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Oxide Clusters as Source of the Third Oxygen Atom for the Formation of Carbonates in Alkaline Earth Dehydrated Zeolites Научная публикация

Журнал Journal of Catalysis
ISSN: 0021-9517 , E-ISSN: 1090-2694
Вых. Данные Год: 2011, Том: 281, Номер: 2, Страницы: 212-221 Страниц : 10 DOI: 10.1016/j.jcat.2011.05.002
Авторы Larin Alexander V. 1 , Rybakov Andrey A. 1 , Zhidomirov Georgii M. 1,2 , Mace Amber 3 , Laaksonen Aatto 3 , Vercauteren Daniel P. 4
Организации
1 Lomonosov MSU, Moscow, Russia
2 Boreskov Institute of Catalysis, Novosibirsk, Russia
3 University of Stockholm, Stockholm, Sweden
4 University of Namur (FUNDP), Namur, Belgium
Реферат: In our paper, we show that carbonates can be formed with almost no energetic barrier from CO2 and metal-oxide binuclear MOXM species (M = Mg, Ca, Sr, Ba, with X = 1–4, depending on the cation) in alkaline earth zeolites, mordenite (MOR) and phillipsite (PHI), on the basis of quantum mechanical density functional theory (DFT) calculations at both isolated cluster and 3D periodic levels. The participation of MOXM species (X = 1 and 3) explains the source of the third O atom in CO3 species in dehydrated zeolites, on the basis of a good agreement between the calculated and experimental positions of the asymmetric and symmetric CO3 vibration bands, of the ratio of their intensities, and of the weak dependence versus the cation and framework type. The reaction of formation of dimethylcarbonate from CaCO3Ca in the 8-membered (8R) ring of MOR and methanol has also been considered, suggesting the carbonate activity as the source of CO2 at elevated temperatures.
Библиографическая ссылка: Larin A.V. , Rybakov A.A. , Zhidomirov G.M. , Mace A. , Laaksonen A. , Vercauteren D.P.
Oxide Clusters as Source of the Third Oxygen Atom for the Formation of Carbonates in Alkaline Earth Dehydrated Zeolites
Journal of Catalysis. 2011. V.281. N2. P.212-221. DOI: 10.1016/j.jcat.2011.05.002 WOS Scopus РИНЦ CAPlusCA OpenAlex Sciact
Даты:
Поступила в редакцию: 8 янв. 2011 г.
Принята к публикации: 1 мая 2011 г.
Опубликована online: 8 июн. 2011 г.
Опубликована в печати: 1 июл. 2011 г.
Идентификаторы БД:
Web of science: WOS:000293422100002
Scopus: 2-s2.0-79960269270
РИНЦ: 17004209
Chemical Abstracts: 2011:872077
Chemical Abstracts (print): 155:283994
OpenAlex: W2017116452
Sciact: 7961
Цитирование в БД:
БД Цитирований
Scopus 17
OpenAlex 19
Альметрики: