Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning

Detalhes bibliográficos
Autor(a) principal: Freires, Eduardo Viana
Data de Publicação: 2023
Outros Autores: Silva Neto, Cláudio Ângelo da, Silva, Maykom Targino da, Duarte, Cynthia Romariz, Verissimo, César Ulisses Vieira, Lopes, Débora Nogueira, Gomes, Daniel Dantas Moreira
Tipo de documento: Artigo
Idioma: por
eng
Título da fonte: Revista de Geociências do Nordeste
Texto Completo: https://periodicos.ufrn.br/revistadoregne/article/view/30719
Resumo: Erosive processes are generated by natural and human causes. Anthropic activities enhance soil loss from inadequate management and compromise agricultural productivity and sustainability. This research aims to perform the mapping of erosivity and erodibility of the humid slope of the Uruburetama/CE Massif and surrounding area in order to support soil protection and management measures against water erosion. The Erosivity Map was obtained by the IDW interpolator through the calculation of erosivity performed based on rainfall records of 23 FUNCEME monitoring stations in a 10-year interval (2010-2019). The classes of erosivity are associated with the performance of local rainfall generating systems, which lose strength towards the continent. Thus, it was observed the occurrence of the classes of erosivity Moderate to Strong (92.66%) and Strong (7.34%). Soil erodibility was processed by Ordinary Kriging from the K factor obtained from the analyses of 92 samples of deformed soils (granulometry, soil structure, organic matter) and 92 undisturbed (permeability) collected in the research area. The erodibility classes are associated with the distribution and characteristics of local soils. The Very Low class (8%) is associated with the Eutrophic Háplico Solus and the Ortic Quartzarenic Neosol. The Lower class (83%) is related to the occurrence of Red-Yellow Argisol and the Litholic Neosol, while the Moderate class (9%) is associated with the Chromic Luvissol. Keywords: Erosive processes. Anthropic activities. Handling.  
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spelling Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planningMapeamento da erosividade e erodibilidade da vertente úmida do Maciço de Uruburetama/CE e entorno como subsidio ao planejamento ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planningErosive processes are generated by natural and human causes. Anthropic activities enhance soil loss from inadequate management and compromise agricultural productivity and sustainability. This research aims to perform the mapping of erosivity and erodibility of the humid slope of the Uruburetama/CE Massif and surrounding area in order to support soil protection and management measures against water erosion. The Erosivity Map was obtained by the IDW interpolator through the calculation of erosivity performed based on rainfall records of 23 FUNCEME monitoring stations in a 10-year interval (2010-2019). The classes of erosivity are associated with the performance of local rainfall generating systems, which lose strength towards the continent. Thus, it was observed the occurrence of the classes of erosivity Moderate to Strong (92.66%) and Strong (7.34%). Soil erodibility was processed by Ordinary Kriging from the K factor obtained from the analyses of 92 samples of deformed soils (granulometry, soil structure, organic matter) and 92 undisturbed (permeability) collected in the research area. The erodibility classes are associated with the distribution and characteristics of local soils. The Very Low class (8%) is associated with the Eutrophic Háplico Solus and the Ortic Quartzarenic Neosol. The Lower class (83%) is related to the occurrence of Red-Yellow Argisol and the Litholic Neosol, while the Moderate class (9%) is associated with the Chromic Luvissol. Keywords: Erosive processes. Anthropic activities. Handling.  