Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA
Autor(a) principal: | |
---|---|
Data de Publicação: | 2022 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Sociedade & natureza (Online) |
Texto Completo: | https://seer.ufu.br/index.php/sociedadenatureza/article/view/63971 |
Resumo: | The watershed is an active environment, defined as an area of land surface drained by a primary river and its tributaries, which are bounded by water dividers. Among the processes that affect water movement in a watershed, the surface runoff stands out, responsible for the transport of soil particles (nutrients and pollutants) to the lower parts of the landscape. The objective of this study was to demonstrate the influence of land use and cover on surface runoff dynamics in the Capivari Basin in Bahia, Brazil. To reach that objective, the Curve Number method (SCS-CN) was employed, with the ALOS/PALSAR RTC Digital Elevation Model; IBGE soil data; data from government weather stations and local agribusiness; land use and land cover from the LC08_L1TP_216069_20170619 landsat8 OLI sensor, through the classifier Bhattacharya. The processing was carried out on a GIS platform, using SPRING and QGIS software. Highest levels of precipitation, the soil features and the higher slope affected the greatest vulnerability to runoff at the mouth, based on the proposed model, however, the most conserved Permanent Preservation Area (PPA) have been effective in maintaining the Capivari River in these areas. The areas considered most critical in terms of the risk of water erosion for the year 2017 were those in the middle of Capivari, because they presented high precipitation in some months, but do not present PPA in riparian forest areas or in hill tops, this increases the vulnerability of these regions to erosion. The proposed model was successful in identifying areas most vulnerable to runoff in the Capivari Basin. |
id |
UFU-6_d33ce42208d0168a64f0a133efea7942 |
---|---|
oai_identifier_str |
oai:ojs.www.seer.ufu.br:article/63971 |
network_acronym_str |
UFU-6 |
network_name_str |
Sociedade & natureza (Online) |
repository_id_str |
|
spelling |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BARunoff, Identification of Sensitive Zones in the Capivari Watershed – BADrainage basinSCS-CNHydrologyDrainage basinSCS-CNHydrologyThe watershed is an active environment, defined as an area of land surface drained by a primary river and its tributaries, which are bounded by water dividers. Among the processes that affect water movement in a watershed, the surface runoff stands out, responsible for the transport of soil particles (nutrients and pollutants) to the lower parts of the landscape. The objective of this study was to demonstrate the influence of land use and cover on surface runoff dynamics in the Capivari Basin in Bahia, Brazil. To reach that objective, the Curve Number method (SCS-CN) was employed, with the ALOS/PALSAR RTC Digital Elevation Model; IBGE soil data; data from government weather stations and local agribusiness; land use and land cover from the LC08_L1TP_216069_20170619 landsat8 OLI sensor, through the classifier Bhattacharya. The processing was carried out on a GIS platform, using SPRING and QGIS software. Highest levels of precipitation, the soil features and the higher slope affected the greatest vulnerability to runoff at the mouth, based on the proposed model, however, the most conserved Permanent Preservation Area (PPA) have been effective in maintaining the Capivari River in these areas. The areas considered most critical in terms of the risk of water erosion for the year 2017 were those in the middle of Capivari, because they presented high precipitation in some months, but do not present PPA in riparian forest areas or in hill tops, this increases the vulnerability of these regions to erosion. The proposed model was successful in identifying areas most vulnerable to runoff in the Capivari Basin.The watershed is an active environment, defined as an area of land surface drained by a primary river and its tributaries, which are bounded by water dividers. Among the processes that affect water movement in a watershed, the surface runoff stands out, responsible for the transport of soil particles (nutrients and pollutants) to the lower parts of the landscape. The objective of this study was to demonstrate the influence of land use and cover on surface runoff dynamics in the Capivari Basin in Bahia, Brazil. To reach that objective, the Curve Number method (SCS-CN) was employed, with the ALOS/PALSAR RTC Digital Elevation Model; IBGE soil data; data from government weather stations and local agribusiness; land use and land cover from the LC08_L1TP_216069_20170619 landsat8 OLI sensor, through the classifier Bhattacharya. The processing was carried out on a GIS platform, using SPRING and QGIS software. Highest levels of precipitation, the soil features and the higher slope affected the greatest vulnerability to runoff at the mouth, based on the proposed model, however, the most conserved Permanent Preservation Area (PPA) have been effective in maintaining the Capivari River in these areas. The areas considered most critical in terms of the risk of water erosion for the year 2017 were those in the middle of Capivari, because they presented high precipitation in some months, but do not present PPA in riparian forest areas or in hill tops, this increases the vulnerability of these regions to erosion. The proposed model was successful