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RbCa2Nb3O10 from X-ray powder data

aDepartment of Chemistry, University of Science and Technology of China, Hefei, Anhui 230026, People's Republic of China, and bDepartment of Nanomaterials and Nanochemistry, Hefei National Laboratory for Physical Sciences at Microscale, University of Science and Technology of China, Hefei, Anhui 230026, People's Republic of China
*Correspondence e-mail: kbtang@ustc.edu.cn

(Received 7 May 2009; accepted 13 May 2009; online 23 May 2009)

Rubidium dicalcium triniobate(V), RbCa2Nb3O10, has been synthesized by solid-state reaction and its crystal structure refined from X-ray powder diffraction data using Rietveld analysis. The compound is a three-layer perovskite Dion–Jacobson phase with the perovskite-like slabs derived by termination of the three-dimensional CaNbO3 perovskite structure along the ab plane. The rubidium ions (4/mmm symmetry) are located in the inter­stitial space.

Related literature

For the synthesis of RbCa2Nb3O10, see: Dion et al. (1981[Dion, M., Ganne, M. & Tournoux, M. (1981). Mater. Res. Bull. 16, 1429-1435.]). For related three-layer Dion–Jacobson analogues, see: CsCa2Nb3O10 (Dion et al., 1984[Dion, M., Ganne, M. & Tournoux, M. (1984). Rev. Chim. Mineral. 21, 92-103.]); RbSr2Nb3O10 (Thangadurai et al., 2001[Thangadurai, V., Beurmann, P. S. & Weppner, W. J. (2001). Solid State Chem. 158, 279-289.]); KCa2Nb3O10 (Fukuoka et al., 2000[Fukuoka, H., Isami, T. & Yamanaka, S. (2000). J. Solid State Chem. 151, 40-45.]). For the application of Dion–Jacobson phases, see: Thangadurai et al. (2001[Thangadurai, V., Beurmann, P. S. & Weppner, W. J. (2001). Solid State Chem. 158, 279-289.]); Li et al. (2007[Li, L., Ma, R., Ebina, Y., Fukuda, K., Takada, K. & Sasaki, T. (2007). J. Am. Chem. Soc. 129, 8000-8007.]); Ida et al. (2008[Ida, S., Ogata, C., Eguchi, M., Youngblood, W. J., Mallouk, T. E. & Matsumoto, Y. (2008). J. Am. Chem. Soc. 130, 7052-7059.]); Compton & Osterloh (2009[Compton, O. C. & Osterloh, F. E. (2009). J. Phys. Chem. C., 113, 479-485.]). For properties of RbCa2Nb3O10, see: Thangadurai & Weppner (2001[Thangadurai, V. & Weppner, W. (2001). Ionics, 7, 22-31.], 2004[Thangadurai, V. & Weppner, W. (2004). Solid State Ionics, 174, 175-183.]); Byeon et al. (2003[Byeon, S. H., Kim, H. J., Kim, D. K. & Hur, N. H. (2003). Chem. Mater. 15, 383-389.]).

Experimental

Crystal data
  • RbCa2Nb3O10

  • Mr = 604.34

  • Tetragonal, P 4/m m m

  • a = 3.85865 (6) Å

  • c = 14.9108 (3) Å

  • V = 222.01 (1) Å3

  • Z = 1

  • Cu Kα radiation

  • T = 298 K

  • Specimen shape: flat sheet

  • 10 × 15 × 1 mm

  • Specimen prepared at 1423 K

  • Particle morphology: plate-like, white

Data collection
  • PANalytical X'pert PRO diffractometer

  • Specimen mounting: packed powder pellet

  • Specimen mounted in reflection mode

  • Scan method: continuous

  • 2θmin = 10.0, 2θmax = 110.0°

  • Increment in 2θ = 0.02°

Refinement
  • Rp = 0.035

  • Rwp = 0.053

  • Rexp = 0.008

  • S = 2.54

  • Wavelength of incident radiation: 1.54178 Å

  • Profile function: pseudo-Voigt

  • 238 reflections

  • 26 parameters

  • Preferred orientation correction: March–Dollase (Dollase, 1986[Dollase, W. A. (1986). J. Appl. Cryst. 19, 267-272.]) AXIS 1 Ratio = 0.95964, h = k = 0, l = 1; correction range: min = 0.94007, max = 1.13156

