Clays and Clay Minerals · 1986 · 312 citations · 15 references
Natural SciencesMaterials EngineeringMaterials ScienceInorganic ChemistryMaterials ChemistrySolid-state ChemistryClay MineralogyClay MineralsInorganic MaterialsMetal OxidesOxide MineralogyClay Crystal ChemistryClay Mineral ChemistryTitanium Oxides
Abstract Titanium was introduced into the montmorillonite structure by cation exchange with polymeric Ti cations, formed by partial hydrolysis of TiCl 4 in HCl. On further hydrolysis and heating, TiO 2 pillars in the form of anastase were formed between the montmorillonite layers. The resulting TiO 2 -cross-linked montmorillonites possessed surface areas in the range 200–350 m 2 /g and pore volumes of about 0.2 cm 3 /g and were thermally and hydrothermally stable to 700°C. The basal spacing of products heated at temperatures > 200°C was about 28Å, as determined by X-ray powder diffraction and by N 2 -desorption pore-size analysis. The surface area increased and the pore volume decreased with increasing HCl-concentration in the Ti-solution. The uptake of TiO 2 by the montmorillonite, the surface area, and the pore volume increased with increasing amount of Ti added in the preparation, to about 10 mmoles of Ti/g of montmorillonite. A further increase in the amount of Ti added resulted in a decrease in surface area, but the pore volume and the uptake of TiO 2 remained almost constant. The high porosity and the interlayer spacing of the product are consistent with a structure similar to that previously proposed for smectites, cross-linked with hydroxy-Al oligocations.
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