The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash
Autor(a) principal: | |
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Data de Publicação: | 2014 |
Outros Autores: | , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | REM. Revista Escola de Minas (Online) |
Texto Completo: | http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000100005 |
Resumo: | The effect of calcination temperature and air flow on the content of organic material, morphology of particles, degree of crystallinity and the reactivity with lime solution of the sugar cane bagasse ash is evaluated. The results show that the long fibers of the bagasse and organic material are retained when calcination occurs without sufficient air flow. Calcining with forced air-flow breaks the fibers, removes organic material and produces fine particles at a temperature of 600ºC. The non-organic material observed in the ash displays a high degree of crystallinity. Experiments show that the crystalline structure observed in the ashes is due to adhered sand which was not previously washed away. The reduction on the conductivity in lime solution and X-rays diffraction pattern suggest that amorphous silica is formed at temperatures lower than 600ºC and cristobalite is formed at higher temperatures. |
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The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ashSugar cane bagasse ashpozzolanic activitymineral admixtureThe effect of calcination temperature and air flow on the content of organic material, morphology of particles, degree of crystallinity and the reactivity with lime solution of the sugar cane bagasse ash is evaluated. The results show that the long fibers of the bagasse and organic material are retained when calcination occurs without sufficient air flow. Calcining with forced air-flow breaks the fibers, removes organic material and produces fine particles at a temperature of 600ºC. The non-organic material observed in the ash displays a high degree of crystallinity. Experiments show that the crystalline structure observed in the ashes is due to adhered sand which was not previously washed away. The reduction on the conductivity in lime solution and X-rays diffraction pattern suggest that amorphous silica is formed at temperatures lower than 600ºC and cristobalite is formed at higher temperatures.Escola de Minas2014-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000100005Rem: Revista Escola de Minas v.67 n.1 2014reponame:REM. Revista Escola de Minas (Online)instname:Escola de Minasinstacron:ESCOLA DE MINAS10.1590/S0370-44672014000100005info:eu-repo/semantics/openAccessSoares,Marcela Maira N. S.Poggiali,Flávia S. J.Bezerra,Augusto Cesar S.Figueiredo,Roberto B.Aguilar,Maria Teresa P.Cetlin,Paulo Robertoeng2014-04-17T00:00:00Zoai:scielo:S0370-44672014000100005Revistahttp://www.scielo.br/remhttps://old.scielo.br/oai/scielo-oai.phpeditor@rem.com.br1807-03530370-4467opendoar:2014-04-17T00:00REM. Revista Escola de Minas (Online) - Escola de Minasfalse |
dc.title.none.fl_str_mv |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
title |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
spellingShingle |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash Soares,Marcela Maira N. S. Sugar cane bagasse ash pozzolanic activity mineral admixture |
title_short |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
title_full |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
title_fullStr |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
title_full_unstemmed |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
title_sort |
The effect of calcination conditions on the physical and chemical characteristics of sugar cane bagasse ash |
author |
Soares,Marcela Maira N. S. |
author_facet |
Soares,Marcela Maira N. S. Poggiali,Flávia S. J. Bezerra,Augusto Cesar S. Figueiredo,Roberto B. Aguilar,Maria Teresa P. Cetlin,Paulo Roberto |
author_role |
author |
author2 |
Poggiali,Flávia S. J. Bezerra,Augusto Cesar S. Figueiredo,Roberto B. Aguilar,Maria Teresa P. Cetlin,Paulo Roberto |
author2_role |
author author author author author |
dc.contributor.author.fl_str_mv |
Soares,Marcela Maira N. S. Poggiali,Flávia S. J. Bezerra,Augusto Cesar S. Figueiredo,Roberto B. Aguilar,Maria Teresa P. Cetlin,Paulo Roberto |
dc.subject.por.fl_str_mv |
Sugar cane bagasse ash pozzolanic activity mineral admixture |
topic |
Sugar cane bagasse ash pozzolanic activity mineral admixture |
description |
The effect of calcination temperature and air flow on the content of organic material, morphology of particles, degree of crystallinity and the reactivity with lime solution of the sugar cane bagasse ash is evaluated. The results show that the long fibers of the bagasse and organic material are retained when calcination occurs without sufficient air flow. Calcining with forced air-flow breaks the fibers, removes organic material and produces fine particles at a temperature of 600ºC. The non-organic material observed in the ash displays a high degree of crystallinity. Experiments show that the crystalline structure observed in the ashes is due to adhered sand which was not previously washed away. The reduction on the conductivity in lime solution and X-rays diffraction pattern suggest that amorphous silica is formed at temperatures lower than 600ºC and cristobalite is formed at higher temperatures. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014-03-01 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000100005 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000100005 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/S0370-44672014000100005 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
text/html |
dc.publisher.none.fl_str_mv |
Escola de Minas |
publisher.none.fl_str_mv |
Escola de Minas |
dc.source.none.fl_str_mv |
Rem: Revista Escola de Minas v.67 n.1 2014 reponame:REM. Revista Escola de Minas (Online) instname:Escola de Minas instacron:ESCOLA DE MINAS |
instname_str |
Escola de Minas |
instacron_str |
ESCOLA DE MINAS |
institution |
ESCOLA DE MINAS |
reponame_str |
REM. Revista Escola de Minas (Online) |
collection |
REM. Revista Escola de Minas (Online) |
repository.name.fl_str_mv |
REM. Revista Escola de Minas (Online) - Escola de Minas |
repository.mail.fl_str_mv |
editor@rem.com.br |
_version_ |
1754122198675619840 |