Data collection: X'pert Data Collector (PANalytical, 2003[PANalytical (2003). X'pert Data collector. PANalytical BV, Almelo, The Netherlands.]); cell refinement: GSAS (Larson & Von Dreele, 2000[Larson, A. C. & Von Dreele, R. B. (2000). GSAS. Los Alamos National Laboratory, New Mexico, USA.]) and EXPGUI (Toby, 2001[Toby, B. H. (2001). J. Appl. Cryst. 34, 210-213.]); data reduction: X'pert Data Collector; method used to solve structure: coordinates taken from an isotypic compound (Thangadurai et al., 2001[Thangadurai, V. & Weppner, W. (2001). Ionics, 7, 22-31.]); program(s) used to refine structure: GSAS and EXPGUI; molecular graphics: VESTA (Momma & Izumi, 2008[Momma, K. & Izumi, F. (2008). J. Appl. Cryst. 41, 653-658.]); software used to prepare material for publication: publCIF (Westrip, 2009[Westrip, S. P. (2009). publCIF. In preparation.]).

Supporting information


Comment top

The Dion-Jacobson phase which was first discovered by Dion et al. (1981), has a general formula A'[An-1BnO3n+1], where A'is a monovalent ion, A is a divalent alkaline earth metal ion and B is a tetravalent or pentavalent transition metal ion. Related crystal structures of three-layer Dion-Jacobson phase have been reported for KCa2Nb3O10 (Dion et al., 1984), RbSr2Nb3O10 (Thangadurai et al., 2001), and KCa2Nb3O10 (Fukuoka et al., 2000). Although the three-layer Dion-Jacobson phase RbCa2Nb3O10 was first synthesized by Dion et al. (1981), its crystal structure has not yet been reported. The structure of RbCa2Nb3O10 has now been refined by the Rietveld method from powder diffraction data in the present communication.

The observed, calculated and intensities difference plots of the Rietveld refinement are shown in Fig. 1. There are some 00 l preferential orientation which were often observed in the Rietveld refinement of the layered perovskites. Then we applied the March-Dollase option for a correction in the EXPGUI program and obtain the best result finally.

The structure of the compound is illustrated in Fig. 2. The structure consists of three layers of corner-sharing NbO6 octahedra that run perpendicular to the c axis; adjacent sets of layers are staggered.

Table 1 shows refined interatomic distances and angles for the RbCa2Nb3O10 structure. The octahedra forming the inner layer are less distorted with Nb—O distances ranging from 1.876 (7) to 1.92932 (3)Å (Table 2), which is typical for layered perovskites involving Nb(V). As it is well known in layered perovskites, the NbO6 octahedra forming the outer layer of the slabs are characterized by off-centering of the Nb atoms, leading to four equal equatorial Nb—O distances within the perovskite layers [1.9663 (11) Å], a short Nb—O bond toward the interlayer spacing [1.650 (8) Å], and a long opposite Nb—O bond [2.379 (7) Å]. Such a distortion is quite similar to that encountered in homologous niobates and tantalates where the niobium shows an out-of-plane distortion, moving away from the more positively charged calcium towards the rubidium layer. Similar behavior has been observed in a number of d0 systems containing niobium, tantalum, and titanium. This has been attributed to a second-order Jahn-Teller effect. Concerning the interlayer, the rubidium ions are coordinated with eight terminal oxygen atoms to form the same eight Rb—O bonds [3.318 (4) Å]. These distances, as for the Ca—O bonds [2.560 (4)–2.9207 (22) Å] are close to those commonly observed in layered perovskites.

