Zeolite diffuse reflectance spectrum

Kojima and co-workers also examined the photo-oxidation of stilbenes in zeolite Y [150]. The presence of O2 in the stilbene-NaY sample led to a red-shifting of the tail end of the diffuse reflectance spectrum and was assigned to the charge-transfer complex with O2. Upon excitation at 313/366 nm, both cis- and /ra .v-stilbene undergo photo-oxygenation to form benzaldehyde. Phenanthrene, the expected product from the ]2 -f 4] cycloaddition reaction of excited m-stilbene, was also formed. The details of the mechanism leading to benzaldehyde and phenanthrene... 

As an illustration of the current state of the art for electronic spectroscopy of transition metal ions in zeolites, refer to the recent review by Schoonheydt of Cu2+ in different zeolites [56]. Schoonheydt shows that experimental measurement of diffuse reflectance spectra (and in the case of Cu2 + EPR spectra) must be combined with theoretical calculations if a complete interpretation is to be made. The exact frequencies of the d-d transitions in the electronic spectrum of Cu2+ are independent of the zeolite structure type, the Si Al ratio, and the co-exchanged cations, but depend solely on the local coordination environment. Figure 20 shows the diffuse reflectance spectrum of dehydrated Cu-chabazite the expanded portion reveals the three d-d transitions in the region around 15000 cm l. 

Garbowski and Mirodatos have recently shown that two charge transfer transitions are present in the u.v. diffuse reflectance spectrum of many zeolites. That at 240 nm, present whatever the zeolite and whatever the chemical or thermal treatment, is related to Al-0 units belonging to the zeolite framework, which are inert towards catalysis. The band at 320 nm, more stable towards dealumination and dehydroxylation, is specifically detected or significantly enhanced for catalytically active samples. The authors relate it to extra-lattice structures, like (AlO)" cations inside the zeolite matrix, in which A1 is highly electron deficient. 

Characterization. In-situ diffuse reflectance FTIR (DRIFT) experiments were carried out with undiluted samples of the zeolites in a Spectratech DRIFT cell and a Nicolet Magna 550 spectrometer. Most experiments were carried out in a flow mode, passing 0.84 ml/s of a gas mixture containing inert (He, Ar or N2) and N2O, NO, CO or mixtures of these gases continuously through the cell at atmospheric pressure. Each spectrum was recorded by addition of 256 scans and a resolution of 8 cm. ... 

Infrared spectra of zeolitic samples can be measured in several different modes. These include transmission, diffuse reflectance, attenuated total internal reflection (ATR) and emission. Transmission and diffuse reflectance are by far the most widely used of these techniques. In the transmission mode, the sample is placed directly in the infrared beam of the instrument and the light passing through or transmitted is measured by the detector. This transmitted signal (T) is ratioed to the open beam (no sample) signal (To) to get the transmission spectrum of the sample. The transmission spectrum is converted to an absorbance spectrum ... 

Additional spectroscopic information which supports these conclusions is available [292], For instance, the diffuse reflectance absorption maxima of valerophenone (97, n = 4) in Li-X and Cs-X zeolites are shifted only slightly from each other and both are similar to the spectrum obtained in methanol solution (Figure 50). Although the absorption spectrum of valerophenone in the less polar ZSM-5 (Si/Al 490) also resembles that in hexane, the... 

The reaction of water with low-loaded [Ru(bpy)3] + entrapped in zeolite Y has been reported [152]. Since translational mobility of the Ru molecules cannot occur in the zeolite, the multimolecular degradation step observed in solution is no longer possible. Instead, O2 was found to be formed from the reaction of [Ru(bpy)3] with water. It was possible to examine the evolution of this reaction at various pHs by spectroscopic methods, such as EPR, diffuse reflectance and Raman spectroscopy. Figure 30 shows the evolution of the diffuse reflectance spectra after exposure of Ru(bpy)3 +-zeolite Y to water at pH 7 [152]. Trace e is the spectrum of the... 

Clearly, both vibrational and UV-visible spectroscopy also play an important role in materials chemistry, and are well described in other texts. The principles involved in carrying out these experiments on solids rather than in solution are similar, but often experimental methods vary. For example, an IR spectrum of a zeolite would be carried out by dispersing the solid in a matrix of potassium bromide and pressing into a disk, rather than in solution. Typically, a UV-visible spectrum of a solid would be carried out in diffuse reflectance mode, where the solid is dispersed in a white matrix (such as barium carbonate) and the UV light is reflected off the surface rather than passing through a solution. 

Characterization of catalysts The zeolite structure was checked by X-ray diffraction patterns recorded on a CGR Theta 60 instrument using Cu Ka, filtered radiation. The chemical composition of the catalysts was determined by atomic absorption analysis after dissolution of the sample (SCA-CNRS, Solaize, France). Micropore volumes were measured by N2 adsorption at 77 K using a Micromeritics ASAP 2000 apparatus and by adsorption of cyclohexane (at P/Po=0.15) using a microbalance apparatus SET ARAM SF 85. Incorporation of tetrahedral cobalt (II) in the framework of Co-Al-BEA and Co-B-BEA was confirmed by electronic spectroscopy [18] using a Perkin Elmer Lambda 14 UV-visible diffuse reflectance spectrophotometer. Acidity measurements were performed by Fourier transform infrared spectroscopy (FT-IR, Nicolet FTIR 320) after pyridine adsorption. Self-supported wafer of pure zeolite (20 mg/cm ) was outgassed at 673 K for 6 hours at a pressure of lO Pa. After cooling at 423 K, the zeolite was saturated with pyridine vapour (30 kPa) for 5 min, evacuated at this temperature for 30 min and the IR spectrum was recorded. 

The local structure of iron sites in Fe-mazzite and Fe-ZSM-5, in which iron was incorporated during zeolite synthesis, was studied by X- and Q-band ESR, electron spin echo detected ESR (ED-ESR), electron spin echo envelope modulation (ESEEM), and diffuse reflectance UV-vis [94G1]. The X-band ESR spectra of Fe-MAZ (100 Fe/(Fe + A1 + Si) = 1.20) render three signals at g = 4.3, g = 2.3, and g = 2.0 - Table 14a. The Q-band spectra testifies only the signal atg = 2.0. The linewidths of the g = 2.0 signals are smaller in the Q-band spectra - Table 14. This narrowing indicates that the linewidth is at least partially due to the second-order broadening of the -l/2> l/2> transition. The X-band spectrum of Fe-MAZ with 100 Fe/(Fe + A1 + Si) = 0.07 exhibits the... 

One potential drawback of devices in which adsorption occurs on a deep bed of catalyst packed in an MAS rotor is the occurrence of a nonuniform distribution of reactant. This problem is illustrated by the Cs MAS spectra of zeolite CsZSM-5 in Fig. 5 [47]. Without adsorbates, the Cs chemical shift was —157 ppm at 298 K. An amount of methanol- C equivalent to 1 methanol molecule for every Cs in the zeolite was then introduced using the apparatus in Fig. 4, and the spectrum in Fig. 5b was obtained. The spectrum shows the consequences of a deep-bed adsorption of a slowly diffusing adsorbate. Rather than a single Cs resonance reflecting the adsorption of one equivalent of the methanol, there are two signals one at — 157 ppm originating from the bottom of the catalyst bed and a second at — 82 ppm from the top of the catalyst bed. The... 

---