Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs)
| Ano de defesa: | 2012 |
|---|---|
| Autor(a) principal: |
Jeune, Wesly
 |
| Orientador(a): |
Francelino, M?rcio Rocha
|
| Banca de defesa: | , |
| Tipo de documento: | Dissertação |
| Tipo de acesso: | Acesso aberto |
| Idioma: | por |
| Instituição de defesa: |
Universidade Federal Rural do Rio de Janeiro
|
| Programa de Pós-Graduação: |
Programa de P?s-Gradua??o em Agronomia - Ci?ncia do Solo
|
| Departamento: |
Instituto de Agronomia
|
| País: |
Brasil
|
| Palavras-chave em Português: | |
| Palavras-chave em Inglês: | |
| Área do conhecimento CNPq: | |
| Link de acesso: | https://tede.ufrrj.br/jspui/handle/jspui/3557 |
Resumo: | This study aimed to model the soil attribute bulk density (BD) by pedotransfer function (PTFs), spatializing it and afterwards mapping the carbon stock (CS) in Guapi-Macacu watershed, in state of Rio de Janeiro, based on Digital Soil Mapping (DSM) methodology. The data used is derived from a high intensity soil survey carried out by ??EMBRAPA Solos?? during the last quarter of 2010 in the area. Thus, 99 soil profiles were sampled and analyzed, and of those, 66 had bulk density values determined. To validate the PTFs developed in the process, comparison with published functions was made from 13 samples that had been reserved. Two bulk density functions were derived from multiple linear regression and nonlinear regression, using 16 variables and relying on the statistical software Statgraphics Centurion XVI. Stepwise procedures and Comparison of Alternative models of the related program helped to choose the best models which have greater simplicity, normal residuals, larger R2, and minimum error. Nevertheless, the non-linear model, the one which involves the single organic carbon (OC) variable and which is easier to be determined, was used for spatialization of BD. This function allowed assessing BD value for the other soil profiles. Geostatistical analysis (semivariogram) performed from GS+ 9 program, showed spatial correlation of A horizon thickness, while OC exhibited high randomness. Since, A horizon thickness was spatialized through kriging interpolator, OC interpolated by the deterministic interpolator IDW (Inverse Distance weight) and BD mapped by using his pedotransfer function through Raster Calculator tools of ArcGIS v. 10. Bulk density varied from 0.87 and 1.95 Mg.m-3. Finally, the estimated carbon stock (CS= Ds.C.E/10, Mg.ha-1) range was 9.2 to 212.2 Mg.ha-1, and was spatialized following the same bulk density process. Variance analysis of CS mapped regarding land use and slope classes were performed by Fisher LSD test. The results indicated that among the different land use classes, only pasture and altitude vegetation are significantly different at 5% risk. For the six slope classes, has been observed significant difference exclusively between flat land and steep area at 5% risk |
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Francelino, M?rcio Rocha825.207.127-91http://lattes.cnpq.br/1335748426615308Carvalho Junior, Waldir dehttp://lattes.cnpq.br/7992394393174495Vasques, Gustavo M.Menezes, Michele Duarte de061.101.297-98http://lattes.cnpq.br/1246058339032923Jeune, Wesly2020-05-26T13:16:15Z2012-02-24JEUNE, Wesly. Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs). 2012. 52 f. Disserta??o (Mestrado em Agronomia - Ci?ncia do Solo) - Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, Serop?dica, 2012.https://tede.ufrrj.br/jspui/handle/jspui/3557This study aimed to model the soil attribute bulk density (BD) by pedotransfer function (PTFs), spatializing it and afterwards mapping the carbon stock (CS) in Guapi-Macacu watershed, in state of Rio de Janeiro, based on Digital Soil Mapping (DSM) methodology. The data used is derived from a high intensity soil survey carried out by ??EMBRAPA Solos?? during the last quarter of 2010 in the area. Thus, 99 soil profiles were sampled and analyzed, and of those, 66 had bulk density values determined. To validate the PTFs developed in the process, comparison with published functions was made from 13 samples that had been reserved. Two bulk density functions were derived from multiple linear regression and nonlinear regression, using 16 variables and relying on the statistical software Statgraphics Centurion XVI. Stepwise procedures and Comparison of Alternative models of the related program helped to choose the best models which have greater simplicity, normal residuals, larger R2, and minimum error. Nevertheless, the non-linear model, the one which involves the single organic carbon (OC) variable and which is easier to be determined, was used for spatialization of BD. This function allowed assessing BD value for the other soil profiles. Geostatistical analysis (semivariogram) performed from GS+ 9 program, showed spatial correlation of A horizon thickness, while