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Côté, A. P.; Benin, A. I.; Ockwig, N. W.; O'Keeffe, M.; Matzger, A. J.; Yaghi, O. M. Science 2005, 310, 1166.
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Yaghi, O.M.6
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El-Kaderi, H. M.; Hunt, J. R.; Mendoza-Cortés, J. L.; Côté, A. P.; Taylor, R. E.; O'Keeffe, M.; Yaghi, O. M. Science 2007, 316, 268.
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35848970681
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2: C, 74.68; H, 3.13. Found: C, 75.08; H, 3.39.
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2: C, 74.68; H, 3.13. Found: C, 75.08; H, 3.39.
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8
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35848946908
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2 Modeling Environment, version 4.2; Molecular Simulations Incorporated: San Diego, CA, 1999
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2 Modeling Environment, version 4.2; Molecular Simulations Incorporated: San Diego, CA, 1999.
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35848936842
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Larson, A. C.; VonDreele, R. B. General Structure Analysis System (GSAS); Los Alamos National Laboratory Report LAUR 86-748, Los Alamos, NM, 2004. Residual factors: COF-8: Rp = 0.0780, wRp = 0.0911. COF-10: Rp = 0.1383, wRp = 0.2114. COF-12; Rp = 0.0467, wRp = 0.0632.
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Larson, A. C.; VonDreele, R. B. General Structure Analysis System (GSAS); Los Alamos National Laboratory Report LAUR 86-748, Los Alamos, NM, 2004. Residual factors: COF-8: Rp = 0.0780, wRp = 0.0911. COF-10: Rp = 0.1383, wRp = 0.2114. COF-12; Rp = 0.0467, wRp = 0.0632.
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10
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35848940391
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It is a multiplicity of possibilities in which COF-8 and -12 can stack and pattern where HHTP stack against BTPA/BPBA (turbostratic disorder) which is crystallographically indistinguishable from PXRD/adsorption data; the tailing to high angle of the (100) lines points to translation faults in the xy basal planes. This feature does not preclude nor detract from the application of COFs as porous materials. Due to its large unit cell parameters, the (100) line of COF-10 appears at a very low angle (2θ = 2.8°) and overlaps with scattering from the X-ray source, resulting in an anomalous tailing to low angle of (100) peak and poorer fit of the Le Bail profile in this region (Figure 2).
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It is a multiplicity of possibilities in which COF-8 and -12 can stack and pattern where HHTP stack against BTPA/BPBA (turbostratic disorder) which is crystallographically indistinguishable from PXRD/adsorption data; the tailing to high angle of the (100) lines points to translation faults in the xy basal planes. This feature does not preclude nor detract from the application of COFs as porous materials. Due to its large unit cell parameters, the (100) line of COF-10 appears at a very low angle (2θ = 2.8°) and overlaps with scattering from the X-ray source, resulting in an anomalous tailing to low angle of (100) peak and poorer fit of the Le Bail profile in this region (Figure 2).
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12
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33751062346
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COF-18A was prepared using similar procedures to that COFs-1 and -5: Tilford, W. R.; Gemmil, W. R.; zur Loye, H.-C.; Lavigne, J. J. Chem. Mater. 2006, 18, 5296.
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COF-18A was prepared using similar procedures to that COFs-1 and -5: Tilford, W. R.; Gemmil, W. R.; zur Loye, H.-C.; Lavigne, J. J. Chem. Mater. 2006, 18, 5296.
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