CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL

Detalhes bibliográficos
Autor(a) principal: de Queiroz, Matheus Silveira
Data de Publicação: 2021
Outros Autores: Alves, Neiliane de Sousa
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Caminhos de Geografia
Texto Completo: https://seer.ufu.br/index.php/caminhosdegeografia/article/view/54842
Resumo: The term “Terras Caídas” is used in Amazon to refer to processes of fluvial erosion and mass movements of large and moderate scale. It is a dynamic and complex multi-causal process that involves hydrodynamic, hydrostatic, climatic, neotectonic, lithological and anthropic factors, occurring together or separately. The objective of this work is to understand the conditioning factors of the phenomenon "Terras Caídas" in lower Solimões River - Brazil. For this purpose, the study area was monitored for 2 years (2017-2018) and data from satellite images; water discharge; flow velocity; suspended sediments; water level; precipitation; wind direction; seismic activity were obtained. The hydrodynamic factors and the rain influence the “Terras Caídas” more intensely during the river flood, the processes influenced by the wind direction occur throughout the hydrological year, but with greater intensity during storms. Hydrostatic pressure occurs more frequently in ebb causing landslides. The lithology influences the stability of the banks due to unconsolidated sediments, providing erosion and mass movements. It is observed that neotectonics was not important in increasing the intensity of the "Terras Caídas" in the study area in recent years. Human activity influences destroying riparian forests and the basal erosion caused by waves formed by boats the region.
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spelling CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL“Terras Caídas”.Amazônia.Rio Solimões.Erosão.Movimento de Massa.“Terras Caídas”.Amazon.Solimões River.Erosion.Mass Movement.The term “Terras Caídas” is used in Amazon to refer to processes of fluvial erosion and mass movements of large and moderate scale. It is a dynamic and complex multi-causal process that involves hydrodynamic, hydrostatic, climatic, neotectonic, lithological and anthropic factors, occurring together or separately. The objective of this work is to understand the conditioning factors of the phenomenon "Terras Caídas" in lower Solimões River - Brazil. For this purpose, the study area was monitored for 2 years (2017-2018) and data from satellite images; water discharge; flow velocity; suspended sediments; water level; precipitation; wind direction; seismic activity were obtained. The hydrodynamic factors and the rain influence the “Terras Caídas” more intensely during the river flood, the processes influenced by the wind direction occur throughout the hydrological year, but with greater intensity during storms. Hydrostatic pressure occurs more frequently in ebb causing landslides. The lithology influences the stability of the banks due to unconsolidated sediments, providing erosion and mass movements. It is observed that neotectonics was not important in increasing the intensity of the "Terras Caídas" in the study area in recent years. Human activity influences destroying riparian forests and the basal erosion caused by waves formed by boats the region.O termo “Terras Caídas” é usado na Amazônia para designar processos de erosão fluvial e movimentos de massa de larga e moderada escala. É um processo dinâmico e complexo multicausal que envolve fatores hidrodinâmicos, hidrostáticos, climáticos, neotectônicos, litológicos e antrópicos, ocorrendo em conjunto ou separados. Este trabalho tem como objetivo compreender os fatores condicionantes do fenômeno das "Terras Caídas" no baixo rio Solimões – Brasil. Para isto a área de estudo foi monitorada durante dois anos (2017-2018) e foram obtidos dados de imagens de satélite; descarga de água; velocidade de fluxo; sedimentos em suspensão; nível da água; precipitação; direção do vento; atividade sísmica. Os fatores hidrodinâmicos e a chuva influenciam as “Terras Caídas” de forma mais intensa durante a cheia, os processos influenciados pela direção do vento ocorrem ao longo de todo o ano hidrológico, mas com maior intensidade durante as tempestades. A litologia influencia na estabilidade das margens devido a sedimentos inconsolidados, proporcionando erosão e movimentos de massa. Observa-se que a neotectônica não foi importante no aumento da intensidade das Terras Caídas na área de estudo nos últimos anos. A atividade humana influencia desmatando matas ciliares e na erosão basal causada pelas ondas formadas por barcos na região.       EDUFU - Editora da Universidade Federal de Uberlândia2021-04-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionAvaliado pelos paresapplication/pdfhttps://seer.ufu.br/index.php/caminhosdegeografia/article/view/5484210.14393/RCG228054842Caminhos de Geografia; Vol. 22 No. 80 (2021): Abril; 220-233Caminhos de Geografia; Vol. 22 Núm. 80 (2021): Abril; 220-233Caminhos de Geografia; v. 22 n. 80 (2021): Abril; 220-2331678-6343reponame:Caminhos de Geografiainstname:Universidade Federal de Uberlândia (UFU)instacron:UFUenghttps://seer.ufu.br/index.php/caminhosdegeografia/article/view/54842/31395Copyright (c) 2021 Matheus Silveira de Queiroz, Neiliane de Sousa Alvesinfo:eu-repo/semantics/openAccessde Queiroz, Matheus SilveiraAlves, Neiliane de Sousa2021-04-22T20:24:22Zoai:ojs.www.seer.ufu.br:article/54842Revistahttps://seer.ufu.br/index.php/caminhosdegeografia/indexPUBhttp://www.seer.ufu.br/index.php/caminhosdegeografia/oaiflaviasantosgeo@gmail.com1678-63431678-6343opendoar:2021-04-22T20:24:22Caminhos de Geografia - Universidade Federal de Uberlândia (UFU)false
dc.title.none.fl_str_mv CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
title CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
spellingShingle CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
de Queiroz, Matheus Silveira
“Terras Caídas”.
