Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES

Detalhes bibliográficos
Autor(a) principal: Lemos, Fernando Henrique
Data de Publicação: 2018
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Repositório Institucional da Universidade Federal do Espírito Santo (riUfes)
Texto Completo: http://repositorio.ufes.br/handle/10/10671
Resumo: Streams and rivers are the main channel of natural and anthropogenic matter flows along the catchment. The different uses and coverages of land, climatic conditions and characteristics of the catchment are factors that control the hydrossedimentological and nutrient flows. Therefore, this work aimed to evaluate the hydrossedimentological and nutrient fluxes along the longitudinal profile of the Duas Bocas river, Cariacica - ES. To that end, suspended solids or sediments, total nitrogen, total phosphorus, pH, total dissolved solids, dissolved oxygen, electrical conductivity, turbidity, water temperature and water discharge were used as parameters. The monitoring of these parameters occurred in 04 sampling stations distributed along the main channel of the Duas Bocas river from August 2016 to August 2017. Rainfall monitoring was carried out from a climatic station located at 740 m altitude inside the Biological Reserve of Duas Bocas. The Kruskal Wallis statistical test was used to analyze the occurrence of differences between samples and sampling stations. For correlations between parameters the Spearman coefficient was used. The monthly rainfall recorded was below the normal precipitation, collaborating to interrupt the flow in stations DB03 and DB04 in the months of lower rainfall. The largest flow rates were recorded at station DB01. The concentrations of suspended solids, total nitrogen and total phosphorus were lower in DB01, Atlantic Forest area, and increased gradually to each downstream season. The decrease of the dissolved oxygen indicates the contribution of organic matter, something corroborated by the positive correlation between the total solids and electrical conductivity, emphasizing the increase of dissolved ions in the water coming from effluent releases.
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spelling Barroso, Gilberto FonsecaMarchioro, EbervalLemos, Fernando HenriqueRocha, Pablo AzevedoBuarque, Diogo Costa2018-12-20T13:35:45Z2018-12-202018-12-20T13:35:45Z2018-08-03Streams and rivers are the main channel of natural and anthropogenic matter flows along the catchment. The different uses and coverages of land, climatic conditions and characteristics of the catchment are factors that control the hydrossedimentological and nutrient flows. Therefore, this work aimed to evaluate the hydrossedimentological and nutrient fluxes along the longitudinal profile of the Duas Bocas river, Cariacica - ES. To that end, suspended solids or sediments, total nitrogen, total phosphorus, pH, total dissolved solids, dissolved oxygen, electrical conductivity, turbidity, water temperature and water discharge were used as parameters. The monitoring of these parameters occurred in 04 sampling stations distributed along the main channel of the Duas Bocas river from August 2016 to August 2017. Rainfall monitoring was carried out from a climatic station located at 740 m altitude inside the Biological Reserve of Duas Bocas. The Kruskal Wallis statistical test was used to analyze the occurrence of differences between samples and sampling stations. For correlations between parameters the Spearman coefficient was used. The monthly rainfall recorded was below the normal precipitation, collaborating to interrupt the flow in stations DB03 and DB04 in the months of lower rainfall. The largest flow rates were recorded at station DB01. The concentrations of suspended solids, total nitrogen and total phosphorus were lower in DB01, Atlantic Forest area, and increased gradually to each downstream season. The decrease of the dissolved oxygen indicates the contribution of organic matter, something corroborated by the positive correlation between the total solids and electrical conductivity, emphasizing the increase of dissolved ions in the water coming from effluent releases.Córregos e rios são os principais caminhos de fluxos de matéria natural e antropogênica ao longo da bacia hidrográfica. Os diferentes usos e coberturas da terra, condições climáticas e características da bacia são fatores que controlam os fluxos hidrossedimentológicos e de nutrientes. Neste sentido, este trabalho teve como objetivo analisar os fluxos hidrossedimentológicos e de nutrientes ao longo do perfil longitudinal do rio Duas Bocas, Cariacica – ES. Para isso, foram utilizados como parâmetros os sólidos em suspensão ou sedimentos, nitrogênio total, fósforo total, pH, sólidos totais dissolvidos, oxigênio dissolvido, condutividade elétrica, turbidez, temperatura da água e vazão fluvial. O monitoramento desses parâmetros ocorreu em 04 estações amostrais distribuídas ao longo do canal principal do rio Duas Bocas no período de agosto de 2016 a agosto de 2017. O monitoramento da precipitação pluvial foi realizado a partir de uma estação climática localizada à 740 m de altitude no interior da Reserva Biológica de Duas Bocas. Foi utilizado o teste estatístico Kruskal Wallis, que possibilitou analisar a ocorrência de diferenças entre as amostragens e estações amostrais. Para correlações entre os parâmetros foi utilizado o coeficiente de Spearman. Os acumulados pluviométricos mensais registrados ficaram abaixo da normal de precipitação, colaborando para a interrupção da vazão nas estações DB03 e DB04 nos meses de menor pluviosidade. As maiores vazões foram registradas na estação DB01. As concentrações de sólidos em suspensão, nitrogênio total e