Los procesos erosivos son generados por causas naturales y humanas. Las actividades antropogénicas potencian la pérdida de suelo por un manejo inadecuado y comprometen la productividad y la sostenibilidad agrícola. Esta investigación tiene como objetivo realizar el mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores con el fin de subsidiar medidas de protección y manejo del suelo contra la erosión hídrica. El mapa de erosividad fue obtenido por el interpolador IDW a través del cálculo de erosividad realizado con base en los registros de lluvia de 23 estaciones de monitoreo de FUNCEME en un intervalo de 10 años (2010-2019). Las clases de erosividad están asociadas a la acción de los sistemas generadores de lluvias locales, que pierden fuerza hacia el continente. Así, se observó la ocurrencia de clases de erosividad moderada a fuerte (92,66%) y fuerte (7,34%). La erosionabilidad del suelo fue procesada por Kriging Ordinario a partir del factor K obtenido del análisis de 92 muestras de suelo deformado (granulometría, estructura del suelo, materia orgánica) y 92 muestras no perturbadas (permeabilidad) recolectadas en el área de investigación. Las clases de erosionabilidad están asociadas con la distribución y características de los suelos locales. La clase Muy Baja (8%) está asociada al Planosol Háplico Eutrófico y al Neosol Cuarzoarénico Órtico. La clase Baja (83%) está relacionada con la ocurrencia de Ultisol Rojo-Amarillo y Neosol Litólico, mientras que la clase Moderada (9%) está asociada con el Luvissol Crómico. Palabras clave: Procesos erosivos. Actividades antropogénicas. Administración.Os processos erosivos são gerados por causas naturais e humanas. As atividades antrópicas potencializam a perda de solos a partir de manejos inadequados e comprometem a produtividade agrícola e a sustentabilidade. Esta pesquisa objetiva realizar o mapeamento de erosividade e erodibilidade da vertente úmida do Maciço de Uruburetama/CE e entorno com o intuito de subsidiar medidas de proteção e manejo dos solos contra a erosão hídrica. O Mapa de erosividade foi obtido pelo interpolador IDW através do cálculo de erosividade realizado com base em registros pluviométricos de 23 estações de monitoramento da FUNCEME num intervalo de 10 anos (2010-2019). As classes de erosividade estão associadas a atuação de sistemas geradores de chuvas locais, que perdem força em direção ao continente. Assim, observou-se a ocorrência das classes de erosividade Moderada a Forte (92,66%) e Forte (7,34%). A erodibilidade dos solos foi processada por Krigagem Ordinária a partir do fator K obtido das análises de 92 amostras de solos deformadas (granulometria, estrutura do solo, matéria orgânica) e 92 indeformadas (permeabilidade) coletadas na área de pesquisa. As classes de erodibilidade estão associadas à distribuição e as características dos solos locais. A classe Muito Baixa (8%) está associada ao Planossolo Háplico Eutrófico e ao Neossolo Quartzarênico Órtico. A classe Baixa (83%) relaciona-se à ocorrência de Argissolo Vermelho-Amarelo e ao Neossolo Litólico, enquanto a classe Moderada (9%) associa-se ao Luvissolo Crômico. Palavras-chave: Processos erosivos. Atividades antrópicas. Manejo.Universidade Federal do Rio Grande do Norte2023-07-24info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfapplication/pdfhttps://periodicos.ufrn.br/revistadoregne/article/view/3071910.21680/2447-3359.2023v9n2ID30719Notheast Geoscience Journal; Vol. 9 No. 2 (2023); 21-40Revista de Geociências do Nordeste; v. 9 n. 2 (2023); 21-402447-335910.21680/2447-3359.2023v9n2reponame:Revista de Geociências do Nordesteinstname:Universidade Federal do Rio Grande do Norte (UFRN)instacron:UFRNporenghttps://periodicos.ufrn.br/revistadoregne/article/view/30719/17258https://periodicos.ufrn.br/revistadoregne/article/view/30719/17260Copyright (c) 2023 Revista de Geociências do Nordestehttps://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessFreires, Eduardo Viana Silva Neto, Cláudio Ângelo daSilva, Maykom Targino daDuarte, Cynthia Romariz Verissimo, César Ulisses VieiraLopes, Débora Nogueira Gomes, Daniel Dantas Moreira2024-01-03T23:27:29Zoai:periodicos.ufrn.br:article/30719Revistahttps://periodicos.ufrn.br/revistadoregne/indexPUBhttps://periodicos.ufrn.br/revistadoregne/oairegneufrn@gmail.com || periodicos@bczm.ufrn.br2447-33592447-3359opendoar:2024-01-03T23:27:29Revista de Geociências do Nordeste - Universidade Federal do Rio Grande do Norte (UFRN)false
dc.title.none.fl_str_mv Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
Mapeamento da erosividade e erodibilidade da vertente úmida do Maciço de Uruburetama/CE e entorno como subsidio ao planejamento ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
title Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
spellingShingle Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
Freires, Eduardo Viana
