsulated in the cages, with Tc up to 37 K.3 Currently, there is strong interest in ferromagnetic semiconductors for spintronic applications,6 and much effort has been devoted to the magnetic doping of semiconductors using low- temperature epitaxy.7 Clathrates offer the possibility of semi- conducting phases containing magnetic atoms at equilibrium, which might be compatible with conventional substrates.8 Here, we report the synthesis of a stable Fe-doped Ge clath- rate, and the observation of a ferromagnetic transition with Tcϭ170 K. Although several transition metals substitute for Ge in the type-I clathrate structure,9 attempts at Fe substitution have failed due to competing Fe–Ge phases. However, we find that higher temperature synthesis produces an Fe- containing clathrate of the recently discovered chiral struc- ture type, Ba6Ge25 .10–12 This clathrate contains an open Ge–Ge bonded framework, threaded by closed dodecahedral cages. The material actually forms as Ba6Ge24 , with vacan- cies occurring preferentially by a Zintl mechanism.12 Our method followed several steps. Elemental mixtures, with excess Ba, were placed in BN crucibles, sealed under Ar, and prereacted by rf induction. The resulting mixtures included type-I clathrates and FeGe2 . Characterization was by x-ray diffraction ͑Bruker D8 Advance Powder, Cu K␣ radiation͒, and refinement using GSAS software.13 To com- plete the reaction and eliminate FeGe2 , the mixtures were arc melted several times in a water-cooled copper crucible. The ingots were then sealed in quartz ampoules and annealed at 700 °C for 100 h. By this method we obtained single- phase or nearly single-phase Ba6Ge25ϪxFex with x up to 3. However, furnace melting and slower cooling through the melting point produced a mixture of FeGe2 and clathrate phases. An x-ray analysis for xϭ3 is shown in Fig. 1. All observed peaks were indexed according to the cubic space group P4132 ͑No. 213͒, as previously reported for Ba6Ge25 .10–12 The lattice constant for xϭ3 is a ϭ1.45520 nm, slightly larger than reported for Ba6Ge24 (a ϭ1.45483 nm).12 Energy-dispersive x-ray spectroscopy ͑EDS͒ and elec- tron diffraction measurements ͑JEOL JEM-2010 electron mi- croscope, 100 kV͒ for the xϭ3 sample showed that Fe was indeed incorporated in the clathrate phase. These measure- ments also showed trace amounts of Ge and FeGe2 to be present, but below the x-ray detectability limit ͑a few per- cent͒. Thus, a minor fraction of the Fe atoms are present as FeGe2 . No other phases were observed. Analysis gave an average clathrate composition Ba6Ge21.9Fe3.1 for the xϭ3 sample, a Ge:Fe ratio close to the starting composition. The Fe content per formula unit was 3.1Ϯ1, with variations ob- served between crystallites, however, the crystallites ap- peared locally homogeneous, with no apparent clustering. The chiral clathrate structure ͑Fig. 1͒ has Ba situated in open channels as well as closed cages. In the Ge25 frame- work, two of the six distinct sites have three Ge–Ge bonds, the others having four. By contrast, type I and II clathrates have only four-bonded Ge sites in approximately tetrahedral bonding configurations, and closed cages. In our x-ray analy- sis we placed Fe predominantly on three of the six sites, similar to the occupation parameters for In-doped Ge25 a͒ Electronic mail: jhross@tamu.edu FIG. 1. X-ray refinement for Ba6Ge22Fe3 . Upper curve: data and fit, with difference plot below. Ticks show peaks indexed according to the chiral clathrate structure. Inset: unit cell with Ge–Fe framework, showing dis- torted dodecahedral cage at the lower left. Three-bonded sites are larger circles. APPLIED PHYSICS LETTERS VOLUME 83, NUMBER 14 6 OCTOBER 2003 28680003-6951/2003/83(14)/2868/3/$20.00 © 2003 American Institute of Physics Downloaded 01 Oct 2003 to 165.91.253.39. Redistribution subject to AIP license or copyright, see http://ojps.aip.org/aplo/aplcr.jsp
  • 2. clathrate,12 and the refinement gave a composition Ba6Ge21.8Fe3.0 , in excellent agreement with the EDS result (Ba6Ge21.9Fe3.1). However, since the Fe and Ge x-ray struc- ture factors are similar, we found that Fe could be redistrib- uted among framework sites to give a similar composition and nearly identical goodness of fit (R values: Rwpϭ0.077 and Rpϭ0.053). The specific Fe locations, therefore, are un- certain, although it is clear that they are distributed in the clathrate framework. Magnetic measurements were made on a Ba6Ge22Fe3 sample using a superconducting quantum interference device magnetometer ͑Quantum Design MPMS-XL͒. Zero-field- cooled ͑ZFC͒ magnetization was measured on warming in fixed field, while field-cooled ͑FC͒ magnetization was mea- sured versus decreasing temperature in constant field. Figure 2 shows data for 0.1 T applied field. The high-temperature behavior was fit to a Curie–Weiss law ␹ϭ C TϪTc ϩ␹dia , where ␹dia denotes a diamagnetic background. The value C ϭ5.6ϫ10Ϫ5 K m3 /kg indicates an effective moment peff ϭ5.5 ␮B per Fe, close to the free-ion value, 5.9 ␮B , for high-spin Fe (peffϭg͓J(Jϩ1)͔1/2 ). Tc obtained from the fit is 180 K. The diamagnetic term, ␹diaϭϪ8.2ϫ10Ϫ8 m3 /kg, is large and may be an overestimation due to rounding of the transition. Some distribution of Tc seems likely because of the observed Fe concentration distribution. However, low temperature magnetization measurements agree with the Cu- rie fit; Tcϭ170 K is estimated from a modified Arrott plot ͑inset to Fig. 3͒. A divergence