ca-al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600...

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Electronic Supplementary Information to an article: Ca-Al double-substituted strontium hexaferrites with giant coercivity By Lev A. Trusov, Evgeny A. Gorbachev, Vasily A. Lebedev, Anastasia E. Sleptsova, Ilya V. Roslyakov, Ekaterina S. Kozlyakova, Alexander V. Vasiliev, Robert E. Dinnebier, Martin Jansen and Pavel E. Kazin Section S1. Sample characterization techniques Powder X-ray diffraction (XRD) phase analysis of all samples was performed using a Rigaku D/MAX 2500 diffractometer (CuKα radiation). For crystal structure refinement experiments we used two different devices. The spectra of samples with x = 3.5 and x = 4 was obtained at a laboratory powder diffractometer in Debye−Scherrer geometry (Stadi P-Diffraktometer, Stoe, Mo Kα1 radiation from primary Ge(111)-Johannson-type monochromator, Mythen 1 K PSD detector). The samples were sealed in a 0.5 mm diameter borosilicate glass capillary (Hilgenberg glass No. 14), which was spun during the measurement. The spectra of samples with x = 3 were collected at the beamline ID22 in European Synchrotron Radiation Facility (ESRF, Grenoble, France) in a transmission mode [A. N. Fitch, J. Res. Natl. Inst. Stand. Technol., 2004, 109, 133]. An X-ray beam with a wavelength 0.1770 Å was used. Samples were sealed in a 1.5 mm diameter kapton spinning capillary. The flat panel Perkin Elmer XRD detector (4096 × 4096 pixels of 100 × 100 μm) installed 0.38 m from the sample position was used for data collection in the q-range up to 30 Å -1 . For the following Rietveld refinement radial intensity distributions with a step 0.0049° were calculated. All spectra were taken at room temperature. The Rietveld refinement was performed with the use of Jana2006 software [V. Petricek, M. Dusek, L. Palatinus, Z. Kristallogr., 2014, 229, 345.]. Interplanar spacing ranges were 0.51 – 4 Å for synchrotron data and 0.51 – 6.7 Å for MoKα1 radiation. Background was refined with 12 Chebyshev terms. To describe the peak shape, the modified Pseudo-Voigt function was used. The Lorentzian component was refined with respect to the anisotropic microstrains component in the (0 0 1) direction. The absorbance correction was performed with respect to the refined composition. The overall sum of oxygen atoms occupancies was fixed by restrictions. ADP parameters for all oxygen positions was set to be equal. For Ca-containing samples (Series 2) the sum of Ca and Sr was fixed to be full, and ADP parameters to be equal by the restrictions. For all the samples the restrictions keep the sum of aluminum and iron occupancies to be full and their ADP parameters to be equal for each iron position separately. The synchrotron diffraction data allows to refine the overall aluminum content. The differences between the theoretical and the calculated composition was found to be less than 5%. For the MoKα1 radiation the aluminum content was fixed to be equal to the theoretical composition. Scanning electron microscopy (SEM) was performed using a LEO Supra 50 VP microscope. Magnetic data were collected using a Cryogenic S700 and a Quantum Design MPMS 7XL SQUID magnetometers in the fields up to 7 T. Curie temperatures were determined by thermogravimetric analysis in a magnetic field (NdFeB magnet) performed with Perkin Elmer Pyris Diamond instrument. Electronic Supplementary Material (ESI) for Chemical Communications. This journal is © The Royal Society of Chemistry 2017

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Page 1: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

Electronic Supplementary Information to an article:

Ca-Al double-substituted strontium hexaferrites with giant coercivity

By Lev A. Trusov, Evgeny A. Gorbachev, Vasily A. Lebedev, Anastasia E. Sleptsova,

Ilya V. Roslyakov, Ekaterina S. Kozlyakova, Alexander V. Vasiliev, Robert E. Dinnebier,

Martin Jansen and Pavel E. Kazin

Section S1. Sample characterization techniques

Powder X-ray diffraction (XRD) phase analysis of all samples was performed using a Rigaku

D/MAX 2500 diffractometer (CuKα radiation).

For crystal structure refinement experiments we used two different devices. The spectra of

samples with x = 3.5 and x = 4 was obtained at a laboratory powder diffractometer in

Debye−Scherrer geometry (Stadi P-Diffraktometer, Stoe, Mo Kα1 radiation from primary

Ge(111)-Johannson-type monochromator, Mythen 1 K PSD detector). The samples were sealed

in a 0.5 mm diameter borosilicate glass capillary (Hilgenberg glass No. 14), which was spun

during the measurement. The spectra of samples with x = 3 were collected at the beamline

ID22 in European Synchrotron Radiation Facility (ESRF, Grenoble, France) in a transmission

mode [A. N. Fitch, J. Res. Natl. Inst. Stand. Technol., 2004, 109, 133]. An X-ray beam with a

wavelength 0.1770 Å was used. Samples were sealed in a 1.5 mm diameter kapton spinning

capillary. The flat panel Perkin Elmer XRD detector (4096 × 4096 pixels of 100 × 100 μm)

installed 0.38 m from the sample position was used for data collection in the q-range up to 30

Å-1. For the following Rietveld refinement radial intensity distributions with a step 0.0049°

were calculated. All spectra were taken at room temperature.

The Rietveld refinement was performed with the use of Jana2006 software [V. Petricek, M.

Dusek, L. Palatinus, Z. Kristallogr., 2014, 229, 345.]. Interplanar spacing ranges were 0.51 – 4 Å

for synchrotron data and 0.51 – 6.7 Å for MoKα1 radiation. Background was refined with 12

Chebyshev terms. To describe the peak shape, the modified Pseudo-Voigt function was used.

