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
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/68885
Ver los metadatos del registro completo
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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 |
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http://sedici.unlp.edu.ar/handle/10915/68885 |
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