scholarly journals Structural Properties and Catalytic Behaviour of CrOx/TiO2 Systems

2017 ◽  
Vol 6 (2) ◽  
pp. 79
Author(s):  
P. Wilson ◽  
P.M. Rao ◽  
R.P. Viswanath

<p>The present investigation comprises of an attempt to investigate the titania supported chromia catalysts using X-ray diffraction measurements (XRD), evolved gas analysis (EGA), FT infrared spectroscopy (FTIR) and FT-Raman spectroscopic techniques with catalytic evaluation by dehydrogenation of cyclohexane. Evolved Gas Analysis shows a modified decomposition pattern than that of bulk chromia and presence of surface heterogeneity owing to the modified surface anchored chromia species formed as a result of interaction between chromia and titania. Above 773 K, Cr<sup>6+</sup> is not stable over TiO<sub>2</sub> surface and the reduction of the Cr<sup>6+</sup> to intermediate chemical states take place. XRD investigations illustrate the significance of X-ray source in examining supported chromia catalysts to study the morphological modifications of the active phase when crystalline supports are employed. FT Raman spectra reveals that on calcining the sample at 573 K, for 2 hours, the chromia phase assumes a monomerically anchored molecular state. Longer calcination time (6 hours) at the same temperature, leads to the diffusion of <em>in</em><em> </em><em>situ </em>formed Cr<sup>3+</sup> ions into the anatase lattice. On calcination at 973 K for 6 hours, amorphous chromia phase is no more stable on TiO<sub>2</sub> support resulting inagglomeration leading to the germination of microcrystalline α–Cr<sub>2</sub>O<sub>3</sub>. Evaluation of catalytic performance of above catalysts by dehydrogenation of cyclohexane confirms the fact that diffusion of part of Cr<sup>3+</sup> species into the bulk of anatase phase occurs under reaction conditions.</p>

1976 ◽  
Vol 29 (4) ◽  
pp. 711 ◽  
Author(s):  
DJ Stabb

The basic halides MoOX(H2O), (X = F, Cl) were examined by vacuogravimetric and evolved gas analysis and by X-ray and electron diffraction techniques. The basic chloride prepared by slow crystallization had y = 3.08, with an orthorhombic unit cell 0.723 by 0.820 by 1.805 nm. Basic chlorides produced by rapid precipitation were less crystalline, of slightly larger unit cell dimensions and had 3.0 < y < 4.3. The water in excess of y = 3 was loosely held, while three water molecules per molybdenum were more strongly held. The fluoride, which could not be obtained with the perfect MoOF(H2O)3 stoichiometry, was isomorphous (cell parameters 0.710 by 0.823 by 1.824 nm for [MoOF0.96(OH)0.04(H2O)3] (H2O)0.28). It is concluded that the only hydrate of MoOX existing under normal conditions is MoOX(H2O)3, not the previously reported tetrahydrate.


1999 ◽  
Vol 14 (5) ◽  
pp. 2138-2146 ◽  
Author(s):  
Eric L. Brosha ◽  
John Davey ◽  
Fernando H. Garzon ◽  
Shimshon Gottesfeld

The dehydrogenation of C60 · H18.7 was studied using thermogravimetric and powder x-ray diffraction analysis. C60 · H18.7 was found to be stable up to 430 °C in Ar at which point the release of hydrogen initiated the collapse of a fraction of fullerene molecules. X-ray diffraction analysis performed on C60 · H18.7 samples dehydrogenated at 454, 475, and 600 °C displayed an increasing volume fraction of amorphous material. The decomposition product comprises randomly oriented, single-layer graphite sheets. Evolved gas analysis using gas chromatograph (GC) mass spectroscopy confirmed the presence of both H2 and methane upon dehydrogenation. Attempts to improve reversibility or reduce hydrogenation/ dehydrogenation temperatures by addition of Ru and Pt catalysts were unsuccessful.


1985 ◽  
Vol 49 (354) ◽  
pp. 717-720 ◽  
Author(s):  
Zoran Maksimović ◽  
György Pantó

AbstractHydroxyl-bastnaesite-(Nd), the Nd- and OH-dominant new member of the bastnaesite group, has been found in the red karstic bauxites near Nikšić, Montenegro. It occurs as whitish, irregular aggregates of crystals usually 100–200 µm in diameter. Hexagonal with the cell dimensions a = 7.191 and c = 9.921 Å, with Z = 6. The strongest lines of the X-ray powder diffraction pattern (d, I, hkl) are: 4.95 80(002); 3.596 79(110); 2.911 100(112); 2.077 29(300); 2.042 51(114); 1.914 30(302). The mineral is uniaxial positive, ω 1.715, ɛ 1.81; Dcalc 4.89 g/cm3.Electron probe analysis, using garnet, apatite and synthetic glass standards, combined with thermogravimetric and evolved gas analysis, gave Y2O3 0.2, La2O3 27.1, Ce2O3 0.3, Pr2O3 8.5, Nd2O3 31.5, Sm2O3 4.4, Eu2O3 1.3, Gd2O3 1.4, CaO 0.3, F 3.3, H2O 2.26, CO2 20.63, sum 101.19, less O = F 1.39, total 99.80%. This analysis calculates to (Nd0.41La0.36Pr0.11Sm0.06Gd0.02 Eu0.02Ca0.01)Σ0.99(CO3)1.03[(OH)0.55F0.38]Σ0.93, or ideally, (Nd,La)CO3(OH,F), with Nd > La and OH > F.


1987 ◽  
Vol 27 (7) ◽  
pp. 669-684 ◽  
Author(s):  
K. Nassau ◽  
P.K. Gallagher ◽  
A.E. Miller ◽  
T.E. Graedel

2010 ◽  
Vol 45 (4) ◽  
pp. 241-273 ◽  
Author(s):  
S. Materazzi ◽  
S. Vecchio

Sign in / Sign up

Export Citation Format

Share Document