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Vibrational spectroscopy room-temperature

Figure 7. Total internal reflection sum frequency generation (TIR-SFG) vibrational spectroscopy of high-pressure room temperature adsorption of carbon monoxide on PVP-protected Pt cube monolayers and calcined (373 K, 3h) monolayers [27], The infrared spectra demonstrate CO is adsorbed at atop sites, but is considerably red-shifted on the PVP-protected Pt cubes. After calcination, the atop frequency blueshifts to 2085 cm in good agreement with CO adsorption on Pt(l 0 0) at high coverages [28], (Reprinted from Ref [27], 2006, with permission from American Chemical Society.)... Figure 7. Total internal reflection sum frequency generation (TIR-SFG) vibrational spectroscopy of high-pressure room temperature adsorption of carbon monoxide on PVP-protected Pt cube monolayers and calcined (373 K, 3h) monolayers [27], The infrared spectra demonstrate CO is adsorbed at atop sites, but is considerably red-shifted on the PVP-protected Pt cubes. After calcination, the atop frequency blueshifts to 2085 cm in good agreement with CO adsorption on Pt(l 0 0) at high coverages [28], (Reprinted from Ref [27], 2006, with permission from American Chemical Society.)...
At room temperature the thermal population of vibrational excited states is low, although not zero. Therefore, the initial state is the ground state, and the scattered photon will have lower energy than the exciting photon. This Stokes shifted scatter is what is usually observed in Raman spectroscopy. Figure la depicts Raman Stokes scattering. [Pg.241]

While the BC configuration for the B—H complex is now accepted, several aspects of the vibrational spectra of the acceptor-H complexes are not understood. The temperature dependence of the B—H complex has been examined by Raman spectroscopy (Stutzmann and Herrero, 1987) and IR absorption (Stavola et al., 1988a). The H-stretching vibration shifts from 1875 to 1903 cm 1 between room temperature and liquid He temperature. Frequency shifts of just a few cm 1 are more typical for local vibrational modes. The vibrational bands are also surprisingly broad. [Pg.162]

The theory of electron-transfer reactions presented in Chapter 6 was mainly based on classical statistical mechanics. While this treatment is reasonable for the reorganization of the outer sphere, the inner-sphere modes must strictly be treated by quantum mechanics. It is well known from infrared spectroscopy that molecular vibrational modes possess a discrete energy spectrum, and that at room temperature the spacing of these levels is usually larger than the thermal energy kT. Therefore we will reconsider electron-transfer reactions from a quantum-mechanical viewpoint that was first advanced by Levich and Dogonadze [1]. In this course we will rederive several of, the results of Chapter 6, show under which conditions they are valid, and obtain generalizations that account for the quantum nature of the inner-sphere modes. By necessity this chapter contains more mathematics than the others, but the calculations axe not particularly difficult. Readers who are not interested in the mathematical details can turn to the summary presented in Section 6. [Pg.259]

ZSM-5 and ZSM-11 samples were prepared as previously described (11) using tetrapropy 1 ammonium hydroxide and tetrabutyl ammonium bromide, respectively. The nature and crystallinity of the materials were verified by X ray diffraction, ir spectroscopy of lattice vibrational bands ( 1 2 ), n-hexane adsorption capacity at room temperature and constraint index (13) measurements. All samples correspond to highly crystalline ZSM-5 or ZSM-11 materials. The chemical compositions of the samples as determined from chemical analysis of A1 and Na contents, are given in table 1. [Pg.253]

Another theoretical frontier involves the study of the vibrational spectroscopy of water at other conditions, or in other phases. Here it will be crucially important to use more robust water models, since many effective two-body simulation models were parameterized to give agreement with experiment at one state point room temperature and one atmosphere pressure. We have already seen that using these models at higher or lower temperatures even for liquid water leads to discrepancies. We note that a significant amount of important theoretical work on ice has already been published by Buch and others [71, 72, 111, 175, 176]. [Pg.96]

CO is an excellent probe molecule for probing the electronic environment of metals atoms either supported or exchanged in zeolites. Hadjiivanov and Vayssilov have published an extensive review of the characteristics and use of CO as a probe molecule for infrared spectroscopy [80]. The oxidation and coordination state of the metal atoms can be determined by the spectral features, stability and other characteristics of the metal-carbonyls that are formed. Depending on the electronic environment of the metal atoms, the vibrational frequency of the C-O bond can shift. When a CO molecule reacts with a metal atom, the metal can back-donate electron density into the anti-bonding pi-orbital. This weakens the C-O bond which results in a shift to lower vibrational frequencies (bathochromic) compared to the unperturbed gas phase CO value (2143 cm ) [62]. These carbonyls form and are stable at room temperature and low CO partial pressures, so low temperature capabilities are not necessary to make these measurements. [Pg.138]

An unusual high-valent carbonyl complex, formulated as [Os(0)2(CO)4](Sb2Fn)2, has been isolated by the reaction of [OsOJ with CO in SbFs at room temperature. The complex was characterized by vibrational spectroscopy. Unfortunately, because of its extreme sensitivity to moisture, satisfactory elemental analysis and X-ray crystal structures have not been obtained. [Pg.769]

If a diffusional model with AHm < kT is appropriate, then the time th between electron hops must approach the period cor of the optical mode vibrations that trap or correlate the electrons. With an wj = 10" s, the hopping time Th would be short relative to the time scale of Mossbauer spectroscopy, ca. 10" s. We can therefore anticipate an isomer shift for the octahedral-site iron that is midway between the values typical for Fe ions and Fe " " ions. From Table 1 and Eq. (1), we can predict a room-temperature isomer shift of 6 0.75 mm/s wrt iron. Consistent with this prediction is the... [Pg.22]

One of the greatest advantages of matrix isolation IR (or Raman) spectroscopy is that vibrational bands are inherently very narrow, because rotations are largely suppressed, which means that much more detailed information can be obtained than in the liquid phase at room temperature. However, this additional information can only be obtained if the spectrometer offers high enough resolution, which in the case of interferometers translates into sufficient displacement of the movable mirror. For most practical purposes, a resolution of 1 cm is adequate for matrix work, altough it is good to have 0.5-cm resoution available in case one needs it, say, for the elucidation of site structures. [Pg.811]

Vibrationally excited nitric oxide has been produced flash photo-lytically at room temperature by Norrish and co-workers.22-24 They monitored the vibrationally excited nitric oxide by the method of kinetic spectroscopy developed in Norrish s laboratory. Information on relaxation processes was obtained as a result. [Pg.171]


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