Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use

Autores
Celleri, Carla; Pratolongo, Paula Daniela; Arena, Maximiliano
Año de publicación
2021
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Soil salinization is considered an environmental threat as high salt content hinders plant growth.Soil salinity is usually associated with climate aridity at a regional scale, while topography,subsurface hydrology and land use combine with climate to produce salinization patterns atlandscape scale. In this study, the first assessment for the study area on the relationship betweenclimate, groundwater level (GWL) changes and soil salinity was provided. For comparison, twoadjacent vegetation units used as marginal grazing lands were selected: thickets of Allenrolfeapatagonica (Ap thicket), located at the base of a scarp, and bushes of Cyclolepis genistoides (Cgbush), located away from the topographic discontinuity. Electrical conductivity (ECrs) mapsderived from Landsat 8/OLI were used to analyze salinity patterns. The results showed thatGWL rose in coincidence with precipitation events and fell during dryer and warmer periods.GWL was always closer to the surface in the Ap thicket, and level changes were more likely tooccur there. ECrs showed a seasonal pattern with significantly higher (p<0.05) values in the Apthicket during summer. Within the Cg bush, relatively higher ECrs appeared around a permanentwater trough. Within this zone, ECrs values during summer were significantly higher (p<0.05).Coupled evaluation of GWL dynamics and soil salinization patterns showed that GWL changesinteract with land use practices to produce local-scale patterns of salinization. Topographyplayed an important role in controlling soil surface properties through its influence on groundwater dynamics and small topographic changes produced largely different conditions forvegetation growth.
Fil: Celleri, Carla. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Centro de Recursos Naturales Renovables de la Zona Semiárida. Universidad Nacional del Sur. Centro de Recursos Naturales Renovables de la Zona Semiárida; Argentina
Fil: Pratolongo, Paula Daniela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Centro de Recursos Naturales Renovables de la Zona Semiárida. Universidad Nacional del Sur. Centro de Recursos Naturales Renovables de la Zona Semiárida; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina
Fil: Arena, Maximiliano. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina
Materia
SOIL SALINIZATION PATTERNS
SEMI-ARID LAND
LAND USE
REMOTE SENSING
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:11336/158480

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network_acronym_str CONICETDig
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network_name_str CONICET Digital (CONICET)
spelling Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land useCelleri, CarlaPratolongo, Paula DanielaArena, MaximilianoSOIL SALINIZATION PATTERNSSEMI-ARID LANDLAND USEREMOTE SENSINGhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Soil salinization is considered an environmental threat as high salt content hinders plant growth.Soil salinity is usually associated with climate aridity at a regional scale, while topography,subsurface hydrology and land use combine with climate to produce salinization patterns atlandscape scale. In this study, the first assessment for the study area on the relationship betweenclimate, groundwater level (GWL) changes and soil salinity was provided. For comparison, twoadjacent vegetation units used as marginal grazing lands were selected: thickets of Allenrolfeapatagonica (Ap thicket), located at the base of a scarp, and bushes of Cyclolepis genistoides (Cgbush), located away from the topographic discontinuity. Electrical conductivity (ECrs) mapsderived from Landsat 8/OLI were used to analyze salinity patterns. The results showed thatGWL rose in coincidence with precipitation events and fell during dryer and warmer periods.GWL was always closer to the surface in the Ap thicket, and level changes were more likely tooccur there. ECrs showed a seasonal pattern with significantly higher (p<0.05) values in the Apthicket during summer. Within the Cg bush, relatively higher ECrs appeared around a permanentwater trough. Within this zone, ECrs values during summer were significantly higher (p<0.05).Coupled evaluation of GWL dynamics and soil salinization patterns showed that GWL changesinteract with land use practices to produce local-scale patterns of salinization. Topographyplayed an important role in controlling soil surface properties through its influence on groundwater dynamics and small topographic changes produced largely different conditions forvegetation growth.Fil: Celleri, Carla. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Centro de Recursos Naturales Renovables de la Zona Semiárida. Universidad Nacional del Sur. Centro de Recursos Naturales Renovables de la Zona Semiárida; ArgentinaFil: Pratolongo, Paula Daniela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Centro de Recursos Naturales Renovables de la Zona Semiárida. Universidad Nacional del Sur. Centro de Recursos Naturales Renovables de la Zona Semiárida; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; ArgentinaFil: Arena, Maximiliano. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; ArgentinaJohn Wiley & Sons Ltd2021-12-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/158480Celleri, Carla; Pratolongo, Paula Daniela; Arena, Maximiliano; Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use; John Wiley & Sons Ltd; Land Degradation & Development; 33; 4-12-2021; 470–4831085-3278CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1002/ldr.4162info:eu-repo/semantics/altIdentifier/doi/10.1002/ldr.4162info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:47:44Zoai:ri.conicet.gov.ar:11336/158480instacron: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 09:47:44.768CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
title Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
spellingShingle Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
Celleri, Carla
SOIL SALINIZATION PATTERNS
SEMI-ARID LAND
LAND USE
REMOTE SENSING
title_short Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
title_full Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
title_fullStr Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
title_full_unstemmed Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
title_sort Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use
dc.creator.none.fl_str_mv Celleri, Carla
Pratolongo, Paula Daniela
Arena, Maximiliano
author Celleri, Carla
author_facet Celleri, Carla
Pratolongo, Paula Daniela
Arena, Maximiliano
author_role author
author2 Pratolongo, Paula Daniela
Arena, Maximiliano
author2_role author
author
dc.subject.none.fl_str_mv SOIL SALINIZATION PATTERNS
SEMI-ARID LAND
LAND USE
REMOTE SENSING
topic SOIL SALINIZATION PATTERNS
SEMI-ARID LAND
LAND USE
REMOTE SENSING
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Soil salinization is considered an environmental threat as high salt content hinders plant growth.Soil salinity is usually associated with climate aridity at a regional scale, while topography,subsurface hydrology and land use combine with climate to produce salinization patterns atlandscape scale. In this study, the first assessment for the study area on the relationship betweenclimate, groundwater level (GWL) changes and soil salinity was provided. For comparison, twoadjacent vegetation units used as marginal grazing lands were selected: thickets of Allenrolfeapatagonica (Ap thicket), located at the base of a scarp, and bushes of Cyclolepis genistoides (Cgbush), located away from the topographic discontinuity. Electrical conductivity (ECrs) mapsderived from Landsat 8/OLI were used to analyze salinity patterns. The results showed thatGWL rose in coincidence with precipitation events and fell during dryer and warmer periods.GWL was always closer to the surface in the Ap thicket, and level changes were more likely tooccur there. ECrs showed a seasonal pattern with significantly higher (p<0.05) values in the Apthicket during summer. Within the Cg bush, relatively higher ECrs appeared around a permanentwater trough. Within this zone, ECrs values during summer were significantly higher (p<0.05).Coupled evaluation of GWL dynamics and soil salinization patterns showed that GWL changesinteract with land use practices to produce local-scale patterns of salinization. Topographyplayed an important role in controlling soil surface properties through its influence on groundwater dynamics and small topographic changes produced largely different conditions forvegetation growth.
Fil: Celleri, Carla. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Centro de Recursos Naturales Renovables de la Zona Semiárida. Universidad Nacional del Sur. Centro de Recursos Naturales Renovables de la Zona Semiárida; Argentina
Fil: Pratolongo, Paula Daniela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Centro de Recursos Naturales Renovables de la Zona Semiárida. Universidad Nacional del Sur. Centro de Recursos Naturales Renovables de la Zona Semiárida; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina
Fil: Arena, Maximiliano. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina
description Soil salinization is considered an environmental threat as high salt content hinders plant growth.Soil salinity is usually associated with climate aridity at a regional scale, while topography,subsurface hydrology and land use combine with climate to produce salinization patterns atlandscape scale. In this study, the first assessment for the study area on the relationship betweenclimate, groundwater level (GWL) changes and soil salinity was provided. For comparison, twoadjacent vegetation units used as marginal grazing lands were selected: thickets of Allenrolfeapatagonica (Ap thicket), located at the base of a scarp, and bushes of Cyclolepis genistoides (Cgbush), located away from the topographic discontinuity. Electrical conductivity (ECrs) mapsderived from Landsat 8/OLI were used to analyze salinity patterns. The results showed thatGWL rose in coincidence with precipitation events and fell during dryer and warmer periods.GWL was always closer to the surface in the Ap thicket, and level changes were more likely tooccur there. ECrs showed a seasonal pattern with significantly higher (p<0.05) values in the Apthicket during summer. Within the Cg bush, relatively higher ECrs appeared around a permanentwater trough. Within this zone, ECrs values during summer were significantly higher (p<0.05).Coupled evaluation of GWL dynamics and soil salinization patterns showed that GWL changesinteract with land use practices to produce local-scale patterns of salinization. Topographyplayed an important role in controlling soil surface properties through its influence on groundwater dynamics and small topographic changes produced largely different conditions forvegetation growth.
publishDate 2021
dc.date.none.fl_str_mv 2021-12-04
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/11336/158480
Celleri, Carla; Pratolongo, Paula Daniela; Arena, Maximiliano; Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use; John Wiley & Sons Ltd; Land Degradation & Development; 33; 4-12-2021; 470–483
1085-3278
CONICET Digital
CONICET
url http://hdl.handle.net/11336/158480
identifier_str_mv Celleri, Carla; Pratolongo, Paula Daniela; Arena, Maximiliano; Spatial and temporal patterns of soil salinization in shallow groundwater environments of the Bahía Blanca Estuary: Influence of topography and land use; John Wiley & Sons Ltd; Land Degradation & Development; 33; 4-12-2021; 470–483
1085-3278
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1002/ldr.4162
info:eu-repo/semantics/altIdentifier/doi/10.1002/ldr.4162
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
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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