Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE

Detalhes bibliográficos
Autor(a) principal: Magalhães, Leila Thaís Soares
Data de Publicação: 2009
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Repositório Institucional da UFS
Texto Completo: https://ri.ufs.br/handle/riufs/6610
Resumo: The basin of the river Piauitinga is located in south-central portion of the state of Sergipe, being responsible for water supply in some municipalities Sergipe, which did not avoid the areas around the springs, framed as environmental protection (as forestry code ) are almost in its entirety cleared. Thus, this study seeks to characterize the soils in their local environment to serve as a benchmark for future comparisons between areas of nascent and degraded in the process of recovery and assess physical attributes, chemical and microbiological soil around the springs of this river for more understanding the dynamics of semi-physical. The sources were classified as its recharge and about their conservation status. We selected the areas for revegetation of each source and these were grouped according to their position in the landscape. The environmental and pedological characteristics of the study sites was performed by observing the local landscape, the opening of micro-trenches and tradagens soil. The soils were described and classified morphologically. Slides were prepared for x-ray diffraction of clay. Could a group of springs according to their positions of landscape and local soil characteristics below (BA), with slope horizon A (EA), slope without horizon A (ES), with slope hydromorphic (EH) and foothills of gentle slope (SE). The attributes were analyzed in samples at depths of 0 to 0.1 m and 0.1 to 0.3 m. Were determined: texture, organic particulate matter, stability of macro aggregates, mean diameter of aggregates, the value of color, pH, organic C, Ca, Ca + Mg, Mg, Al, Na, K, P, H + Al, N, sum of bases, cation exchange capacity, base saturation, Al saturation of, microbial respiration, C and N microbial biomass and enzyme activity (FDA). The similarity and / or dissimilarity among sites (spatial) was investigated by multivariate analysis "non-metric multidimensional scaling (NMS), from the distance of Sorensen. Were determined by Pearson's correlation coefficients between the axes of the NMS ordination by and between the different attributes. The sites around the headwaters of the River High Piauitinga positions are distributed in erosicionais (breaking-of-focus), and download a single case of foot gentle slope of the top of coastal tablelands. Its main features are the strong hydromorphic (Gleissolos Cambisols and Haplic Gleissolos), and / or the low level of development (Cambisols and Haplic Plinthosols, both with much skeletal material - quartz and petroplinthite - many with eroded phase). The physical, chemical and biological studied by means of multivariate analysis allowed the construction of an environmental gradient, with decreasing quality of soil in the sequence: BA, EH, EA and ES. It is believed that it is possible redefinitions of strategies for the revegetation of the upper course of the spring basin, extrapolate soil quality in areas of springs of water bodies with similar characteristics and reflect on strategies for restoring degraded areas.
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spelling Magalhães, Leila Thaís Soareshttp://lattes.cnpq.br/9527039294611376Netto, Antenor de Oliveira Aguiarhttp://lattes.cnpq.br/94979556515751392017-10-02T12:49:49Z2017-10-02T12:49:49Z2009-06-19MAGALHÃES, Leila Thaís Soares. Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE. 2009. 109 f. Dissertação (Mestrado em Agroecossistemas) - Universidade Federal de Sergipe, São Cristóvão, 2009.https://ri.ufs.br/handle/riufs/6610The basin of the river Piauitinga is located in south-central portion of the state of Sergipe, being responsible for water supply in some municipalities Sergipe, which did not avoid the areas around the springs, framed as environmental protection (as forestry code ) are almost in its entirety cleared. Thus, this study seeks to characterize the soils in their local environment to serve as a benchmark for future comparisons between areas of nascent and degraded in the process of recovery and assess physical attributes, chemical and microbiological soil around the springs of this river for more