supporting information - rutgers physics & astronomycroft/papers/203-si-mn2femoo6...powder...

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Supporting Information # Wiley-VCH 2014 69451 Weinheim, Germany Magnetic-Structure-Stabilized Polarization in an Above-Room- Temperature Ferrimagnet** Man-Rong Li, Maria Retuerto, David Walker, Tapati Sarkar, PeterW. Stephens, Swarnakamal Mukherjee, Tanusri Saha Dasgupta, Jason P. Hodges, Mark Croft, Christoph P. Grams, Joachim Hemberger, Javier SƁnchez-Benȷtez, Ashfia Huq, Felix O. Saouma, Joon I. Jang, and Martha Greenblatt* anie_201406180_sm_miscellaneous_information.pdf

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Page 1: Supporting Information - Rutgers Physics & Astronomycroft/papers/203-SI-Mn2FeMoO6...Powder synchrotron x-ray diffraction (PSXD) data were recorded on beam line X-16C (λ = 0.69991

Supporting Information

� Wiley-VCH 2014

69451 Weinheim, Germany

Magnetic-Structure-Stabilized Polarization in an Above-Room-Temperature Ferrimagnet**Man-Rong Li, Maria Retuerto, David Walker, Tapati Sarkar, Peter W. Stephens,Swarnakamal Mukherjee, Tanusri Saha Dasgupta, Jason P. Hodges, Mark Croft,Christoph P. Grams, Joachim Hemberger, Javier S�nchez-Ben�tez, Ashfia Huq, Felix O. Saouma,Joon I. Jang, and Martha Greenblatt*

anie_201406180_sm_miscellaneous_information.pdf

Page 2: Supporting Information - Rutgers Physics & Astronomycroft/papers/203-SI-Mn2FeMoO6...Powder synchrotron x-ray diffraction (PSXD) data were recorded on beam line X-16C (λ = 0.69991

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SUPPORTING INFORMATIOIN

Full information of References [3], [4], [7] and [13a]:

[3] J. Wang, J. B. Neaton, H. Zheng, V. Nagarajan, S. B. Ogale, B. Liu, D. Viehland, V.

Vaithyanathan, D. G. Schlom, U. V. Waghmare, N. A. Spaldin, K. M. Rabe, M. Wuttig, R.

Ramesh, Science 2003, 299, 1719-1722

[4] N. Ikeda, Ohsumi, K. Ohwada, K. Ishii, T. Inami, K. Kakurai, Y. Murakami, K. Yoshii, S.

Mori, Y. Horibe, H. Kitô, Nature 2005, 436, 1136-1138.

[7] T. Varga, A. Kumar, E. Vlahos, S. Denev, M. Park, S. Hong,T. Sanehira, Y. Wang, C. J. Fennie, S. K.

Streiffer,X. Ke, P. Schiffer, V. Gopalan, & J. F. Mitchell, Phys. Rev. Lett. 2009, 103, 047601.

[13a] M. R. Li, D. Walker, M. Retuerto, T. Sarkar, J. Hadermann, P. W. Stephens, M. Croft, A. Ignatov,

C. P. Grams, J. Hemberger, I. Nowik, P. S. Halasyamani, T. T. Tran, S. Mukherjee, T. Saha-Dasgupta, M.

Greenblatt, Angew. Chem. 2013, 125, 8564-8568; Angew. Chem. Int. Ed. 2013, 52, 8406-8410.

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Content

1. Cation Ordering in Corundum Derivatives

2. High Pressure Synthesis and Powder Synchrotron X-ray and Neutron Diffraction Studies

3. Second Harmonic Generation Measurements

4. X-ray Absorption Near-Edge Spectroscopy

5. Magnetic, Magnetotransport, and Electrical Conductivity Properties Measurements

6. Theoretical Calculations

7. Dielectric and Polarization Measurements

1. Cation Ordering in Corundum Derivatives

The crystal structure of corundum-type (A2O3) oxides consists of hexagonal close packing

of the oxygen atoms, where the metal atoms occupy two-thirds of the octahedral sites, the

remaining one-third of the octahedral sites are vacant (Fig. S1a).1-3

Each AO6 octahedron shares

edges with three other AO6 octahedra to form an intralayer edge-sharing (ES) infinite sheet in the

ab plane which is 2/3 occupied and 1/3 vacant. The intralayer ES octahedral sheets are bonded to

form a three-dimensional structure via interlayer face-sharing (FS) to form octahedral pairs along

the c direction, these pairs corner share with the edge-sharing slabs of alternative layers. The

metal atoms near the center of FS octahedral pairs tend to displace away in opposite directions

towards the vacant sites in order to reduce the electrostatic repulsions.

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(a) Corundum (R-3c)

(b) Ilmenite (R-3) (c) LiNbO3 (R3c)

(d) Ordered ilmenite (R3) (e) Ni3TeO6 (R3)

Intralayer ES

Interlayer FS

AO6/BO6

BO6

AO6

A1O6/A2O6

BO6/B O6

A1A2

A1O6/BO6

A2O6/B O6

Fig. S1 Cation ordering tree in corundum-related phases with (a) A2O3-type corundum;

(b) ABO3-type ilmenite; (c) ABO3-type LiNbO3; (d) A2BB´O6-type ordered ilmenite, and

(e) A2BB´O6-type Ni3TeO6 crystal structures viewed along the [110] direction.

