Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”

Autores
Bustingorry, José Fernando; Escaray, Roberto Ulises; Conzonno, Víctor H.
Año de publicación
2012
Idioma
español castellano
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Chascomús pond was affected between June-2001 and September-2002 by two periods of flood events (more than 8 m IGM reference) that had two maximum peaks of nearly 9 m. Such events were studied weekly in surface samples taken in three stations: centre and the zones with influence of the tributaries Vitel (affluent) and Arroyo Girado (effluent). The supply of water promoted a dilution that made the salinity to decrease to one third of the mean value of 1,570 mg/l obtained during 1999-2000. In March-2002 it was registered the maximum value of precipitation (538 mm) that caused the beginning of the second flood period. On March 18 differences were detected between the centre with the other two stations of parameters like salinity (222.5 with respect to 324.9 and 304.1 mg/l), specific conductivity (0.38; 0.55 and 0.56 mS/cm), pH (7.71; 7.94 and 8.00) and agar plate count (31,200; 7,260 and 6,600 UCF/ml). These differences were not detected in the next sampling. The phenomena is tried to explain on the basis of the runoff (physical hypothesis) and by the influence of the groundwater (chemical hypothesis). Because of the occasional separation into different quality of waters such phenomena was called “Moises effect”.
Instituto de Limnología "Raúl A. Ringuelet"
Materia
Ciencias Naturales
Calidad del Agua
Chascomús (Buenos Aires, Argentina)
Inundaciones
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-nd/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/68885

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spelling Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”Bustingorry, José FernandoEscaray, Roberto UlisesConzonno, Víctor H.Ciencias NaturalesCalidad del AguaChascomús (Buenos Aires, Argentina)InundacionesChascomús pond was affected between June-2001 and September-2002 by two periods of flood events (more than 8 m IGM reference) that had two maximum peaks of nearly 9 m. Such events were studied weekly in surface samples taken in three stations: centre and the zones with influence of the tributaries Vitel (affluent) and Arroyo Girado (effluent). The supply of water promoted a dilution that made the salinity to decrease to one third of the mean value of 1,570 mg/l obtained during 1999-2000. In March-2002 it was registered the maximum value of precipitation (538 mm) that caused the beginning of the second flood period. On March 18 differences were detected between the centre with the other two stations of parameters like salinity (222.5 with respect to 324.9 and 304.1 mg/l), specific conductivity (0.38; 0.55 and 0.56 mS/cm), pH (7.71; 7.94 and 8.00) and agar plate count (31,200; 7,260 and 6,600 UCF/ml). These differences were not detected in the next sampling. The phenomena is tried to explain on the basis of the runoff (physical hypothesis) and by the influence of the groundwater (chemical hypothesis). Because of the occasional separation into different quality of waters such phenomena was called “Moises effect”.Instituto de Limnología "Raúl A. Ringuelet"2012info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf61-70http://sedici.unlp.edu.ar/handle/10915/68885spainfo:eu-repo/semantics/altIdentifier/issn/0326-1638info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-nd/4.0/Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-03T10:42:48Zoai:sedici.unlp.edu.ar:10915/68885Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-03 10:42:48.834SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
title Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
spellingShingle Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
Bustingorry, José Fernando
Ciencias Naturales
Calidad del Agua
Chascomús (Buenos Aires, Argentina)
Inundaciones
title_short Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
title_full Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
title_fullStr Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
title_full_unstemmed Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
title_sort Cambio puntual de la calidad de agua en la laguna Chascomús durante la inundación 2001-2002: “efecto Moisés”
dc.creator.none.fl_str_mv Bustingorry, José Fernando
Escaray, Roberto Ulises
Conzonno, Víctor H.
author Bustingorry, José Fernando
author_facet Bustingorry, José Fernando
Escaray, Roberto Ulises
Conzonno, Víctor H.
author_role author
author2 Escaray, Roberto Ulises
Conzonno, Víctor H.
author2_role author
author
dc.subject.none.fl_str_mv Ciencias Naturales
Calidad del Agua
Chascomús (Buenos Aires, Argentina)
Inundaciones
topic Ciencias Naturales
Calidad del Agua
Chascomús (Buenos Aires, Argentina)
Inundaciones
dc.description.none.fl_txt_mv Chascomús pond was affected between June-2001 and September-2002 by two periods of flood events (more than 8 m IGM reference) that had two maximum peaks of nearly 9 m. Such events were studied weekly in surface samples taken in three stations: centre and the zones with influence of the tributaries Vitel (affluent) and Arroyo Girado (effluent). The supply of water promoted a dilution that made the salinity to decrease to one third of the mean value of 1,570 mg/l obtained during 1999-2000. In March-2002 it was registered the maximum value of precipitation (538 mm) that caused the beginning of the second flood period. On March 18 differences were detected between the centre with the other two stations of parameters like salinity (222.5 with respect to 324.9 and 304.1 mg/l), specific conductivity (0.38; 0.55 and 0.56 mS/cm), pH (7.71; 7.94 and 8.00) and agar plate count (31,200; 7,260 and 6,600 UCF/ml). These differences were not detected in the next sampling. The phenomena is tried to explain on the basis of the runoff (physical hypothesis) and by the influence of the groundwater (chemical hypothesis). Because of the occasional separation into different quality of waters such phenomena was called “Moises effect”.
Instituto de Limnología "Raúl A. Ringuelet"
description Chascomús pond was affected between June-2001 and September-2002 by two periods of flood events (more than 8 m IGM reference) that had two maximum peaks of nearly 9 m. Such events were studied weekly in surface samples taken in three stations: centre and the zones with influence of the tributaries Vitel (affluent) and Arroyo Girado (effluent). The supply of water promoted a dilution that made the salinity to decrease to one third of the mean value of 1,570 mg/l obtained during 1999-2000. In March-2002 it was registered the maximum value of precipitation (538 mm) that caused the beginning of the second flood period. On March 18 differences were detected between the centre with the other two stations of parameters like salinity (222.5 with respect to 324.9 and 304.1 mg/l), specific conductivity (0.38; 0.55 and 0.56 mS/cm), pH (7.71; 7.94 and 8.00) and agar plate count (31,200; 7,260 and 6,600 UCF/ml). These differences were not detected in the next sampling. The phenomena is tried to explain on the basis of the runoff (physical hypothesis) and by the influence of the groundwater (chemical hypothesis). Because of the occasional separation into different quality of waters such phenomena was called “Moises effect”.
publishDate 2012
dc.date.none.fl_str_mv 2012
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
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Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
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rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-nd/4.0/
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
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