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Non-Hydrothermal Synthesis of Copper-, Zinc- and Copper-Zinc Hydrosilicates Научная публикация

Журнал Materials Research Innovations
ISSN: 1432-8917 , E-ISSN: 1433-075X
Вых. Данные Год: 2001, Том: 5, Номер: 1, Страницы: 3-11 Страниц : 9 DOI: 10.1007/s100190100127
Ключевые слова CuO/SiO2, CuO/ZnO/SiO2, Homogeneous deposition-precipitation, Non-hydrothermal synthesis of layer silicates, ZnO/SiO2
Авторы Yurieva Tamara M. 1 , Kustova Galina N. 1 , Minyukova Tatyana P. 1 , Poels Eduard K. 2 , Bliek Alfred 2 , Demeshkina Maragrita P. 1 , Plyasova Ludmila M. 1 , Krieger Tamara A. 1 , Zaikovskii Vladimir I. 1
Организации
1 Boreskov Institute of Catalysis, Novosibirsk 630090, Russia
2 University of Amsterdam, Amsterdam, The Netherlands

Информация о финансировании (2)

1 Netherlands Organisation for Scientific Research 047.005.03.96
2 Российский фонд фундаментальных исследований 96-03-33887

Реферат: Cu/SiO2, Zn/SiO2 and Cu-Zn/SiO2 samples have been prepared by the homogeneous deposition-precipitation method. The samples were analyzed by thermal analysis, X-ray diffraction and infrared spectroscopy after various heat treatments and compared with data obtained for several minerals. It has been shown that interaction between the components occurs through formation of hydrosilicates. Copper-silica system at a Cu:Si ratio ≤ 1, gives rise to a hydrosilicate stable up to a calcination temperature of 930 K resembling the mineral Chrisocolla; at higher ratios a hydroxonitrate (gerhardite type) is also formed. Zinc-silica interaction produces two hydrosilicates such as a well crystallized Hemimorphite at Zn:Si = 2 and highly dispersed Zincsilite at Zn:Si ≤ 0.75, both stable up to 1073 K. The Zincsilite structure consists of three layered sheets (an octahedral layer sandwiched by two tetrahedral ones) like the Stevensite mineral group. For the copper-zinc-silica system no copper hydrosilicate is formed. Copper merely enters the Zincsilite structure independenly of the applied (Cu + Zn):Si ratio. Resulting layered copper-zinc hydrosilicate may be described by formula Znx-yCuy(Zn3-x–zCuz–y▪x)[Si4O10](OH)2.nH2O, where Zn3-x-zCuz-y– ions are located in octahedral sites, Znx-yCuy–ions in the interlayer; ▪x are vacancies in the layers. Copper and zinc in excess of the Zincsilite ratio of Me:Si = 0.75, gives rise to copper and copper-zinc hydroxonitrates.
Библиографическая ссылка: Yurieva T.M. , Kustova G.N. , Minyukova T.P. , Poels E.K. , Bliek A. , Demeshkina M.P. , Plyasova L.M. , Krieger T.A. , Zaikovskii V.I.
Non-Hydrothermal Synthesis of Copper-, Zinc- and Copper-Zinc Hydrosilicates
Materials Research Innovations. 2001. V.5. N1. P.3-11. DOI: 10.1007/s100190100127 WOS Scopus РИНЦ CAPlusCA OpenAlex
Даты:
Поступила в редакцию: 7 нояб. 2000 г.
Принята к публикации: 23 янв. 2001 г.
Опубликована в печати: 1 июн. 2001 г.
Опубликована online: 13 окт. 2016 г.
Идентификаторы БД:
Web of science: WOS:000169953700002
Scopus: 2-s2.0-0035374242
РИНЦ: 13365095
Chemical Abstracts: 2001:585397
Chemical Abstracts (print): 135:326539
OpenAlex: W2054107411
Цитирование в БД:
БД Цитирований
Web of science 25
Scopus 27
РИНЦ 31
OpenAlex 25
Альметрики: