dc.creatorCOGO, S.L.
dc.creatorBRINATTI, A.M.
dc.creatorSAAB, S.C.
dc.creatorSIMÕES, M.L.
dc.creatorMARTIN-NETO, L.
dc.creatorROSA, J.A.
dc.creatorMascarenhas, Yvonne Primerano
dc.date.accessioned2012-03-26T21:44:53Z
dc.date.accessioned2018-07-04T14:24:33Z
dc.date.available2012-03-26T21:44:53Z
dc.date.available2018-07-04T14:24:33Z
dc.date.created2012-03-26T21:44:53Z
dc.date.issued2009
dc.identifierBrazilian Journal of Physics, v.39, n.1, p.31-34, 2009
dc.identifier0103-9733
dc.identifierhttp://producao.usp.br/handle/BDPI/11876
dc.identifier10.1590/S0103-97332009000100005
dc.identifierhttp://www.scielo.br/scielo.php?script=sci_arttext&pid=S0103-97332009000100005
dc.identifierhttp://www.scielo.br/pdf/bjp/v39n1/a05v39n1.pdf
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1609666
dc.description.abstractIn this study, sedimentary organic matter of oil shale rejects, calschist, shale fine and the so called retorted shale from Irati formation was characterized. EPR was used to analyse the samples regarding loss of signal in g = 2.003 associated to the organic free radical with the calcined samples and washing with hydrogen peroxide. The radical signal was detected in all samples, however, for the calschist and shale fine samples another signal was identified at g = 2.000 which disappeared when the sample was heated at 400 ºC. Hydrogen peroxide washing was also performed and it was noted that after washing the signal appeared around g = 2.000 for all samples, including retorted shale, which might be due to the quartz E1 defect.
dc.languageeng
dc.publisherSociedade Brasileira de Física
dc.relationBrazilian Journal of Physics
dc.rightsCopyright Sociedade Brasileira de Física
dc.rightsopenAccess
dc.subjectOil shale
dc.subjectEPR
dc.subjectQuartz
dc.titleCharacterization of oil shale residue and rejects from irati formation by electron paramagnetic resonance
dc.typeArtículos de revistas


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