Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities
- Autores
- Marchetti, Zuleica Yael; Carrillo Rivera, José Joel
- Año de publicación
- 2014
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Groundwater discharge can be an important determinant of the functioning of aquatic environments and their associated biological communities. However, the presence and the importance of groundwater have not been considered in the Parana River floodplain owing to the large quantity of surface water. The present study aimed to identify groundwater discharge conditions in a sector of the middle of the floodplain of the Parana River by studying groundwater flow systems. Eight piezometers were installed to record groundwater movement in the vertical plane weekly for 2years. Water samples were collected in piezometers, domestic wells, the river and other water bodies to study the groundwater flow systems. Rising of the water level during piezometer installation and recording suggested that the study zone represents groundwater discharge conditions. Residence time proxy allowed identification of local flows and intermediate flows. Local rainfall (in Santa Fe) showed an isotopic signature (δD and δ18O) similar to some local flows detected in the study zone, and this suggested local recharge. The chemical characteristics of an intermediate flow suggest that water would have travelled from a recharge area ~30km from the study zone. Local rainfall and the intermediate flow have different isotopic signature. Results suggest that the willow forest is associated with the recharge area of a local flow, which plurispecific-canopy forest is related to a transit area of a semi-intermediate flow, and that tall grassland and marshy community colonize discharge areas of local and intermediate flows, respectively.
Fil: Marchetti, Zuleica Yael. Centro de Investigaciones Científicas y Transferencia de Tecnología A la Producción Cicyttpconicet; Argentina
Fil: Carrillo Rivera, José Joel. Universidad Nacional Autónoma de México; México - Materia
-
SURFACE WATER AND GROUNDWATER INTERACTIONS
FLOW SYSTEMS
FLOODPLAIN ECOSYSTEMS
GROUNDWATER DISCHARGE - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/92756
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Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communitiesMarchetti, Zuleica YaelCarrillo Rivera, José JoelSURFACE WATER AND GROUNDWATER INTERACTIONSFLOW SYSTEMSFLOODPLAIN ECOSYSTEMSGROUNDWATER DISCHARGEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Groundwater discharge can be an important determinant of the functioning of aquatic environments and their associated biological communities. However, the presence and the importance of groundwater have not been considered in the Parana River floodplain owing to the large quantity of surface water. The present study aimed to identify groundwater discharge conditions in a sector of the middle of the floodplain of the Parana River by studying groundwater flow systems. Eight piezometers were installed to record groundwater movement in the vertical plane weekly for 2years. Water samples were collected in piezometers, domestic wells, the river and other water bodies to study the groundwater flow systems. Rising of the water level during piezometer installation and recording suggested that the study zone represents groundwater discharge conditions. Residence time proxy allowed identification of local flows and intermediate flows. Local rainfall (in Santa Fe) showed an isotopic signature (δD and δ18O) similar to some local flows detected in the study zone, and this suggested local recharge. The chemical characteristics of an intermediate flow suggest that water would have travelled from a recharge area ~30km from the study zone. Local rainfall and the intermediate flow have different isotopic signature. Results suggest that the willow forest is associated with the recharge area of a local flow, which plurispecific-canopy forest is related to a transit area of a semi-intermediate flow, and that tall grassland and marshy community colonize discharge areas of local and intermediate flows, respectively.Fil: Marchetti, Zuleica Yael. Centro de Investigaciones Científicas y Transferencia de Tecnología A la Producción Cicyttpconicet; ArgentinaFil: Carrillo Rivera, José Joel. Universidad Nacional Autónoma de México; MéxicoJohn Wiley & Sons Ltd2014-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/92756Marchetti, Zuleica Yael; Carrillo Rivera, José Joel; Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities; John Wiley & Sons Ltd; River Research And Applications; 30; 2-2014; 166-1791535-1459CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1002/rra.2629info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:50:52Zoai:ri.conicet.gov.ar:11336/92756instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:50:53.016CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
title |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
spellingShingle |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities Marchetti, Zuleica Yael SURFACE WATER AND GROUNDWATER INTERACTIONS FLOW SYSTEMS FLOODPLAIN ECOSYSTEMS GROUNDWATER DISCHARGE |
title_short |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