understanding the dynamics of semi-physical. The sources were classified as its recharge and about their conservation status. We selected the areas for revegetation of each source and these were grouped according to their position in the landscape. The environmental and pedological characteristics of the study sites was performed by observing the local landscape, the opening of micro-trenches and tradagens soil. The soils were described and classified morphologically. Slides were prepared for x-ray diffraction of clay. Could a group of springs according to their positions of landscape and local soil characteristics below (BA), with slope horizon A (EA), slope without horizon A (ES), with slope hydromorphic (EH) and foothills of gentle slope (SE). The attributes were analyzed in samples at depths of 0 to 0.1 m and 0.1 to 0.3 m. Were determined: texture, organic particulate matter, stability of macro aggregates, mean diameter of aggregates, the value of color, pH, organic C, Ca, Ca + Mg, Mg, Al, Na, K, P, H + Al, N, sum of bases, cation exchange capacity, base saturation, Al saturation of, microbial respiration, C and N microbial biomass and enzyme activity (FDA). The similarity and / or dissimilarity among sites (spatial) was investigated by multivariate analysis "non-metric multidimensional scaling (NMS), from the distance of Sorensen. Were determined by Pearson's correlation coefficients between the axes of the NMS ordination by and between the different attributes. The sites around the headwaters of the River High Piauitinga positions are distributed in erosicionais (breaking-of-focus), and download a single case of foot gentle slope of the top of coastal tablelands. Its main features are the strong hydromorphic (Gleissolos Cambisols and Haplic Gleissolos), and / or the low level of development (Cambisols and Haplic Plinthosols, both with much skeletal material - quartz and petroplinthite - many with eroded phase). The physical, chemical and biological studied by means of multivariate analysis allowed the construction of an environmental gradient, with decreasing quality of soil in the sequence: BA, EH, EA and ES. It is believed that it is possible redefinitions of strategies for the revegetation of the upper course of the spring basin, extrapolate soil quality in areas of springs of water bodies with similar characteristics and reflect on strategies for restoring degraded areas.A bacia hidrográfica do rio Piauitinga está localizada na porção centro-sul do estado de Sergipe, sendo responsável pelo abastecimento de água de alguns municípios sergipanos, o que não evitou que as áreas do entorno de nascentes, enquadradas como de proteção ambiental (conforme código florestal), estejam quase em sua totalidade desmatadas. Assim, o presente estudo procura caracterizar os solos locais na sua ambiência para servir como um referencial em futuras comparações entre áreas de nascentes degradadas e em processo de recuperação e avaliar atributos físicos, químicos e microbiológicos do solo no entorno de nascentes deste rio, para maior entendimento da dinâmica do meio-físico. As nascentes foram classificadas quanto a sua recarga e quanto ao seu estado de conservação. Foram selecionadas as áreas de revegetação de cada nascente e estas foram agrupados de acordo com a sua posição na paisagem. A caracterização ambiental e pedológica dos sítios de estudo foi realizada pela observação da paisagem local, pela abertura de micro-trincheiras e por tradagens dos solos. Os solos foram descritos morfologicamente e classificados. Foram confeccionadas lâminas para a difração de raios-x da fração argila. Foi possível o agrupamento das nascentes de acordo com suas posições de paisagem e das características dos solos locais em baixada (BA), encosta com horizonte A (EA), encosta sem horizonte A (ES), encosta com hidromorfismo (EH) e sopé de encosta suave (SE). Os atributos foram analisados em amostras nas profundidades de 0 a 0,1m e 0,1 a 0,3m. Foram determinados: textura, matéria orgânica particulada, estabilidade de macro agregados, diâmetro médio de agregados, valor da cor, pH, C orgânico, Ca, Ca+Mg, Mg, Al, Na, K, P, H+Al, N, soma de bases, capacidade de troca catiônica, saturação de bases, saturação de Al, respiração microbiana, C e N da biomassa microbiana e atividade enzimática (FDA). A similaridade e/ou, dissimilaridade entre os sítios (ordenamento) foi