Interaction of lithium-titanium ceramics with air during sintering

Podrobná bibliografie
Parent link:Russian Physics Journal
Vol. 50, iss. 2.— 2007.— [P. 134-139]
Další autoři: Gyngazov (Ghyngazov) S. A. Sergey Anatolievich, Lysenko E. N. Elena Nikolaevna, Petyukevich M. S. Mariya Stanislavovna, Frangulyan (Franguljyan) Т. S. Tamara Semenovna
Shrnutí:Title screen
Interaction of lithium-titanium polycrystalline ferrites with ambient air during their sintering is investigated using the methods of electroconductivity and thermal gravimetry within the temperature interval T = 600-1300 K. It is found out that the temperatures exceeding T = 1100 K correspond to effective course of reducing reactions in this material, which results in the formation of an oxygen-deficient ceramic structure in the stage of isothermal tempering (T = 1280 K). It is shown that in the final cooling stage the process of exchange of the ferrite ceramics with the ambient atmosphere exhibits a pronounced oxidative character. The role of these redox processes in the formation of the oxygen non-stoichiometry of the sintered specimen and the depth of its distribution are analyzed.
Режим доступа: по договору с организацией-держателем ресурса
Jazyk:angličtina
Vydáno: 2007
Témata:
On-line přístup:http://dx.doi.org/10.1007/s11182-007-0018-3
Médium: Elektronický zdroj Kapitola
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=647127
Popis
Shrnutí:Title screen
Interaction of lithium-titanium polycrystalline ferrites with ambient air during their sintering is investigated using the methods of electroconductivity and thermal gravimetry within the temperature interval T = 600-1300 K. It is found out that the temperatures exceeding T = 1100 K correspond to effective course of reducing reactions in this material, which results in the formation of an oxygen-deficient ceramic structure in the stage of isothermal tempering (T = 1280 K). It is shown that in the final cooling stage the process of exchange of the ferrite ceramics with the ambient atmosphere exhibits a pronounced oxidative character. The role of these redox processes in the formation of the oxygen non-stoichiometry of the sintered specimen and the depth of its distribution are analyzed.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1007/s11182-007-0018-3