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02/12/2008
GDR MICO, Autrans, 2008
1
Magnetic Order and Magnetoelectric effect in the frustrated Fe langasites
V. Simonet, M. Loire, R. Ballou
Outline : - Structure- Magnetic properties- Dielectric properties- Conclusion
K. Marty, P. Bordet, P. Lejay, O. Isnard
E. RessoucheINAC/SPSMS/MDN, CEA, Grenoble, France
Institut Néel, CNRS/UJF, Grenoble, France
02/12/2008
GDR MICO, Autrans, 2008
2
b
a
Ba3NbFe3Si2O14 : space group P321
Fe-langasite : structure
c
Geometrical frustrationAcentric structure
Crystal grown by floating zone methodin image furnace
triangular lattice of Fe3+ triangles, S=5/2
⇒Magnetic properties?⇒Magnetoelectric effect?
⇒Multiferroism?
02/12/2008
GDR MICO, Autrans, 2008
3
Fe-langasite : magnetic properties
Magnetic transition → antiferromagnetic order at TN∼28 K
0 50 100 150 200 250 3000.000
0.005
0.010
0.015
0.020M
/H (e
mu/
mol
Fe)
T (K)
Ba3NbFe3Si2O14 single crystal
H ⊥ c H // c
Macroscopic measurementsTN
02/12/2008
GDR MICO, Autrans, 2008
4
20 30 40 50 60 70 80
0
50000
100000
150000
200000
250000 T=30 K T=1.5 K 1.5 K - 30 K Calc 1.5 K
Neu
tron
coun
ts (a
. u.)
2θ (°)
D1Bλ=2.52 Å
Below TN=28 K, AF order withpropagation vector k=(0,0,∼1/7)
Fe-langasite: magnetic structureNeutron diffractionon powder (D1B), and single crystal (D15) at ILL
Powder pattern
02/12/2008
GDR MICO, Autrans, 2008
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Fe-langasite: magnetic structureHelices propagating along c120° moments on triangles
in the (a, b) plane → signature of frustration
02/12/2008
GDR MICO, Autrans, 2008
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Chirality
• Structural chirality : acentric structureX-ray (anomalous) ⇒ aenantiomorph
What about Fe-langasite?
• Chirality domains unbalanced by external constrains• Single domain in non-centrosymmetric crystals
e. g. MnSi - helical modulation and sense of rotation- due to Dzyaloshinskii-Moryia interaction
• Triangular chirality [ ]∑ ×=triangle
jiT SSCrrr
332
• Helicity [ ]jiH SSCrrr
×=
02/12/2008
GDR MICO, Autrans, 2008
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Fe-langasite: magnetic domainsDiffraction on single crystalwith unpolarized neutrons&with polarized neutron andspherical polarization analysis
-1.0 -0.5 0.0 0.5 1.0
-1.0
-0.5
0.0
0.5
1.0100% single helicity
Cal
cula
ted
PfObserved Pf
CRYOPAD (IN22, ILL)
⇒Monodomain magnetic structure(helicity & triangular chirality)
Calculated vs measured final polarization for several magnetic reflections
02/12/2008
GDR MICO, Autrans, 2008
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c axis
Mean-field analysis: probe of the microscopic mechanisms
Fe-langasite: magnetic properties
J4
J3
J5
Heisenberg Hamiltonian :super-exchange interactions2 intra-plane3 between adjacent planes
J1
J2
AF J1, J2J3 ≠ J5
02/12/2008
GDR MICO, Autrans, 2008
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c axis
Mean-field analysis: probe of the microscopic mechanisms
Fe-langasite: magnetic properties
J3
Heisenberg Hamiltonian :super-exchange interactions2 intra-plane3 between adjacent planes
⇒ Describe the magnetic structure⇒ selects two pairs of helicity and triangular chirality (CH, CT)
02/12/2008
GDR MICO, Autrans, 2008
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Link between the magnetic chiralities (CH, CT) and the structural one
2
13
Fe-langasite: magnetic properties
3’
Structure : Left handedness
Left triangular chirality
1’
2’
k=(0,0,1/6) ⇐ 60°
Right helicity
Marty et al., Phys. Rev. Lett. (in press)
02/12/2008
GDR MICO, Autrans, 2008
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Chirality and ferroelectricity
Case of RbFe(MoO4)2 : triangular lattice of Fe3+
Kenzelmann et al. PRL (2007)
120° magnetic structurebut centro-symmetric ⇒ 2 domains of magnetic chiralities∃ PE at TN ⇒ symmetry based phenomenological theoryProportional to the chirality unbalance
Conclusion :«trigonal stacked triangular antiferromagnetswith 120° structure are multiferroics.»