Related literature top

For the synthesis of RbCa2Nb3O10, see: Dion et al. (1981). For related three-layer Dion–Jacobson analogues, see: CsCa2Nb3O10 (Dion et al., 1984); RbSr2Nb3O10 (Thangadurai et al., 2001); KCa2Nb3O10 (Fukuoka et al., 2000). For the application of Dion–Jacobson phases, see: Thangadurai et al. (2001); Li et al. (2007); Ida et al. (2008); Compton et al. (2009). For properties of RbCa2Nb3O10, see: Thangadurai & Weppner (2001); Byeon et al. (2003); Thangadurai & Weppner (2004).

Experimental top

RbCa2Nb3O10 powders were prepared by a conventional solid state reaction described previously (Byeon et al., 2003). All starting materials were of analytical grade and were used without further purification. Stoichiometric amounts of CaCO3 and Nb2O5 with a 50% molar excess of Rb2CO3 were mixed together and heated in air at 1423 K for 24 h (heating rate 5 K /min). The calcination procedure was repeated one time after grinding to ensure a complete reaction. A 50% molar excess of Rb2CO3 was used in the reaction to offset the volatilization of the alkali oxides at the synthesis temperature. The products were washed thoroughly with distilled water to remove excess alkali oxides, and were then dried at 393 K overnight.

Refinement top

All peaks of the XRD pattern could be indexed on a tetragonal cell and the systematic absences show simple tetragonal symmetry. The P4/mmm crystal structure of RbSr2Nb3O10 (Thangadurai et al., 2001) was used as a starting model for the Rietveld refinement of the structure of RbCa2Nb3O10. The corresponding isotropic atomic displacement parameters of all oxygen atoms are constrained to be equal. The March-Dollase option in the EXPGUI program was applied to correct 00 l preferential orientation which were often observed in the Rietveld refinement of the layered perovskites.

Computing details top

Data collection: X'pert Data Collector (PANalytical, 2003); cell refinement: GSAS (Larson & Von Dreele, 2000) and EXPGUI (Toby, 2001); data reduction: X'pert Data Collector (PANalytical, 2003); program(s) used to solve structure: coordinates taken from an isotypic compound (Thangadurai et al., 2001); program(s) used to refine structure: GSAS (Larson & Von Dreele, 2000) and EXPGUI (Toby, 2001); molecular graphics: VESTA (Momma & Izumi, 2008); software used to prepare material for publication: publCIF (Westrip, 2009).

