Abstract

Abstract The intercalation of two saponites and a montmorillonite with various zirconium oligomers, prepared from the hydrolysis of zirconyl chloride or zirconium acetate, has been studied. The structure of the intercalated clays strongly depended on the method of preparation and on the nature and crystallinity of the clays studied. In some cases, well-ordered intercalated clays (with basal spacings between 18 and 20 A) were obtained, while in other cases non-crystalline solids were obtained. Delamination and/or an acid activation of the clays seem to take place when the intercalation suspensions obtained from zirconyl chloride are subjected to a reflux treatment. The specific total surface area and specific micropore volume of the solids reached values up to 300 m 2 g −1 and 0.120 cm 3 g −1 , respectively. The amount of ZrO 2 fixed varied between 10 and 28% of the weight of the intercalated samples. In general, best results were obtained when using zirconium acetate as precursor, instead of zirconyl chloride.

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