The incommensurate modulated crystal structure of Bi2.27Sr1.73CuO6 + δ (2201) phase [a = 5.3874 (5), b = 5.3869 (4), c = 24.579 (3) Å; β = 90.01 (1)°, q = 0.2105 (3)a* + 0.538 (4)c*, Z = 4, the (3 + 1)-dimensional monoclinic A2/a(α0γ) group] has been refined with R = 0.041, wR = 0.052 from X-ray single-crystal data including up to third-order satellite reflections. The same structure has also been considered as incommensurate composite with a2 = 2.437, b2 = 5.387, c2 = 24.614, β2 = 93.06, q2 = 0.4524a2*−0.243c2* and the (3 + 1)-dimensional A2/m(α0γ)0s group for the second component. Both approaches give quite similar results. The structure possesses oxygen disorder in the oxygen-rich region of the BiO layer. An extra O atom is determined in the bridging position shifted ∼ 0.6 Å from BiO towards the SrO layer. Its presence is the cause of the tremendous increase of the bismuth U11 atomic displacement parameter in ∼ 20% of the unit cells (t = −0.05–0.15). Vacancies are determined in the oxygen site of the SrO layer, which may result in the oxygen content variation with annealing at different oxygen pressures. The total refined oxygen content 6.18 (1) corresponds to the results of chemical analysis.
Supporting information
B-IncStrDB reference: 11772EV1Tdj
CCDC reference: 1472455
Program(s) used to refine structure: Jana2000 (Petricek, Dusek & Palatinus, 2000); software used to prepare material for publication: Jana2000 (Petricek, Dusek & Palatinus, 2000).
Crystal data top
Bi2.27CuO6.18Sr1.73 | Z = 4 |
Mr = 788.5 | F(000) = 1331 |
Monoclinic, A2/a(α0γ)00† | Dx = 7.340 Mg m−3 |
q = 0.21050a* + 0.53800c* | Mo Kα radiation, λ = 0.71069 Å |
a = 5.3869 (5) Å | µ = 71.58 mm−1 |
b = 5.3874 (4) Å | T = 293 K |
c = 24.579 (3) Å | , black |
β = 90.01 (1)° | 0.46 × 0.1 × 0.01 mm |
V = 713.32 (12) Å3 | |
† Symmetry operations: (1) x1, x2, x3, x4; (2) 1/2−x1, x2, −x3, −x4; (3) −x1, −x2, −x3, −x4; (4) 1/2+x1, −x2, x3, x4; (5) x1, 1/2+x2, 1/2+x3, x4; (6) 1/2−x1, 1/2+x2, 1/2−x3, −x4; (7) −x1, 1/2−x2, 1/2−x3, −x4; (8) 1/2+x1, 1/2−x2, 1/2+x3, x4.
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Data collection top
CAD4 diffractometer | 7115 independent reflections |
Radiation source: sealed tube | 4194 reflections with I > 3σ(I) |
Graphite monochromator | |
Refinement top
Refinement on F | Weighting scheme based on measured s.u.'s w = 1/(σ2(F) + 0.000025F2) |
R[F2 > 2σ(F2)] = 0.041 | (Δ/σ)max = 0.010 |
wR(F2) = 0.052 | Δρmax = 7.01 e Å−3 |
S = 3.78 | Δρmin = −7.82 e Å−3 |
4194 reflections | Extinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974) |
241 parameters | Extinction coefficient: 0 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Uiso*/Ueq | Occ. (<1) |
Bi1 | −0.00100 (5) | 0.27368 (5) | 0.065418 (11) | 0.01539 (8) | |
Sr1 | 0.49973 (10) | 0.24779 (9) | 0.17907 (3) | 0.01935 (19) | 0.865 (3) |
Bi2 | 0.499728 | 0.247792 | 0.179067 | 0.01935 (19) | 0.135 (3) |
Cu | 0 | 0.25 | 0.25 | 0.0078 (2) | |
O1 | 0.2505 (8) | 0.5014 (8) | 0.2488 (2) | 0.0138 (11) | |
O2 | 0.0005 (15) | 0.2231 (11) | 0.1465 (2) | 0.0176 (14) | |
