TY - JOUR
T1 - Synthesis of BEA by dry gel conversion and its characterization
AU - Hari Prasad Rao, P. R.
AU - Leon Y Leon, C. A.
AU - Ueyama, K.
AU - Matsukata, M.
N1 - Funding Information:
This study was partially supported by Grant-in-Aid for Scientific Reasearch (No. 09750839, 09555247), from the Ministry of Education, Science, Sports and Culture. PR thanks the Japan Society for the Promotion of Science for a. postdoctoral fellowship. PR, KU and MM express their appreciation to Yuasa Ionics Co. foi-their assistance with the gas sorption study.
PY - 1998/5
Y1 - 1998/5
N2 - Zeolite BEA with SiO2/Al2O3 ratios ranging from 30 to 740 were crystallized at 413 and 453 K by the dry gel conversion technique. The particle size of the products increased with increasing SiO2/Al2O3 ratio as well as with increasing crystallization temperature. In as-synthesized BEA, the TEA+ ions interacting with Si-O- decomposed between 473 and 673 K and those interacting with Al-O- were cleaved between 673 and 798 K. During their elimination, the TEA+ ions interacting with Al-O- underwent higher degradation than those interacting with Si-O-. Chemical compositions showed the least influence on the fractions of decomposition product during the elimination between 473 and 673 K. The framework of H-BEA and NH4-BEA zeolites with SiO2/Al2O3 ratios ranging from 400 to 740 were stable even at 1373 K, whereas H-BEA with SiO2/Al2O3 = 30 was stable only up to 1173 K and became amorphous when calcined at 1373 K. After calcination at 1373 K, Na-BEA with SiO2/Al2O3 = 400 and 730 were transformed to tridymite (dense phase) whereas that with SiO2/Al2O3 = 30 became amorphous. The elimination of Na+ ions is necessary to have a BEA remain stable above 1173 K.
AB - Zeolite BEA with SiO2/Al2O3 ratios ranging from 30 to 740 were crystallized at 413 and 453 K by the dry gel conversion technique. The particle size of the products increased with increasing SiO2/Al2O3 ratio as well as with increasing crystallization temperature. In as-synthesized BEA, the TEA+ ions interacting with Si-O- decomposed between 473 and 673 K and those interacting with Al-O- were cleaved between 673 and 798 K. During their elimination, the TEA+ ions interacting with Al-O- underwent higher degradation than those interacting with Si-O-. Chemical compositions showed the least influence on the fractions of decomposition product during the elimination between 473 and 673 K. The framework of H-BEA and NH4-BEA zeolites with SiO2/Al2O3 ratios ranging from 400 to 740 were stable even at 1373 K, whereas H-BEA with SiO2/Al2O3 = 30 was stable only up to 1173 K and became amorphous when calcined at 1373 K. After calcination at 1373 K, Na-BEA with SiO2/Al2O3 = 400 and 730 were transformed to tridymite (dense phase) whereas that with SiO2/Al2O3 = 30 became amorphous. The elimination of Na+ ions is necessary to have a BEA remain stable above 1173 K.
KW - Crystallization
KW - Dry gel conversion
KW - High silica zeolite
KW - Interaction of TEA ions with zeolite
KW - Thermal stability
KW - Zeolite BEA (beta)
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U2 - 10.1016/S1387-1811(98)00033-X
DO - 10.1016/S1387-1811(98)00033-X
M3 - Article
AN - SCOPUS:0032068235
SN - 1387-1811
VL - 21
SP - 305
EP - 313
JO - Microporous and Mesoporous Materials
JF - Microporous and Mesoporous Materials
IS - 4-6
ER -