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- W1998589616 abstract "Vanadium was introduced in dealuminated β zeolite by impregnation with a VIVOSO4 aqueous solution at 353 K in air or argon (to prevent oxidation of VIV), leading to VSiβ and VSiβ-Ar zeolites, respectively. The samples were characterized by spectroscopy, XRD, and N2-physisorption. The oxidation state and environment of V in Siβ zeolite depend on the preparation parameters (i.e., on the way the solid is recovered after impregnation and on the drying temperature). In solids recovered by centrifugation, washed with distilled water, and then dried overnight at 298 K in argon, vanadium is found as extra-lattice octahedral VIV ions as evidenced by EPR. In contrast, in solids not washed but directly dried overnight at 353 K in air or argon, vanadium is found in both cases as lattice tetrahedral VV ions. These ions are incorporated into vacant T sites associated with SiOH, SiO-, oxygen vacancies (OVs) or nonbridging oxygen (NBOs) defects as shown by diffuse reflectance UV−visible, 51V MAS NMR, FT-IR, and photoluminescence. The oxidation to VV ions is suggested to be due to an electron transfer from VO2+ to trigonal ≡Si+ defect sites followed by reaction of the resulting VO2+ ions with particular defects of vacant T sites. These processes occur already upon drying of V-impregnated Siβ at 353 K. 51V MAS NMR allows detection of one kind of lattice tetrahedral V ions in VSiβ and two kinds in VSiβ-Ar. The formation of different kinds of tetrahedral V species is related to the presence in vacant T sites of Siβ zeolite of different types of defect sites such as trigonal ≡Si+ defect or SiOH and SiO- groups." @default.
- W1998589616 created "2016-06-24" @default.
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- W1998589616 date "2005-10-29" @default.
- W1998589616 modified "2023-09-24" @default.
- W1998589616 title "Oxidation State of Vanadium Introduced in Dealuminated β Zeolite by Impregnation with V<sup>IV</sup>OSO<sub>4</sub> Solution: Influence of Preparation Parameters" @default.
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- W1998589616 doi "https://doi.org/10.1021/jp0582134" @default.
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