OC exhibited high randomness. Since, A horizon thickness was spatialized through kriging interpolator, OC interpolated by the deterministic interpolator IDW (Inverse Distance weight) and BD mapped by using his pedotransfer function through Raster Calculator tools of ArcGIS v. 10. Bulk density varied from 0.87 and 1.95 Mg.m-3. Finally, the estimated carbon stock (CS= Ds.C.E/10, Mg.ha-1) range was 9.2 to 212.2 Mg.ha-1, and was spatialized following the same bulk density process. Variance analysis of CS mapped regarding land use and slope classes were performed by Fisher LSD test. The results indicated that among the different land use classes, only pasture and altitude vegetation are significantly different at 5% risk. For the six slope classes, has been observed significant difference exclusively between flat land and steep area at 5% riskO presente trabalho teve como objetivo estimar e mapear a densidade do solo (Ds) e o estoque de carbono (EC) na bacia hidrogr?fica Guapi-Macacu, no Estado do Rio de Janeiro, utilizando metodologia de Mapeamento Digital de Solos (MDS). Os dados foram originados do levantamento de solos de alta intensidade, realizado pela EMBRAPA Solos durante o ?ltimo trimestre de 2010 na regi?o de estudo. Nessa etapa foram amostrados 99 perfis e destes, 66 tiveram valores de densidade determinados. Para validar as fun??es de pedotransfer?ncia desenvolvidas, 13 amostras foram reservadas e utilizadas na compara??o com outras fun??es obtidas na literatura. Na an?lise do estoque de carbono, classes de cobertura do solo e de declividade foram usadas. Duas fun??es de pedotransfer?ncia da densidade do solo (Ds) foram derivadas a partir da regress?o linear m?ltipla e da regress?o n?o linear, utilizando 16 vari?veis do solo e auxiliando-se no aplicativo estat?stico Statgraphics Centurion XVI. Os procedimentos Stepwise e Comparison of Alternative models do referente programa permitiram escolher os melhores modelos mais simples, com res?duos normais, R2 maior e erro m?nimo. No entanto, o modelo n?o linear, envolvendo somente a vari?vel carbono org?nico (C) foi utilizado para a espacializa??o da Ds. Essa fun??o permitiu estimar os valores de Ds para os outros perfis. A espessura do horizonte A apresentou correla??o espacial na an?lise geoestat?stica realizada no programa GS+ 9, enquanto o C apresentou alta aleatoriedade. Em fun??o disso, a espessura foi interpolada atrav?s da krigagem, o Corg atrav?s do interpolador determin?stico IDW (Inverse Distance weight) e a Ds espacializada pela pr?pria fun??o de pedotransfer?ncia, usando a ferramenta Raster Calculator do programa ArcGIS v. 10. A Ds variou de 0,87 a 1,95 Mg.m-3 e o estoque de carbono (Ec= Ds.C.E/10, em Mg.ha-1) de 9,2 a 212,2 Mg.ha-1. A an?lise de vari?ncia do estoque de carbono mapeado com rela??o ao uso do solo e as classes de declividade foi realizada atrav?s do teste LSD (Least significant difference) de Fisher. O resultado indicou que entre as classes de uso existe diferen?a significativa ao n?vel 5% de signific?ncia apenas entre as classes pastagem e campo de altitude. Para as seis classes de relevo, observou-se diferen?a significativa somente entre relevo plano e escarpado ao n?vel de 5%.Submitted by Celso Magalhaes (celsomagalhaes@ufrrj.br) on 2020-05-26T13:16:15Z No. of bitstreams: 1 2012 - Wesly Jeune.pdf: 3487608 bytes, checksum: ea3b30e909a15f93aabf038f993c6c63 (MD5)Made available in DSpace on 2020-05-26T13:16:15Z (GMT). No. of bitstreams: 1 2012 - Wesly Jeune.pdf: 3487608 bytes, checksum: ea3b30e909a15f93aabf038f993c6c63 (MD5) Previous issue date: 2012-02-24Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gico - CNPQapplication/pdfhttps://tede.ufrrj.br/retrieve/59844/2012%20-%20Wesly%20Jeune.pdf.jpgporUniversidade Federal Rural do Rio de JaneiroPrograma de P?s-Gradua??o em Agronomia - Ci?ncia do SoloUFRRJBrasilInstituto de AgronomiaAMADOR, E. S. Ba?a de Guanabara e Ecossistemas Perif?ricos: homem e natureza. Tese de Doutorado. PPGG Instituto de Geoci?ncias/UFRJ, Ed. Reproarte Gr?fica e Editora, 1997. 539p. ARROUAYS, D., PELISSIER, P. 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Texture and organic carbon relations described by a profile pedotransfer function for Brazilian Cerrado soils. 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| dc.title.por.fl_str_mv |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| dc.title.alternative.eng.fl_str_mv |
Spatialization of the soil bulk density and carbon stock in Guapi-Macacu (RJ) Basin, assessed by pedotransfer functions (PTFs) |
| title |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| spellingShingle |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) Jeune, Wesly Mapeamento digital An?lise multivariada Modelagem Digital mapping Multivariate analysis Modeling Agronomia |
| title_short |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| title_full |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| title_fullStr |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| title_full_unstemmed |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| title_sort |
Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs) |
| author |
Jeune, Wesly |
| author_facet |
Jeune, Wesly |
| author_role |
author |
| dc.contributor.advisor1.fl_str_mv |
Francelino, M?rcio Rocha |
| dc.contributor.advisor1ID.fl_str_mv |
825.207.127-91 |
| dc.contributor.advisor1Lattes.fl_str_mv |
http://lattes.cnpq.br/1335748426615308 |
| dc.contributor.advisor-co1.fl_str_mv |
Carvalho Junior, Waldir de |
| dc.contributor.advisor-co1Lattes.fl_str_mv |
http://lattes.cnpq.br/7992394393174495 |
| dc.contributor.referee1.fl_str_mv |
Vasques, Gustavo M. |
| dc.contributor.referee2.fl_str_mv |
Menezes, Michele Duarte de |
| dc.contributor.authorID.fl_str_mv |
061.101.297-98 |
| dc.contributor.authorLattes.fl_str_mv |
http://lattes.cnpq.br/1246058339032923 |
| dc.contributor.author.fl_str_mv |
Jeune, Wesly |
| contributor_str_mv |
Francelino, M?rcio Rocha Carvalho Junior, Waldir de Vasques, Gustavo M. Menezes, Michele Duarte de |
| dc.subject.por.fl_str_mv |
Mapeamento digital An?lise multivariada Modelagem |
| topic |
Mapeamento digital An?lise multivariada Modelagem Digital mapping Multivariate analysis Modeling Agronomia |
| dc.subject.eng.fl_str_mv |
Digital mapping Multivariate analysis Modeling |
| dc.subject.cnpq.fl_str_mv |
Agronomia |
| description |
This study aimed to model the soil attribute bulk density (BD) by pedotransfer function (PTFs), spatializing it and afterwards mapping the carbon stock (CS) in Guapi-Macacu watershed, in state of Rio de Janeiro, based on Digital Soil Mapping (DSM) methodology. The data used is derived from a high intensity soil survey carried out by ??EMBRAPA Solos?? during the last quarter of 2010 in the area. Thus, 99 soil profiles were sampled and analyzed, and of those, 66 had bulk density values determined. To validate the PTFs developed in the process, comparison with published functions was made from 13 samples that had been reserved. Two bulk density functions were derived from multiple linear regression and nonlinear regression, using 16 variables and relying on the statistical software Statgraphics Centurion XVI. Stepwise procedures and Comparison of Alternative models of the related program helped to choose the best models which have greater simplicity, normal residuals, larger R2, and minimum error. Nevertheless, the non-linear model, the one which involves the single organic carbon (OC) variable and which is easier to be determined, was used for spatialization of BD. This function allowed assessing BD value for the other soil profiles. Geostatistical analysis (semivariogram) performed from GS+ 9 program, showed spatial correlation of A horizon thickness, while OC exhibited high randomness. Since, A horizon thickness was spatialized through kriging interpolator, OC interpolated by the deterministic interpolator IDW (Inverse Distance weight) and BD mapped by using his pedotransfer function through Raster Calculator tools of ArcGIS v. 10. Bulk density varied from 0.87 and 1.95 Mg.m-3. Finally, the estimated carbon stock (CS= Ds.C.E/10, Mg.ha-1) range was 9.2 to 212.2 Mg.ha-1, and was spatialized following the same bulk density process. Variance analysis of CS mapped regarding land use and slope classes were performed by Fisher LSD test. The results indicated that among the different land use classes, only pasture and altitude vegetation are significantly different at 5% risk. For the six slope classes, has been observed significant difference exclusively between flat land and steep area at 5% risk |
| publishDate |
2012 |
| dc.date.issued.fl_str_mv |
2012-02-24 |
| dc.date.accessioned.fl_str_mv |
2020-05-26T13:16:15Z |
| dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
| dc.type.driver.fl_str_mv |
info:eu-repo/semantics/masterThesis |
| format |
masterThesis |
| status_str |
publishedVersion |
| dc.identifier.citation.fl_str_mv |
JEUNE, Wesly. Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs). 2012. 52 f. Disserta??o (Mestrado em Agronomia - Ci?ncia do Solo) - Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, Serop?dica, 2012. |
| dc.identifier.uri.fl_str_mv |
https://tede.ufrrj.br/jspui/handle/jspui/3557 |
| identifier_str_mv |
JEUNE, Wesly. Espacializa??o da densidade do solo e do estoque de carbono da Bacia Guapi-Macacu/RJ, determinados por meio de fun??es de pedotransfer?ncia (FPTs). 2012. 52 f. Disserta??o (Mestrado em Agronomia - Ci?ncia do Solo) - Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, Serop?dica, 2012. |
| url |
https://tede.ufrrj.br/jspui/handle/jspui/3557 |
| dc.language.iso.fl_str_mv |
por |
| language |
por |
| dc.relation.references.por.fl_str_mv |
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