Indigo-blue exists as a pure phase only in the solid state, melting at approximately . Reed and Lipscomb discovered that single crystals become polycrystalline due to a phase transformation when cooled below . Therefore, extensive powder diffraction experiments, using the modified Guinier technique, were performed in order to optimize crystal growth conditions. The samples, prepared from and NO, showed a very complex behaviour (Figure 1). Depending on temperature and thermal treatment we were able to identify six different powder diagrams besides those of .
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| Figure 1: Investigation with the modified Guinier technique of containing samples which were sealed in X-ray cappilaries under vacuum (I) and 1 bar NO (II), respectively. Arrows indicate directions of temperature changes (numbers in ; dotted lines for T changes without X-ray observations, full lines for simultaneous X-ray diffraction). Cooling always starts from room temperature, k and m denote the diagrams of cubic and monoclinic , respectively. Diagrams A to D are observed together with those of in contrast to diagrams E and F. |
Above approximately the intense powder lines of the cubic diagram k of occur with all samples. After quenching to , diagram k is observed at when the amorphous sample (I) is slowly heated up. A little later, diagram A of appears in addition. Obviously, crystallizes easier than . Therefore, it is surprising that with both a quenched or a slowly cooled sample (II), respectively, the diagrams (E,F) after crystallization of the amorphous phase do not show any lines of . At in both cases the cubic diagram of (k) together with diagram B of is developed. These results are best explained with the existence of at least one hitherto unknown oxide below , the composition of which has to be between and . Diagrams A to D obviously belong to different modifications of .
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| Figure 2: Projection of the orthorhombic unit cell of (phase B). The distances and angles are: N1-N2 = 189.06(6), N1-O1 = 111.96(6), N2-O2 = 120.87(6), N2-O3 = 120.57(5); O1-N1-N2 = 105.12(4), O2-N2-O3 = 128.61(5), Co2-N2-N1 = 119.55(4), O3-N2-N1 = 111.84(3) |
A single crystal of was grown after the compound had been enriched locally in the sample by zone melting. Probably this is the reason why a crystal of phase B grew, in spite of the fact that in powder diagrams phase A was reproducibly observed in the same temperature range. Figure 2 shows a projection of the structure on (100) of the orthorhombic unit cell. As had been proposed early and supported by IR-, Raman- and NMR-experiments, has to be described as nitroso-nitro compound. There are only slight changes in geometric details determined in the solid state compared to the molecular shape as revealed from microwave spectra in the gas phase. Especially the very long N-N distance (189.1 pm) is rather close to the value (186.4 pm) in the gas phase, and represents a Pauling bond order of about 0.2. A formal description as nitrosyl nitrite is also supported by the N-O distances and the O-N-O angle (N1-O1=112 pm compared to 115 pm in NO and 106.5 pm in and O-N-O=128.6 in comparison with 118 pm and 134.3 in or 124 pm and in , respectively). The molecule is almost planar; on the average the atoms are only 1.5 pm off the least squares plane. However, as the angles around N2 are adding up to exactly , this deviation is mainly due to the position of O1, which lies 7.8 pm above the plane through N1, N2, O2 and O3 (mean deviation 0.3 pm). The nitrosyl group is therefore tilted by around the N-N bond relative to the nitrite unit. The planarity of was explained as a consequence of bonding interaction between oxygen atoms. This explanation seems also reasonable for as the O-O distance in is even shorter than in , despite the longer N-N distance. Recently published quantum mechanical calculations of the electronic structure of were performed for the planar geometry without further explanation. The calculated N-N distances are 10-15% shorter than the experimental value for all basis sets tested.
(A. Simon, J. Horakh, A. Obermeyer, H. Borrmann)
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