averiguada pela análise multivariada non-metric multidimensional scaling (NMS), a partir da distância de Sorensen. Determinaram-se os coeficientes de correlação de Pearson entre os eixos da ordenação por NMS e entre os diferentes atributos. Os sítios do entorno das nascentes do alto curso do rio Piauitinga estão distribuídos em posições erosicionais (quebra-de-relevo), baixadas e um único caso de sopé de encosta suave de topo de tabuleiros costeiros. Suas principais características são o forte hidromorfismo (Gleissolos e Cambissolos Háplicos gleissólicos) e/ou, o baixo grau de desenvolvimento (Cambissolos Háplicos e Plintossolos, ambos com muito material esquelético quartzo e petroplintita muitos com fase erodida). As variáveis físicas, químicas e biológicas estudadas, por meio da análise multivariada, permitiram a construção de um gradiente ambiental, com a qualidade dos solos decrescente na seqüência: BA, EH, EA e ES. Acredita-se que seja possível redefinições de estratégias para a revegetação das nascentes do alto curso dessa bacia hidrográfica, extrapolar a qualidade do solo para áreas de nascentes de cursos d água com características semelhantes e refletir sobre estratégias para restauração de áreas degradadas.application/pdfporUniversidade Federal de SergipePós-Graduação em AgroecossistemasUFSBRAnálise químicaAnálise físicaAnálise microbiológicaBacia hidrográficaNascentesRio Piauitinga (SE)Chemical analysisPhysical analysisMicrobiologicalRiver basinSpringsRiver Piauitinga (SE)CNPQ::CIENCIAS AGRARIAS::AGRONOMIAQualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SEQUALITY OF SOIL IN AREAS OF HIGH SOURCE OF THE RIVER PIAUITINGA, LAGARTO-SEinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFSinstname:Universidade Federal de Sergipe (UFS)instacron:UFSORIGINALLEILA_THAIS_SOARES_MAGALHAES.pdfapplication/pdf27763891https://ri.ufs.br/jspui/bitstream/riufs/6610/1/LEILA_THAIS_SOARES_MAGALHAES.pdf5332b23049dac7da5015638c6b8d1e03MD51TEXTLEILA_THAIS_SOARES_MAGALHAES.pdf.txtLEILA_THAIS_SOARES_MAGALHAES.pdf.txtExtracted texttext/plain181303https://ri.ufs.br/jspui/bitstream/riufs/6610/2/LEILA_THAIS_SOARES_MAGALHAES.pdf.txt020ef8bf14890a57e26c3cbd1f723c36MD52THUMBNAILLEILA_THAIS_SOARES_MAGALHAES.pdf.jpgLEILA_THAIS_SOARES_MAGALHAES.pdf.jpgGenerated Thumbnailimage/jpeg1319https://ri.ufs.br/jspui/bitstream/riufs/6610/3/LEILA_THAIS_SOARES_MAGALHAES.pdf.jpge5a462add559a0447182d9916efcf21fMD53riufs/66102017-11-24 21:04:16.983oai:ufs.br:riufs/6610Repositório InstitucionalPUBhttps://ri.ufs.br/oai/requestrepositorio@academico.ufs.bropendoar:2017-11-25T00:04:16Repositório Institucional da UFS - Universidade Federal de Sergipe (UFS)false
dc.title.por.fl_str_mv Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
dc.title.alternative.eng.fl_str_mv QUALITY OF SOIL IN AREAS OF HIGH SOURCE OF THE RIVER PIAUITINGA, LAGARTO-SE
title Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
spellingShingle Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
Magalhães, Leila Thaís Soares
Análise química
Análise física
Análise microbiológica
Bacia hidrográfica
Nascentes
Rio Piauitinga (SE)
Chemical analysis
Physical analysis
Microbiological
River basin
Springs
River Piauitinga (SE)
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
title_short Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
title_full Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
title_fullStr Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
title_full_unstemmed Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
title_sort Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE
author Magalhães, Leila Thaís Soares
author_facet Magalhães, Leila Thaís Soares
author_role author
dc.contributor.author.fl_str_mv Magalhães, Leila Thaís Soares
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/9527039294611376
dc.contributor.advisor1.fl_str_mv Netto, Antenor de Oliveira Aguiar
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/9497955651575139
contributor_str_mv Netto, Antenor de Oliveira Aguiar
dc.subject.por.fl_str_mv Análise química
Análise física
Análise microbiológica
Bacia hidrográfica
Nascentes
Rio Piauitinga (SE)
topic Análise química
Análise física
Análise microbiológica
Bacia hidrográfica
Nascentes
Rio Piauitinga (SE)
Chemical analysis
Physical analysis
Microbiological
River basin
Springs
River Piauitinga (SE)
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