Octahedral color: carmine, AO6; purple, BO6; cyan, B´O6.

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Given the same corundum-type rhombohedral stacking of octahedra, different crystal

structures can be derived when the octahedral metal sites are occupied by more than one distinct

cation (similar to the double perovskite related A2BB´O6). Fig. S1 shows the cation ordering tree

in corundum-derived systems, including ilmenite (IL), LiNbO3 (LN), ordered IL (OIL), and

Ni3TeO6 type structures,2,4,5

where the FS octahedral pairs along the c axis are formed by two

different cation octahedra. The crystal structures are highly strained: stretched in the ab plane

and compressed in the c direction due to the electrostatic repulsions between the cations across

the ES and FS octahedral pairs, respectively.

1.1 IL and LN type Structures

The IL and LN structures have two distinct cation-orderings in ABO3. IL adopts a

centrosymmetric R-3 space group, built by alternating ES AO6 and BO6 octahedral layers in the

ab plane stacked via FS between unlike A and B cations (Fig. S1b). While in the non-

centrosymmetric LN structure (R3c), the ES octahedral layers consist of both AO6 and BO6

octahedra to avoid intralayer ES between identical cations (Fig. S1c). The number of reports on

related phases increased in the past years, but because of the requirement of relatively high

pressures for their preparation, these systems are far less explored than normal ABO3 perovskites.

1.2 Ordered Ilmenite and Ni3TeO6-type Structures

The A2BB´O6 system is more complex (than IL and LN ABO3), as an additional ordering

parameter is introduced into the B-sites. The crystal structure transforms to either OIL or

Ni3TeO6 type. Generally, B´ has a higher oxidation state than B; A is typically a monovalent-to-

trivalent cation. So far, only a few compounds have been reported in this system: Li2GeTeO6 is

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the only phase with OIL structure bearing some B-site cationic disorder, which results in

Li2[(Ge0.82Te0.18)B(Te0.82Ge0.18)B’]O6.2 Several Ni3TeO6-type compounds were reported with

A+

2B4+

B´6+

O6,6 A

2+2B

2+B´

6+O6,

4,5 A

2+2B

3+B´

5+O6,

7 and A

3+2B

2+B´

4+O6

8 formulae, all of which

contain an ion with electronic configuration (n-1)d10

ns0 such as Ge

4+,8 Sb

5+,7 and Te

6+,4-6

at the

B'-site. Compared with IL, the OIL (R3) has two crystallographically independent A cations

(designated as A1 and A2). The ES layers are formed by either A or B octahedra and the

intralayer ordering gives cystallographically unlike neighbors in ES A1O6/A2O6 layers and ES

BO6/B'O6 layers (Fig. S1d), respectively. The interlayer FS A1O6/B'O6 and A2O6/BO6

octahedral pairs form A1-B'-A2-B columns parallel to the c axis. As shown in Fig. S1d, the A

cations displace away from their FS partner cations (A1-B'; A2-B) toward opposite directions

along the c axis; this displacement is largely responsible for the two crystallographically

different A-site positions due to the size and charge difference between B and B’ cations. The

Ni3TeO6 structure is a close derivate of the LN structure; compared with OIL it has additional

intralayer octahedral ordering to avoid ES between like A or B cations, and thus forming

alternative stacking of A1O6/BO6 and A2O6/B'O6 octahedral layers in the ab-plane (Fig. S1e).

The cation ordering in corundum derivatives is complex and can be driven by many factors,

including the cationic size and charge difference, structural tolerance factor (t), electron

configuration, and synthesis condition. The larger the size or charge difference between the

cations, the greater is the chance of ordering. The corundum-derived ABO3 and A2BB'O6

systems can be regarded as highly distorted perovskite-related structures with very small

tolerance factor (t) values9, due to the unusually small size of A cations. The A-site 12-fold

coordination of the ideal perovskite structure transforms to an octahedral 6-fold coordination.

These structures are highly distorted and compact, most are metastable at ambient pressure and

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often require very high pressure for their synthesis. 10-12

For example, some IL-type structures

transform into LN-polymorphs under higher pressure.13,14

Another important effect on the cation

ordering is the electronic configuration. For example, Mn2FeMO6 (M = Nb5+

and Ta5+

, d0

,)

adopt a polar LN structure,12

while Mn2Fe3+

Sb5+

O6 (Sb5+

, d10

) a non-polar IL structure. We

believe the latter behavior is due to the absence of a second-order Jahn-Teller d0 cation at the B’-

sites, which favors distortion of the octahedra.11

Generally, the cation ordering is affected by the competition and/or combination of several

factors for the lowest energy of the system, and the real outcome can be complicated and subtle

case by case. For example, both Bi2FeCrO6 and Bi2FeTiO6 were predicted to stabilize in the

Ni3TeO6 structure.15,16

However, Bi2FeCrO6 prepared under HP crystallizes in the LN structure

(R3c),11

while Bi2FeTiO6 has not been experimentally prepared yet.17

2. High Pressure Synthesis and Powder Synchrotron X-ray and Neutron Diffraction Studies

Polycrystalline Mn2FeMoO6 was prepared from stoichiometric mixtures of MnO (99.99%,

Alfa Aesar), Fe (99.999%, Alfa Aesar), Fe2O3 (99.999%, Sigma Aldrich) and MoO3 (99.998%

Alfa Aesar) under high pressure. The oxide mixture was placed in a Pt capsule, pressurized

typically over 8-12 hours, and reacted at 1623 K under 8 GPa for 30 minutes in a LaCrO3 heater

inside a MgO crucible in a multi-anvil press,18

and then quenched to RT by turning off the

voltage supply to the resistance furnace, which reduced the temperature to RT in a few seconds.