fósforo total foram menores na estação DB01, área de Mata Atlântica, e aumentaram gradativamente a cada estação a jusante. Os parâmetros físicos e químicos evidenciaram efeitos de atividades antrópicas a partir da estação DB02. A diminuição do oxigênio dissolvido aponta o aporte de matéria orgânica, algo corroborado pela correlação positiva entre os sólidos totais e condutividade elétrica, salientando o aumento de íons dissolvidos nas águas provenientes de lançamentos de efluentes.Texthttp://repositorio.ufes.br/handle/10/10671porUniversidade Federal do Espírito SantoMestrado em GeografiaPrograma de Pós-Graduação em GeografiaUFESBRCatchmentsErosionSedimentNutrientsBacia hidrográficaSedimentoBacias hidrográficas - Cariacica (ES)ErosãoSedimentos fluviaisNutrientesGeografia91Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ESinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da Universidade Federal do Espírito Santo (riUfes)instname:Universidade Federal do Espírito Santo (UFES)instacron:UFESORIGINALtese_12692_Dissertacao_FHL.pdfapplication/pdf5011762http://repositorio.ufes.br/bitstreams/fadc59cc-43e1-473b-809d-2ed72e5203fe/download11bf98cbcfadd61fbdd63506a197268aMD5110/106712024-07-01 20:33:37.398oai:repositorio.ufes.br:10/10671http://repositorio.ufes.brRepositório InstitucionalPUBhttp://repositorio.ufes.br/oai/requestopendoar:21082024-07-11T14:35:10.784775Repositório Institucional da Universidade Federal do Espírito Santo (riUfes) - Universidade Federal do Espírito Santo (UFES)false
dc.title.none.fl_str_mv Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
title Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
spellingShingle Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
Lemos, Fernando Henrique
Catchments
Erosion
Sediment
Nutrients
Bacia hidrográfica
Sedimento
Geografia
Bacias hidrográficas - Cariacica (ES)
Erosão
Sedimentos fluviais
Nutrientes
91
title_short Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
title_full Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
title_fullStr Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
title_full_unstemmed Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
title_sort Fluxos hidrossedimentológicos e de nutrientes no rio Duas Bocas, Cariacica-ES
author Lemos, Fernando Henrique
author_facet Lemos, Fernando Henrique
author_role author
dc.contributor.advisor-co1.fl_str_mv Barroso, Gilberto Fonseca
dc.contributor.advisor1.fl_str_mv Marchioro, Eberval
dc.contributor.author.fl_str_mv Lemos, Fernando Henrique
dc.contributor.referee1.fl_str_mv Rocha, Pablo Azevedo
dc.contributor.referee2.fl_str_mv Buarque, Diogo Costa
contributor_str_mv Barroso, Gilberto Fonseca
Marchioro, Eberval
Rocha, Pablo Azevedo
Buarque, Diogo Costa
dc.subject.eng.fl_str_mv Catchments
Erosion
Sediment
Nutrients
topic Catchments
Erosion
Sediment
Nutrients
Bacia hidrográfica
Sedimento
Geografia
Bacias hidrográficas - Cariacica (ES)
Erosão
Sedimentos fluviais
Nutrientes
91
dc.subject.por.fl_str_mv Bacia hidrográfica
Sedimento
dc.subject.cnpq.fl_str_mv Geografia
dc.subject.br-rjbn.none.fl_str_mv Bacias hidrográficas - Cariacica (ES)
Erosão
Sedimentos fluviais
Nutrientes
dc.subject.udc.none.fl_str_mv 91
description Streams and rivers are the main channel of natural and anthropogenic matter flows along the catchment. The different uses and coverages of land, climatic conditions and characteristics of the catchment are factors that control the hydrossedimentological and nutrient flows. Therefore, this work aimed to evaluate the hydrossedimentological and nutrient fluxes along the longitudinal profile of the Duas Bocas river, Cariacica - ES. To that end, suspended solids or sediments, total nitrogen, total phosphorus, pH, total dissolved solids, dissolved oxygen, electrical conductivity, turbidity, water temperature and water discharge were used as parameters. The monitoring of these parameters occurred in 04 sampling stations distributed along the main channel of the Duas Bocas river from August 2016 to August 2017. Rainfall monitoring was carried out from a climatic station located at 740 m altitude inside the Biological Reserve of Duas Bocas. The Kruskal Wallis statistical test was used to analyze the occurrence of differences between samples and sampling stations. For correlations between parameters the Spearman coefficient was used. The monthly rainfall recorded was below the normal precipitation, collaborating to interrupt the flow in stations DB03 and DB04 in the months of lower rainfall. The largest flow rates were recorded at station DB01. The concentrations of suspended solids, total nitrogen and total phosphorus were lower in DB01, Atlantic Forest area, and increased gradually to each downstream season. The decrease of the dissolved oxygen indicates the contribution of organic matter, something corroborated by the positive correlation between the total solids and electrical conductivity, emphasizing the increase of dissolved ions in the water coming from effluent releases.
publishDate 2018
dc.date.accessioned.fl_str_mv 2018-12-20T13:35:45Z
dc.date.available.fl_str_mv 2018-12-20
2018-12-20T13:35:45Z
dc.date.issued.fl_str_mv 2018-08-03
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
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dc.language.iso.fl_str_mv por
language por
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv Text
dc.publisher.none.fl_str_mv Universidade Federal do Espírito Santo
Mestrado em Geografia
dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Geografia
dc.publisher.initials.fl_str_mv UFES
dc.publisher.country.fl_str_mv BR
publisher.none.fl_str_mv Universidade Federal do Espírito Santo
Mestrado em Geografia
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