dc.subject.eng.fl_str_mv Chemical analysis
Physical analysis
Microbiological
River basin
Springs
River Piauitinga (SE)
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
description The basin of the river Piauitinga is located in south-central portion of the state of Sergipe, being responsible for water supply in some municipalities Sergipe, which did not avoid the areas around the springs, framed as environmental protection (as forestry code ) are almost in its entirety cleared. Thus, this study seeks to characterize the soils in their local environment to serve as a benchmark for future comparisons between areas of nascent and degraded in the process of recovery and assess physical attributes, chemical and microbiological soil around the springs of this river for more understanding the dynamics of semi-physical. The sources were classified as its recharge and about their conservation status. We selected the areas for revegetation of each source and these were grouped according to their position in the landscape. The environmental and pedological characteristics of the study sites was performed by observing the local landscape, the opening of micro-trenches and tradagens soil. The soils were described and classified morphologically. Slides were prepared for x-ray diffraction of clay. Could a group of springs according to their positions of landscape and local soil characteristics below (BA), with slope horizon A (EA), slope without horizon A (ES), with slope hydromorphic (EH) and foothills of gentle slope (SE). The attributes were analyzed in samples at depths of 0 to 0.1 m and 0.1 to 0.3 m. Were determined: texture, organic particulate matter, stability of macro aggregates, mean diameter of aggregates, the value of color, pH, organic C, Ca, Ca + Mg, Mg, Al, Na, K, P, H + Al, N, sum of bases, cation exchange capacity, base saturation, Al saturation of, microbial respiration, C and N microbial biomass and enzyme activity (FDA). The similarity and / or dissimilarity among sites (spatial) was investigated by multivariate analysis "non-metric multidimensional scaling (NMS), from the distance of Sorensen. Were determined by Pearson's correlation coefficients between the axes of the NMS ordination by and between the different attributes. The sites around the headwaters of the River High Piauitinga positions are distributed in erosicionais (breaking-of-focus), and download a single case of foot gentle slope of the top of coastal tablelands. Its main features are the strong hydromorphic (Gleissolos Cambisols and Haplic Gleissolos), and / or the low level of development (Cambisols and Haplic Plinthosols, both with much skeletal material - quartz and petroplinthite - many with eroded phase). The physical, chemical and biological studied by means of multivariate analysis allowed the construction of an environmental gradient, with decreasing quality of soil in the sequence: BA, EH, EA and ES. It is believed that it is possible redefinitions of strategies for the revegetation of the upper course of the spring basin, extrapolate soil quality in areas of springs of water bodies with similar characteristics and reflect on strategies for restoring degraded areas.
publishDate 2009
dc.date.issued.fl_str_mv 2009-06-19
dc.date.accessioned.fl_str_mv 2017-10-02T12:49:49Z
dc.date.available.fl_str_mv 2017-10-02T12:49:49Z
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dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
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dc.identifier.citation.fl_str_mv MAGALHÃES, Leila Thaís Soares. Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE. 2009. 109 f. Dissertação (Mestrado em Agroecossistemas) - Universidade Federal de Sergipe, São Cristóvão, 2009.
dc.identifier.uri.fl_str_mv https://ri.ufs.br/handle/riufs/6610
identifier_str_mv MAGALHÃES, Leila Thaís Soares. Qualidade dos solos nas áreas de nascentes do alto curso do rio Piauitinga, Lagarto - SE. 2009. 109 f. Dissertação (Mestrado em Agroecossistemas) - Universidade Federal de Sergipe, São Cristóvão, 2009.
url https://ri.ufs.br/handle/riufs/6610
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dc.publisher.program.fl_str_mv Pós-Graduação em Agroecossistemas
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publisher.none.fl_str_mv Universidade Federal de Sergipe
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