Pirólise do pireno sob pressão com nitrogênio em temperaturas moderadas
Ano de defesa: | 2008 |
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Autor(a) principal: | |
Orientador(a): | |
Banca de defesa: | |
Tipo de documento: | Dissertação |
Tipo de acesso: | Acesso aberto |
Idioma: | por |
Instituição de defesa: |
Universidade Federal do Espírito Santo
BR Mestrado em Física Centro de Ciências Exatas UFES Programa de Pós-Graduação em Física |
Programa de Pós-Graduação: |
Não Informado pela instituição
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Departamento: |
Não Informado pela instituição
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País: |
Não Informado pela instituição
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Palavras-chave em Português: | |
Link de acesso: | http://repositorio.ufes.br/handle/10/4765 |
Resumo: | We made an study to help the understanding of the formation process ofpitches using a homogeneous compound, pyrene,whichis a polycyclic aromatic hydrocarbon constituted byfour benzene rings,meltingpointbetween145 and148 °C anda boilingpoint of 404 °C. The pyrene wassubmitted toheat treatmentsunder nitrogen atmospherein an experimentalset updeveloped at the Laboratory of Carbon MaterialsoftheFederal University of Espírito Santo. The heat treatments were performed at 400, 450 and 500 °C, with residence timeof 0, 1, 2, 4, 8 and 16 hours, under a final pressureof 6,9 MPa. The samples were characterized bythermogravimetry, differential scanning calorimetry, X-ray diffraction, solid-state 13C nuclear magnetic resonance spectroscopy,and scanning electron microscopy. We did not observe significant modifications of the samples heat treated at 400 and 450 °Cfor all studied residence times in relation to the original precursor. The samplesobtained at 500 °C suffered significant modifications from 4 hoursof residue time; the treatments for8 h and 16 h produced segregation, the samplesbeingdivided into two well-defined regions (A and B regions). The 500-8hBand 500-16hBsamples sufferedthe mostnoticeablemodifications in relation to the precursor. Theelementalanalysis and thermogravimetric results indicatedthat the 500-8hBsamplepresentedcharacteristics similar topitches, additionalstudieswillbenecessarytoverifyiftheanisotropiccarbonmaterialisreallyapitch. The elementalanalysis, X-ray diffraction and scanning electron microscopy resultsindicatedthat the 500-16hBsample presentedcharacteristicsof acoke. The X-ray diffraction patternsand NMR spectraresults of the 500-16hBsample indicate the formation of aromatic lamellae typicalof the turbostratic structure of grafitizable carbon materialswith a relatively hight value of Lcobtained at a low heat treatment temperature. |