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
.jpg)
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/77419
Ver los metadatos del registro completo
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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. |
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2019 |
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2019-06 |
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info:eu-repo/semantics/conferenceObject info:eu-repo/semantics/publishedVersion Objeto de conferencia http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia |
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eng |
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eng |
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