in identifying areas most vulnerable to runoff in the Capivari Basin.Universidade Federal de Uberlândia2022-03-31info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://seer.ufu.br/index.php/sociedadenatureza/article/view/6397110.14393/SN-v34-2022-63971Sociedade & Natureza; Vol. 34 No. 1 (2022): Sociedade & Natureza; v. 34 n. 1 (2022): 1982-45130103-1570reponame:Sociedade & natureza (Online)instname:Universidade Federal de Uberlândia (UFU)instacron:UFUenghttps://seer.ufu.br/index.php/sociedadenatureza/article/view/63971/33658Copyright (c) 2021 Geisa Nascimento Santana, Luiz Artur dos Santos da Silva, Rosangela Leal Santos; Jesus Manuel Delgado-Mendez; Claudia Bloisi Vaz Sampaiohttps://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessSantana, Geisa Nascimento Silva, Luiz Artur SantosSantos, Rosangela LealDelgado-Mendez, Jesus ManuelSampaio, Claudia Bloisi Vaz2023-04-06T20:32:29Zoai:ojs.www.seer.ufu.br:article/63971Revistahttp://www.sociedadenatureza.ig.ufu.br/PUBhttps://seer.ufu.br/index.php/sociedadenatureza/oai||sociedade.natureza.ufu@gmail.com|| lucianamelo@ufu.br1982-45130103-1570opendoar:2023-04-06T20:32:29Sociedade & natureza (Online) - Universidade Federal de Uberlândia (UFU)false |
dc.title.none.fl_str_mv |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
title |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
spellingShingle |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA Santana, Geisa Nascimento Drainage basin SCS-CN Hydrology Drainage basin SCS-CN Hydrology |
title_short |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
title_full |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
title_fullStr |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
title_full_unstemmed |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
title_sort |
Runoff, Identification of Sensitive Zones in the Capivari Watershed – BA |
author |
Santana, Geisa Nascimento |
author_facet |
Santana, Geisa Nascimento Silva, Luiz Artur Santos Santos, Rosangela Leal Delgado-Mendez, Jesus Manuel Sampaio, Claudia Bloisi Vaz |
author_role |
author |
author2 |
Silva, Luiz Artur Santos Santos, Rosangela Leal Delgado-Mendez, Jesus Manuel Sampaio, Claudia Bloisi Vaz |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Santana, Geisa Nascimento Silva, Luiz Artur Santos Santos, Rosangela Leal Delgado-Mendez, Jesus Manuel Sampaio, Claudia Bloisi Vaz |
dc.subject.por.fl_str_mv |
Drainage basin SCS-CN Hydrology Drainage basin SCS-CN Hydrology |
topic |
Drainage basin SCS-CN Hydrology Drainage basin SCS-CN Hydrology |
description |
The watershed is an active environment, defined as an area of land surface drained by a primary river and its tributaries, which are bounded by water dividers. Among the processes that affect water movement in a watershed, the surface runoff stands out, responsible for the transport of soil particles (nutrients and pollutants) to the lower parts of the landscape. The objective of this study was to demonstrate the influence of land use and cover on surface runoff dynamics in the Capivari Basin in Bahia, Brazil. To reach that objective, the Curve Number method (SCS-CN) was employed, with the ALOS/PALSAR RTC Digital Elevation Model; IBGE soil data; data from government weather stations and local agribusiness; land use and land cover from the LC08_L1TP_216069_20170619 landsat8 OLI sensor, through the classifier Bhattacharya. The processing was carried out on a GIS platform, using SPRING and QGIS software. Highest levels of precipitation, the soil features and the higher slope affected the greatest vulnerability to runoff at the mouth, based on the proposed model, however, the most conserved Permanent Preservation Area (PPA) have been effective in maintaining the Capivari River in these areas. The areas considered most critical in terms of the risk of water erosion for the year 2017 were those in the middle of Capivari, because they presented high precipitation in some months, but do not present PPA in riparian forest areas or in hill tops, this increases the vulnerability of these regions to erosion. The proposed model was successful in identifying areas most vulnerable to runoff in the Capivari Basin. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022-03-31 |
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://seer.ufu.br/index.php/sociedadenatureza/article/view/63971 10.14393/SN-v34-2022-63971 |
url |
https://seer.ufu.br/index.php/sociedadenatureza/article/view/63971 |
identifier_str_mv |
10.14393/SN-v34-2022-63971 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://seer.ufu.br/index.php/sociedadenatureza/article/view/63971/33658 |
dc.rights.driver.fl_str_mv |
https://creativecommons.org/licenses/by/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal de Uberlândia |
publisher.none.fl_str_mv |
Universidade Federal de Uberlândia |
dc.source.none.fl_str_mv |
Sociedade & Natureza; Vol. 34 No. 1 (2022): Sociedade & Natureza; v. 34 n. 1 (2022): 1982-4513 0103-1570 reponame:Sociedade & natureza (Online) instname:Universidade Federal de Uberlândia (UFU) instacron:UFU |
instname_str |
Universidade Federal de Uberlândia (UFU) |
instacron_str |
UFU |
institution |
UFU |
reponame_str |
Sociedade & natureza (Online) |
collection |
Sociedade & natureza (Online) |
repository.name.fl_str_mv |
Sociedade & natureza (Online) - Universidade Federal de Uberlândia (UFU) |
repository.mail.fl_str_mv |
||sociedade.natureza.ufu@gmail.com|| lucianamelo@ufu.br |
_version_ |
1799943982919188480 |