Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil
The Manacapuru hydrometric gauge station has been used for more than 30 years by the Brazilian National hydrometric network to provide data on the Solimões-Amazon River. At this place, the Solimões river average water discharge is about 103,000 m³ s-1, the mean width is 3,000 m and the mean depth i...
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Format: | Article |
Language: | English |
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Asociación Argentina de Sedimentología
2021-03-01
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Series: | Latin American Journal of Sedimentology and Basin Analysis |
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Online Access: | https://www.lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/108 |
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author | Naziano Filizola Frederique Seyler Maria Helena Mourão Warley Arruda Nikolas Spínola Jean Loup Guyot |
author_facet | Naziano Filizola Frederique Seyler Maria Helena Mourão Warley Arruda Nikolas Spínola Jean Loup Guyot |
author_sort | Naziano Filizola |
collection | DOAJ |
description |
The Manacapuru hydrometric gauge station has been used for more than 30 years by the Brazilian National hydrometric network to provide data on the Solimões-Amazon River. At this place, the Solimões river average water discharge is about 103,000 m³ s-1, the mean width is 3,000 m and the mean depth is 20 m. The gauge station record represents the whole upstream contribution of the total suspended solids (TSS) from the Solimões basin, whose total area is approximately 2 x 106 km2, representing a runoff of 0.48 m³ s-1 km-2. TSS annual flow is approximately 400 x 106 t. The systematic TSS sampling procedures traditionally used at the Brazilian hydrometric network has limitations, some of them being related to local effects affecting the TSS flow. This article aims to study the local variability of TSS flow at Manacapuru station. The study was conducted in the scope of MESASOL and PIATAM IV projects, whose objectives are precisely to consider alternative methods for TSS flow assessment in the Amazon basin. It was identified that local geologic-geomorphologic features are related with the TSS flux spatial variability at the vicinity of the Manacapuru section. This results induce a new interpretation to the general sediment flux for the Solimões river basin, were local flux can’t be see as a total flux from the hole up-stream river basin.
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first_indexed | 2024-03-08T21:52:36Z |
format | Article |
id | doaj.art-db10b16724574916a43abbb76a3f2037 |
institution | Directory Open Access Journal |
issn | 1669-7316 1851-4979 |
language | English |
last_indexed | 2024-03-08T21:52:36Z |
publishDate | 2021-03-01 |
publisher | Asociación Argentina de Sedimentología |
record_format | Article |
series | Latin American Journal of Sedimentology and Basin Analysis |
spelling | doaj.art-db10b16724574916a43abbb76a3f20372023-12-20T06:18:27ZengAsociación Argentina de SedimentologíaLatin American Journal of Sedimentology and Basin Analysis1669-73161851-49792021-03-01162Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, BrazilNaziano FilizolaFrederique SeylerMaria Helena MourãoWarley ArrudaNikolas SpínolaJean Loup Guyot The Manacapuru hydrometric gauge station has been used for more than 30 years by the Brazilian National hydrometric network to provide data on the Solimões-Amazon River. At this place, the Solimões river average water discharge is about 103,000 m³ s-1, the mean width is 3,000 m and the mean depth is 20 m. The gauge station record represents the whole upstream contribution of the total suspended solids (TSS) from the Solimões basin, whose total area is approximately 2 x 106 km2, representing a runoff of 0.48 m³ s-1 km-2. TSS annual flow is approximately 400 x 106 t. The systematic TSS sampling procedures traditionally used at the Brazilian hydrometric network has limitations, some of them being related to local effects affecting the TSS flow. This article aims to study the local variability of TSS flow at Manacapuru station. The study was conducted in the scope of MESASOL and PIATAM IV projects, whose objectives are precisely to consider alternative methods for TSS flow assessment in the Amazon basin. It was identified that local geologic-geomorphologic features are related with the TSS flux spatial variability at the vicinity of the Manacapuru section. This results induce a new interpretation to the general sediment flux for the Solimões river basin, were local flux can’t be see as a total flux from the hole up-stream river basin. https://www.lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/108Suspended sediments; Acoustic Doppler Profiler; Amazon River |
spellingShingle | Naziano Filizola Frederique Seyler Maria Helena Mourão Warley Arruda Nikolas Spínola Jean Loup Guyot Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil Latin American Journal of Sedimentology and Basin Analysis Suspended sediments; Acoustic Doppler Profiler; Amazon River |
title | Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil |
title_full | Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil |
title_fullStr | Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil |
title_full_unstemmed | Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil |
title_short | Study of the variability in suspended sediment discharge at Manacapuru, Amazon River, Brazil |
title_sort | study of the variability in suspended sediment discharge at manacapuru amazon river brazil |
topic | Suspended sediments; Acoustic Doppler Profiler; Amazon River |
url | https://www.lajsba.sedimentologia.org.ar/index.php/lajsba/article/view/108 |
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