Decline of fine suspended sediments in the Madeira River basin (2003-2017)
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Outros Autores: | , , , , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional do INPA |
Texto Completo: | https://repositorio.inpa.gov.br/handle/1/15526 |
Resumo: | The Madeira River is the second largest Amazon tributary, contributing up to 50% of the Amazon River's sediment load. The Madeira has significant hydropower potential, which has started to be used by the Madeira Hydroelectric Complex (MHC), with two large dams along the middle stretch of the river. In this study, fine suspended sediment concentration (FSC) data were assessed downstream of the MHC at the Porto Velho gauging station and at the outlet of each tributary (Beni and Mamoré Rivers, upstream from the MHC), from 2003 to 2017. When comparing the pre-MHC (2003-2008) and post-MHC (2015-2017) periods, a 36% decrease in FSC was observed in the Beni River during the peak months of sediment load (December-March). At Porto Velho, a reduction of 30% was found, which responds to the Upper Madeira Basin and hydroelectric regulation. Concerning water discharge, no significant change occurred, indicating that a lower peak FSC cannot be explained by changes in the peak discharge months. However, lower FSCs are associated with a downward break in the overall time series registered at the outlet of the major sediment supplier-the Beni River-during 2010. © 2019 by the authors. |
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Rivera, Irma AyesCardenas, Elisa ArmijosEspinoza-Villar, RaúlEspinoza, J. C.Molina-Carpio, JorgeAyala, José MaxGutierrez-Cori, OmarMartinez, Jean MichelFilizola, Naziano Pantoja2020-05-14T20:03:46Z2020-05-14T20:03:46Z2019https://repositorio.inpa.gov.br/handle/1/1552610.3390/w11030514The Madeira River is the second largest Amazon tributary, contributing up to 50% of the Amazon River's sediment load. The Madeira has significant hydropower potential, which has started to be used by the Madeira Hydroelectric Complex (MHC), with two large dams along the middle stretch of the river. In this study, fine suspended sediment concentration (FSC) data were assessed downstream of the MHC at the Porto Velho gauging station and at the outlet of each tributary (Beni and Mamoré Rivers, upstream from the MHC), from 2003 to 2017. When comparing the pre-MHC (2003-2008) and post-MHC (2015-2017) periods, a 36% decrease in FSC was observed in the Beni River during the peak months of sediment load (December-March). At Porto Velho, a reduction of 30% was found, which responds to the Upper Madeira Basin and hydroelectric regulation. Concerning water discharge, no significant change occurred, indicating that a lower peak FSC cannot be explained by changes in the peak discharge months. However, lower FSCs are associated with a downward break in the overall time series registered at the outlet of the major sediment supplier-the Beni River-during 2010. © 2019 by the authors.Volume 11, Número 3Attribution-NonCommercial-NoDerivs 3.0 Brazilhttp://creativecommons.org/licenses/by-nc-nd/3.0/br/info:eu-repo/semantics/openAccessHydroelectric Power PlantsSuspended SedimentsAmazon RiverGauging StationsHydroelectric DamsHydropower PotentialPeak DischargeSediment LoadsSuspended Sediment ConcentrationsWater DischargesRiversConcentration (composition)Fine Grained SedimentFluvial DepositHydroelectric PowerPeak DischargeSediment TransportSuspended SedimentAmazon RiverBeni RiverBoliviaBrasilMadeira BasinPorto VelhoRondoniaDecline of fine suspended sediments in the Madeira River basin (2003-2017)info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleWater (Switzerland)engreponame:Repositório Institucional do INPAinstname:Instituto Nacional de Pesquisas da Amazônia (INPA)instacron:INPAORIGINALartigo-inpa.pdfartigo-inpa.pdfapplication/pdf2544119https://repositorio.inpa.gov.br/bitstream/1/15526/1/artigo-inpa.pdfe0ed5bb6efebcd6d0815ffc920a6c0bfMD511/155262020-05-14 19:03:09.435oai:repositorio:1/15526Repositório de PublicaçõesPUBhttps://repositorio.inpa.gov.br/oai/requestopendoar:2020-05-14T23:03:09Repositório Institucional do INPA - Instituto Nacional de Pesquisas da Amazônia (INPA)false |
dc.title.en.fl_str_mv |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
title |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
