Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River

Formation of mountain ranges results from complex coupling between lithospheric deformation, mechanisms linked to subduction and surface processes: weathering, erosion, and climate. Today, erosion of the eastern Andean cordillera and sub-Andean foothills supplies over 99% of the sediment load passin...

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Main Authors: W. Santini, J.-M. Martinez, R. Espinoza-Villar, G. Cochonneau, P. Vauchel, J.-S. Moquet, P. Baby, J.-C. Espinoza, W. Lavado, J. Carranza, J.-L. Guyot
Format: Article
Language:English
Published: Copernicus Publications 2015-03-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/367/320/2015/piahs-367-320-2015.pdf
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author W. Santini
W. Santini
J.-M. Martinez
J.-M. Martinez
R. Espinoza-Villar
G. Cochonneau
G. Cochonneau
P. Vauchel
P. Vauchel
J.-S. Moquet
P. Baby
P. Baby
J.-C. Espinoza
W. Lavado
J. Carranza
J.-L. Guyot
J.-L. Guyot
author_facet W. Santini
W. Santini
J.-M. Martinez
J.-M. Martinez
R. Espinoza-Villar
G. Cochonneau
G. Cochonneau
P. Vauchel
P. Vauchel
J.-S. Moquet
P. Baby
P. Baby
J.-C. Espinoza
W. Lavado
J. Carranza
J.-L. Guyot
J.-L. Guyot
author_sort W. Santini
collection DOAJ
description Formation of mountain ranges results from complex coupling between lithospheric deformation, mechanisms linked to subduction and surface processes: weathering, erosion, and climate. Today, erosion of the eastern Andean cordillera and sub-Andean foothills supplies over 99% of the sediment load passing through the Amazon Basin. Denudation rates in the upper Ucayali basin are rapid, favoured by a marked seasonality in this region and extreme precipitation cells above sedimentary strata, uplifted during Neogene times by a still active sub-Andean tectonic thrust. Around 40% of those sediments are trapped in the Ucayali retro-foreland basin system. Recent advances in remote sensing for Amazonian large rivers now allow us to complete the ground hydrological data. In this work, we propose a first estimation of the erosion and sedimentation budget of the Ucayali River catchment, based on spatial and conventional HYBAM Observatory network.
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spelling doaj.art-469ae83ffbb84a2d8fc2fd3f2f25b11e2022-12-22T01:20:43ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2015-03-0136732032510.5194/piahs-367-320-2015Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon RiverW. Santini0W. Santini1J.-M. Martinez2J.-M. Martinez3R. Espinoza-Villar4G. Cochonneau5G. Cochonneau6P. Vauchel7P. Vauchel8J.-S. Moquet9P. Baby10P. Baby11J.-C. Espinoza12W. Lavado13J. Carranza14J.-L. Guyot15J.-L. Guyot16IRD (Institut de Recherche pour le Développement), FranceGET (Géosciences Environnement Toulouse), Casilla 18-1209, Lima 18, PeruIRD (Institut de Recherche pour le Développement), FranceGET (Géosciences Environnement Toulouse), Casilla 18-1209, Lima 18, PeruUnB-IG (Universidade de Brasilia- Instituto de Geociencias), Campus Universitário Darcy Ribeiro, Brasilia, BrazilIRD (Institut de Recherche pour le Développement), FranceGET (Géosciences Environnement Toulouse), Casilla 18-1209, Lima 18, PeruIRD (Institut de Recherche pour le Développement), FranceGET (Géosciences Environnement Toulouse), Casilla 18-1209, Lima 18, PeruUSP (Universidade de São Paulo), Av. Prof. Almeida Prado, nº1280 - Butantã, São Paulo, BrazilIRD (Institut de Recherche pour le Développement), FranceGET (Géosciences Environnement Toulouse), Casilla 18-1209, Lima 18, PeruIGP (Instituto Geofisíco del Perú), Calle Badajoz #169 - Mayorazgo IV Etapa - Ate Vitarte, Lima, PeruSENAMHI (Servicio Nacional de Meteorología e Hidrología), Casilla 11-1308, Lima 11, PeruSENAMHI (Servicio Nacional de Meteorología e Hidrología), Casilla 11-1308, Lima 11, PeruIRD (Institut de Recherche pour le Développement), FranceGET (Géosciences Environnement Toulouse), Casilla 18-1209, Lima 18, PeruFormation of mountain ranges results from complex coupling between lithospheric deformation, mechanisms linked to subduction and surface processes: weathering, erosion, and climate. Today, erosion of the eastern Andean cordillera and sub-Andean foothills supplies over 99% of the sediment load passing through the Amazon Basin. Denudation rates in the upper Ucayali basin are rapid, favoured by a marked seasonality in this region and extreme precipitation cells above sedimentary strata, uplifted during Neogene times by a still active sub-Andean tectonic thrust. Around 40% of those sediments are trapped in the Ucayali retro-foreland basin system. Recent advances in remote sensing for Amazonian large rivers now allow us to complete the ground hydrological data. In this work, we propose a first estimation of the erosion and sedimentation budget of the Ucayali River catchment, based on spatial and conventional HYBAM Observatory network.https://www.proc-iahs.net/367/320/2015/piahs-367-320-2015.pdf
spellingShingle W. Santini
W. Santini
J.-M. Martinez
J.-M. Martinez
R. Espinoza-Villar
G. Cochonneau
G. Cochonneau
P. Vauchel
P. Vauchel
J.-S. Moquet
P. Baby
P. Baby
J.-C. Espinoza
W. Lavado
J. Carranza
J.-L. Guyot
J.-L. Guyot
Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River
Proceedings of the International Association of Hydrological Sciences
title Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River
title_full Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River
title_fullStr Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River
title_full_unstemmed Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River
title_short Sediment budget in the Ucayali River basin, an Andean tributary of the Amazon River
title_sort sediment budget in the ucayali river basin an andean tributary of the amazon river
url https://www.proc-iahs.net/367/320/2015/piahs-367-320-2015.pdf
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