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77is

Fig. 1.17. Representation of the molecular orbitals of carbon monoxide. Energies are given in atomic units (1 a.u. 27.21 eV). (From W L. Jorgensen and L. Salem, 77i Organic Chemist s Book of Orbitals, Academic Press, New York, 1973. Reproduced wifli permission.)... Fig. 1.17. Representation of the molecular orbitals of carbon monoxide. Energies are given in atomic units (1 a.u. 27.21 eV). (From W L. Jorgensen and L. Salem, 77i Organic Chemist s Book of Orbitals, Academic Press, New York, 1973. Reproduced wifli permission.)...
Find the number of atoms, N, in the sample from N = 77i(sample)//H(atom). [Pg.837]

Other hand, when an equimolar mixture of 2,5-DSP and l OEt is recrystallized from benzene, yellow crystals, comprising 2,5-DSP and l OEt in a molar ratio of 1 2, deposit. In the DSC curve of this crystal, a single endothermic peak is observed at 166°C, which is different from the melting point of either 2,5-DSP (223°C) or l OEt (156°C). Furthermore, the X-ray powder diffraction pattern of the crystal is quite different from those of the homocrystals 2,5-DSP and l OEt. Upon irradiation the cocrystal 2,5-DSP-l OEt affords a crystalline polymer (77i h = 1.0 dl g in trifluoroacetic acid). The nmr spectrum of the polymer coincides perfectly with that of a 1 2 mixture of poly-2,5-DSP and poly-1 OEt. In the dimer, only 2,5-DSP-dimer and l OEt-dimer are detected by hplc analysis, but the corresponding cross-dimer consisting of 2,5-DSP and l OEt is not detected at all (Hasegawa et al., 1993). These observations by nmr and hplc indicate that the photoproduct obtained from the cocrystal 2,5-DSP-l OEt is not a copolymer but a mixture of poly-2,5-DSP and poly-l OEt in the ratio 1 2. [Pg.167]

The fluxes of POC determined by the " Th method applied to the world s oceans are summarized in Table 1. Where possible we have tabulated the ratio of Th-derived POC export to independent estimates of primary production. As noted above, this ratio, termed the 77i ratio (Buesseler 1998), is important in the euphotic zone carbon balance as it represents the leakage of POC out of the euphotic zone (The ThE ratio is so named to evoke the e ratio, which is defined as the ratio of POC flux measured with sediment traps to primary production). [Pg.476]

Viscasil (10,000) Witcamide 511 Tween 61 Hoechst Wax OP Ross Ozokerite 77Y Isopar M Part B ... [Pg.118]


See other pages where 77is is mentioned: [Pg.393]    [Pg.287]    [Pg.360]    [Pg.410]    [Pg.58]    [Pg.104]    [Pg.946]    [Pg.62]    [Pg.118]    [Pg.309]    [Pg.135]    [Pg.220]    [Pg.101]    [Pg.289]    [Pg.313]    [Pg.45]    [Pg.169]    [Pg.51]    [Pg.42]    [Pg.355]    [Pg.99]    [Pg.101]    [Pg.53]    [Pg.196]    [Pg.360]    [Pg.756]    [Pg.112]    [Pg.36]    [Pg.209]    [Pg.1154]    [Pg.85]    [Pg.88]    [Pg.149]    [Pg.846]    [Pg.228]    [Pg.1567]    [Pg.103]    [Pg.86]    [Pg.114]    [Pg.123]    [Pg.193]    [Pg.661]    [Pg.662]    [Pg.188]    [Pg.184]   
See also in sourсe #XX -- [ Pg.363 ]




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