Figures top
[Figure 1] Fig. 1. Rietveld difference plot for the multi-phase refinement of RbCa2Nb3O10. The red crosses, and green and pink lines show respectively the observed, calculated and difference plots. Calculated Bragg reflection positions are indicated by black lines for the RbCa2Nb3O10 phase.
[Figure 2] Fig. 2. The crystal structure of RbCa2Nb3O10. blue octahedron show NbO3 units with Nb5+ cations as black spheres and O2- anions as red spheres. Large green spheres represent Ca2+ cations and large blue spheres Rb+ cations.
Rubidium dicalcium triniobate(V) top
Crystal data top
RbCa2Nb3O10Dx = 4.520 Mg m3
Mr = 604.34Cu Kα radiation, λ = 1.54178 Å
Tetragonal, P4/mmmT = 298 K
Hall symbol: -P 4 2Particle morphology: plate-like
a = 3.85865 (6) Åwhite
c = 14.9108 (3) Åflat sheet, 10 × 15 mm
V = 222.01 (1) Å3Specimen preparation: Prepared at 1423 K
Z = 1
Data collection top
PANalytical X'pert PRO
diffractometer
Data collection mode: reflection
Radiation source: sealed tubeScan method: continuous
Graphite monochromator2θmin = 10.008°, 2θmax = 109.985°, 2θstep = 0.017°
Specimen mounting: packed powder pellet
Refinement top
Refinement on F2? data points
Least-squares matrix: fullProfile function: pseudo-Voigt
Rp = 0.03526 parameters
Rwp = 0.0530 restraints
Rexp = 0.008 w = 1/[σ2(Fo2) + (0.0677P)2]
where P = (Fo2 + 2Fc2)/3
R(F2) = 0.08530(Δ/σ)max = 0.020
χ2 = 6.452Preferred orientation correction: March–Dollase (Dollase, 1986) AXIS 1 Ratio= 0.95964, h = k = 0, l = 1. Prefered orientation correction range: min = 0.94007, Max = 1.13156
Crystal data top
RbCa2Nb3O10V = 222.01 (1) Å3
Mr = 604.34Z = 1
Tetragonal, P4/mmmCu Kα radiation, λ = 1.54178 Å
a = 3.85865 (6) ÅT = 298 K
c = 14.9108 (3) Åflat sheet, 10 × 15 mm
Data collection top
PANalytical X'pert PRO
diffractometer
Scan method: continuous
Specimen mounting: packed powder pellet2θmin = 10.008°, 2θmax = 109.985°, 2θstep = 0.017°
Data collection mode: reflection
Refinement top
Rp = 0.035χ2 = 6.452
Rwp = 0.053? data points
Rexp = 0.00826 parameters
R(F2) = 0.085300 restraints
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/Ueq
Rb10.50.50.50.0433 (8)*
Ca10.50.50.14706 (19)0.0281 (8)*
Nb10.00.00.00.0127 (6)*
Nb20.00.00.28537 (8)0.0134 (5)*
O10.00.50.00.0716 (14)*
O20.00.00.1258 (5)0.0716 (14)*
O30.00.50.2599 (4)0.0716 (14)*
O40.00.00.3960 (6)0.0716 (14)*
Geometric parameters (Å, º) top
Rb1—O43.138 (4)Ca1—O32.560 (4)
Rb1—O4i3.138 (4)Ca1—O3ii2.560 (4)
Rb1—O4ii3.138 (4)Ca1—O3iv2.560 (4)
Rb1—O4iii3.138 (4)Ca1—O3v2.560 (4)
Rb1—O43.138 (4)Nb1—O1vi1.9293 (1)
Rb1—O43.138 (4)Nb1—O11.9293 (1)
Rb1—O43.138 (4)Nb1—O1vii1.9293 (1)
Rb1—O43.138 (4)Nb1—O1iv1.9293 (1)
Ca1—O12.921 (2)Nb1—O21.877 (7)
Ca1—O1ii2.921 (2)Nb1—O21.877 (7)
Ca1—O1iv2.921 (2)Nb2—O22.379 (7)
Ca1—O1v2.921 (2)Nb2—O3vi1.9663 (11)
Ca1—O22.7468 (9)Nb2—O31.9663 (11)
Ca1—O2i2.7468 (9)Nb2—O3vii1.9663 (11)
Ca1—O2ii2.7468 (9)Nb2—O3iv1.9663 (11)
Ca1—O2iii2.7468 (9)Nb2—O41.650 (8)
O1vi—Nb1—O1180.0O1iv—Nb1—O290.0
O1vi—Nb1—O1vii90.0O2—Nb1—O2180.0
O1vi—Nb1—O1iv90.0O3vi—Nb2—O3157.8 (3)
O1vi—Nb1—O290.0O3vi—Nb2—O3vii87.87 (6)
O1vi—Nb1—O290.0O3vi—Nb2—O3iv87.87 (6)
O1—Nb1—O1vii90.0O3vi—Nb2—O4101.12 (16)
O1—Nb1—O1iv90.0O3—Nb2—O3vii87.87 (6)
O1—Nb1—O290.0O3—Nb2—O3iv87.87 (6)
O1—Nb1—O290.0O3—Nb2—O4101.12 (16)
O1vii—Nb1—O1iv180.0O3vii—Nb2—O3iv157.8 (3)
O1vii—Nb1—O290.0O3vii—Nb2—O4101.12 (16)
O1vii—Nb1—O290.0O3iv—Nb2—O4101.12 (16)
O1iv—Nb1—O290.0
Symmetry codes: (i) x, y+1, z; (ii) x+1, y, z; (iii) x+1, y+1, z; (iv) y+1, x, z; (v) y+1, x+1, z; (vi) x, y1, z; (vii) y, x, z.

