Hydrothermal syntheses were made mainly in the binary system SiO2-H20 in a temperature range between 300 ~ C and 500 ~ C and pressures from 0.2 kbar up to 4.0 kbar with various starting materials. In this way the transformation behavior of different amorphous silicas via cristobalite and keatite to
Transformation of amorphous silica colloids to nanosized MEL zeolite
✍ Scribed by S. Mintova; N. Petkov; K. Karaghiosoff; T. Bein
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 179 KB
- Volume
- 50
- Category
- Article
- ISSN
- 1387-1811
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✦ Synopsis
Si-MEL molecular sieve is prepared from aged colloidal precursor solutions under hydrothermal treatment (HT) at 90 °C. In situ dynamic light scattering (DLS) investigations of the precursor solutions and the crystalline Si-MEL sols are performed with the original concentrations. Sub-colloidal particles with a mean radius of about 1 nm and colloidal aggregates with a radius of 10 nm are detected in the precursor colloidal solutions after 5 h aging at room temperature. Consumption of the sub-colloidal particles with time and an increase of the colloidal fraction of 10 nm particles after 48 h aging is observed. After heating of the aged precursor solution at 90 °C for 30 h, three particle populations of 1, 10, and 100 nm radius are formed. Complete transformation from amorphous to crystalline colloidal particles is observed after 68 h extended HT of the aged precursor solution. The mean hydrodynamic radius of the crystalline Si-MEL particles is about 100 nm based on the DLS measurements. The size of the MEL crystals was also confirmed with SEM. Additional time-dependent 29 Si NMR measurements of the aged precursor colloidal solutions prior to further crystal growth show that the amount of Q 0 species ðd ¼ À71:2Þ decreases, while signals of high intensity in the range between d ¼ À88:6 and À98.9 indicating the formation of Q 3 6 and Q 3 8 silicon species appear. IR data reveal that with aging of the precursor colloidal solutions at room temperature, an increased ordering of the silica species similar to those found in the final MEL product is observed.
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