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dc.contributor.author
Bécher Quinodóz, Fátima Noelia  
dc.contributor.author
Blarasin, Mónica Teresa  
dc.contributor.author
Cabrera, Adriana Edith  
dc.contributor.author
Eric, Carlos  
dc.contributor.author
Felizzia, Juan Alcides  
dc.date.available
2022-12-02T19:46:51Z  
dc.date.issued
2016-05  
dc.identifier.citation
Bécher Quinodóz, Fátima Noelia; Blarasin, Mónica Teresa; Cabrera, Adriana Edith; Eric, Carlos; Felizzia, Juan Alcides; Groundwater dynamics and recharge assessment in an unconfined aeolian sand aquifer; Nextgen Research Publication; International Journal of New Technology and Research; 2; 5; 5-2016; 144-149  
dc.identifier.issn
2454-4116  
dc.identifier.uri
http://hdl.handle.net/11336/180067  
dc.description.abstract
In the sandy plain of the South of Córdoba province, Argentina) the unconfined aquifer is used mainly for agricultural activities. The objective of this work is to show the estimation of the recharge (R) rate in the unconfined aquifer, using the water table fluctuation method (WTF). Furthermore, considerations in relation to monthly recharge and discharge (D) rhythms were performed. The studied unconfined aquifer consists mainly of sandy aeolian sediments with values of hydraulic conductivity in the order of 1.5 m/d. The water table is slightly undulating and hydraulic gradients and flow velocities are low, controlled by lithology and the regional plain topography. The relationship between groundwater and surface water bodies is variable, but in general, the aquifer provides water to the river and to the lagoons. The parabolic dunes of this sandy plain environment show a typical behavior of preferential recharge areas. That is, an important and quick answer of water table to the arrival of precipitations and then the discharge to the base level, the neighboring lagoon in the parabolic dune. Using monthly estimation, an annual average recharge value of 12% of total precipitation was obtained. When the relationship between P and R was analyzed, the 91 % of recharge episodes were clearly dependent on the rainfall behavior. Winter shows very low recharge but a great effectiveness because the recharge arrives to the aquifer from delayed wetting fronts, although almost there were not rainfalls. Nevertheless, the major amount of recharge has occurred in the end of spring, summer, and early autumn. The ratio R/D for the whole series was positive which means that the aquifer recharge predominated, a fact that is coherent with the higher position of the water table at the end of the studied series. These results assure the existence of annual water replacement to the aquifer, a very important feature for a region that depends on groundwater resources.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Nextgen Research Publication  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
UNCONFINED AEOLIAN AQUIFER  
dc.subject
RECHARGE  
dc.subject
WATER TABLE FLUCTUATION  
dc.subject
DYNAMICS  
dc.subject.classification
Oceanografía, Hidrología, Recursos Hídricos  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
Groundwater dynamics and recharge assessment in an unconfined aeolian sand aquifer  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2022-11-30T22:36:08Z  
dc.journal.volume
2  
dc.journal.number
5  
dc.journal.pagination
144-149  
dc.journal.pais
India  
dc.journal.ciudad
Jaipur  
dc.description.fil
Fil: Bécher Quinodóz, Fátima Noelia. 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, Mónica Teresa. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
dc.description.fil
Fil: Cabrera, Adriana Edith. Universidad Nacional de Rio Cuarto. Facultad de Cs.exactas Fisicoquimicas y Naturales. Departamento de Geologia. Cat.de Hidrogeologia; Argentina  
dc.description.fil
Fil: Eric, Carlos. Universidad Nacional de Río Cuarto. Facultad de Ciencias Exactas, Fisicoquímicas y Naturales. Departamento de Geología; Argentina  
dc.description.fil
Fil: Felizzia, Juan Alcides. Universidad Nacional de Río Cuarto. Facultad de Ciencias Exactas, Fisicoquímicas y Naturales. Departamento de Geología; Argentina  
dc.journal.title
International Journal of New Technology and Research  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.ijntr.org/groundwater-dynamics-and-recharge-assessment-in-an-unconfined-aeolian-sand-aquifer