Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines)
Autor(a) principal: | |
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Data de Publicação: | 2013 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Geografia (Londrina) |
Texto Completo: | https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/14411 |
Resumo: | This study aimed at evaluating the influence of the contact of animals with water bodies and hence their interference on the movement of river bed at Faxinal Marmeleiro de Cima, located in the municipality of Rebouças, Paraná State. The Faxinal System is a peculiar way of using and occupying the land, where there is a consortium between exploitation of natural resources and unrestricted animal husbandry, which has negative impacts on the water bodies. The direct contact of animals with water bodies implies in lack of riparian vegetation, contributing with the process of connecting the sediments of the slopes with river channels, forming sediment banks. In order to monitor the movement of these sediment banks in the riverbed, it was used the transverse profile method. Collections were conducted every two months, amounting 8 (eight) collections in 2009 and 2010. For assessing the progress of the margins it was used erosion pins. To monitor the rainfall, a direct measurement pluviometer was used. At the end of the monitoring, it was identified the degree of movement of river beds, with summer and autumn representing the periods with greater movement. |
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Geografia (Londrina) |
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Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines)Movimentação de leito de rio em cabeceira de drenagem potencializada por ação de animais domésticos (suínos)River channelsFaxinalMargin erosionDegradationCanais FluviaisFaxinalErosão de margensDegradação.This study aimed at evaluating the influence of the contact of animals with water bodies and hence their interference on the movement of river bed at Faxinal Marmeleiro de Cima, located in the municipality of Rebouças, Paraná State. The Faxinal System is a peculiar way of using and occupying the land, where there is a consortium between exploitation of natural resources and unrestricted animal husbandry, which has negative impacts on the water bodies. The direct contact of animals with water bodies implies in lack of riparian vegetation, contributing with the process of connecting the sediments of the slopes with river channels, forming sediment banks. In order to monitor the movement of these sediment banks in the riverbed, it was used the transverse profile method. Collections were conducted every two months, amounting 8 (eight) collections in 2009 and 2010. For assessing the progress of the margins it was used erosion pins. To monitor the rainfall, a direct measurement pluviometer was used. At the end of the monitoring, it was identified the degree of movement of river beds, with summer and autumn representing the periods with greater movement. O presente trabalho objetivou a avaliação da influência do contato dos animais com os corpos hídricos e, por conseguinte, sua interferência na mobilização do leito de rio no Faxinal Marmeleiro de Cima, localizado no município de Rebouças-PR. O Sistema de Faxinal é uma forma peculiar de uso e ocupação do solo, onde há um consorciamento entre exploração dos recursos naturais e criação de animais sem restrições de áreas (criadouro comunitário), o que provoca impacto negativo nos cursos d’água. O contato direto dos animais com os corpos hídricos implica na inexistência da mata ciliar, o que contribui nos processo de conexão dos sedimentos das vertentes com os canais fluviais, formando bancos de sedimentos. Para monitorar a movimentação desses bancos de sedimentos no leito do rio, foi utilizado o método de perfil transversal. As coletas foram realizadas a cada dois meses, totalizando 8 (oito) campanhas nos anos de 2009 e 2010. Para avaliar o avanço das margens foram utilizados pinos de erosão. Para monitorar a precipitação foi utilizado um pluviômetro de medida direta. Ao término do monitoramento foi possível identificar o nível de movimentação do leito dos rios, tento as estações da primavera e do outono, como os períodos com maior movimentação.Universidade Estadual de Londrina2013-12-16info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionAvaliado pelos paresapplication/pdfhttps://ojs.uel.br/revistas/uel/index.php/geografia/article/view/1441110.5433/2447-1747.2012v21n3p75GEOGRAFIA (Londrina); v. 21 n. 3 (2012); 75-932447-1747reponame:Geografia (Londrina)instname:Universidade Estadual de Londrina (UEL)instacron:UELporhttps://ojs.uel.br/revistas/uel/index.php/geografia/article/view/14411/13765Copyright (c) 2013 GEOGRAFIA (Londrina)info:eu-repo/semantics/openAccessBednarz, João AnésioAntoneli, ValdemirAndrade, Aparecido Ribeiro deCarvalho, Marlon Fabio Abreu de2013-12-16T22:17:00Zoai:ojs.pkp.sfu.ca:article/14411Revistahttps://www.uel.br/revistas/uel/index.php/geografiaPUBhttps://www.uel.br/revistas/uel/index.php/geografia/oairevista.geografia.uel@gmail.com||marcar@uel.br||laudi@uel.br2447-17470102-3888opendoar:2013-12-16T22:17Geografia (Londrina) - Universidade Estadual de Londrina (UEL)false |
