This work was supported by the American Chemical Society
Petroleum Research Fund (39039-G3) and the National Science
Foundation (NSF-01300985).
Evgeny V. Dikarev,*a Bo Li,a Vladimir V. Chernyshev,b
Roman V. Shpanchenkob and Marina A. Petrukhina*a
aDepartment of Chemistry, University at Albany, SUNY, Albany,
New York, 12222, USA. E-mail: dikarev@albany.edu;
marina@albany.edu; Fax: +1-518-442-3462;
Tel: +1-518-442-4401 (E. V. D.) Tel: +1-518-442-4406 (M. A. P.)
bDepartment of Chemistry, Moscow State University, Moscow, 119992,
Russia
Notes and references
{ Crystal data for 1: C27H15.5ClF12N2O8Rh2, M 5 965.18, orthorhombic,
˚
Pnma (no. 62), a 5 16.3302(10), b 5 24.7253(15), c 5 8.7079(5) A,
V 5 3516.0(4) A , Z 5 4, T 5 173(2) K, m(Mo–Ka) 5 1.126 mm21, 4260
3
˚
reflections measured, 3849 unique (Rint 5 0.0550). The final R1 5 0.0595,
wR2 5 0.1437 for all data. For 2: the data were collected on an automated
˚
STADI-P (STOE) diffractometer, Cu Ka1-radiation, l 5 1.5406 A, 2h 5 6–
65.0u, step 0.01u, C16H4F12N2O8Rh2, M 5 786.03, monoclinic, C 2/c (no.
Fig. 3 The Rietveld plot of the powder diffraction pattern for
[Rh2(O2CCF3)4?C6H4(CN)2] (2) at 293 K. The observed pattern (black
crosses), the best calculated fit (red), and the difference profile (blue) are
given. The black lines at the bottom show the allowed peak positions.
˚
15), a 5 19.411(20), b 5 16.879(19), c 5 8.348(4) A, b 5 114.91(2)u,
3
˚
V 5 2481(4) A , Z 5 4, T 5 293(2) K, 438 reflections used in calculations.
The final Rp 5 0.0324, Rwp 5 0.0426, and x2 5 1.246. CCDC 266399–
graphic data in CIF or other electronic format.
important role in crystal packing due to their low p-electron
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addition, the chains undergo a shift relative to each other by ca.
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3276 | Chem. Commun., 2005, 3274–3276
This journal is ß The Royal Society of Chemistry 2005