of ␹FC and ␹ZFC starts near 170 K, and becomes much more pronounced below 110 K ͑Fig. 2͒. The remanence was also measured, warming the sample after re- moval of the field, and found to decrease with temperature, and vanish near 110 K. The magnetization at 2 K ͑Fig. 3͒ is polarized to 0.75 ␮B per Fe in a small field. However, full saturation is not reached even at 7 T, where the magnetiza- tion corresponds to 1 ␮B per Fe. This value is considerably lower than expected, given the value peffϭ5.5 ␮B obtained from the Curie fit. This suggests a canted or noncollinear spin configuration. The observed magnetic behavior cannot be due to the small amount of FeGe2 , which has a spiral spin structure below 289 K, becoming commensurate at 263 K.14 These do not correspond to the observed transitions, and the observed moments clearly could not result from inclusions of this phase at the few percent level. To further understand the magnetic behavior, in-phase (␹Ј) and out-of-phase (␹Љ) ac susceptibilities were mea- sured under a 0.6 mT ac field, with the results shown in Fig. 4. The higher-temperature data could be fit to a Curie law with Tcϭ180 K, in accord with the dc results. ␹Ј exhibits a strong rise below 200 K, corresponding to the ferromagnetic transition. However, below a maximum, ␹Ј decreases at lower temperatures and becomes frequency dependent, while ␹Љ also becomes frequency dependent. The frequency depen- dence, combined with the decrease of ZFC vs FC magneti- zation below 110 K, are characteristic of reentrant spin glass systems.15,16 We conclude that the transition near 170 K is ferromagnetic, while the 110 K irreversibility point corre- sponds to a spin-glass freezing transition. Frequency dependent ␹ac is found in spin glasses, while for ordinary ferromagnets the time scale is much too small, even for the critical slowing down region near Tc .15,16 Canted ferromagnets with a low-temperature antiferromag- FIG. 2. Ba6Ge22Fe3 ZFC, FC, and remanent magnetization vs temperature, with Hϭ0.1 T. Insets at right: FC data at high temperatures, dashed curve showing a Curie–Weiss fit. FIG. 3. M –H hysteresis at 2 K, with the low-field region expanded at the right. Left inset: modified Arrott plot of M vs H, with ␥ϭ1.0 and ␤ ϭ0.45. FIG. 4. Ac susceptibility vs temperature, measured in zero dc field. Fre- quency increases from top to bottom as shown, for both ␹Ј and ␹Љ. 2869Appl. Phys. Lett., Vol. 83, No. 14, 6 October 2003 Y. Li and J. H. Ross, Jr. Downloaded 01 Oct 2003 to 165.91.253.39. Redistribution subject to AIP license or copyright, see http://ojps.aip.org/aplo/aplcr.jsp
  • 3. netism have exhibited ac behavior similar to that of a reen- trant spin glass,17 however, ␹Љ in that case shows only an increase with frequency, and no shift in canting transition temperature. The variation of ␹Љ peak position, Tp , per de- cade of frequency, ͓dTp /d(log f )/Tp͔, is 0.042 for Ba6Ge22Fe3 , which is in the range of values observed for spin glasses, 0.004–0.08.16 Spin-glass reentrance is attributed to the freezing of transverse degrees of freedom in a ferromagnet containing disorder.18 Alternatively, a cluster-glass mechanism has been argued,19 and it is clear that ferromagnetic clusters and con- siderable disorder in the ferromagnetic state20 do play a role in real materials. However, a cluster glass alone does not explain the present data, particularly the low-temperature saturation. A remanence increase on cooling in the glassy state is also typical of such spin glasses.21 Fe occupancy of framework sites is below the percola- tion threshold, even for second-neighbor bonds, so it is likely that the mechanism for magnetic ordering is conduction– electron mediation, as in diluted magnetic semiconductors. For comparison, in (Ga1ϪxMnx)As, Mn carries about 5 ␮B , and Tc scales linearly with small values of x, reaching Tc ϭ110 K for xϭ0.05.7 The present system is quite similar in Tc vs x. Band-structure calculations22 indicate a gap below the Fermi level in Ba6Ge25 , which may quite possibly be the EF location in the Zintl composition Ba6Ge24 . The Zintl concept23 involves valence counting to give a closed-shell bonding configuration. Assuming valence 3 for Fe, Ba6Ge21(3/4)Fe3 is also a Zintl phase, and very close to the average composition found here. Thus, it seems likely that EF is near a band edge in this material, and the semiconduc- tor model is appropriate. There is considerable interest in the effects of disorder on the magnetic behavior of magnetic semiconductors;24–26 the conduction–electron mediated interaction provides frus- tration, giving a noncollinear ordered state.24 For the case of ͑Ga,Mn͒N, the ground state appears to be a spin glass with no ferromagnetism.27 Here, we observe a ferromagnetic tran- sition and spin-glass state in the same material. In summary, a Ba6Ge22Fe3 clathrate was synthesized, exhibiting a ferromagnetic Tcϭ170 K. Below 110 K, a tran- sition to a reentrant spin glass was evidenced by the onset of frequency-dependent ac susceptibility and a characteristic field-dependent magnetization. This work was supported by the Robert A. Welch Foun- dation, Grant No. A-1526, and by the National Science Foundation, Grant No. DMR-0103455. 1 B. Roy, K. E. Sim, and A. D. Caplin, Philos. Mag. A 65, 1445 ͑1992͒. 2 G. S. Nolas, J. L. Cohn, G. A. Slack, and S. B. Schujman, Appl. Phys. Lett. 73, 178 ͑1998͒. 3 B. C. Sales, B. C. 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