Zobrazeno 1 - 10
of 36
pro vyhledávání: '"E. Czárán"'
Autor:
E. Czárán
Publikováno v:
Reaction Kinetics & Catalysis Letters. 51:555-558
Publikováno v:
Zeolites. 13:43-49
Preparation of zeolite—AgI inclusion complexes and their optical properties are discussed. The existence of inclusion has been proved by X-ray diffraction and thermoanalytical measurements. Properties of AgI after incorporation into the zeolite lat
Publikováno v:
Reaction Kinetics & Catalysis Letters. 48:105-113
MnO2 supported on Na-Y,FAU prepared as described in a previous paper has been tested for selective oxidation of benzyl alcohol to benzaldehyde. Experimental results have shown that oxidation is selective and stoichiometric under the conditions used,
Publikováno v:
Reaction Kinetics & Catalysis Letters. 43:261-267
Publikováno v:
Journal of Molecular Catalysis. 62:321-330
In order to reproducibly prepare MnO 2 samples for use in mild oxidation of organic substances, three different types of zeolites have been applied as supports for ‘active MnO 2 ’. After ion-exchanging the Y-FAU, MOR and 4A zeolites with MnSO 4 s
Autor:
E. Czárán
Publikováno v:
Reaction Kinetics & Catalysis Letters. 46:241-243
Autor:
E. Czárán
Publikováno v:
Reaction Kinetics & Catalysis Letters. 45:161-163
Publikováno v:
Reaction Kinetics and Catalysis Letters. 7:211-218
Electron microscopic studies reveal that repeated air/hydrogen regeneration cycles cause irreversible structural changes of a Pt/C catalyst involving sintering and migration of the platinum over the support. This is reflected by a serious decrease of
Publikováno v:
Reaction Kinetics and Catalysis Letters. 5:21-28
The texture and adsorption properties of a natural, Hungarian mordenite were investigated by electron microscopy and BET adsorption measurements. The properties of the ion-exchanged adsorbents were characterized by CO2 and SO2 isotherms. The measurem
Publikováno v:
Journal of Radioanalytical and Nuclear Chemistry Letters. 128:9-14
Some Hungarian zeolites have been studied by Mossbauer spectroscopy. It has been found that Fe3+ ions substitute for Si4+ in tetrahedral position, while Fe2+ ions are chargecompensating cations in octahedral sites.