Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina

Autores
Alvarez, Maria del Pilar; Carol, Eleonora Silvina; Hernández, Mario A.; Bouza, Pablo Jose
Año de publicación
2015
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The processes regulating the relationship between tidal fl ows and shallow groundwater dynamics, temperature and salinity in a coastal wetland in an arid climate are analysed in a detailed fi eld study carried out in the marsh located at Playa Fracasso (Argentina). The continuous records of groundwater level, temperature and electrical conductivity from a transect perpendicular to the coastline were studied during a period ranging from summer to winter, together with the information obtained in hydro- geomorphological fi eld surveys and soil pro fi les. An assessment of the processes conditioning marsh hydrology was carried out contemplating seasonal (summer e winter) and periodical variations caused by tidal fl ows. The study showed that the dynamics of groundwater in relation to tidal fl ows depends almost exclusively on the in fi ltration of tidal water when the marsh is fl ooded during spring tides (syzygy), with an increase in the groundwater discharge level at the onset of syzygy. The differences in temperature between sea and continental water were very useful in de fi ning the origin of the different contributions. Groundwater salinity is mainly associated with the leaching of the soil salts that enter with the sea water in fi ltrating during fl ood events. The presence of saline soils in the marsh is regulated by the evapo- transpiration predominating in arid zones. The conceptual hydrological model suggested may help in the understanding of the hydrological processes in other similar marshes of Patagonia, as well as in coastal wetlands of arid zones worldwide.
Fil: Alvarez, Maria del Pilar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico; Argentina
Fil: Carol, Eleonora Silvina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Hernández, Mario A.. Universidad Nacional de La Plata; Argentina
Fil: Bouza, Pablo Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico para el Estudio de los Ecosistemas Continentales; Argentina
Materia
Hydrodinamics
Salt Marsh
Playa Fracasso
Patagonia
Arid Climate
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/29454

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network_name_str CONICET Digital (CONICET)
spelling Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, ArgentinaAlvarez, Maria del PilarCarol, Eleonora SilvinaHernández, Mario A.Bouza, Pablo JoseHydrodinamicsSalt MarshPlaya FracassoPatagoniaArid Climatehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The processes regulating the relationship between tidal fl ows and shallow groundwater dynamics, temperature and salinity in a coastal wetland in an arid climate are analysed in a detailed fi eld study carried out in the marsh located at Playa Fracasso (Argentina). The continuous records of groundwater level, temperature and electrical conductivity from a transect perpendicular to the coastline were studied during a period ranging from summer to winter, together with the information obtained in hydro- geomorphological fi eld surveys and soil pro fi les. An assessment of the processes conditioning marsh hydrology was carried out contemplating seasonal (summer e winter) and periodical variations caused by tidal fl ows. The study showed that the dynamics of groundwater in relation to tidal fl ows depends almost exclusively on the in fi ltration of tidal water when the marsh is fl ooded during spring tides (syzygy), with an increase in the groundwater discharge level at the onset of syzygy. The differences in temperature between sea and continental water were very useful in de fi ning the origin of the different contributions. Groundwater salinity is mainly associated with the leaching of the soil salts that enter with the sea water in fi ltrating during fl ood events. The presence of saline soils in the marsh is regulated by the evapo- transpiration predominating in arid zones. The conceptual hydrological model suggested may help in the understanding of the hydrological processes in other similar marshes of Patagonia, as well as in coastal wetlands of arid zones worldwide.Fil: Alvarez, Maria del Pilar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico; ArgentinaFil: Carol, Eleonora Silvina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Hernández, Mario A.. Universidad Nacional de La Plata; ArgentinaFil: Bouza, Pablo Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico para el Estudio de los Ecosistemas Continentales; ArgentinaPergamon-Elsevier Science Ltd2015-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/29454Alvarez, Maria del Pilar; Carol, Eleonora Silvina; Hernández, Mario A.; Bouza, Pablo Jose; Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 62; 5-2015; 1-110895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/J.JSAMES.2015.04.006info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0895981115000656info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:01:09Zoai:ri.conicet.gov.ar:11336/29454instacron: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:34982025-09-29 10:01:09.865CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
title Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
spellingShingle Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
Alvarez, Maria del Pilar
Hydrodinamics
Salt Marsh
Playa Fracasso
Patagonia
Arid Climate
title_short Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
title_full Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
title_fullStr Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
title_full_unstemmed Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
title_sort Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina
dc.creator.none.fl_str_mv Alvarez, Maria del Pilar
Carol, Eleonora Silvina
Hernández, Mario A.
Bouza, Pablo Jose
author Alvarez, Maria del Pilar
author_facet Alvarez, Maria del Pilar
Carol, Eleonora Silvina
Hernández, Mario A.
Bouza, Pablo Jose
author_role author
author2 Carol, Eleonora Silvina
Hernández, Mario A.
Bouza, Pablo Jose
author2_role author
author
author
dc.subject.none.fl_str_mv Hydrodinamics
Salt Marsh
Playa Fracasso
Patagonia
Arid Climate
topic Hydrodinamics
Salt Marsh
Playa Fracasso
Patagonia
Arid Climate
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The processes regulating the relationship between tidal fl ows and shallow groundwater dynamics, temperature and salinity in a coastal wetland in an arid climate are analysed in a detailed fi eld study carried out in the marsh located at Playa Fracasso (Argentina). The continuous records of groundwater level, temperature and electrical conductivity from a transect perpendicular to the coastline were studied during a period ranging from summer to winter, together with the information obtained in hydro- geomorphological fi eld surveys and soil pro fi les. An assessment of the processes conditioning marsh hydrology was carried out contemplating seasonal (summer e winter) and periodical variations caused by tidal fl ows. The study showed that the dynamics of groundwater in relation to tidal fl ows depends almost exclusively on the in fi ltration of tidal water when the marsh is fl ooded during spring tides (syzygy), with an increase in the groundwater discharge level at the onset of syzygy. The differences in temperature between sea and continental water were very useful in de fi ning the origin of the different contributions. Groundwater salinity is mainly associated with the leaching of the soil salts that enter with the sea water in fi ltrating during fl ood events. The presence of saline soils in the marsh is regulated by the evapo- transpiration predominating in arid zones. The conceptual hydrological model suggested may help in the understanding of the hydrological processes in other similar marshes of Patagonia, as well as in coastal wetlands of arid zones worldwide.
Fil: Alvarez, Maria del Pilar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico; Argentina
Fil: Carol, Eleonora Silvina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Hernández, Mario A.. Universidad Nacional de La Plata; Argentina
Fil: Bouza, Pablo Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico para el Estudio de los Ecosistemas Continentales; Argentina
description The processes regulating the relationship between tidal fl ows and shallow groundwater dynamics, temperature and salinity in a coastal wetland in an arid climate are analysed in a detailed fi eld study carried out in the marsh located at Playa Fracasso (Argentina). The continuous records of groundwater level, temperature and electrical conductivity from a transect perpendicular to the coastline were studied during a period ranging from summer to winter, together with the information obtained in hydro- geomorphological fi eld surveys and soil pro fi les. An assessment of the processes conditioning marsh hydrology was carried out contemplating seasonal (summer e winter) and periodical variations caused by tidal fl ows. The study showed that the dynamics of groundwater in relation to tidal fl ows depends almost exclusively on the in fi ltration of tidal water when the marsh is fl ooded during spring tides (syzygy), with an increase in the groundwater discharge level at the onset of syzygy. The differences in temperature between sea and continental water were very useful in de fi ning the origin of the different contributions. Groundwater salinity is mainly associated with the leaching of the soil salts that enter with the sea water in fi ltrating during fl ood events. The presence of saline soils in the marsh is regulated by the evapo- transpiration predominating in arid zones. The conceptual hydrological model suggested may help in the understanding of the hydrological processes in other similar marshes of Patagonia, as well as in coastal wetlands of arid zones worldwide.
publishDate 2015
dc.date.none.fl_str_mv 2015-05
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/11336/29454
Alvarez, Maria del Pilar; Carol, Eleonora Silvina; Hernández, Mario A.; Bouza, Pablo Jose; Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 62; 5-2015; 1-11
0895-9811
CONICET Digital
CONICET
url http://hdl.handle.net/11336/29454
identifier_str_mv Alvarez, Maria del Pilar; Carol, Eleonora Silvina; Hernández, Mario A.; Bouza, Pablo Jose; Groundwater dynamic, temperature and salinity response to the tide in Patagonian marshes: Observations on a coastal wetland in San José Gulf, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 62; 5-2015; 1-11
0895-9811
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/J.JSAMES.2015.04.006
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0895981115000656
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
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science 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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