dc.creatorTURTELLI, R. Sato
dc.creatorNUNES, C. Bormio
dc.creatorTEIXEIRA, L. C.
dc.creatorGROESSINGER, R.
dc.creatorSUZUKI, P. A.
dc.creatorBARBATTI, C.
dc.date.accessioned2012-10-18T23:52:17Z
dc.date.accessioned2018-07-04T14:46:31Z
dc.date.available2012-10-18T23:52:17Z
dc.date.available2018-07-04T14:46:31Z
dc.date.created2012-10-18T23:52:17Z
dc.date.issued2009
dc.identifierJOURNAL OF ALLOYS AND COMPOUNDS, v.471, n.1/Fev, p.52-55, 2009
dc.identifier0925-8388
dc.identifierhttp://producao.usp.br/handle/BDPI/17464
dc.identifier10.1016/j.jallcom.2008.03.038
dc.identifierhttp://dx.doi.org/10.1016/j.jallcom.2008.03.038
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1614266
dc.description.abstractThe longitudinal and transverse magnetostriction and microstructure of polycrystalline Fe(100-x)Ge(x) (x= 8, 12, 15, 20) alloys were investigated in order to correlate the magnetostriction with microstructure. In order to obtain different microstructures in the Fe(100-x)Ge(x) alloys, the samples were annealed at 600 degrees C during 2 h and at 1150 degrees C for half hour and then quenched in cold water. For Ge concentrations lower than 14 at.%, the longitudinal magnetostriction is positive and increases positively up to 22 ppm at 12 at.% Ge then decreases and vanishes at about 14 at.% Ge. For further Ge concentration increase the longitudinal magnetostriction is negative and reaches -30 ppm for Fe(80)Ge(20). This behavior, that is very similar to that reported for Fe-Si alloys, is explained by the structural changes caused by different thermal histories of the alloys. (C) 2008 Published by Elsevier B. V.
dc.languageeng
dc.publisherELSEVIER SCIENCE SA
dc.relationJournal of Alloys and Compounds
dc.rightsCopyright ELSEVIER SCIENCE SA
dc.rightsrestrictedAccess
dc.subjectMagnetostriction
dc.subjectMicrostructure
dc.subjectTransition metal alloys and compounds
dc.subjectMagnetic measurements
dc.titleMagnetostriction of polycrystalline Fe-Ge alloys
dc.typeArtículos de revistas


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