dc.title.none.fl_str_mv |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) Movimentação de leito de rio em cabeceira de drenagem potencializada por ação de animais domésticos (suínos) |
title |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) |
spellingShingle |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) Bednarz, João Anésio River channels Faxinal Margin erosion Degradation Canais Fluviais Faxinal Erosão de margens Degradação. |
title_short |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) |
title_full |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) |
title_fullStr |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) |
title_full_unstemmed |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) |
title_sort |
Movement of river bed in drainage headwaters enhanced by the activity of domestic animals (swines) |
author |
Bednarz, João Anésio |
author_facet |
Bednarz, João Anésio Antoneli, Valdemir Andrade, Aparecido Ribeiro de Carvalho, Marlon Fabio Abreu de |
author_role |
author |
author2 |
Antoneli, Valdemir Andrade, Aparecido Ribeiro de Carvalho, Marlon Fabio Abreu de |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Bednarz, João Anésio Antoneli, Valdemir Andrade, Aparecido Ribeiro de Carvalho, Marlon Fabio Abreu de |
dc.subject.por.fl_str_mv |
River channels Faxinal Margin erosion Degradation Canais Fluviais Faxinal Erosão de margens Degradação. |
topic |
River channels Faxinal Margin erosion Degradation Canais Fluviais Faxinal Erosão de margens Degradação. |
description |
This study aimed at evaluating the influence of the contact of animals with water bodies and hence their interference on the movement of river bed at Faxinal Marmeleiro de Cima, located in the municipality of Rebouças, Paraná State. The Faxinal System is a peculiar way of using and occupying the land, where there is a consortium between exploitation of natural resources and unrestricted animal husbandry, which has negative impacts on the water bodies. The direct contact of animals with water bodies implies in lack of riparian vegetation, contributing with the process of connecting the sediments of the slopes with river channels, forming sediment banks. In order to monitor the movement of these sediment banks in the riverbed, it was used the transverse profile method. Collections were conducted every two months, amounting 8 (eight) collections in 2009 and 2010. For assessing the progress of the margins it was used erosion pins. To monitor the rainfall, a direct measurement pluviometer was used. At the end of the monitoring, it was identified the degree of movement of river beds, with summer and autumn representing the periods with greater movement. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013-12-16 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Avaliado pelos pares |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/14411 10.5433/2447-1747.2012v21n3p75 |
url |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/14411 |
identifier_str_mv |
10.5433/2447-1747.2012v21n3p75 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/14411/13765 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2013 GEOGRAFIA (Londrina) info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2013 GEOGRAFIA (Londrina) |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Estadual de Londrina |
publisher.none.fl_str_mv |
Universidade Estadual de Londrina |
dc.source.none.fl_str_mv |
GEOGRAFIA (Londrina); v. 21 n. 3 (2012); 75-93 2447-1747 reponame:Geografia (Londrina) instname:Universidade Estadual de Londrina (UEL) instacron:UEL |
instname_str |
Universidade Estadual de Londrina (UEL) |
instacron_str |
UEL |
institution |
UEL |
reponame_str |
Geografia (Londrina) |
collection |
Geografia (Londrina) |
repository.name.fl_str_mv |
Geografia (Londrina) - Universidade Estadual de Londrina (UEL) |
repository.mail.fl_str_mv |
revista.geografia.uel@gmail.com||marcar@uel.br||laudi@uel.br |
_version_ |
1799315431250460672 |