The pressure is maintained during the temperature quenching and then decompressed in 8-12

hours. Powder synchrotron x-ray diffraction (PSXD) data were recorded on beam line X-16C (λ

= 0.69991 Å) at the National Synchrotron Light Source (NSLS), Brookhaven National

Laboratory (US). Powder neutron diffraction (PND) data were collected at 10 and 300 K on

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~220 mg sample at the POWGEN instrument in the Spallation Neutron Source in the Oak Ridge

National Laboratory (US). Diffraction data analysis and Rietveld refinements19

were performed

with the TOPAS software package20

and EXPGUI interface of GSAS programs21

.

Original powder synchrotron x-ray diffraction (PSXD) data can be indexed to either

centrosymmetric R-3 or noncentrosymmetric R3 cell, corresponding to IL (R-3), OIL (R3), or

Ni3TeO6 (R3) type structure. Although the two space groups have the same reflection conditions,

Rietveld refinements on PSXD data indicated unambiguously the non-centrosymmetric Ni3TeO6

structure based on the structural model in Ref. 4. More important than the relatively small

difference in the refinement statistics (Rwp = 7.72% (OIL), 7.29% (Ni3TeO6), and 8.62% (IL))

was the fact that the IL and OIL structural models yielded unrealistic atomic displacement

parameters. The Ni3TeO6-type structure was further reinforced by combined PSXD and PND

refinements attributed to the different counting of the electron and neutron scattering ability

(electron numbers for PSXD: ZMn = 25, ZFe = 26, ZMo = 42, ZO = 8; neutron scattering lengths for

PND: bc,Mn = -3.73 × 10-15

m; bc,Fe = 9.45 × 10-15

m, bc,Mo = 6.715 × 10-15

m; bc,O = 5.803 × 10-15

m), as totally unacceptable fitting of the 300 K data in IL (χ2 = 21.28, Rp/Rwp = 10.99/10.50%)

and OIL (χ2 = 26.17, Rp/Rwp = 14.75/11.75%) models obtained. The final refined plots from

Ni3TeO6 structure are presented in Fig. S2 (combined PSXD and PND refinements on 300 K

data (χ2 = 1.91, Rp/Rwp = 7.69/3.04%)) and Fig. S3 (PND data at 10 K (χ

2 = 2.33, Rp/Rwp =

3.73/1.99%), the fitting and crystallographic parameters are listed in Table S1. Selected

interatomic distances and bond angles are listed in Table S2. There are two crystallographically

independent Mn atoms (Mn1 and Mn2) occupying the A-sites (3a, (0 0 z)), and Fe (3a, (0 0 z))

and Mo (3a, (0 0 0)) are ordered over the B-sties. The oxygen atoms are driven to two positions

(9h (x ,y ,z)) due to the higher degree of cation ordering compared with that of the IL structure.

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The anti-site disorder was also refined (constrained to the initial stoichiometry Fe : Mo = 1 : 1), by

assuming that some Fe can randomly replace Mo atoms, and vice versa, giving ~7% of Fe/Mo

disordering. The octahedral chains in the crystal structure of Mn2FeMoO6 are connected to form

infinite octahedral slabs (thickness ~3.4 Å, Fig. S4, left) via corner-sharing between Mn1O6-

MoO6 and Mn2O6-FeO6 neighboring chains (Fig. S4, right). The zigzag chains and slab packing

leave vacancies right above and below the face-shared octahedral pairs, which favor the

stabilization of the structure.

The octahedral distortions (Figures 1b and c) lead to three short and three long metal-

oxygen bonds for each metal site (Table S2), with the average <Mn1-O> and <Mn2-O>

distances of 2.195(3) Å at RT, which are comparable to those of the MnO6 octahedra in the

corundum derivatives, Mn22+

FeSbO6 (2.173 Å)10

and Mn22+

FeMO6 (M = Nb (2.16 Å) and Ta

(2.22 Å))12

. The <Fe-O> distance (2.033(4) Å) is also comparable to octahedral <Fe-O> in

similar phases as in Mn22+

Fe3+

SbO6 (2.006 Å)10

and Mn2Fe3+

MO6 (M = Nb (2.030 Å) and Ta

(2.012 Å));12

the <Mo- O> average distance (2.008(2) Å) is larger than in other related ordered

double perovskites, e.g., Sr2FeMoO6 where it is 1.947 Å22

, which indicates a lower oxidation

state of Mo in Mn2FeMoO6 compared to the ordered double perovskite where Mo is considered

5+/6+ mixed valent23

. The crystal structure at 10 K is similar to that at 300 K, but with smaller

unit cell and atomic displacement parameters as expected.

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2θ (degree, λ = 0.69991 Å)10 20 30 40

Inte

nsi

ty (

a.u

.)

2 4 6 8D-space (Å)

Inte

nsi

ty (

a.u

.)

