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Distortion of the Tetrahedral Coordination of Fe(III) Ions Stabilized in ZSM-5 Zeolite Framework Научная публикация

Журнал Journal of Structural Chemistry
ISSN: 0022-4766 , E-ISSN: 1573-8779
Вых. Данные Год: 2007, Том: 48, Номер: 5, Страницы: 855-861 Страниц : 7 DOI: 10.1007/s10947-007-0127-4
Ключевые слова D-d-transitions, Fe-ZSM-5 zeolite, Fe3+ in tetrahedral coordination
Авторы Malykhin S.E. 1 , Anufrienko V.F. 1 , Hansen E.J.M. 2 , Kuznetsova E.V. 1 , Larina T.V. 1 , Zhidomirov G.M. 1
Организации
1 G. K. Boreskov Institute of Catalysis, Siberian Division, Russian Academy of Sciences, Novosibirsk
2 Technical University Eindhoven, The Netherlands

Информация о финансировании (3)

1 Netherlands Organisation for Scientific Research 047.015.001
2 Российский фонд фундаментальных исследований 05-03-33103
3 Российский фонд фундаментальных исследований 06-03-33087

Реферат: A simple qualitative method to analyze d-d-electronic transitions in cations of the transition elements in oxide matrices is proposed. In the particular case, all the excited states of interest differ only in the electronic configuration of d-orbitals, and the energies of transitions can be computed via the configuration interaction (CI) method restricted by the active space of five cation d-orbitals. An ordinary cluster model that takes into account the first coordination sphere of transition metal ion consisting of the framework of oxygen ions is sufficient for this purpose. The systematic overestimation error of transition energies can be corrected through the empirical factor calculated to fit experimental UV-VIS spectra. The physical meaning of the scaling factor proposed is the dynamic part of electron correlation that remains unaccounted for in the chosen active CI space. The observed d-d-transitions of Fe3+ ions in MFI zeolites are analyzed in detail. It is suggested that the specifics of the observed electronic spectra are caused by the distortion of the tetrahedron of oxygen atoms around Fe3+. The latter can be easily taken into account when selecting an appropriate Fe3+ cluster model in the framework. It is shown that the occurrence of the weak low-frequency band below 21,000 cm−1 indicates the distortion of the tetrahedral environment around Fe3+.
Библиографическая ссылка: Malykhin S.E. , Anufrienko V.F. , Hansen E.J.M. , Kuznetsova E.V. , Larina T.V. , Zhidomirov G.M.
Distortion of the Tetrahedral Coordination of Fe(III) Ions Stabilized in ZSM-5 Zeolite Framework
Journal of Structural Chemistry. 2007. V.48. N5. P.855-861. DOI: 10.1007/s10947-007-0127-4 WOS Scopus РИНЦ CAPlusCA OpenAlex
Оригинальная: Малыхин С.Е. , Ануфриенко В.Ф. , Хэнсен Е.Д.М. , Кузнецова Е.В. , Ларина Т.В. , Жидомиров Г.М.
Искажение тетраэдрической координации ионов Fe(III), стабилизированных в решетке ZSM-5 цеолита
Журнал структурной химии. 2007. Т.45. №5. С.914-920. RSCI РИНЦ
Даты:
Поступила в редакцию: 21 февр. 2007 г.
Опубликована в печати: 1 сент. 2007 г.
Идентификаторы БД:
Web of science: WOS:000252171100008
Scopus: 2-s2.0-37749017360
РИНЦ: 13534240
Chemical Abstracts: 2008:24054
Chemical Abstracts (print): 148:457025
OpenAlex: W2137967717
Цитирование в БД:
БД Цитирований
Web of science 6
Scopus 5
РИНЦ 4
OpenAlex 6
Альметрики: