Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin

This article analyzes the flows of water and total suspended sediment in different reaches in the lower course of the Negro River, the largest fluvial blackwater system in the world. The area under study is the Anavilhanas Archipelago, which is a complex multichannel reach on the Negro River. Betwee...

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Main Authors: Rogério Ribeiro Marinho, Naziano Pantoja Filizola Junior, Édipo Henrique Cremon
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/4/1073
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spelling doaj-4338c00f4bde41a987fd5e56338fda612020-11-25T02:33:57ZengMDPI AGWater2073-44412020-04-01121073107310.3390/w12041073Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon BasinRogério Ribeiro Marinho0Naziano Pantoja Filizola Junior1Édipo Henrique Cremon2Postgraduation Program CLIAMB, Instituto Nacional de Pesquisas da Amazônia (INPA)—Universidade do Estado do Amazonas (UEA), Ave. André Araújo, 2936, Manaus CEP 69060-001, BrazilPostgraduation Program CLIAMB, Instituto Nacional de Pesquisas da Amazônia (INPA)—Universidade do Estado do Amazonas (UEA), Ave. André Araújo, 2936, Manaus CEP 69060-001, BrazilGrupo de Estudos em Geomática (GEO), Instituto Federal de Goiás (IFG), Rua 75, 46, Setor Central, Goiânia CEP 74055-110, BrazilThis article analyzes the flows of water and total suspended sediment in different reaches in the lower course of the Negro River, the largest fluvial blackwater system in the world. The area under study is the Anavilhanas Archipelago, which is a complex multichannel reach on the Negro River. Between the years 2016 and 2019, data about water discharge, velocity, and concentration of total suspended solids (TSS) were acquired in sample sections of the Negro River channels located upstream, inside, and downstream of the Anavilhanas Archipelago. In the study area, the Negro River drains an area greater than 700,000 km<sup>2</sup>, and the mean water discharge observed before the Anavilhanas was about 28.655 m<sup>3</sup>·s<sup>−1</sup>, of which 97% flows through two channels of the Archipelago close to the right and left banks. The mean TSS concentration of the Negro River upstream and downstream the Archipelago was 3.28 mg·L<sup>−1</sup> and 1.63 mg·L<sup>−1</sup>, respectively. Within the Archipelago, we observed more TSS in the channel on the left bank of the Negro River (mean of 4.50 mg·L<sup>−1</sup>). The total suspended sediment discharge of the Negro River before (3.14 Mt·year<sup>−1</sup>) and after (1.43 Mt·year<sup>−1</sup>) the Anavilhanas Archipelago indicates a 55% retention of the suspended load due to the low water slope and reduced flow velocity caused by the backwater effect of Solimões River on the Negro River. The hydro-sedimentary scenario of the low course of the Negro River characterized in this study indicates a slow and continuous sedimentation process in the Anavilhanas Archipelago. The results presented will serve as a baseline to assess the impacts of the dams on the Branco River, the main tributary for both water and sediment in the Negro River basin.https://www.mdpi.com/2073-4441/12/4/1073large riverssediment transportanabranchingfloodplainamazon basinfluvial archipelago
collection DOAJ
language English
format Article
sources DOAJ
author Rogério Ribeiro Marinho
Naziano Pantoja Filizola Junior
Édipo Henrique Cremon
spellingShingle Rogério Ribeiro Marinho
Naziano Pantoja Filizola Junior
Édipo Henrique Cremon
Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin
Water
large rivers
sediment transport
anabranching
floodplain
amazon basin
fluvial archipelago
author_facet Rogério Ribeiro Marinho
Naziano Pantoja Filizola Junior
Édipo Henrique Cremon
author_sort Rogério Ribeiro Marinho
title Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin
title_short Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin
title_full Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin
title_fullStr Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin
title_full_unstemmed Analysis of Suspended Sediment in the Anavilhanas Archipelago, Rio Negro, Amazon Basin
title_sort analysis of suspended sediment in the anavilhanas archipelago, rio negro, amazon basin
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-04-01
description This article analyzes the flows of water and total suspended sediment in different reaches in the lower course of the Negro River, the largest fluvial blackwater system in the world. The area under study is the Anavilhanas Archipelago, which is a complex multichannel reach on the Negro River. Between the years 2016 and 2019, data about water discharge, velocity, and concentration of total suspended solids (TSS) were acquired in sample sections of the Negro River channels located upstream, inside, and downstream of the Anavilhanas Archipelago. In the study area, the Negro River drains an area greater than 700,000 km<sup>2</sup>, and the mean water discharge observed before the Anavilhanas was about 28.655 m<sup>3</sup>·s<sup>−1</sup>, of which 97% flows through two channels of the Archipelago close to the right and left banks. The mean TSS concentration of the Negro River upstream and downstream the Archipelago was 3.28 mg·L<sup>−1</sup> and 1.63 mg·L<sup>−1</sup>, respectively. Within the Archipelago, we observed more TSS in the channel on the left bank of the Negro River (mean of 4.50 mg·L<sup>−1</sup>). The total suspended sediment discharge of the Negro River before (3.14 Mt·year<sup>−1</sup>) and after (1.43 Mt·year<sup>−1</sup>) the Anavilhanas Archipelago indicates a 55% retention of the suspended load due to the low water slope and reduced flow velocity caused by the backwater effect of Solimões River on the Negro River. The hydro-sedimentary scenario of the low course of the Negro River characterized in this study indicates a slow and continuous sedimentation process in the Anavilhanas Archipelago. The results presented will serve as a baseline to assess the impacts of the dams on the Branco River, the main tributary for both water and sediment in the Negro River basin.
topic large rivers
sediment transport
anabranching
floodplain
amazon basin
fluvial archipelago
url https://www.mdpi.com/2073-4441/12/4/1073
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