1 2 3

Inte

nsi

ty (

a.u

.)

(a)

(b)

(c)

Fig. S2 Experimental, calculated, and difference of (a) PSXD and (b-c) PND patterns of

Mn2FeMoO6 at 300 K, corresponding to the combined refinements in Ni3TeO6-type

structure. In (b) and (c) PND data are from the low and high D-spacing banks,

respectively. The vertical bars (│) show the peak index of vanadium (sample can), and

nuclear and magnetic structure, respectively, from top to bottom.

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10

Fig. S3 Experimental, calculated, and difference of PND patterns of Mn2FeMoO6 at 10

K, corresponding to the refinements in Ni3TeO6-type structure. (a) and (b): PND data

from low and high D-spacing banks, respectively. Inset of (b) shows the peak intensity

differences of data at 10 and 300 K due to the evolution of the magnetic structure. The

vertical bars (│) show the peak index of vanadium (sample can), and nuclear and

magnetic structure, respectively, from top to bottom.

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Table S1 Atomic parameters and agreement factors after the Rietveld refinements of

PND (10 K) and combined PND and PSXD (300 K) data of Mn2FeMoO6 in Ni3TeO6-type

structure (rhombohedral, space group of R3 (No. 146), Z = 3).

Temperature/K 10 300

a/Å

c/Å

V/Å3

Mn1 (3a, 0 0 zp)

zp

Uiso (× 100)/Å2

Mag. mom./µB

Mn2 (3a, 0 0 zp)

zp

Uiso (× 100)/Å2

Mag. mom./µB

(Fe/Mo)1 (3a, 0 0 zp)

Occ.

zp

Uiso (× 100)/Å2

Mag. mom./µBiii

(Mo/Fe)2 (3a, 0 0 0)

Occ.

Uiso (× 100)/Å2

Mag. mom./µBiii

O1 (9b, xp yp zp)

5.2394(1)

13.8305(2)

328.8(1)

0.2258(6)

0.71(2) i

+4.0(3)

0.7144(7)

0.71(2) i

-3.8(2)

0.93(1)/0.07(1)

0.4995(8)

0.71(2) i

+3.4(5)

0.93(1)/0.07(1)

0.71(2) i

-1.1(1)

5.2505(1)

13.8355(1)

330.3(1)

0.2175(2)

0.99(2) i

+1.8(7)

0.7160(2)

0.99(2) i

-1.8(7)

0.93(1)/0.07(1)

0.4949(4)

0.99(2) i

+1.1(9)

0.93(1)/0.07(1)

0.99(2) i

-0.3(9)

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xp

yp

zp

Uiso (× 100)/Å2

O2 (9b, xp yp zp)

xp

yp

zp

Uiso (× 100)/Å2

Rp/wRp/% (PND #1)

Rp/wRp/% (PND #2)

Rp/wRp/% (SXRD)

Rp/wRp/% (Total)

RMag

χ2

0.0338(12)

0.3120(7)

0.0996(5)

0.52(2)ii

0.0410(12)

0.7121(12)

0.6007(5)

0.52(2)ii

2.93/1.68

4.19/3.12

-

3.73/1.99

2.15

2.33

0.0376(1)

0.3198(1)

0.0976(2)

1.00(2)ii

0.0417(1)

0.7164(1)

0.5975(2)

0.98(2)ii

3.14/1.95

4.66/3.74

7.84/10.29

7.69/3.04

5.91

1.91

i Uiso for all cations are constrained to be the same value during refinements of 10 and

300 K data, respectively; ii Uiso for all oxygen atoms are constrained to be the same

value during refinements of 10 and 300 K data, respectively; iii The moments on Fe and

Mo are constrained to be 5.92 : 1.73 according to the expected full spin moments.

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Table S2 Selected bond lengths (Å), octahedral distortion parameters (Δ), atomic bond

valence sums (BVS), and bond angles (º) of crystal structure of Mn2FeMoO6 at 10 and

300 K, respectively

10 K 300 K

Selected bond lengths (Å)

Mn1O6

Mn1-O1 × 3

-O2 × 3

<Mn1-O>

ΔMn1 (× 10-3

)i

BVS

2.337(9)

2.055(7)

2.196(8)

4.12

2.14

2.298(3)

2.093(2)

2.195(3)

2.18

2.08

Mn2O6

Mn2-O1 × 3

-O2 × 3

<Mn2-O>

ΔMn2 (× 10-3

) i

BVS

2.108(6)

2.262(9)

2.185(8)

1.24

2.11

2.093(1)

2.298(3)

2.195(3)

2.18

2.08

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(Fe/Mo)1O6

(Fe/Mo)1-O1 × 3

-O2 × 3

<(Fe/Mo)1-O>

Δ(Fe/Mo)1 (× 10-3

) i

BVS

1.961(7)

2.146(9)

2.054(6)

2.03

2.89

1.920(3)

2.146(4)

2.033(4)

3.09

3.10

(Mo/Fe)2O6

(Mo/Fe)2-O1 × 3

-O2 × 3

<(Mo/Fe)2-O>

Δ(Mo/Fe)2 (× 10-3

) i

BVS

2.076(7)

1.897(5)

1.986(7)

2.03

4.85

2.085(2)

1.931(2)

2.008(2)

1.47

4.56

Selected bond angles (º)

