Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar
Ano de defesa: | 2016 |
---|---|
Autor(a) principal: | |
Orientador(a): | |
Banca de defesa: | , |
Tipo de documento: | Dissertação |
Tipo de acesso: | Acesso aberto |
Idioma: | por |
Instituição de defesa: |
Universidade Federal Rural do Semi-Árido
|
Programa de Pós-Graduação: |
Programa de Pós-graduação em Manejo de Solo e Água
|
Departamento: |
Não Informado pela instituição
|
País: |
Brasil
|
Palavras-chave em Português: | |
Área do conhecimento CNPq: | |
Link de acesso: | http://repositorio.ufersa.edu.br/handle/tede/622 |
Resumo: | In understanding a more appropriate management, the soil survey in a region it has a fundamental importance. Thus, a constant updating of the soil classes is necessary for the various agricultural uses are analyzed and established the most appropriate way possible. The Rio Grande do Norte has hills formations that differ from the soil and climatic conditions prevailing in the state, with deeper soils and acidic and milder weather. Among these formations, there is the Santana’s Hill, which is embedded in the Martins Formation with deposits settled in disagreement over the lens and inserted basis in the Potiguar Seridó region, with important agricultural use for the region, with mainly cashew cultivation and cassava. With this, the objective of this study was to understand the genesis of representative soils of the Santana’s Hill and draw up an exploratory soil map of the region. Morphological, physical, chemical and mineralogical analyzes of representative profiles were performed that make up the Santana’s Hill. Representative profiles were classified as Typic Haplustox; Xanthic Eutrustox; Typic Eutrustox; Ustic Quartzipsamments; Lithic Ustorthents; Typic Ustipsamments and Dystric Haplustepts. By observing morphological attributes it was noticed that there was a great influence of the parent material factor in distinguishing the main soil types found in the study area, since the topography and climatic conditions are similar throughout the territorial extension. The textural class of the profiles studied ranged from sandy to sandy-clay-sandy due to high existing levels in sand horizons, identifying minerals that were more resistant to weathering process and the strong link with the material of sedimentary origin. All profiles showed acid reaction, wide range of base saturation between profiles and low values of electrical conductivity. The mineralogical composition of the clay fraction of the profiles were similar, with clay type Illite/Mica, Kaolinite and Goethite, and Quartz peaks. The use of GIS allows updating existing soil classes in the Santana’s Hill, as well as updating the percentage of occupation of each soil type |
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Martins, Carolina Malala05165780490Silva, Paulo Cesar Moura da91358540497http://lattes.cnpq.br/4070582933073155Silva, Eulene Francisco da86629760182http://lattes.cnpq.br/4243362476220476Ernesto Sobrinho, Francisco06745210487http://lattes.cnpq.br/694215601104013508248891429http://lattes.cnpq.br/7691085061826580http://lattes.cnpq.br/9637230855429508Farias, Phamella Kalliny Pereira2017-03-21T15:05:51Z2016-02-22FARIAS, Phamella Kalliny Pereira. Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar. 2016. 82 f. Dissertação (Mestrado) - Curso de Pós-graduação em Manejo de Solo e Água, Universidade Federal Rural do Semi-Árido, Mossoró, 2016.http://repositorio.ufersa.edu.br/handle/tede/622In understanding a more appropriate management, the soil survey in a region it has a fundamental importance. Thus, a constant updating of the soil classes is necessary for the various agricultural uses are analyzed and established the most appropriate way possible. The Rio Grande do Norte has hills formations that differ from the soil and climatic conditions prevailing in the state, with deeper soils and acidic and milder weather. Among these formations, there is the Santana’s Hill, which is embedded in the Martins Formation with deposits settled in disagreement over the lens and inserted basis in the Potiguar Seridó region, with important agricultural use for the region, with mainly cashew