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Some Aspects of NU-86 Zeolite Crystallization Тезисы доклада

Конференция 13th International Zeolite Conference
08-13 июн. 2001 , Montpellier
Сборник Zeolites and Mesoporous Materials at the dawn of the 21st century : Proceedings of the 13th International Zeolite Conference, 8-13 June 2001, Montpellier, France
Сборник, 2001. 443 c. ISBN 9780444502384.
Журнал Studies in Surface Science and Catalysis
ISSN: 0167-2991
Вых. Данные Год: 2001, Том: 135, Номер статьи : 02-P-20, Страниц : 1 DOI: 10.1016/S0167-2991(01)81359-8
Авторы Dudarev S.V. 1 , Toktarev A.V. 1 , Echevsky G.V. 1 , Kibby C.L. 2 , O'Rear D.J. 2
Организации
1 Boreskov Institute of Catalysis, Ak. Lavrentieva Av. 5, Novosibirsk, 630090, Russia
2 Chevron Research and Technology Company, 100 Chevron Way, Richmond, CA 94802, USA.

Реферат: Crystallization of wide-pore NU-86 zeolite was investigated using different templates and silica sources, different chemical compositions of the reaction gels, and with or without seeding. It was found that NU-86 zeolite forms best from thick and seeded reaction gels based on Cab-O-Sil fumed silica. Seeding with NU-88 zeolite leads to formation of a pure NU-86 zeolitic phase. Other concurrent zeolitic phases are ZSM-23, mordenite, ZSM-12, and analcime. We found a higher optimum alkalinity for the reaction gel and a lower optimum stirring rate than those reported in the literature.
Библиографическая ссылка: Dudarev S.V. , Toktarev A.V. , Echevsky G.V. , Kibby C.L. , O'Rear D.J.
Some Aspects of NU-86 Zeolite Crystallization
В сборнике Zeolites and Mesoporous Materials at the dawn of the 21st century : Proceedings of the 13th International Zeolite Conference, 8-13 June 2001, Montpellier, France. 2001. – C.189. – ISBN 9780444502384. DOI: 10.1016/S0167-2991(01)81359-8 РИНЦ CAPlusCA OpenAlex
Даты:
Опубликована в печати: 1 янв. 2001 г.
Опубликована online: 2 сент. 2007 г.
Идентификаторы БД:
РИНЦ: 30705962
Chemical Abstracts: 2001:772398
Chemical Abstracts (print): 136:55945
OpenAlex: W1582560918
Цитирование в БД:
БД Цитирований
РИНЦ 2
Альметрики: