Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different?
Main Author: | |
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Publication Date: | 2019 |
Other Authors: | |
Format: | Article |
Language: | eng |
Source: | Materials research (São Carlos. Online) |
Download full: | http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392019000700245 |
Summary: | A comparative investigation on the firing behavior of a natural kaolinitic clay from Campos dos Goytacazes, Brazil, and its specific clay fraction was performed. The clay fraction, equivalent diameter less than 2 µm, was separated from the precursor clay by a sedimentation method. Chemical analysis, X-ray diffraction (XRD) and scanning electron microscopy were used to characterize the unfired materials. Thermoanalysis and dilatometry were applied to follow the structural transformations. The firing behavior was studied by water absorption and XRD of samples fired in the temperature range from 400 to 1100°C. Differences were found between the natural kaolinitic clay and its clay fraction. The absence of quartz and smaller particles of the clay fraction result in a comparatively lower temperature for structural consolidation associated with reduced open porosity. This can be attributed to solid state sintering alone, in contrast to a higher temperature liquid phase sintering needed for complete consolidation of the natural kaolinitic clay. |
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Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different?Clay fractionkaolinitic clayfiringsolid state sinteringliquid phase sinteringporosityA comparative investigation on the firing behavior of a natural kaolinitic clay from Campos dos Goytacazes, Brazil, and its specific clay fraction was performed. The clay fraction, equivalent diameter less than 2 µm, was separated from the precursor clay by a sedimentation method. Chemical analysis, X-ray diffraction (XRD) and scanning electron microscopy were used to characterize the unfired materials. Thermoanalysis and dilatometry were applied to follow the structural transformations. The firing behavior was studied by water absorption and XRD of samples fired in the temperature range from 400 to 1100°C. Differences were found between the natural kaolinitic clay and its clay fraction. The absence of quartz and smaller particles of the clay fraction result in a comparatively lower temperature for structural consolidation associated with reduced open porosity. This can be attributed to solid state sintering alone, in contrast to a higher temperature liquid phase sintering needed for complete consolidation of the natural kaolinitic clay.ABM, ABC, ABPol2019-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392019000700245Materials Research v.22 suppl.1 2019reponame:Materials research (São Carlos. Online)instname:Universidade Federal de São Carlos (UFSCAR)instacron:ABM ABC ABPOL10.1590/1980-5373-mr-2019-0172info:eu-repo/semantics/openAccessVieira,Carlos Maurício FontesMonteiro,Sergio Neveseng2019-10-18T00:00:00Zoai:scielo:S1516-14392019000700245Revistahttp://www.scielo.br/mrPUBhttps://old.scielo.br/oai/scielo-oai.phpdedz@power.ufscar.br1980-53731516-1439opendoar:2019-10-18T00:00Materials research (São Carlos. Online) - Universidade Federal de São Carlos (UFSCAR)false |
dc.title.none.fl_str_mv |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
title |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
spellingShingle |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? Vieira,Carlos Maurício Fontes Clay fraction kaolinitic clay firing solid state sintering liquid phase sintering porosity |
title_short |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
title_full |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
title_fullStr |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
title_full_unstemmed |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
title_sort |
Firing Behavior of the Clay Fraction of a Natural Kaolinitic Clay: Are They Different? |
author |
Vieira,Carlos Maurício Fontes |
author_facet |
Vieira,Carlos Maurício Fontes Monteiro,Sergio Neves |
author_role |
author |
author2 |
Monteiro,Sergio Neves |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Vieira,Carlos Maurício Fontes Monteiro,Sergio Neves |
dc.subject.por.fl_str_mv |
Clay fraction kaolinitic clay firing solid state sintering liquid phase sintering porosity |
topic |
Clay fraction kaolinitic clay firing solid state sintering liquid phase sintering porosity |
description |
A comparative investigation on the firing behavior of a natural kaolinitic clay from Campos dos Goytacazes, Brazil, and its specific clay fraction was performed. The clay fraction, equivalent diameter less than 2 µm, was separated from the precursor clay by a sedimentation method. Chemical analysis, X-ray diffraction (XRD) and scanning electron microscopy were used to characterize the unfired materials. Thermoanalysis and dilatometry were applied to follow the structural transformations. The firing behavior was studied by water absorption and XRD of samples fired in the temperature range from 400 to 1100°C. Differences were found between the natural kaolinitic clay and its clay fraction. The absence of quartz and smaller particles of the clay fraction result in a comparatively lower temperature for structural consolidation associated with reduced open porosity. This can be attributed to solid state sintering alone, in contrast to a higher temperature liquid phase sintering needed for complete consolidation of the natural kaolinitic clay. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-01-01 |
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=S1516-14392019000700245 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392019000700245 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/1980-5373-mr-2019-0172 |
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 |
ABM, ABC, ABPol |
publisher.none.fl_str_mv |
ABM, ABC, ABPol |
dc.source.none.fl_str_mv |
Materials Research v.22 suppl.1 2019 reponame:Materials research (São Carlos. Online) instname:Universidade Federal de São Carlos (UFSCAR) instacron:ABM ABC ABPOL |
instname_str |
Universidade Federal de São Carlos (UFSCAR) |
instacron_str |
ABM ABC ABPOL |
institution |
ABM ABC ABPOL |
reponame_str |
Materials research (São Carlos. Online) |
collection |
Materials research (São Carlos. Online) |
repository.name.fl_str_mv |
Materials research (São Carlos. Online) - Universidade Federal de São Carlos (UFSCAR) |
repository.mail.fl_str_mv |
dedz@power.ufscar.br |
_version_ |
1754212676047732736 |