Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)

Autores
Depetris, Pedro José
Año de publicación
2019
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The multinational Paraná River (drainage basin, ~2.6 106 km2; annual discharge, ~500 km3 y-1) has a long (~900 km) and wide (~30 – 50 km) flood valley, which occupies its middle and lower stretches. Most of the valley’s area (estimated area of ~50000 kmkm2) holds a myriad of ponds, ox-bows, and channels which, following the seasonal variation of the prevailing discharge regime, exchanges water, dissolved species, sediment, and biological materials with the Paraná’s main stem. Exceptional hydrological events (e.g., ENSO-triggered) flood almost totally the expanse of the flood valley. A ten year-long (1965 – 1975) continuous series of alkalinity measurements allowed probing into the mechanisms that determine the observed alkalinity variability -controlled by several biogeochemical processes (e.g., photosynthesis/respiration, nitrification/denitrification, etc.) occurring in the riparian environment-, which are associated with the Paraná’s hydrological stage.
Centro de Investigaciones Geológicas
Materia
Geología
alkalinity
flood regime
ENSO effect
biogeochemistry
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-nd/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/77419

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spelling Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)An interpretation of the factors influencing alkalinity variability in the middle Paraná river (Argentina)Depetris, Pedro JoséGeologíaalkalinityflood regimeENSO effectbiogeochemistryThe multinational Paraná River (drainage basin, ~2.6 10<SUP>6</SUP> km<SUP>2</SUP>; annual discharge, ~500 km<SUP>3</SUP> y<SUP>-1</SUP>) has a long (~900 km) and wide (~30 – 50 km) flood valley, which occupies its middle and lower stretches. Most of the valley’s area (estimated area of ~50000 kmkm<SUP>2</SUP>) holds a myriad of ponds, ox-bows, and channels which, following the seasonal variation of the prevailing discharge regime, exchanges water, dissolved species, sediment, and biological materials with the Paraná’s main stem. Exceptional hydrological events (e.g., ENSO-triggered) flood almost totally the expanse of the flood valley. A ten year-long (1965 – 1975) continuous series of alkalinity measurements allowed probing into the mechanisms that determine the observed alkalinity variability -controlled by several biogeochemical processes (e.g., photosynthesis/respiration, nitrification/denitrification, etc.) occurring in the riparian environment-, which are associated with the Paraná’s hydrological stage.Centro de Investigaciones Geológicas2019-06info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdf98-101http://sedici.unlp.edu.ar/handle/10915/77419enginfo:eu-repo/semantics/altIdentifier/isbn/978-987-96296-7-3info:eu-repo/semantics/reference/hdl/10915/77067info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-nd/4.0/Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2026-06-23T10:36:22Zoai:sedici.unlp.edu.ar:10915/77419Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292026-06-23 10:36:23.196SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
An interpretation of the factors influencing alkalinity variability in the middle Paraná river (Argentina)
title Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
spellingShingle Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
Depetris, Pedro José
Geología
alkalinity
flood regime
ENSO effect
biogeochemistry
title_short Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
title_full Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
title_fullStr Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
title_full_unstemmed Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
title_sort Una interpretación de los factores que influyen sobre la variabilidad de la alcalinidad en el Río Paraná medio (Argentina)
dc.creator.none.fl_str_mv Depetris, Pedro José
author Depetris, Pedro José
author_facet Depetris, Pedro José
author_role author
dc.subject.none.fl_str_mv Geología
alkalinity
flood regime
ENSO effect
biogeochemistry
topic Geología
alkalinity
flood regime
ENSO effect
biogeochemistry
dc.description.none.fl_txt_mv The multinational Paraná River (drainage basin, ~2.6 10<SUP>6</SUP> km<SUP>2</SUP>; annual discharge, ~500 km<SUP>3</SUP> y<SUP>-1</SUP>) has a long (~900 km) and wide (~30 – 50 km) flood valley, which occupies its middle and lower stretches. Most of the valley’s area (estimated area of ~50000 kmkm<SUP>2</SUP>) holds a myriad of ponds, ox-bows, and channels which, following the seasonal variation of the prevailing discharge regime, exchanges water, dissolved species, sediment, and biological materials with the Paraná’s main stem. Exceptional hydrological events (e.g., ENSO-triggered) flood almost totally the expanse of the flood valley. A ten year-long (1965 – 1975) continuous series of alkalinity measurements allowed probing into the mechanisms that determine the observed alkalinity variability -controlled by several biogeochemical processes (e.g., photosynthesis/respiration, nitrification/denitrification, etc.) occurring in the riparian environment-, which are associated with the Paraná’s hydrological stage.
Centro de Investigaciones Geológicas
description The multinational Paraná River (drainage basin, ~2.6 10<SUP>6</SUP> km<SUP>2</SUP>; annual discharge, ~500 km<SUP>3</SUP> y<SUP>-1</SUP>) has a long (~900 km) and wide (~30 – 50 km) flood valley, which occupies its middle and lower stretches. Most of the valley’s area (estimated area of ~50000 kmkm<SUP>2</SUP>) holds a myriad of ponds, ox-bows, and channels which, following the seasonal variation of the prevailing discharge regime, exchanges water, dissolved species, sediment, and biological materials with the Paraná’s main stem. Exceptional hydrological events (e.g., ENSO-triggered) flood almost totally the expanse of the flood valley. A ten year-long (1965 – 1975) continuous series of alkalinity measurements allowed probing into the mechanisms that determine the observed alkalinity variability -controlled by several biogeochemical processes (e.g., photosynthesis/respiration, nitrification/denitrification, etc.) occurring in the riparian environment-, which are associated with the Paraná’s hydrological stage.
publishDate 2019
dc.date.none.fl_str_mv 2019-06
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info:eu-repo/semantics/publishedVersion
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