spellingShingle |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) Rivera, Irma Ayes Hydroelectric Power Plants Suspended Sediments Amazon River Gauging Stations Hydroelectric Dams Hydropower Potential Peak Discharge Sediment Loads Suspended Sediment Concentrations Water Discharges Rivers Concentration (composition) Fine Grained Sediment Fluvial Deposit Hydroelectric Power Peak Discharge Sediment Transport Suspended Sediment Amazon River Beni River Bolivia Brasil Madeira Basin Porto Velho Rondonia |
title_short |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
title_full |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
title_fullStr |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
title_full_unstemmed |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
title_sort |
Decline of fine suspended sediments in the Madeira River basin (2003-2017) |
author |
Rivera, Irma Ayes |
author_facet |
Rivera, Irma Ayes Cardenas, Elisa Armijos Espinoza-Villar, Raúl Espinoza, J. C. Molina-Carpio, Jorge Ayala, José Max Gutierrez-Cori, Omar Martinez, Jean Michel Filizola, Naziano Pantoja |
author_role |
author |
author2 |
Cardenas, Elisa Armijos Espinoza-Villar, Raúl Espinoza, J. C. Molina-Carpio, Jorge Ayala, José Max Gutierrez-Cori, Omar Martinez, Jean Michel Filizola, Naziano Pantoja |
author2_role |
author author author author author author author author |
dc.contributor.author.fl_str_mv |
Rivera, Irma Ayes Cardenas, Elisa Armijos Espinoza-Villar, Raúl Espinoza, J. C. Molina-Carpio, Jorge Ayala, José Max Gutierrez-Cori, Omar Martinez, Jean Michel Filizola, Naziano Pantoja |
dc.subject.eng.fl_str_mv |
Hydroelectric Power Plants Suspended Sediments Amazon River Gauging Stations Hydroelectric Dams Hydropower Potential Peak Discharge Sediment Loads Suspended Sediment Concentrations Water Discharges Rivers Concentration (composition) Fine Grained Sediment Fluvial Deposit Hydroelectric Power Peak Discharge Sediment Transport Suspended Sediment Amazon River Beni River Bolivia Brasil Madeira Basin Porto Velho Rondonia |
topic |
Hydroelectric Power Plants Suspended Sediments Amazon River Gauging Stations Hydroelectric Dams Hydropower Potential Peak Discharge Sediment Loads Suspended Sediment Concentrations Water Discharges Rivers Concentration (composition) Fine Grained Sediment Fluvial Deposit Hydroelectric Power Peak Discharge Sediment Transport Suspended Sediment Amazon River Beni River Bolivia Brasil Madeira Basin Porto Velho Rondonia |
description |
The Madeira River is the second largest Amazon tributary, contributing up to 50% of the Amazon River's sediment load. The Madeira has significant hydropower potential, which has started to be used by the Madeira Hydroelectric Complex (MHC), with two large dams along the middle stretch of the river. In this study, fine suspended sediment concentration (FSC) data were assessed downstream of the MHC at the Porto Velho gauging station and at the outlet of each tributary (Beni and Mamoré Rivers, upstream from the MHC), from 2003 to 2017. When comparing the pre-MHC (2003-2008) and post-MHC (2015-2017) periods, a 36% decrease in FSC was observed in the Beni River during the peak months of sediment load (December-March). At Porto Velho, a reduction of 30% was found, which responds to the Upper Madeira Basin and hydroelectric regulation. Concerning water discharge, no significant change occurred, indicating that a lower peak FSC cannot be explained by changes in the peak discharge months. However, lower FSCs are associated with a downward break in the overall time series registered at the outlet of the major sediment supplier-the Beni River-during 2010. © 2019 by the authors. |
publishDate |
2019 |
dc.date.issued.fl_str_mv |
2019 |
dc.date.accessioned.fl_str_mv |
2020-05-14T20:03:46Z |
dc.date.available.fl_str_mv |
2020-05-14T20:03:46Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://repositorio.inpa.gov.br/handle/1/15526 |
dc.identifier.doi.none.fl_str_mv |
10.3390/w11030514 |
url |
https://repositorio.inpa.gov.br/handle/1/15526 |
identifier_str_mv |
10.3390/w11030514 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartof.pt_BR.fl_str_mv |
Volume 11, Número 3 |
dc.rights.driver.fl_str_mv |
Attribution-NonCommercial-NoDerivs 3.0 Brazil http://creativecommons.org/licenses/by-nc-nd/3.0/br/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Attribution-NonCommercial-NoDerivs 3.0 Brazil http://creativecommons.org/licenses/by-nc-nd/3.0/br/ |
eu_rights_str_mv |
openAccess |
dc.publisher.none.fl_str_mv |
Water (Switzerland) |
publisher.none.fl_str_mv |
Water (Switzerland) |
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Repositório Institucional do INPA |
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