O1-Mn1-O1

O2-Mn1-O2

O1-Mn1-O2

70.3(3)

112.5(3)

80.3(3)

73.6(1)

110.9(1)

79.9(1)

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87.2(3)

147.5(3)

88.2(1)

151.1(2)

O1-Mn2-O1

O2-Mn2-O2

O1-Mn2-O2

109.0(3)

77.0(3)

78.9(3)

89.9(3)

154.6(4)

110.3(1)

74.7(1)

79.3(1)

89.1(1)

152.1(2)

O1-(Fe/Mo)1-O1

O2-(Fe/Mo)1-O2

O1-(Fe/Mo)1-O2

99.8(4)

82.1(3)

87.4(4)

89.4(4)

167.2(4)

100.4(2)

81.0(1)

87.8(1)

89.0(1)

166.0(2)

O1-(Mo/Fe)2-O1

O2-(Mo/Fe)2-O2

O1-(Mo/Fe)2-O2

80.8(2)

98.8(3)

88.7(3)

90.3(3)

82.6(1)

97.6(1)

88.5(1)

90.3(1)

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167.1(3) 169.3(1)

Mn1-O1-Mn2

-(Fe/Mo)1

-(Mo/Fe)2

Mn1-O2-Mn2

-(Fe/Mo)1

-(Mo/Fe)2

122.6(3)

93.3(3)

89.9(3)

118.4(4)

96.6(3)

117.0(3)

120.9(1)

95.4(1)

86.6(1)

119.6(1)

95.1(2)

116.9(1)

Mn2-O1-(Fe/Mo)1

-(Mo/Fe)2

Mn2-O2-(Fe/Mo)1

-(Mo/Fe)2

115.4(4)

95.5(3)

84.7(3)

95.8(3)

116.1(1)

96.1(1)

86.9(2)

94.1(1)

(Fe/Mo)1-O1-(Mo/Fe)2 140.4(4) 140.2(1)

(Fe/Mo)1-O2-(Mo/Fe)2 140.6(4) 141.7(1)

i The octahedral distortion parameter Δ is defined as Δ = 1/6Σ{(d -dav)/dav}2, where d and

dav denote the individual interatomic distance and the average distance, respectively. 24

In the well-known polar LiNbO325, ΔLi = 1.8 × 10-3, ΔNb = 4.0 × 10-3.

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Mo

Mn1

Fe

Mn2

Fig. S4 Octahedral slab (thickness of ~3.4 Å) in the crystal structure of Mn2FeMoO6

viewed along the [-110] (left) and the [110] (right) directions, respectively, to show the

octahedral zigzag chains by edge-sharing connection of face-shared octahedral pairs

along the c-axis. Mn1O6, blue; Mn2O6, yellow; FeO6, carmine; MoO6, light green; O1,

red; O2, deep purple.

3. Second Harmonic Generation Measurements

Broadband SHG experiments were conducted at RT on a powder sample26

. The

fundamental beam covering a wide wavelength range ( = 1100 – 2000 nm) was produced from

an optical parametric oscillator at increments of 100 nm, which was synchronously pumped by

an Nd:YAG laser with a pulse width of 30 ps and a repetition rate of 50 Hz. The input irradiance

was about 0.7 GW/cm2 and the SHG signals (SHG = /2 = 550–1000 nm) were collected with a

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reflection geometry by a fiber-optic bundle, which was coupled to a spectrometer equipped with

a charge-couple device camera. Surface-induced SHG as well as SHG signals from other optical

components were negligible. The relative SHG signals (Fig. S5) spectrally resolved in a broad

wavelength range were precisely calibrated with the known and measured efficiencies of all

optical components to produce the wavelength-dependent SHG response.

Fig. S5 Wavelength-dependent SHG spectra of Mn2FeMoO6

4. X-ray Absorption Near-Edge Spectroscopy

X-ray absorption near-edge spectra (XANES) were collected on the beam line X-19A at

Brookhaven NSLS, to confirm the formal oxidation state of the cations. Mn and Fe spectra were

collected in both transmission and fluorescence modes with simultaneous standards. The Mo

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XANES was collected in fluorescence mode in a He-atmosphere-chamber with standards run in

temporal proximity. The main edge features at 3-d transition metal K edges are dominated by 1s

to 4p transitions. These features, and the step- continuum onset which lies underneath them,

manifest a chemical shift to higher energy with increasing valence. The 4p features can also be

split into multiple features by the local atomic coordination/bonding and by final state effects (i.e.

admixed 3d configurations). The chemical shift of the K edge has been widely used to chronicle

the evolution of the transition metal valence state in oxide-based materials.12,27-34

.

