dc.contributorUniv Fed Acre
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorFundacao Univ Fed Rondonia
dc.contributorUniversidade de Brasília (UnB)
dc.contributorUniv Toulouse 3
dc.date.accessioned2020-12-10T22:01:56Z
dc.date.accessioned2022-12-19T20:28:20Z
dc.date.available2020-12-10T22:01:56Z
dc.date.available2022-12-19T20:28:20Z
dc.date.created2020-12-10T22:01:56Z
dc.date.issued2009-01-01
dc.identifierIsiame 2008. New York: Springer, p. 159-+, 2009.
dc.identifierhttp://hdl.handle.net/11449/197392
dc.identifier10.1007/978-3-642-01369-0_20
dc.identifierWOS:000273775100019
dc.identifier2115942621694174
dc.identifier0000-0003-0195-3885
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5378028
dc.description.abstractMossbauer spectroscopy was used in this study to investigate magnetite nanoparticles, obtained by spray pyrolysis and thermal treatment under H-2 reduction atmosphere. Room temperature XRD data indicate the formation of magnetite phase and a second phase (metallic iron) which amount increases as the time of reduction under H-2 is increased. While room temperature Mossbauer data confirm the formation of the cubic phase of magnetite and the occurrence of metallic iron phase, the more complex features of 77 K-Mossbauer spectra suggest the occurrence of electronic localization favored by the different crystalline phase of magnetite at low temperatures which transition to the lower symmetry structure should occur at T similar to 120 K (Verwey transition).
dc.languageeng
dc.publisherSpringer
dc.relationIsiame 2008
dc.sourceWeb of Science
dc.subjectMagnetite
dc.subjectHematite
dc.subjectSpray pyrolysis
dc.subjectMossbauer spectroscopy
dc.titleMossbauer spectroscopy study of iron oxide nanoparticles obtained by spray pyrolysis
dc.typeActas de congresos


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