Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin
Autor(a) principal: | |
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Data de Publicação: | 2020 |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Revista Geotemas |
Texto Completo: | https://periodicos.apps.uern.br/index.php/GEOTemas/article/view/2777 |
Resumo: | The Negro River before the confluence with the Amazon River presents a complex fluvial system composed of islands, channels and lakes interconnected to the floodplain, which is known as the Anavilhanas Archipelago. This study analyzed the morphodynamics characteristics of the lakes inside the Anavilhanas Archipelago using images from the Sentinel-1 (SAR sensor) and Landsat-5 (TM sensor) satellites. Bathymetric data, suspended sediment concentration and grain size from the Apacú Lake, the largest lake in Anavilhanas, are also presented. Based on images from the Sentinel1 satellite, a water surface ranging from 390 to 340 km2 was detected in the hydrological year 2017. The Anavilhanas fluvial complex has a surface of 2000 km2, of which 20% of this area is occupied by more than 300 lakes with elongated and narrow morphometry, with size ranging from 0.01 to 59 km2, where 63% are less than 0.53 km2. The annual hydrological dynamics of the Negro River causes low changes in the water surface of the Anavilhanas lake system, with a variation of 15% in the area occupied by the lakes between the period of high water and low water levels. The largest lake in Anavilhanas (Apacú Lake) has an annual average of suspended sediment concentration of 4.15 mg L-1, composed of fine particles (D50 0.02 mm). This paper presents to the scientific community a detailed morphometric survey of the Anavilhanas lakes and the analysis of their local characteristics in relation to the geomorphological style of the lower Negro River. |
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Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin Estudio morfodinámico del ambiente lacustre en el Archipiélago de Anavilhanas, Río Negro, Cuenca AmazónicaESTUDO MORFODINÂMICO DO AMBIENTE LACUSTRE NO ARQUIPÉLAGO DE ANAVILHANAS, RIO NEGRO, BACIA AMAZÔNICA Planície de inundaçãoGeomorfologia fluvialSedimento suspensoSensoriamento remotoFloodplainFluvial geomorphologySuspended sedimentRemote sensingLlanura de inundaciónGeomorfología fluvialSedimento en suspensiónTeledetecciónThe Negro River before the confluence with the Amazon River presents a complex fluvial system composed of islands, channels and lakes interconnected to the floodplain, which is known as the Anavilhanas Archipelago. This study analyzed the morphodynamics characteristics of the lakes inside the Anavilhanas Archipelago using images from the Sentinel-1 (SAR sensor) and Landsat-5 (TM sensor) satellites. Bathymetric data, suspended sediment concentration and grain size from the Apacú Lake, the largest lake in Anavilhanas, are also presented. Based on images from the Sentinel1 satellite, a water surface ranging from 390 to 340 km2 was detected in the hydrological year 2017. The Anavilhanas fluvial complex has a surface of 2000 km2, of which 20% of this area is occupied by more than 300 lakes with elongated and narrow morphometry, with size ranging from 0.01 to 59 km2, where 63% are less than 0.53 km2. The annual hydrological dynamics of the Negro River causes low changes in the water surface of the Anavilhanas lake system, with a variation of 15% in the area occupied by the lakes between the period of high water and low water levels. The largest lake in Anavilhanas (Apacú Lake) has an annual average of suspended sediment concentration of 4.15 mg L-1, composed of fine particles (D50 0.02 mm). This paper presents to the scientific community a detailed morphometric survey of the Anavilhanas lakes and the analysis of their local characteristics in relation to the geomorphological style of the lower Negro River.El Río Negro antes de la confluencia con el Río Amazonas presenta un complejo sistema fluvial compuesto por islas, canales y lagos interconectados a la llanura de inundación, que se conoce como el archipiélago de Anavilhanas. Este estudio analizó las características morfométricas de los lagos en el archipiélago de Anavilhanas utilizando imágenes de los satélites Sentinel-1 (sensor SAR) y Landsat-5 (sensor TM). También se