In Fig. S6a-c, the Mn- and Fe-K edges are compared to a series of standard compounds.27-

29 The nominal proximity of the main edge rise for various formal valence states is indicated by a

square in the figures. It is worth noting that the MnO and FeO standards (with edge sharing

Mn/Fe-O octahedra) manifest a robust two feature rise and the chemical shift is identified (here)

roughly with the inflection point between the two. The less structured steeply rising Mn-K edge

of the Mn2FeMoO6 exhibits a chemical shift consistent with MnO, which is the Mn2+

standard

and are clearly much lower in energy than the Mn3+

and Mn4+

standards. Thus, the formal

oxidation state at the Mn sites in this compounds is consistent with Mn2+

. Similarly, the chemical

shift for the Fe-K edge for Mn2FeMoO6 (Fig. S6b) falls in the formal Fe3+

valence range. The Fe

K-pre-edge region (7.11-7.12 KeV, Fig. S6c) is shown on an expanded scale. The features in the

pre-edge are quadrupole and dipole (through p-d hybridization) allowed transitions into final

states with 3d character. The onset energy and structure of the pre-edge features are typically

coupled to the transition metal valence. The Fe-K pre-edge features of Mn2FeMoO6 occurs at an

energy comparable to that of the Fe~3+

standards and intermediate between those of the Fe2+

and

Fe~4+

standards. This provides additional support for the Fe~3+

state in this material.

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(a) (b)

(c) (d)

Fig. S6 XANES spectra of Mn2FeMoO6. The Mn-K edge spectra (a) along with a series

of octahedral O-coordinated Mn compounds with varying formal valences: Mn2+O,

Mn2+2FeNbO6 , LaMn3+O3, and CaMn4+O3; the Fe-K edge spectra (b) and its pre-edge

region (c) along with a series of octahedral O-coordinated Fe compounds with varying

formal valences: Fe2+O, LiFe2+PO4, LaSrFe~3+O4, Mn2Fe~3+NbO6 and SrFe~4+O3; the

Mo-L3 edge (d) compared to reference edges for elemental Mo, the pyrochlore

Sm2Mo2O7 (Mo4+~4d2), the double perovskite SrMo0.5Fe0.5O3 (Mo5+~4d1) and, the

(Mo6+~4d0) MoO3 and the quadruple perovskite Sr4Fe3MoO12 (Mo6+~4d0). Here the

formal valence is used ignoring more subtle hybridization/covalency effects.

Fig. S6d shows the Mo L3-edges for Mn2FeMoO6 along with a number of standard spectra.

The intense peak features at the L3-edges of 4d transition metals involve dipole allowed 2p-core

to 4d final-state transitions. These features can provide a probe of the empty 4d state energy

distribution, albeit modified by the transition matrix element, core–hole interaction and multiplet

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effects.35-37

The transition metal d-states are split by the octahedral coordination ligand- field into

lower energy, t2g (sextet) and a higher energy eg (quartet) states. In low-d-occupancy transition

metal ions like Mo5+

(d1), the T L3-edges display a robust two peak structure with the lower

energy peak (A) involving transitions into empty t2g states; and the high-energy peak (B)

involving excitations into empty eg states. For d-hole counts greater than 4, the B-feature

intensity reflects the empty eg states and the intensity of the A-feature scales with the number of

t2g-holes. Thus the A-feature intensity, relative to that of the B-feature, provides an indicator of

the T 4d count/valence state. This trend can be seen in the Mo4+

/d2, Mo

5+/d

1, and Mo

6+/d

0

standard spectra sequence. The relative A/B feature intensity of the Mn2FeMoO6 spectrum places

it in the nominally Mo5+

/d1 configuration regime. Comparing to the conventionally synthesized

perovskite, SrMo0.5Fe0.5O3,35

one notes that the t2g-eg ligand field splitting in the Mn2FeMoO6

compound is substantially larger resulting in a larger/better resolved A-B feature splitting. Thus,

the formal oxidation states of Mn2+

2Fe3+

Mo5+

O6 were manifested. Here, the d1-electron

configuration of Mo5+

is ascribed to the formation of Ni3TeO6-type structure compared with the

Nb5+

and Ta5+

(d0-electron configuration) analogs, which adopt the polar LN-type structure.

12

5. Magnetic, Magnetotransport Properties, and Electrical Conductivity Measurements

Magnetization measurements were carried out with a commercial Quantum Design

superconducting quantum interference device (SQUID) magnetometer. The susceptibility was

measured in zero field cooled (ZFC) and field cooled (FC) conditions under a 0.1 T magnetic

field, for temperatures ranging from 5 to 400 K. Isothermal magnetization curves were obtained

at T = 5-300 K under an applied magnetic field varied from -5 to 5 T. The dc electrical

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conductivity properties were measured on the pellet sample with the standard four probe

technique in a physical property measurement system (PPMS) from Quantum Design. The

magnetotransport properties were measured on the pellet sample with the standard four probe

technique in a physical property measurement system (PPMS) from Quantum Design. To avoid

the Joule heating effect, measurements were carried out with less than 0.5 μA current. The

magnetoresistance is defined as)0(

)0()(100)(

R

RHRHMR

, where R(H) is the resistivity at applied

magnetic field H and R(0) is the resistivity without magnetic field. The magnetotransport

properties were measured between -9 and 9 T at 100 and 300 K, respectively, showing a

maximum negative magnetoresistance about -2% and -2.5% at 9 T at 300 and 100 K,

respectively as shown in Fig. S7, thus enhance the multifunctional properties of this material.

Fig. S7 Magnetoresistance measurements results of Mn2FeMoO6 with magnetic field

between 0 and 9 T,showing maximum negative magnetoresistance of about -2.5% and -

2% at 9 T for 100 and 300 K, respectively.