Experimental details

Crystal data
Chemical formulaRbCa2Nb3O10
Mr604.34
Crystal system, space groupTetragonal, P4/mmm
Temperature (K)298
a, c (Å)3.85865 (6), 14.9108 (3)
V3)222.01 (1)
Z1
Radiation typeCu Kα, λ = 1.54178 Å
Specimen shape, size (mm)Flat sheet, 10 × 15
Data collection
DiffractometerPANalytical X'pert PRO
diffractometer
Specimen mountingPacked powder pellet
Data collection modeReflection
Scan methodContinuous
2θ values (°)2θmin = 10.008 2θmax = 109.985 2θstep = 0.017
Refinement
R factors and goodness of fitRp = 0.035, Rwp = 0.053, Rexp = 0.008, R(F2) = 0.08530, χ2 = 6.452
No. of data points?
No. of parameters26

Computer programs: X'pert Data Collector (PANalytical, 2003), GSAS (Larson & Von Dreele, 2000) and EXPGUI (Toby, 2001), coordinates taken from an isotypic compound (Thangadurai et al., 2001), VESTA (Momma & Izumi, 2008), publCIF (Westrip, 2009).

 

Acknowledgements

The authors are grateful for financial support by the National Natural Science Foundation of China, the 973 Projects of China and the Program for New Century Excellent Talents in Universities (NCET).

References

First citationByeon, S. H., Kim, H. J., Kim, D. K. & Hur, N. H. (2003). Chem. Mater. 15, 383–389.  Web of Science CrossRef CAS Google Scholar
First citationCompton, O. C. & Osterloh, F. E. (2009). J. Phys. Chem. C., 113, 479–485.  Web of Science CrossRef CAS Google Scholar
First citationDion, M., Ganne, M. & Tournoux, M. (1981). Mater. Res. Bull. 16, 1429–1435.  CrossRef CAS Web of Science Google Scholar
First citationDion, M., Ganne, M. & Tournoux, M. (1984). Rev. Chim. Mineral. 21, 92–103.  CAS Google Scholar
First citationDollase, W. A. (1986). J. Appl. Cryst. 19, 267–272.  CrossRef CAS Web of Science IUCr Journals Google Scholar
First citationIda, S., Ogata, C., Eguchi, M., Youngblood, W. J., Mallouk, T. E. & Matsumoto, Y. (2008). J. Am. Chem. Soc. 130, 7052–7059.  Web of Science CrossRef PubMed CAS Google Scholar
First citationFukuoka, H., Isami, T. & Yamanaka, S. (2000). J. Solid State Chem. 151, 40–45.  Web of Science CrossRef CAS Google Scholar
First citationLarson, A. C. & Von Dreele, R. B. (2000). GSAS. Los Alamos National Laboratory, New Mexico, USA.  Google Scholar
First citationLi, L., Ma, R., Ebina, Y., Fukuda, K., Takada, K. & Sasaki, T. (2007). J. Am. Chem. Soc. 129, 8000–8007.  Web of Science CrossRef PubMed CAS Google Scholar
First citationMomma, K. & Izumi, F. (2008). J. Appl. Cryst. 41, 653–658.  Web of Science CrossRef CAS IUCr Journals Google Scholar
First citationPANalytical (2003). X'pert Data collector. PANalytical BV, Almelo, The Netherlands.  Google Scholar
First citationThangadurai, V., Beurmann, P. S. & Weppner, W. J. (2001). Solid State Chem. 158, 279–289.  Web of Science CrossRef CAS Google Scholar
First citationThangadurai, V. & Weppner, W. (2001). Ionics, 7, 22–31.  Web of Science CrossRef CAS Google Scholar
First citationThangadurai, V. & Weppner, W. (2004). Solid State Ionics, 174, 175–183.  Web of Science CrossRef CAS Google Scholar
First citationToby, B. H. (2001). J. Appl. Cryst. 34, 210–213.  Web of Science CrossRef CAS IUCr Journals Google Scholar
First citationWestrip, S. P. (2009). publCIF. In preparation.  Google Scholar

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