Amazônia.
Rio Solimões.
Erosão.
Movimento de Massa.
“Terras Caídas”.
Amazon.
Solimões River.
Erosion.
Mass Movement.
title_short CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
title_full CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
title_fullStr CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
title_full_unstemmed CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
title_sort CONDITIONING FACTORS OF “TERRAS CAÍDAS” IN LOWER SOLIMÕES RIVER - BRAZIL
author de Queiroz, Matheus Silveira
author_facet de Queiroz, Matheus Silveira
Alves, Neiliane de Sousa
author_role author
author2 Alves, Neiliane de Sousa
author2_role author
dc.contributor.author.fl_str_mv de Queiroz, Matheus Silveira
Alves, Neiliane de Sousa
dc.subject.por.fl_str_mv “Terras Caídas”.
Amazônia.
Rio Solimões.
Erosão.
Movimento de Massa.
“Terras Caídas”.
Amazon.
Solimões River.
Erosion.
Mass Movement.
topic “Terras Caídas”.
Amazônia.
Rio Solimões.
Erosão.
Movimento de Massa.
“Terras Caídas”.
Amazon.
Solimões River.
Erosion.
Mass Movement.
description The term “Terras Caídas” is used in Amazon to refer to processes of fluvial erosion and mass movements of large and moderate scale. It is a dynamic and complex multi-causal process that involves hydrodynamic, hydrostatic, climatic, neotectonic, lithological and anthropic factors, occurring together or separately. The objective of this work is to understand the conditioning factors of the phenomenon "Terras Caídas" in lower Solimões River - Brazil. For this purpose, the study area was monitored for 2 years (2017-2018) and data from satellite images; water discharge; flow velocity; suspended sediments; water level; precipitation; wind direction; seismic activity were obtained. The hydrodynamic factors and the rain influence the “Terras Caídas” more intensely during the river flood, the processes influenced by the wind direction occur throughout the hydrological year, but with greater intensity during storms. Hydrostatic pressure occurs more frequently in ebb causing landslides. The lithology influences the stability of the banks due to unconsolidated sediments, providing erosion and mass movements. It is observed that neotectonics was not important in increasing the intensity of the "Terras Caídas" in the study area in recent years. Human activity influences destroying riparian forests and the basal erosion caused by waves formed by boats the region.
publishDate 2021
dc.date.none.fl_str_mv 2021-04-05
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://seer.ufu.br/index.php/caminhosdegeografia/article/view/54842
10.14393/RCG228054842
url https://seer.ufu.br/index.php/caminhosdegeografia/article/view/54842
identifier_str_mv 10.14393/RCG228054842
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://seer.ufu.br/index.php/caminhosdegeografia/article/view/54842/31395
dc.rights.driver.fl_str_mv Copyright (c) 2021 Matheus Silveira de Queiroz, Neiliane de Sousa Alves
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2021 Matheus Silveira de Queiroz, Neiliane de Sousa Alves
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv EDUFU - Editora da Universidade Federal de Uberlândia
publisher.none.fl_str_mv EDUFU - Editora da Universidade Federal de Uberlândia
dc.source.none.fl_str_mv Caminhos de Geografia; Vol. 22 No. 80 (2021): Abril; 220-233
Caminhos de Geografia; Vol. 22 Núm. 80 (2021): Abril; 220-233
Caminhos de Geografia; v. 22 n. 80 (2021): Abril; 220-233
1678-6343
reponame:Caminhos de Geografia
instname:Universidade Federal de Uberlândia (UFU)
instacron:UFU
instname_str Universidade Federal de Uberlândia (UFU)
instacron_str UFU
institution UFU
reponame_str Caminhos de Geografia
collection Caminhos de Geografia
repository.name.fl_str_mv Caminhos de Geografia - Universidade Federal de Uberlândia (UFU)
repository.mail.fl_str_mv flaviasantosgeo@gmail.com
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