cultivation and cassava. With this, the objective of this study was to understand the genesis of representative soils of the Santana’s Hill and draw up an exploratory soil map of the region. Morphological, physical, chemical and mineralogical analyzes of representative profiles were performed that make up the Santana’s Hill. Representative profiles were classified as Typic Haplustox; Xanthic Eutrustox; Typic Eutrustox; Ustic Quartzipsamments; Lithic Ustorthents; Typic Ustipsamments and Dystric Haplustepts. By observing morphological attributes it was noticed that there was a great influence of the parent material factor in distinguishing the main soil types found in the study area, since the topography and climatic conditions are similar throughout the territorial extension. The textural class of the profiles studied ranged from sandy to sandy-clay-sandy due to high existing levels in sand horizons, identifying minerals that were more resistant to weathering process and the strong link with the material of sedimentary origin. All profiles showed acid reaction, wide range of base saturation between profiles and low values of electrical conductivity. The mineralogical composition of the clay fraction of the profiles were similar, with clay type Illite/Mica, Kaolinite and Goethite, and Quartz peaks. The use of GIS allows updating existing soil classes in the Santana’s Hill, as well as updating the percentage of occupation of each soil typeNa compreensão de um manejo mais adequado, o levantamento do tipo de solo em uma região possui uma importância fundamental. Desse modo, uma atualização constante das classes de solos se faz necessária para que os diversos usos agrícolas sejam analisados e estabelecidos da forma mais adequada possível. O Rio Grande do Norte possui formações serranas que diferem das condições edafoclimáticas predominantes no estado, apresentando solos mais profundos e ácidos e clima mais ameno. Dentre estas formações, destaca-se a Serra de Santana, que está inserida na Formação dos Martins com depósitos assentados em discordância sobre o embasamento cristalino e inserida na região do Seridó Potiguar, apresentando importante uso agrícola para a região, com o cultivo principalmente de caju e mandioca. Com isto, objetivou-se neste trabalho compreender a gênese dos solos representativos da Serra de Santana e elaborar um mapa de solos exploratório da região. Foram realizadas análises morfológicas, físicas, químicas e mineralógicas de perfis representativos que compõem a Serra de Santana. Os perfis representativos foram classificados como: LATOSSOLO AMARELO Distrófico argissólico; LATOSSOLO AMARELO Eutrófico argissólico; NEOSSOLO QUARTZARÊNICO Órtico típico; NEOSSOLO LITÓLICO Eutrófico fragmentário; NEOSSOLO REGOLÍTICO Eutrófico típico e CAMBISSOLO HÁPLICO Tb Eutrófico léptico. Ao observar os atributos morfológicos percebeu-se que houve grande influência do fator material de origem na distinção das principais classes de solo encontradas na área de estudo, já que o relevo e condição climática são similares ao longo de toda extensão territorial. A classe textural dos perfis estudados variou de areia a franco-argilo-arenosa devido aos altos teores de areia existentes nos horizontes, identificando minerais que foram mais resistentes ao processo de intemperismo e a forte ligação com o material de origem sedimentar. Todos os perfis apresentaram reação ácida, grande variação de saturação por bases entre os perfis e baixos valores de condutividade elétrica. A composição mineralógica da fração argila dos perfis foi similar, apresentando argilominerais do tipo Ilita/Mica, Caulinita e Goethita, além de picos de Quartzo. O uso do geoprocessamento permitiu atualização das classes de solo existentes na Serra de Santana, bem como a atualização da percentagem de ocupação de cada classe de soloSubmitted by Socorro Pontes (socorrop@ufersa.edu.br) on 2016-11-17T15:53:38Z No. of bitstreams: 1 PhâmellaKPF_DISSERT.pdf: 2697111 bytes, checksum: 6489ccb9ad9ef120c49053934aaa3387 (MD5)Approved for entry into archive by Vanessa Christiane (referencia@ufersa.edu.br) on 2017-03-21T14:37:44Z (GMT) No. of bitstreams: 1 PhâmellaKPF_DISSERT.pdf: 2697111 