Planosol soil sample size for computerized tomography measurement of physical parameters
Autor(a) principal: | |
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Data de Publicação: | 2003 |
Outros Autores: | , , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Scientia Agrícola (Online) |
Texto Completo: | http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162003000400019 |
Resumo: | Computerized tomography (CT) is an important tool in Soil Science for noninvasive measurement of density and water content of soil samples. This work aims to describe the aspects of sample size adequacy for Planosol (Albaqualf) and to evaluate procedures for statistical analysis, using a CT scanner with a 241Am source. Density errors attributed to the equipment are 0.051 and 0.046 Mg m-3 for horizons A and B, respectively. The theoretical value for sample thickness for the Planosol, using this equipment, is 4.0 cm for the horizons A and B. The ideal thickness of samples is approximately 6.0 cm, being smaller for samples of the horizon B in relation to A. Alternatives for the improvement of the efficiency analysis and the reliability of the results obtained by CT are also discussed, and indicate good precision and adaptability of the application of this technology in Planosol (Albaqualf) studies. |
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Scientia Agrícola (Online) |
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Planosol soil sample size for computerized tomography measurement of physical parameterslowlandalbaqualfbulk densitycompactionsoil moistureComputerized tomography (CT) is an important tool in Soil Science for noninvasive measurement of density and water content of soil samples. This work aims to describe the aspects of sample size adequacy for Planosol (Albaqualf) and to evaluate procedures for statistical analysis, using a CT scanner with a 241Am source. Density errors attributed to the equipment are 0.051 and 0.046 Mg m-3 for horizons A and B, respectively. The theoretical value for sample thickness for the Planosol, using this equipment, is 4.0 cm for the horizons A and B. The ideal thickness of samples is approximately 6.0 cm, being smaller for samples of the horizon B in relation to A. Alternatives for the improvement of the efficiency analysis and the reliability of the results obtained by CT are also discussed, and indicate good precision and adaptability of the application of this technology in Planosol (Albaqualf) studies.Escola Superior de Agricultura "Luiz de Queiroz"2003-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162003000400019Scientia Agricola v.60 n.4 2003reponame:Scientia Agrícola (Online)instname:Universidade de São Paulo (USP)instacron:USP10.1590/S0103-90162003000400019info:eu-repo/semantics/openAccessPedrotti,AlceuPauletto,Eloy AntonioCrestana,SilvioCruvinel,Paulo EstevãoVaz,Carlos Manoel PedroNaime,João de MendonçaSilva,Alvaro Macedo daeng2003-10-24T00:00:00Zoai:scielo:S0103-90162003000400019Revistahttp://revistas.usp.br/sa/indexPUBhttps://old.scielo.br/oai/scielo-oai.phpscientia@usp.br||alleoni@usp.br1678-992X0103-9016opendoar:2003-10-24T00:00Scientia Agrícola (Online) - Universidade de São Paulo (USP)false |
dc.title.none.fl_str_mv |
Planosol soil sample size for computerized tomography measurement of physical parameters |
title |
Planosol soil sample size for computerized tomography measurement of physical parameters |
spellingShingle |
Planosol soil sample size for computerized tomography measurement of physical parameters Pedrotti,Alceu lowland albaqualf bulk density compaction soil moisture |
title_short |
Planosol soil sample size for computerized tomography measurement of physical parameters |
title_full |
Planosol soil sample size for computerized tomography measurement of physical parameters |
title_fullStr |
Planosol soil sample size for computerized tomography measurement of physical parameters |
title_full_unstemmed |
Planosol soil sample size for computerized tomography measurement of physical parameters |
title_sort |
Planosol soil sample size for computerized tomography measurement of physical parameters |
author |
Pedrotti,Alceu |
author_facet |
Pedrotti,Alceu Pauletto,Eloy Antonio Crestana,Silvio Cruvinel,Paulo Estevão Vaz,Carlos Manoel Pedro Naime,João de Mendonça Silva,Alvaro Macedo da |
author_role |
author |
author2 |
Pauletto,Eloy Antonio Crestana,Silvio Cruvinel,Paulo Estevão Vaz,Carlos Manoel Pedro Naime,João de Mendonça Silva,Alvaro Macedo da |
author2_role |
author author author author author author |
dc.contributor.author.fl_str_mv |
Pedrotti,Alceu Pauletto,Eloy Antonio Crestana,Silvio Cruvinel,Paulo Estevão Vaz,Carlos Manoel Pedro Naime,João de Mendonça Silva,Alvaro Macedo da |
dc.subject.por.fl_str_mv |
lowland albaqualf bulk density compaction soil moisture |
topic |
lowland albaqualf bulk density compaction soil moisture |
description |
Computerized tomography (CT) is an important tool in Soil Science for noninvasive measurement of density and water content of soil samples. This work aims to describe the aspects of sample size adequacy for Planosol (Albaqualf) and to evaluate procedures for statistical analysis, using a CT scanner with a 241Am source. Density errors attributed to the equipment are 0.051 and 0.046 Mg m-3 for horizons A and B, respectively. The theoretical value for sample thickness for the Planosol, using this equipment, is 4.0 cm for the horizons A and B. The ideal thickness of samples is approximately 6.0 cm, being smaller for samples of the horizon B in relation to A. Alternatives for the improvement of the efficiency analysis and the reliability of the results obtained by CT are also discussed, and indicate good precision and adaptability of the application of this technology in Planosol (Albaqualf) studies. |
publishDate |
2003 |
dc.date.none.fl_str_mv |
2003-12-01 |
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=S0103-90162003000400019 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162003000400019 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/S0103-90162003000400019 |
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 Superior de Agricultura "Luiz de Queiroz" |
publisher.none.fl_str_mv |
Escola Superior de Agricultura "Luiz de Queiroz" |
dc.source.none.fl_str_mv |
Scientia Agricola v.60 n.4 2003 reponame:Scientia Agrícola (Online) instname:Universidade de São Paulo (USP) instacron:USP |
instname_str |
Universidade de São Paulo (USP) |
instacron_str |
USP |
institution |
USP |
reponame_str |
Scientia Agrícola (Online) |
collection |
Scientia Agrícola (Online) |
repository.name.fl_str_mv |
Scientia Agrícola (Online) - Universidade de São Paulo (USP) |
repository.mail.fl_str_mv |
scientia@usp.br||alleoni@usp.br |
_version_ |
1748936459196301312 |