The Lorentzian component was refined with respect to the anisotropic microstrains component

in the (0 0 1) direction. The absorbance correction was performed with respect to the refined

composition. The overall sum of oxygen atoms occupancies was fixed by restrictions. ADP

parameters for all oxygen positions was set to be equal. For Ca-containing samples (Series 2)

the sum of Ca and Sr was fixed to be full, and ADP parameters to be equal by the restrictions.

For all the samples the restrictions keep the sum of aluminum and iron occupancies to be full

and their ADP parameters to be equal for each iron position separately. The synchrotron

diffraction data allows to refine the overall aluminum content. The differences between the

theoretical and the calculated composition was found to be less than 5%. For the MoKα1

radiation the aluminum content was fixed to be equal to the theoretical composition.

Scanning electron microscopy (SEM) was performed using a LEO Supra 50 VP microscope.

Magnetic data were collected using a Cryogenic S700 and a Quantum Design MPMS 7XL SQUID

magnetometers in the fields up to 7 T. Curie temperatures were determined by

thermogravimetric analysis in a magnetic field (NdFeB magnet) performed with Perkin Elmer

Pyris Diamond instrument.

Electronic Supplementary Material (ESI) for Chemical Communications.This journal is © The Royal Society of Chemistry 2017

Page 2: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

Section S2. Tables

Table S1. Occupancy factors for Al3+ cation in hexaferrite sublattices.

Seriesa x 2a 2b 4f1 4f2 12k

1 3

0.65(4) 0.07(4) 0.07(2) 0.05(2) 0.34(2)

2 0.66(2) 0.08(2) 0.08(4) 0.08(5) 0.35(2)

1 3.5

0.72(1) 0.07(1) 0.12(1) 0.07(1) 0.39(1)

2 0.72(2) 0.08(2) 0.11(4) 0.07(4) 0.39(4)

1

4

0.76(1) 0.10(1) 0.14(2) 0.10(2) 0.44(2)

2 0.74(1) 0.04(1) 0.17(2) 0.10(2) 0.45(2)

Sandiumengeb 0.77(4) 0.22(4) 0.19(2) 0.20(2) 0.38(2) a SrFe12-xAlxO19 (Series 1) and Sr1-x/12Cax/12Fe12-xAlxO19 (Series 2) b F. Sandiumenge, S. Gali, J. Rodriguez, Mater. Res. Bull., 1988, 23, 685.

Section S3. Figures

Fig. S1. Lattice parameters of SrFe12-xAlxO19 (Series 1) and Sr1-x/12Cax/12Fe12-xAlxO19 (Series 2)

samples. Some parameters were taken from the literature: SrFe12O19 (X. Obradors, et al. J. Solid

State Chem., 1988, 72, 218), SrAl12O19 (Y. Goto, et al. Jpn. J. Appl. Phys., 1973, 12, 948) and

CaAl12O19 (A.M. Hofmeister, et al. Geochim. Cosmochim. Ac., 2004, 68, 4485).

0 2 4 6 8 10 12

22,0

22,2

22,4

22,6

22,8

23,0

c, A

x

Series 1

Series 2

0 2 4 6 8 10 12

5,55

5,60

5,65

5,70

5,75

5,80

5,85

5,90

a, A

x

Series 1

Series 2

Page 3: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

200 400 600 800 1000 1200 14000

20

40

60

80

Co

unt

D, nm

SrFe8Al

4O

19

Sr0.67

Ca0.33

Fe8Al

4O

19

Fig. S2. Particle diameter distributions for SrFe8Al4O19 (Series 1) and

Sr0.67Ca0.33Fe8Al4O19 (Series 2).

Page 4: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

Fig. S3a. Refined synchrotron powder X-ray diffraction patterns of the samples SrFe9Al3O19 (top)

and Sr0.75Ca0.25Fe9Al3O19 (bottom).

Gof = 2.76

Rp = 1.19 %

Rwp = 1.35 %

Rall = 1.22 %

Gof = 2.92

Rp = 1.19 %

Rwp = 1.35 %

Rall = 1.26 %

Page 5: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

Fig. S3b. Refined powder X-ray diffraction patterns of the samples SrFe8.5Al3.5O19 (top) and

Sr0.71Ca0.29Fe8.5Al3.5O19 (bottom).

Gof = 1.08

Rp = 0.98 %

Rwp = 1.26 %

Rall = 3.24 %

Gof = 1.06

Rp = 1.57 %

Rwp = 2.06 %

Rall = 3.85 %

Page 6: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

Fig. S3c. Refined powder X-ray diffraction patterns of the samples SrFe8Al4O19 (top) and

Sr0.67Ca0.33Fe8Al4O19 (bottom).

Gof = 1.02

Rp = 1.55 %

Rwp = 1.96 %

Rall = 3.34 %

Gof = 0.99

Rp = 1.12 %

Rwp = 1.4 %

Rall = 3.11 %

Page 7: Ca-Al double-substituted strontium hexaferrites with giant coercivity · 2017-12-20 · 200 400 600 800 1000 1200 1400 0 20 40 60 80 t D , nm SrFe 8 Al 4 O 19 Sr 0.67 Ca 0.33 Fe 8

0 1 2 3 4

500

550

600

650

700

750

Tc (

K)

x (Al)

Series 1

Series 2

Fig. S4. Curie temperature vs aluminum content plots of SrFe12-xAlxO19 (Series 1) and

Sr1-x/12Cax/12Fe12-xAlxO19 (Series 2).