Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type
Autor(a) principal: | |
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Data de Publicação: | 2006 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10284/272 |
Resumo: | Five commercially available high volatile bituminous coals from different origins were studied with the objective of characterizing their petrographic nature with respect to emissions of NOx and N2O. The chars produced [at temperatures ranging from 700 to 1000 °C] from these coals were also petrographically analyzed to assess the contribution of char to NOx and N2O formation during combustion. Vitrinite-rich coals produced higher porous chars (cenospheres and tenuinetworks) than those that are rich in inertinite. The former coals were, however, found to release lower concentrations of NO. Consistent with previous works, N2O emissions were observed to decrease significantly with temperature, however, on the whole, the N2O emissions from vitrinite-rich high volatile coals were less than those from inertinite-rich coals. Additionally, high porous chars were found to give rise to lower emissions of NO and N2O. |
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Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal typeCoalPetrographyMicrolithotypeChar morphotypeNOxN2OFluidised bed combustion (FBC)Five commercially available high volatile bituminous coals from different origins were studied with the objective of characterizing their petrographic nature with respect to emissions of NOx and N2O. The chars produced [at temperatures ranging from 700 to 1000 °C] from these coals were also petrographically analyzed to assess the contribution of char to NOx and N2O formation during combustion. Vitrinite-rich coals produced higher porous chars (cenospheres and tenuinetworks) than those that are rich in inertinite. The former coals were, however, found to release lower concentrations of NO. Consistent with previous works, N2O emissions were observed to decrease significantly with temperature, however, on the whole, the N2O emissions from vitrinite-rich high volatile coals were less than those from inertinite-rich coals. Additionally, high porous chars were found to give rise to lower emissions of NO and N2O.ElsevierRepositório Institucional da Universidade Fernando PessoaValentim, B.Lemos de Sousa, M. J.Abelha, P.Boavida, D.Gulyurtlu, I.2007-05-08T07:23:33Z2006-01-01T00:00:00Z2006-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10284/272engInternational Journal of Coal Geology. 67 (2006), pp. 191-201info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2022-09-06T02:00:22Zoai:bdigital.ufp.pt:10284/272Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T15:38:12.274788Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
title |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
spellingShingle |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type Valentim, B. Coal Petrography Microlithotype Char morphotype NOx N2O Fluidised bed combustion (FBC) |
title_short |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
title_full |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
title_fullStr |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
title_full_unstemmed |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
title_sort |
Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type |
author |
Valentim, B. |
author_facet |
Valentim, B. Lemos de Sousa, M. J. Abelha, P. Boavida, D. Gulyurtlu, I. |
author_role |
author |
author2 |
Lemos de Sousa, M. J. Abelha, P. Boavida, D. Gulyurtlu, I. |
author2_role |
author author author author |
dc.contributor.none.fl_str_mv |
Repositório Institucional da Universidade Fernando Pessoa |
dc.contributor.author.fl_str_mv |
Valentim, B. Lemos de Sousa, M. J. Abelha, P. Boavida, D. Gulyurtlu, I. |
dc.subject.por.fl_str_mv |
Coal Petrography Microlithotype Char morphotype NOx N2O Fluidised bed combustion (FBC) |
topic |
Coal Petrography Microlithotype Char morphotype NOx N2O Fluidised bed combustion (FBC) |
description |
Five commercially available high volatile bituminous coals from different origins were studied with the objective of characterizing their petrographic nature with respect to emissions of NOx and N2O. The chars produced [at temperatures ranging from 700 to 1000 °C] from these coals were also petrographically analyzed to assess the contribution of char to NOx and N2O formation during combustion. Vitrinite-rich coals produced higher porous chars (cenospheres and tenuinetworks) than those that are rich in inertinite. The former coals were, however, found to release lower concentrations of NO. Consistent with previous works, N2O emissions were observed to decrease significantly with temperature, however, on the whole, the N2O emissions from vitrinite-rich high volatile coals were less than those from inertinite-rich coals. Additionally, high porous chars were found to give rise to lower emissions of NO and N2O. |
publishDate |
2006 |
dc.date.none.fl_str_mv |
2006-01-01T00:00:00Z 2006-01-01T00:00:00Z 2007-05-08T07:23:33Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10284/272 |
url |
http://hdl.handle.net/10284/272 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
International Journal of Coal Geology. 67 (2006), pp. 191-201 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Elsevier |
publisher.none.fl_str_mv |
Elsevier |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799130244318232576 |