bytes, checksum: 6489ccb9ad9ef120c49053934aaa3387 (MD5)Approved for entry into archive by Vanessa Christiane (referencia@ufersa.edu.br) on 2017-03-21T15:04:17Z (GMT) No. of bitstreams: 1 PhâmellaKPF_DISSERT.pdf: 2697111 bytes, checksum: 6489ccb9ad9ef120c49053934aaa3387 (MD5)Made available in DSpace on 2017-03-21T15:05:51Z (GMT). No. of bitstreams: 1 PhâmellaKPF_DISSERT.pdf: 2697111 bytes, checksum: 6489ccb9ad9ef120c49053934aaa3387 (MD5) Previous issue date: 2016-02-22Coordenação de Aperfeiçoamento de Pessoal de Nível Superior2016-11-17application/pdfhttp://repositorio.ufersa.edu.br/retrieve/1357/Ph%c3%a2mellaKPF_DISSERT.pdf.jpgporUniversidade Federal Rural do Semi-ÁridoPrograma de Pós-graduação em Manejo de Solo e ÁguaUFERSABrasilUso agrícolaGeorreferenciamentoProcessos pedogenéticosRochas sedimentaresAgricultural useGeoreferencingPedogenic processesSedimentary rocksCNPQ::CIENCIAS AGRARIASGênese e levantamento de solos da Serra de Santana no Seridó Potiguarinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/openAccessreponame:Biblioteca Digital de Teses e Dissertações da UFERSAinstname:Universidade Federal Rural do Semi-Árido (UFERSA)instacron:UFERSAORIGINALPhâmellaKPF_DISSERT.pdfPhâmellaKPF_DISSERT.pdfapplication/pdf2697111http://200.137.6.41:8080/jspui/bitstream/tede/622/1/Ph%c3%a2mellaKPF_DISSERT.pdf6489ccb9ad9ef120c49053934aaa3387MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-82165http://200.137.6.41:8080/jspui/bitstream/tede/622/2/license.txtbd3efa91386c1718a7f26a329fdcb468MD52TEXTPhâmellaKPF_DISSERT.pdf.txtPhâmellaKPF_DISSERT.pdf.txtExtracted Texttext/plain142170http://200.137.6.41:8080/jspui/bitstream/tede/622/3/Ph%c3%a2mellaKPF_DISSERT.pdf.txtebeaa878a9e0bdf65cd37f8736059b5aMD53THUMBNAILPhâmellaKPF_DISSERT.pdf.jpgPhâmellaKPF_DISSERT.pdf.jpgGenerated Thumbnailimage/jpeg3153http://200.137.6.41:8080/jspui/bitstream/tede/622/4/Ph%c3%a2mellaKPF_DISSERT.pdf.jpg10cc253e2ecbae1c5e93404c0be4aa6dMD54tede/6222018-05-23 14:06:12.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Biblioteca Digital de Teses e Dissertaçõeshttps://repositorio.ufersa.edu.br/ |
dc.title.por.fl_str_mv |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
title |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
spellingShingle |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar Farias, Phamella Kalliny Pereira Uso agrícola Georreferenciamento Processos pedogenéticos Rochas sedimentares Agricultural use Georeferencing Pedogenic processes Sedimentary rocks CNPQ::CIENCIAS AGRARIAS |
title_short |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
title_full |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
title_fullStr |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
title_full_unstemmed |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
title_sort |
Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar |
author |
Farias, Phamella Kalliny Pereira |
author_facet |
Farias, Phamella Kalliny Pereira |
author_role |
author |
dc.contributor.authorID.por.fl_str_mv |
08248891429 |
dc.contributor.authorLattes.por.fl_str_mv |
http://lattes.cnpq.br/7691085061826580 |
dc.contributor.advisorLattes.por.fl_str_mv |
http://lattes.cnpq.br/9637230855429508 |
dc.contributor.advisor1.fl_str_mv |
Martins, Carolina Malala |
dc.contributor.advisor1ID.fl_str_mv |
05165780490 |
dc.contributor.advisor-co1.fl_str_mv |
Silva, Paulo Cesar Moura da |
dc.contributor.advisor-co1ID.fl_str_mv |
91358540497 |
dc.contributor.advisor-co1Lattes.fl_str_mv |
http://lattes.cnpq.br/4070582933073155 |
dc.contributor.referee1.fl_str_mv |
Silva, Eulene Francisco da |
dc.contributor.referee1ID.fl_str_mv |
86629760182 |
dc.contributor.referee1Lattes.fl_str_mv |
http://lattes.cnpq.br/4243362476220476 |
dc.contributor.referee2.fl_str_mv |
Ernesto Sobrinho, Francisco |
dc.contributor.referee2ID.fl_str_mv |
06745210487 |
dc.contributor.referee2Lattes.fl_str_mv |
http://lattes.cnpq.br/6942156011040135 |
dc.contributor.author.fl_str_mv |
Farias, Phamella Kalliny Pereira |
contributor_str_mv |
Martins, Carolina Malala Silva, Paulo Cesar Moura da Silva, Eulene Francisco da Ernesto Sobrinho, Francisco |
dc.subject.por.fl_str_mv |
