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dc.contributor.authorTsvetkov, D. S.en
dc.contributor.authorIvanov, I. L.en
dc.contributor.authorZuev, A. Y.en
dc.date.accessioned2017-09-04T14:45:10Z-
dc.date.available2017-09-04T14:45:10Z-
dc.date.issued2012-
dc.identifier.citationTsvetkov D. S. Oxygen nonstoichiometry, crystal and defect structure of the double perovskite GdBaCo 1.8Fe 0.2O 6 - δ / D. S. Tsvetkov, I. L. Ivanov, A. Y. Zuev // Solid State Ionics. — 2012. — Vol. 218. — P. 13-17.en
dc.identifier.issn0167-2738-
dc.identifier.other1good_DOI
dc.identifier.other6f707d58-6abe-4f2d-ae96-f87bd5680b7cpure_uuid
dc.identifier.otherhttp://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=84861392542m
dc.identifier.urihttp://elar.urfu.ru/handle/10995/51039-
dc.description.abstractCrystal structure of the double perovskite GdBaCo 1.8Fe 0.2O 6 - δ was investigated by means of in situ X-ray diffraction at temperatures between 25 and 800°C in air. Pmmm-P4/mmm phase transition was found to occur in GdBaCo 1.8Fe 0.2O 6 - δ at 515°C. The results of oxygen nonstoichiometry, δ, measured as a function of oxygen partial pressure, p O2, in temperature range 700 ≤ T,°C ≤ 1025 by means of thermogravimetric technique are presented for this double perovskite. Partial molar enthalpy and entropy of oxygen in the GdBaCo 1.8Fe 0.2O 6 - δ structure were calculated. Both thermodynamic properties were shown to increase dramatically in the vicinity of the oxygen nonstoichiometry value equal to 1. The p O2 dependences of oxygen nonstoichiometry were found to have inflections when the oxygen content of GdBaCo 1.8Fe 0.2O 6 - δ is equal to 5.0 exactly. The analysis of the defect structure of the double perovskite GdBaCo 1.8Fe 0.2O 6 - δ was carried out using the model based on the simple cubic perovskite GdCoO 3 as a reference state. Equilibrium constants of the appropriate defects reactions were, therefore, determined. As a consequence, concentrations of all defect species defined within the framework of the model proposed were calculated as functions of temperature and oxygen nonstoichiometry. Oxygen vacancies were shown to be formed during p O2 diminution in gas environment in the layers of GdBaCo 1.8Fe 0.2O 6 - δ crystal lattice where they are ordered until oxygen nonstoichiometry of the oxide becomes equal to unity afterwards oxygen vacancies are formed randomly in oxygen polyhedrons. © 2012 Elsevier B.V. All rights reserved.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.rightsinfo:eu-repo/semantics/restrictedAccessen
dc.sourceSolid State Ionicsen
dc.subjectCOULOMETRIC TITRATIONen
dc.subjectDEFECT STRUCTUREen
dc.subjectDOUBLE PEROVSKITEen
dc.subjectOXYGEN NONSTOICHIOMETRYen
dc.subjectPARTIAL MOLAR QUANTITIESen
dc.titleOxygen nonstoichiometry, crystal and defect structure of the double perovskite GdBaCo 1.8Fe 0.2O 6 - δen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.typeinfo:eu-repo/semantics/articleen
dc.identifier.doi10.1016/j.ssi.2012.04.024-
dc.identifier.scopus84861392542-
local.contributor.employeeЦветков Дмитрий Сергеевичru
local.contributor.employeeИванов Иван Леонидовичru
local.contributor.employeeЗуев Андрей Юрьевичru
local.description.firstpage13-
local.description.lastpage17-
local.volume218-
dc.identifier.wos000306824000003-
local.contributor.departmentИнститут естественных наук и математикиru
local.identifier.pure1081355-
local.identifier.eid2-s2.0-84861392542-
local.identifier.wosWOS:000306824000003-
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