presentan datos batimétricos, concentración y granulometría de sedimentos en suspensión del lago Apacú, el lago más grande de Anavilhanas. Basado en imágenes del satélite Sentinel-1, se detectó una superficie de agua que oscila entre 390 y 340 km2 en el año hidrológico de 2017. El complejo fluvial de Anavilhanas tiene una superficie de 2000 km2, de los cuales el 20% de esta área está ocupada por más de 300 lagos con morfometria alargada y estrecha, con un tamaño que varía de 0.01 a 59 km2, donde el 63% tiene menos de 0.53 km2. La dinámica hidrológica anual del Río Negro causa pocos cambios en la superficie del agua del sistema de lagos de Anavilhanas, con una variación del 15% en el área ocupada por los lagos entre el período de crecida y estiaje. El lago más grande de Anavilhanas (lago Apacú) tiene un promedio anual de concentración de sedimento en suspensión de 4.15 mg L-1, compuesto de partículas finas (D50 0.02 mm). Este artículo presenta a la comunidad científica un estudio morfométrico detallado de los lagos Anavilhanas y el examen de sus características locales en relación con el estilo geomorfológico del bajo Río Negro.O rio Negro antes da confluência com o rio Amazonas apresenta um complexo sistema de ilhas, canais e lagos interconectados à planície de inundação, conhecido como Arquipélago de Anavilhanas. Este estudo teve como objetivo analisar a morfodinâmica dos lagos situados no interior das ilhas de Anavilhanas. Imagens dos satélites Sentinel-1 e Landsat-5 foram utilizadas para mapear as unidades fluviais de Anavilhanas e estimar o comprimento, área, perímetro, largura e forma dos lagos. Dados de batimetria, de granulometria e concentração de sedimentos suspensos coletados no maior lago de Anavilhanas são apresentados. Através da classificação de imagens do Sentinel-1 foi detectada uma superfície de água que variou de 340 a 390 km2 no ano hidrológico de 2017. O Complexo fluvial de Anavilhanas possui uma superfície de 2000 km2 dos quais 20% desta área é ocupada por mais de 300 lagos de forma alongada e estreita, com tamanho variando de 0,01 a 59 km2, onde 63% são menores que 0,53 km2. A dinâmica hidrológica anual do rio Negro ocasiona pouca mudança na superfície de água no ambiente lacustre de Anavilhanas, com variação de 15% na área ocupada pelos lagos entre o período de cheia e de seca. O maior lago de Anavilhanas (lago Apacú) apresenta média anual da concentração de sedimentos suspensos de 4,15 mg L-1, composto de partículas finas (D50 0,02 mm). Este trabalho apresenta para a comunidade científica um detalhado levantamento morfométrico dos lagos de Anavilhanas e uma análise de suas características locais com relação ao estilo geomorfológico do baixo rio Negro.Universidade do Estado do Rio Grande do Norte (UERN)2020-12-29info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersion Peer reviewed Revisado por paresAvaliado pelos paresapplication/pdfhttps://periodicos.apps.uern.br/index.php/GEOTemas/article/view/2777Journal Geotemas; Vol. 10 No. 3 (2020): Revista Geotemas; 81-105Revista Geotemas; Vol. 10 Núm. 3 (2020): Revista Geotemas; 81-105Revista Geotemas; v. 10 n. 3 (2020): Revista Geotemas; 81-1052236-255Xreponame:Revista Geotemasinstname:Universidade do Estado do Rio Grande do Norte (UERN)instacron:UERNporhttps://periodicos.apps.uern.br/index.php/GEOTemas/article/view/2777/2511Copyright (c) 2020 Revista Geotemasinfo:eu-repo/semantics/openAccessMarinho, Rogério Ribeiro 2020-12-29T15:34:09Zoai:ojs2.periodicos.apps.uern.br:article/2777Revistahttp://periodicos.apps.uern.br/index.php/GEOTemas/indexPUBhttp://periodicos.apps.uern.br/index.php/GEOTemas/oaigeotemas@uern.br||josielguedes@yahoo.com.br2236-255X2236-255Xopendoar:2020-12-29T15:34:09Revista Geotemas - Universidade do Estado do Rio Grande do Norte (UERN)false |
dc.title.none.fl_str_mv |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin Estudio morfodinámico del ambiente lacustre en el Archipiélago de Anavilhanas, Río Negro, Cuenca Amazónica ESTUDO MORFODINÂMICO DO AMBIENTE LACUSTRE NO ARQUIPÉLAGO DE ANAVILHANAS, RIO NEGRO, BACIA AMAZÔNICA |
title |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin |
spellingShingle |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin Marinho, Rogério Ribeiro Planície de inundação Geomorfologia fluvial Sedimento suspenso Sensoriamento remoto Floodplain Fluvial geomorphology Suspended sediment Remote sensing Llanura de inundación Geomorfología fluvial Sedimento en suspensión Teledetección |