Uso agrícola Georreferenciamento Processos pedogenéticos Rochas sedimentares Agricultural use Georeferencing Pedogenic processes Sedimentary rocks |
topic |
Uso agrícola Georreferenciamento Processos pedogenéticos Rochas sedimentares Agricultural use Georeferencing Pedogenic processes Sedimentary rocks CNPQ::CIENCIAS AGRARIAS |
dc.subject.cnpq.fl_str_mv |
CNPQ::CIENCIAS AGRARIAS |
description |
In understanding a more appropriate management, the soil survey in a region it has a fundamental importance. Thus, a constant updating of the soil classes is necessary for the various agricultural uses are analyzed and established the most appropriate way possible. The Rio Grande do Norte has hills formations that differ from the soil and climatic conditions prevailing in the state, with deeper soils and acidic and milder weather. Among these formations, there is the Santana’s Hill, which is embedded in the Martins Formation with deposits settled in disagreement over the lens and inserted basis in the Potiguar Seridó region, with important agricultural use for the region, with mainly cashew cultivation and cassava. With this, the objective of this study was to understand the genesis of representative soils of the Santana’s Hill and draw up an exploratory soil map of the region. Morphological, physical, chemical and mineralogical analyzes of representative profiles were performed that make up the Santana’s Hill. Representative profiles were classified as Typic Haplustox; Xanthic Eutrustox; Typic Eutrustox; Ustic Quartzipsamments; Lithic Ustorthents; Typic Ustipsamments and Dystric Haplustepts. By observing morphological attributes it was noticed that there was a great influence of the parent material factor in distinguishing the main soil types found in the study area, since the topography and climatic conditions are similar throughout the territorial extension. The textural class of the profiles studied ranged from sandy to sandy-clay-sandy due to high existing levels in sand horizons, identifying minerals that were more resistant to weathering process and the strong link with the material of sedimentary origin. All profiles showed acid reaction, wide range of base saturation between profiles and low values of electrical conductivity. The mineralogical composition of the clay fraction of the profiles were similar, with clay type Illite/Mica, Kaolinite and Goethite, and Quartz peaks. The use of GIS allows updating existing soil classes in the Santana’s Hill, as well as updating the percentage of occupation of each soil type |
publishDate |
2016 |
dc.date.issued.fl_str_mv |
2016-02-22 |
dc.date.accessioned.fl_str_mv |
2017-03-21T15:05:51Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
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info:eu-repo/semantics/masterThesis |
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masterThesis |
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publishedVersion |
dc.identifier.citation.fl_str_mv |
FARIAS, Phamella Kalliny Pereira. Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar. 2016. 82 f. Dissertação (Mestrado) - Curso de Pós-graduação em Manejo de Solo e Água, Universidade Federal Rural do Semi-Árido, Mossoró, 2016. |
dc.identifier.uri.fl_str_mv |
http://repositorio.ufersa.edu.br/handle/tede/622 |
identifier_str_mv |
FARIAS, Phamella Kalliny Pereira. Gênese e levantamento de solos da Serra de Santana no Seridó Potiguar. 2016. 82 f. Dissertação (Mestrado) - Curso de Pós-graduação em Manejo de Solo e Água, Universidade Federal Rural do Semi-Árido, Mossoró, 2016. |
url |
http://repositorio.ufersa.edu.br/handle/tede/622 |
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por |
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por |
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openAccess |
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Universidade Federal Rural do Semi-Árido |
dc.publisher.program.fl_str_mv |
Programa de Pós-graduação em Manejo de Solo e Água |
dc.publisher.initials.fl_str_mv |
UFERSA |
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Brasil |
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Universidade Federal Rural do Semi-Árido |
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