Application of birnessite-type solids prepared by sol-gel and oxidation methods in photocatalytic degradation of 4-nitrophenol.

Potassium birnessites were prepared using two methods, sol-gel or oxidation. The solids were characterised by element chemical analysis, powder X-ray diffraction, FT-IR spectroscopy, thermal analyses, and nitrogen adsorption. The evolution of the properties as a function of the preparation method was discussed. The photocatalytic performance of these solids was preliminarily tested for the degradation of 4-nitrophenol. The degradation pathway and the nature of the by-products were investigated by mass spectrometry. The solids showed good catalytic behaviour, although their preparation must be improved, mainly concerning the calcination step involved in sol-gel synthesis, which led to the formation of Mn2O3 that worsened the catalytic behaviour.

Magnetic properties of nickel and cobalt catalysts supported on nanoporous oxides.

The aim of this work is to use magnetic measurements as a research tool in the study of possible metal-support interactions in nickel and cobalt nanoporous catalysts. Several physicochemical techniques, namely nitrogen adsorption, X-ray diffraction, temperature-programmed reduction and chemical analysis, were used to analyze the role of the preparation method and the nature of the support on the existence of such metal-support interactions and to relate them with the magnetic response of these nanoporous systems. The catalysts were prepared by incipient wetness impregnation and precipitation-deposition with two commercial oxides, gamma-Al2O3 and SiO2, as supports. The magnetic behavior of the catalysts is drastically affected by the existence of interactions between the metal and the support during the preparation procedure. The samples with weak metal-support interactions have characteristic magnetic behavior of antiferromagnetic metal oxide nanoparticles, while the ones having strong interactions display spin-glass like behavior.

Effect of the intercalation conditions of a montmorillonite with octadecylamine.

Intercalation of montmorillonite with octadecylamine under several conditions is reported. Octadecylamine was protonated in situ with HCl to obtain octadecylammonium cations. Water and water/ethanol mixtures were used as reaction medium, and the ratios amine/clay and HCl/amine were also varied. Intercalation was successful when the amine/clay ratio was in the range 1-3 mmol/g; optimal results were obtained for an amine/clay ratio of 2.0 mmol/g. For a given amine/clay ratio, the HCl/amine ratio also influences the intercalation. Basal spacings of the intercalated solids were between 13.4-36.7 angstroms. The amount of organic matter incorporated into the solids also varied widely; up to 40 wt% is fixed. Specific surface area is very low in all the intercalated solids because of the blockage of the clay porosity by the organic molecules. Co-intercalation of octadecylammonium and of the inorganic polycation [Al13O4(OH)24(H2O)12]7+ was also considered, giving rise to intercalated solids with basal spacings between 17 and 22 A, also with a high fixation of organic matter.

Preparation and Study of Decavanadate-Pillared Hydrotalcite-like Anionic Clays Containing Cobalt and Chromium.

Hydrotalcite-like compounds containing Co(II) and Cr(III) in the brucite-like layers have been prepared. The interlayer anion was carbonate or decavanadate. The chemical formulas of the samples are [Co(0.65)Cr(0.35)(OH)(2)] (CO(3))(0.175).1.22H(2)O (sample CoCrC) and [Co(0.61)Cr(0.39)(OH)(2)](V(10)O(28))(0.065).1.35H(2)O (sample CoCrV). The compounds have been characterized by X-ray diffraction, XAS, vis-UV, FT-IR, and Raman spectroscopies, while the surface textures were assessed by nitrogen adsorption. Reducibility has been studied by temperature-programmed reduction. A similar characterization study has been carried out on samples obtained after calcination of the parent samples in air at increasing temperatures. Results indicate an ordered structure, with Co(II) and Cr(III) ions in octahedral holes of the brucite-like layers and, in CoCrV, decavanadate species with its main C(2) axis parallel to the layers. Thermal decomposition at increasing temperatures takes place, for CoCrC, through intermediate formation of Cr(VI) species, which are again reduced to Cr(III) at higher temperatures; simultaneously, Co(II) is oxidized to Co(III) (even at 673 K), thus leading to formation of Co(II)Co(III)Cr(III)O(4). However, decomposition of CoCrV takes place through partial depolymerization of decavanadate species and formation of Co(II)Cr(2)O(4) and Co(II)(2)V(2)O(7), without intermediate formation of Cr(VI) species.