-8 -6 -4 -2 0 2 4 6 8

0.0

0.5

1.0

1.5

2.0

2.5

3.0

-MR

(%

)

H (T)

100 K

300 K

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6. Theoretical Calculations

The theoretical calculations have been performed within the generalized gradient

approximation (GGA)38

of the exchange-correlation functional with the choice of Perdew-Burke-

Ernzerhof (PBE) functional39

in a spin polarized scheme. To improve the description of

correlation effects in Mn and Fe-d electrons, a DFT+U40-42

method within the Dudarev et al.’s

approach was used. We have varied the U value between 4-8 eV at Fe and Mn sites and between

1-4 eV at Mo site, with a choice of Hund's coupling constant, JH = 0.8 eV. The variation did not

produce significant changes in the result. The calculations were performed in plane wave basis as

implemented in Vienna Ab-initio Simulation Package (VASP)43

. For these plane wave

calculations, we used projector augmented wave (PAW) potentials44

and the wave functions

were expanded in the plane wave basis with a kinetic energy cutoff of 600 eV. Reciprocal space

integrations were carried out with a k mesh of 5 x 5 x 5.

Calculations of electronic and magnetic structure have been carried out using the

generalized gradient approximation (GGA) of density functional theory (DFT), supplemented

with Hubbard U correction (GGA+U) to take care of strong electron-electron correlation at the

transition metal sites, as implemented in plane wave based Vienna Ab-initio Simulation code45

.

The calculated spin-polarized electronic structure, with chosen U values of 5 eV at the 3d

transition metal sites, Mn and Fe, and 2 eV at the 4d transition metal site of Mo, shows Fe and

Mn d-dominated states to be fully filled in the majority spin channels and empty in the minority

spin channel, while Mo d states to be partially filled in one of the spin channel, and empty in

other. The calculated electron configuration and dp hybridization are found to hold good for a

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variation of U value between 4-8 eV at the 3d transition metal sites (Mn and Fe), 1-4 eV at the

4d transition metal (Mo) site, confirming the robustness of the obtained results.

The ferromagnetic solution with spins of Mn, Fe, Mo all aligned parallel are found to be

energetically unfavorable by a large energy difference of about 300 meV compared to the

ferrimagnetic solution where the spins of two nonequivalent Mn sites (Mn1 and Mn2) are

aligned antiparallel. The lowest energy magnetic structure, turned out to be the ferrimagnetic

structure with spins of Mn1 and Fe aligned parallel, which are antiparallel to the spins of Mn2

and Mo, giving rise to layers of ferromagnetically ordered Mn1 and Fe, coupled

antiferromagnetically to the next layer of ferromagnetically ordered Mn2 and Mo, in perfect

agreement with the magnetic structure obtained from PND data analysis. This magnetic

structure, cited as up-up-down-down (along the zig-zag chain) in the following, is found to be

energetically lower compared to the ferrimagnetic solution with antiparallel alignment of Mn1

and Mn2, and parallel alignment of Fe and Mo, (up-up-down-up) by an energy difference of

about 80 meV. This suggests a very strong antiferromagnetic exchange between Mn1 and Mn2

and a moderately strong antiferromagnetic exchange between Fe and Mo, mediated via the

corner sharing super-exchange paths. We also computed the polarization, for the insulating

solution assuming perfect ordering of Fe and Mn, in ground state magnetic configuration, using

Berry phase formalism46,47

.

Mn2FeMoO6 lacks any (n-1)d10

ns0 or d

0 ion, and adopts the polar Ni3TeO6 structure

instead of others in the corundum family shown in Fig. S1, breaking the polarization rules in

perovskite-related oxides. As far as we know, to date, all known polar perovskite-related and

corundum based compounds, including the above LN, ordered IL, and Ni3TeO6 structures,

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contain at least an (n-1)d10

ns0 electronic configuration ion at the A-site (such as Zn

2+ in

ZnSnO325

, Sc3+

in ScFeO348

, and In3+

in (In1-xMx)MO3 (M = Fe0.5Mn0.5)49

), or B-site (such as Ge4+

in La2MgGeO68, Sb

5+ in Ni2InSbO6 and Ni2ScSbO6,

7 and Te

6+ in Ni3TeO6 and Li2ZrTeO6

4-6), or

a lone pair electron ion at the A-site (such as Bi3+

in BiFeO350

and Pb2+

in PbVO351

), or a SOJT

ion at the B-site (such as Nb5+

and Ta5+

in Mn2+

2Fe3+

M5+

O6 (M = Nb, Ta)12

and W6+

in

NaLaFeWO652

), no polarization was observed in oxides without any of the above ions, which

either favor the essential hybridization between the metal nd and oxygen 2p states53

, or provide

stereoactive lone pair electrons such as the 6s2 lone pair electron in Bi

3+ in BiFeO3

50. As far as

we knew, the polar ε-Fe2O3 is an exception but the crystal structure is different from

perovksite/corundum and contains mixed FeO6 and FeO4 coordination environment54-66

.

We calculated the total energy of different possible structural arrangements (Fig. S1) to

reveal the reason for the formation of the Ni3TeO6 structure. In order to check the influence of

disorder on the electronic structure, we considered three different configurations in a supercell,

which is three times the primitive unit cell, namely (i) perfect ordering (Fe-Mo-Fe-Mo-Fe-Mo),

(ii) segregation (Fe-Fe-Fe-Mo-Mo-Mo), and (iii) mixed configuration (Fe-Fe-Mo-Fe-Mo-Mo).