O3 | 0.510 (2) | 0.3424 (11) | 0.0694 (3) | 0.0261 (18) | |
O4 | 0.236 (4) | 0.519 (7) | 0.0873 (13) | 0.060 (13) | 0.123 (12) |
Atomic displacement parameters (Å2) top | U11 | U22 | U33 | U12 | U13 | U23 |
Bi1 | 0.02252 (17) | 0.01233 (11) | 0.01130 (11) | −0.00011 (12) | −0.00143 (9) | −0.0005 (1) |
Sr1 | 0.0115 (3) | 0.0089 (3) | 0.0377 (4) | −0.0003 (2) | −0.0010 (2) | −0.0029 (2) |
Bi2 | 0.0115 (3) | 0.0089 (3) | 0.0377 (4) | −0.0003 (2) | −0.0010 (2) | −0.0029 (2) |
Cu | 0.0046 (3) | 0.0033 (4) | 0.0157 (5) | 0.0001 (3) | −0.0006 (3) | 0.0005 (4) |
O1 | 0.0076 (16) | 0.0051 (17) | 0.029 (3) | −0.0042 (13) | 0.0001 (17) | −0.0004 (18) |
O2 | 0.022 (2) | 0.021 (3) | 0.010 (2) | −0.001 (2) | −0.003 (2) | 0.003 (2) |
O3 | 0.040 (4) | 0.011 (2) | 0.027 (3) | 0.004 (2) | −0.005 (3) | 0.000 (2) |
O4 | 0.020 (13) | 0.11 (3) | 0.05 (2) | 0.005 (13) | −0.011 (12) | −0.03 (2) |
Bond lengths (Å) top | Average | Minimum | Maximum |
Bi1—O2 | 2.03 (3) | 1.98 (3) | 2.12 (4) |
Bi1—O3i | 2.67 (4) | 1.75 (6) | 4.25 (6) |
Bi1—O3 | 2.80 (4) | 1.84 (6) | 4.34 (6) |
Bi1—O3ii | 3.40 (2) | 2.99 (3) | 3.75 (2) |
Bi1—O3iii | 2.15 (2) | 2.05 (2) | 2.34 (4) |
Bi1—O4 | 2.13 (3) | 2.05 (3) | 2.21 (3) |
Bi1—O4iii | 2.01 (3) | 1.89 (3) | 2.13 (3) |
Sr1—O1 | 2.577 (19) | 2.456 (18) | 2.645 (19) |
Sr1—O1iv | 2.607 (19) | 2.537 (19) | 2.688 (19) |
Sr1—O1v | 2.599 (19) | 2.480 (18) | 2.639 (18) |
Sr1—O1vi | 2.575 (19) | 2.483 (19) | 2.648 (17) |
Sr1—O2 | 2.83 (6) | 2.31 (8) | 3.86 (8) |
Sr1—O2vii | 2.82 (6) | 2.41 (8) | 3.83 (8) |
Sr1—O2viii | 2.68 (4) | 2.57 (4) | 2.77 (3) |
Sr1—O2vi | 2.97 (4) | 2.83 (4) | 3.26 (4) |
Sr1—O3 | 2.82 (3) | 2.74 (2) | 3.09 (3) |
Sr1—O4 | 2.84 (3) | 2.78 (3) | 2.90 (3) |
Sr1—O4vi | 2.77 (3) | 2.66 (3) | 2.88 (3) |
Cu—O1 | 1.916 (14) | 1.906 (13) | 1.932 (15) |
Cu—O1ix | 1.916 (14) | 1.906 (14) | 1.931 (15) |
Cu—O1v | 1.901 (14) | 1.867 (15) | 1.923 (13) |
Cu—O1iii | 1.901 (14) | 1.867 (15) | 1.923 (14) |
Cu—O2 | 2.58 (3) | 2.45 (3) | 2.69 (3) |
Cu—O2ix | 2.58 (3) | 2.45 (3) | 2.69 (3) |
O1—O1v | 2.69 (2) | 2.664 (19) | 2.73 (2) |
O1—O1x | 2.69 (2) | 2.66 (2) | 2.725 (19) |
O1—O1iii | 2.70 (2) | 2.65 (2) | 2.74 (2) |
O1—O1vi | 2.70 (2) | 2.65 (2) | 2.74 (2) |
O1—O2ix | 3.18 (4) | 2.81 (4) | 3.44 (6) |
O1—O2x | 3.17 (4) | 2.81 (4) | 3.51 (6) |
O2—O3i | 3.33 (6) | 2.85 (7) | 5.05 (9) |
O2—O3 | 3.43 (6) | 2.94 (7) | 5.11 (9) |
O2—O3iii | 3.04 (4) | 2.97 (4) | 3.14 (4) |
O2—O4 | 2.85 (7) | 2.73 (6) | 2.98 (7) |
O2—O4iii | 2.67 (7) | 2.02 (5) | 2.94 (7) |
O3—O3iii | 3.24 (5) | 2.90 (7) | 5.33 (8) |
O3—O3vi | 3.24 (5) | 2.91 (6) | 5.34 (8) |
O3—O4 | 2.63 (5) | 1.19 (4) | 2.94 (6) |
O3—O4vi | 2.66 (6) | 2.52 (5) | 2.80 (6) |
O4—O4iii | 2.70 (3) | 2.70 (3) | 2.70 (3) |
O4—O4vi | 2.70 (3) | 2.70 (3) | 2.70 (3) |
Symmetry codes: (i) x1−1, x2, x3, x4; (ii) −x1+1/2, x2, −x3, −x4; (iii) x1−1/2, −x2+1, x3, x4; (iv) −x1+1, −x2+1/2, −x3+1/2, −x4; (v) −x1+1/2, x2−1/2, −x3+1/2, −x4; (vi) x1+1/2, −x2+1, x3, x4; (vii) x1+1, x2, x3, x4; (viii) x1+1/2, −x2, x3, x4; (ix) −x1, −x2+1/2, −x3+1/2, −x4; (x) −x1+1/2, x2+1/2, −x3+1/2, −x4. |