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dc.contributor.author
Giacobone, Daniela Beatriz  
dc.contributor.author
Lutri, Veronica Florencia  
dc.contributor.author
Blarasin, M.  
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Matteoda, E.  
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Cabrera, A. E.  
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Bécher Quinodóz, Fátima Noelia  
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Schroeter, G.  
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Pramparo, Santiago Javier  
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Pascuini, Miguel Angel  
dc.date.available
2024-01-08T11:32:24Z  
dc.date.issued
2023-08  
dc.identifier.citation
Giacobone, Daniela Beatriz; Lutri, Veronica Florencia; Blarasin, M.; Matteoda, E.; Cabrera, A. E.; et al.; Hydrodynamic and hydrogeochemical evaluation of groundwater and linkage with herbicide pollution: Central Argentina; Springer; Sustainable Water Resources Management; 9; 5; 8-2023; 1-16  
dc.identifier.issn
2363-5037  
dc.identifier.uri
http://hdl.handle.net/11336/222702  
dc.description.abstract
Surface water and unconfined and semiconfined (SAC B) aquifers of Marcos Juárez plain, in the central Pampa of Argentina, were studied to assess hydrogeological features and the presence and distribution of herbicides in water. The studied area, located near a regional hydrological discharge area shows streams and channels of high salinity fed by the groundwater with low values of herbicides as a consequence of hydrodynamic dispersion. The unconfined and semiconfined aquifers (SAC B) are impacted by the presence of herbicides although the percentage of positive samples is low. The unconfined aquifer, directly connected to the atmospheric phase, has a shallow water table being more likely to be reached by effective water infiltration. Despite their high Koc and low GUS index, glyphosate and AMPA were present in the highest concentrations in the unconfined aquifer. It is assumed that this situation is the result of its widespread use, its high solubility in water, and its high persistence. The chemical characteristics of metolachlor and imazethapyr, such as their relatively low Koc, moderate and high GUS index, and high persistence have allowed also their leaching into groundwater. Herbicide migration from the unconfined aquifer to the semiconfined aquifer layer in the loessical plain can occur due to the differences in their hydraulic potential. This situation facilitates the mixing of water, a process that is interpreted through fractures or cracks in the confining units (aquitards) or due to the presence of broken old pipes. The multivariate statistical analysis of the unconfined groundwater chemistry leads us to the conclusion that approximately 53% of the variance is explained by different levels of salinization resulting from natural geochemical processes (such as cation exchange, dissolution of salts, etc.), while the remaining 47% is attributed to contamination processes (arrival of herbicides and nitrates). The second and third positions of herbicides in the PCA analysis demonstrate the impact of agricultural activity, especially in the unconfined aquifer.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Springer  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
AGRICULTURE  
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AMPA  
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GLYPHOSATE  
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GROUNDWATER QUALITY  
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IMAZETHAPYR  
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METOLACHLOR  
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Otras Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
Hydrodynamic and hydrogeochemical evaluation of groundwater and linkage with herbicide pollution: Central Argentina  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2024-01-03T12:25:10Z  
dc.journal.volume
9  
dc.journal.number
5  
dc.journal.pagination
1-16  
dc.journal.pais
Reino Unido  
dc.description.fil
Fil: Giacobone, Daniela Beatriz. Universidad Nacional de Río Cuarto; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina  
dc.description.fil
Fil: Lutri, Veronica Florencia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
dc.description.fil
Fil: Blarasin, M.. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
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Fil: Matteoda, E.. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
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Fil: Cabrera, A. E.. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
dc.description.fil
Fil: Bécher Quinodóz, Fátima Noelia. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina  
dc.description.fil
Fil: Schroeter, G.. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
dc.description.fil
Fil: Pramparo, Santiago Javier. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina  
dc.description.fil
Fil: Pascuini, Miguel Angel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
dc.journal.title
Sustainable Water Resources Management  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/10.1007/s40899-023-00930-2  
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info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s40899-023-00930-2