Our total energy calculations suggest that the ordered arrangement of Fe and Mo [case (i)] is

preferred over the segregated arrangement of Fe-Mo [case (ii)] by a large energy difference of

about 600 meV/f.u., and by an energy difference of about 150 meV/f.u. over the mixed

configuration [case (iii)] when the magnetism is turned on. This result is evidence for the

important role of magnetism in the finite d configuration of Fe and Mo in stabilizing the

observed Ni3TeO6 structure, which allows for two nonequivalent positions of B and B' ions. Note

that ilmenite (R-3) or LiNbO3 (R3c) structures do not allow for two nonequivalent positions of B

and B'. The Ni3TeO6 structure is also found to be stable over the ordered ilmenite (R3) structure

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by about 30 meV/f.u., which arises due to the large size mismatch between the ionic sizes of

Mn2+

in octahedral environment (~0.83 Å) and that of Fe3+

or Mo5+

(0.65 and 0.61 Å,

respectively)67

. In the ordered ilmenite structure Mn1-Mn2 edge share within the layer, while in

Ni3TeO6, the unlike atoms, e.g. Mn1 and Fe, edge share within the layer.

7. Dielectric and Polarization Measurements

Dielectric measurements were carried out in two-point geometry. For these investigations

polycrystalline pellets were prepared as plate-like capacitors with typical area of 4 mm2, a

thickness of 0.5 mm and silver-paint electrodes. For the spectroscopic measurements in the

frequency range from 1 Hz < < 1 MHz a frequency response analyzer [Novocontrol] was

utilized; the polarization measurements at low temperatures were carried out in a Sawyer-Tower

circuit using an electrometer (Keithley 6517) and linear E-field ramping with a frequency of one

cycle per minute.

At high temperatures the dielectric properties are completely determined by the finite

conductivity', which effectively is connected to the measured imaginary part of the complex

permittivity ' = 20''. In addition to the experimental obstacles to perform polarization or

pyro-current measurements in this conductive regime, and to precisely determine ' in the

presence of a large dielectric loss '', one has to consider further intrinsic and non-intrinsic

contributions to the dielectric response. On the one hand the presence of VRH as demonstrated in

in Figure 3 will lead to a contribution to the real part of the permittivity ' 68,69

. On the other hand

heterogeneities in the sample, i.e. grain boundaries and electrodes (contacts) will lead to highly

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capacitive depletion layers, which (like Schottky diodes) give rise to highly dispersive dielectric

response as they form effective RC-elements 68,69

. Measurements of the complex dielectric

permittivity are shown in Fig. S9. The high values of ' for high temperatures and small

frequencies are accompanied by much higher values in '' denoting the influence of sample

conductivity together with non-intrinsic resistivities and capacitances of contacts and grain

boundaries. Nevertheless, one can try to evaluate the resulting effective conductivity as it is

shown in Fig. S8 in the vicinity of the magnetic phase transition. The data is presented as

Arrhenius-plot ln'(1/T) between 295 and 385 K to demonstrate the thermally activated nature of

Fig. S8 Logarithm of the conductivity measured at 1 Hz (left scale) and magnetization

measured in a field of 0.1 T (right scale) plotted vs reciprocal temperature. The linear

regions above and below the magnetic transition temperature of 337 K are fitted

assuming thermal activation with an energy barrier .

0.0026 0.0028 0.0030 0.0032 0.0034

-3.0

-2.5

-2.0

-1.5

' ~ e-/(k

BT)

/kB= 1830 K

ln(

'(S

/m))

1/T (1/K)

/kB= 2135 K

385 K 333 K 295 K

0.0

0.1

0.2

0.3

M (

B/f

.u.)

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Fig. S9 Real (upper frame) and imaginary (lower frame) part of the complex permittivity

* vs temperature as measured in zero magnetic field for frequencies between 1 Hz and

1 MHz. the inset shows a P(E)-curve measured with a frequency of one cycle per

minute.

the transport in this temperature regime. At the ferrimagnetic transition (which in Fig. S8 is

nicely denoted by the onset of spontaneous magnetization) the effective energy barrier changes:

102

103

'

0 100 200 300

100

103

106

1 Hz ... 1 MHz

''

T (K)

-200 -100 0 100 200-100

0

100

T = 2 KP

(C

/m2)

E (V/mm)

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29

in the magnetically ordered regime the energy barrier is lowered. This meets the evaluation of

the magneto-resistive properties of the previous section, even though the details of this effect, e.g.

the role of inter-grain contacts, cannot be elucidated at this point.

For low temperatures and high frequencies the impact of the residual conductivity on the

dielectric properties is reduced. On cooling, the large values for ' drop via two steps (due to

electrode and inter-grain contacts) towards the intrinsic value of ε'which still is a relatively

high value compared to other transition metal oxides. In this low temperature regime the residual

conductivity ' vanishes and the dielectric loss '' becomes much smaller than ' Therefore it is

possible to conduct direct polarization measurements. The inset of Fig. S9 displays a P(E)-loop

measured at 2 K in fields up to 170 V/mm. No hint towards a ferroelectric component can be

found as denoted e.g. via switchable or at least non-linear polarization. However, these findings

do not exclude the presence of possible structurally induced pyroelectricity in the polycrystalline

sample.

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