title_full |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
title_fullStr |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
title_full_unstemmed |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
title_sort |
Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities |
dc.creator.none.fl_str_mv |
Marchetti, Zuleica Yael Carrillo Rivera, José Joel |
author |
Marchetti, Zuleica Yael |
author_facet |
Marchetti, Zuleica Yael Carrillo Rivera, José Joel |
author_role |
author |
author2 |
Carrillo Rivera, José Joel |
author2_role |
author |
dc.subject.none.fl_str_mv |
SURFACE WATER AND GROUNDWATER INTERACTIONS FLOW SYSTEMS FLOODPLAIN ECOSYSTEMS GROUNDWATER DISCHARGE |
topic |
SURFACE WATER AND GROUNDWATER INTERACTIONS FLOW SYSTEMS FLOODPLAIN ECOSYSTEMS GROUNDWATER DISCHARGE |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Groundwater discharge can be an important determinant of the functioning of aquatic environments and their associated biological communities. However, the presence and the importance of groundwater have not been considered in the Parana River floodplain owing to the large quantity of surface water. The present study aimed to identify groundwater discharge conditions in a sector of the middle of the floodplain of the Parana River by studying groundwater flow systems. Eight piezometers were installed to record groundwater movement in the vertical plane weekly for 2years. Water samples were collected in piezometers, domestic wells, the river and other water bodies to study the groundwater flow systems. Rising of the water level during piezometer installation and recording suggested that the study zone represents groundwater discharge conditions. Residence time proxy allowed identification of local flows and intermediate flows. Local rainfall (in Santa Fe) showed an isotopic signature (δD and δ18O) similar to some local flows detected in the study zone, and this suggested local recharge. The chemical characteristics of an intermediate flow suggest that water would have travelled from a recharge area ~30km from the study zone. Local rainfall and the intermediate flow have different isotopic signature. Results suggest that the willow forest is associated with the recharge area of a local flow, which plurispecific-canopy forest is related to a transit area of a semi-intermediate flow, and that tall grassland and marshy community colonize discharge areas of local and intermediate flows, respectively. Fil: Marchetti, Zuleica Yael. Centro de Investigaciones Científicas y Transferencia de Tecnología A la Producción Cicyttpconicet; Argentina Fil: Carrillo Rivera, José Joel. Universidad Nacional Autónoma de México; México |
description |
Groundwater discharge can be an important determinant of the functioning of aquatic environments and their associated biological communities. However, the presence and the importance of groundwater have not been considered in the Parana River floodplain owing to the large quantity of surface water. The present study aimed to identify groundwater discharge conditions in a sector of the middle of the floodplain of the Parana River by studying groundwater flow systems. Eight piezometers were installed to record groundwater movement in the vertical plane weekly for 2years. Water samples were collected in piezometers, domestic wells, the river and other water bodies to study the groundwater flow systems. Rising of the water level during piezometer installation and recording suggested that the study zone represents groundwater discharge conditions. Residence time proxy allowed identification of local flows and intermediate flows. Local rainfall (in Santa Fe) showed an isotopic signature (δD and δ18O) similar to some local flows detected in the study zone, and this suggested local recharge. The chemical characteristics of an intermediate flow suggest that water would have travelled from a recharge area ~30km from the study zone. Local rainfall and the intermediate flow have different isotopic signature. Results suggest that the willow forest is associated with the recharge area of a local flow, which plurispecific-canopy forest is related to a transit area of a semi-intermediate flow, and that tall grassland and marshy community colonize discharge areas of local and intermediate flows, respectively. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014-02 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/92756 Marchetti, Zuleica Yael; Carrillo Rivera, José Joel; Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities; John Wiley & Sons Ltd; River Research And Applications; 30; 2-2014; 166-179 1535-1459 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/92756 |
identifier_str_mv |
Marchetti, Zuleica Yael; Carrillo Rivera, José Joel; Tracing groundwater discharge in the floodplain of the Parana River, Argentina: Implications for its biological communities; John Wiley & Sons Ltd; River Research And Applications; 30; 2-2014; 166-179 1535-1459 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1002/rra.2629 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
John Wiley & Sons Ltd |
publisher.none.fl_str_mv |
John Wiley & Sons Ltd |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1842269059588030464 |
score |
13.13397 |