02/12/2008
GDR MICO, Autrans, 2008
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Fe-langasite: dielectric properties
Dielectric constantvia capacity measurementsAnomaly near TN for E ⊥ c
0 10 20 30 40
7.88
7.90
7.92
7.94
Coll. with B. Zawilsky, J. Marcus, Institut Néeland C. Simon, B. Kundys, CRISMAT, ENSICAEN
ε
T (K)
TN=27 Kν=100 kHzE⊥c
02/12/2008
GDR MICO, Autrans, 2008
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0 20000 40000 60000 80000 100000-0.01
0.00
0.01
0.02
0.03
0.04
0.05
0.06
0 10 20 30 400.0
2.0x10-12
4.0x10-12
6.0x10-12
8.0x10-12
Δε/ε
(%)
20 K 27 K 35 K
H (Oe)
B
T (K)
Δε/ε = BH2TNMagnetodielectric
couplingquadratic in HMaximum at TN
Fe-langasite: dielectric properties
02/12/2008
GDR MICO, Autrans, 2008
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Why?
Pyroelectric current measurement No evidence of spontaneous electrical polarization?
Fe-langasite: dielectric properties
...21
21
0 +−−−−= jiijjiijiiii HHEEHMEPFF χε
Results similar to YMnO3, ferroelectric at TE= 930 Kand 120° antiferromagnetic order at TN=74 K Bellido et al.
Free Energy :
lkjiijklkjiijkkjiijkiiij HHEEHEEHHEHE δγβα21
21
21
−−−−
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GDR MICO, Autrans, 2008
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ConclusionNon-centrosymmetric Ba3NbFe3Si2O14 langasite :
• Very original magnetic structure below TN=28 Ksingle triangular chirality and helicity linkedby the twist of the magnetic interactions
• Magnetodielectric coupling/ No ferroelectricity (?)
→Further investigation of dielectric properties →Many other possible chemical substitutions→Probe of the excitations
02/12/2008
GDR MICO, Autrans, 2008
16ECOLE THÉMATIQUEApport des symétries en matière condensée
Presqu'île de Giens, 11-17 mai 2009
[email protected]. Grenier UJF&CEA, GrenobleV. Simonet CNRS, GrenobleH. Schober ILL, Grenoble
Site WEB opérationnel courant juinhttp://www.ill.eu/news-events/workshops-events/ecole-theorie-des-groupes/
Programme- Formalisme de la théorie des groupes et des représentations, théorie de Landau- Applications : groupes d'espace et transitions de phase cristallographiques,
structures magnétiques, excitations (phonons, champ cristallin, …)- Exemples : multiferroïques et supraconductivité
OrateursJ. Villain, D. Fruchart, R. Ballou, B. Canals, B. Grenier, V. Simonet, P. Toledano, J. M. Perez-Mato, M. I. Aroyo, J. Rodriguez-Carvajal, F. Bourée, J. Schweizer,
M. Amara, B. Ouladdiaf, G. Eckold, J. Kreisel, S. Raymond, L. Chapon, M. Houzet
02/12/2008
GDR MICO, Autrans, 2008
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(-1,-1)(1,1)
Link between the magnetic chiralitiesand the structural one
1’
(-1,1)(1,-1)2
3’
2’
13
Fe-langasite: magnetic properties
Left handedness right handedness
02/12/2008
GDR MICO, Autrans, 2008
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0 10 20 30 40
8.7
8.8
8.9
9.0
εν=100 kHzE//c
T (K)
TN=27 K