title_short |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin |
title_full |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin |
title_fullStr |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin |
title_full_unstemmed |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin |
title_sort |
Morphodynamic study of the lacustrine environment in Anavilhanas archipelago, Negro River, Amazon basin |
author |
Marinho, Rogério Ribeiro |
author_facet |
Marinho, Rogério Ribeiro |
author_role |
author |
dc.contributor.author.fl_str_mv |
Marinho, Rogério Ribeiro |
dc.subject.por.fl_str_mv |
Planície de inundação Geomorfologia fluvial Sedimento suspenso Sensoriamento remoto Floodplain Fluvial geomorphology Suspended sediment Remote sensing Llanura de inundación Geomorfología fluvial Sedimento en suspensión Teledetección |
topic |
Planície de inundação Geomorfologia fluvial Sedimento suspenso Sensoriamento remoto Floodplain Fluvial geomorphology Suspended sediment Remote sensing Llanura de inundación Geomorfología fluvial Sedimento en suspensión Teledetección |
description |
The Negro River before the confluence with the Amazon River presents a complex fluvial system composed of islands, channels and lakes interconnected to the floodplain, which is known as the Anavilhanas Archipelago. This study analyzed the morphodynamics characteristics of the lakes inside the Anavilhanas Archipelago using images from the Sentinel-1 (SAR sensor) and Landsat-5 (TM sensor) satellites. Bathymetric data, suspended sediment concentration and grain size from the Apacú Lake, the largest lake in Anavilhanas, are also presented. Based on images from the Sentinel1 satellite, a water surface ranging from 390 to 340 km2 was detected in the hydrological year 2017. The Anavilhanas fluvial complex has a surface of 2000 km2, of which 20% of this area is occupied by more than 300 lakes with elongated and narrow morphometry, with size ranging from 0.01 to 59 km2, where 63% are less than 0.53 km2. The annual hydrological dynamics of the Negro River causes low changes in the water surface of the Anavilhanas lake system, with a variation of 15% in the area occupied by the lakes between the period of high water and low water levels. The largest lake in Anavilhanas (Apacú Lake) has an annual average of suspended sediment concentration of 4.15 mg L-1, composed of fine particles (D50 0.02 mm). This paper presents to the scientific community a detailed morphometric survey of the Anavilhanas lakes and the analysis of their local characteristics in relation to the geomorphological style of the lower Negro River. |
publishDate |
2020 |
dc.date.none.fl_str_mv |
2020-12-29 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer reviewed Revisado por pares Avaliado pelos pares |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://periodicos.apps.uern.br/index.php/GEOTemas/article/view/2777 |
url |
https://periodicos.apps.uern.br/index.php/GEOTemas/article/view/2777 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://periodicos.apps.uern.br/index.php/GEOTemas/article/view/2777/2511 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2020 Revista Geotemas info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2020 Revista Geotemas |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade do Estado do Rio Grande do Norte (UERN) |
publisher.none.fl_str_mv |
Universidade do Estado do Rio Grande do Norte (UERN) |
dc.source.none.fl_str_mv |
Journal Geotemas; Vol. 10 No. 3 (2020): Revista Geotemas; 81-105 Revista Geotemas; Vol. 10 Núm. 3 (2020): Revista Geotemas; 81-105 Revista Geotemas; v. 10 n. 3 (2020): Revista Geotemas; 81-105 2236-255X reponame:Revista Geotemas instname:Universidade do Estado do Rio Grande do Norte (UERN) instacron:UERN |
instname_str |
Universidade do Estado do Rio Grande do Norte (UERN) |
instacron_str |
UERN |
institution |
UERN |
reponame_str |
Revista Geotemas |
collection |
Revista Geotemas |
repository.name.fl_str_mv |
Revista Geotemas - Universidade do Estado do Rio Grande do Norte (UERN) |
repository.mail.fl_str_mv |
geotemas@uern.br||josielguedes@yahoo.com.br |
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1805033581281542144 |