title_short Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
title_full Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
title_fullStr Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
title_full_unstemmed Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
title_sort Mapeo de erosividad y erosionabilidad del talud húmedo del Macizo de Uruburetama/CE y alrededores como subsidio a la planificación ambiental: Erosivity and erodibility mapping of the humid slope of the Uruburetama/CE Massif and surroundings as a subsidy for environmental planning
author Freires, Eduardo Viana
author_facet Freires, Eduardo Viana
Silva Neto, Cláudio Ângelo da
Silva, Maykom Targino da
Duarte, Cynthia Romariz
Verissimo, César Ulisses Vieira
Lopes, Débora Nogueira
Gomes, Daniel Dantas Moreira
author_role author
author2 Silva Neto, Cláudio Ângelo da
Silva, Maykom Targino da
Duarte, Cynthia Romariz
Verissimo, César Ulisses Vieira
Lopes, Débora Nogueira
Gomes, Daniel Dantas Moreira
author2_role author
author
author
author
author
author
dc.contributor.author.fl_str_mv Freires, Eduardo Viana
Silva Neto, Cláudio Ângelo da
Silva, Maykom Targino da
Duarte, Cynthia Romariz
Verissimo, César Ulisses Vieira
Lopes, Débora Nogueira
Gomes, Daniel Dantas Moreira
description Erosive processes are generated by natural and human causes. Anthropic activities enhance soil loss from inadequate management and compromise agricultural productivity and sustainability. This research aims to perform the mapping of erosivity and erodibility of the humid slope of the Uruburetama/CE Massif and surrounding area in order to support soil protection and management measures against water erosion. The Erosivity Map was obtained by the IDW interpolator through the calculation of erosivity performed based on rainfall records of 23 FUNCEME monitoring stations in a 10-year interval (2010-2019). The classes of erosivity are associated with the performance of local rainfall generating systems, which lose strength towards the continent. Thus, it was observed the occurrence of the classes of erosivity Moderate to Strong (92.66%) and Strong (7.34%). Soil erodibility was processed by Ordinary Kriging from the K factor obtained from the analyses of 92 samples of deformed soils (granulometry, soil structure, organic matter) and 92 undisturbed (permeability) collected in the research area. The erodibility classes are associated with the distribution and characteristics of local soils. The Very Low class (8%) is associated with the Eutrophic Háplico Solus and the Ortic Quartzarenic Neosol. The Lower class (83%) is related to the occurrence of Red-Yellow Argisol and the Litholic Neosol, while the Moderate class (9%) is associated with the Chromic Luvissol. Keywords: Erosive processes. Anthropic activities. Handling.  
publishDate 2023
dc.date.none.fl_str_mv 2023-07-24
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://periodicos.ufrn.br/revistadoregne/article/view/30719
10.21680/2447-3359.2023v9n2ID30719
url https://periodicos.ufrn.br/revistadoregne/article/view/30719
identifier_str_mv 10.21680/2447-3359.2023v9n2ID30719
dc.language.iso.fl_str_mv por
eng
language por
eng
dc.relation.none.fl_str_mv https://periodicos.ufrn.br/revistadoregne/article/view/30719/17258
https://periodicos.ufrn.br/revistadoregne/article/view/30719/17260
dc.rights.driver.fl_str_mv Copyright (c) 2023 Revista de Geociências do Nordeste
https://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2023 Revista de Geociências do Nordeste
https://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio Grande do Norte
publisher.none.fl_str_mv Universidade Federal do Rio Grande do Norte
dc.source.none.fl_str_mv Notheast Geoscience Journal; Vol. 9 No. 2 (2023); 21-40
Revista de Geociências do Nordeste; v. 9 n. 2 (2023); 21-40
2447-3359
10.21680/2447-3359.2023v9n2
reponame:Revista de Geociências do Nordeste
instname:Universidade Federal do Rio Grande do Norte (UFRN)
instacron:UFRN
instname_str Universidade Federal do Rio Grande do Norte (UFRN)
instacron_str UFRN
institution UFRN
reponame_str Revista de Geociências do Nordeste
collection Revista de Geociências do Nordeste
repository.name.fl_str_mv Revista de Geociências do Nordeste - Universidade Federal do Rio Grande do Norte (UFRN)
repository.mail.fl_str_mv regneufrn@gmail.com || periodicos@bczm.ufrn.br
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