Combustion studies in a fluidised bed—The link between temperature, NOx and N2O formation,char morphology and coal type

Detalhes bibliográficos
Autor(a) principal: Valentim, B.
Data de Publicação: 2006
Outros Autores: Lemos de Sousa, M. J., Abelha, P., Boavida, D., Gulyurtlu, I.
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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spelling 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
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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
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reponame_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
collection Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
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