Role of heteroatoms in precursor formation of zeolites
The structures of amorphous precursors formed prior to the onset of crystallization of microporous aluminosilicates (mordenite) and zincosilicates (VPI-7) are determined employing high-energy X-ray diffraction (HEXRD) technique. Without heteroatoms, silicate ring size is distributed around 6 ring (6R). Aluminum incorporation promotes the formation of smaller rings (especially 4R), while zinc incorporation promotes the formation of 3R before their crystallizations. The ring statistics for the crystalline zeolites are formed in the corresponding amorphous precursors.
Toru Wakihara Wei Fan Yasuhiro Suzuki Masaru Ogura Shinji Kohara Gopinathan Sankar Tatsuya Okubo
Department of Chemical System Engineering, The University of Tokyo, Tokyo 113-8656,Japan Japan Synchrotron Radiation Research Institute and CREST-JST, Hyogo 679-5198, Japan Davy Faraday Research Laboratory, Royal Institution of Great Britain, London W1S 4BS,U.K
国际会议
北京
英文
2007-08-12(万方平台首次上网日期,不代表论文的发表时间)