Contribution to the limnological knowledge of the Bermejo river in its lower course

The main limnological features of the Bermejo river have been recorded at Puerto Velaz, 30 kilometers upstream the river mouth.The most stricking feature of the Bermejo river is an extremely high rate of suspended solid. The low water transparency limited the phytoplankton growth. Therefore phytopla...

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Autores principales: Bonetto, Argentino A., Zalocar, Yolanda, Pedrozo, Fernando L., Bonetto, Carlos
Formato: Artículo revista
Lenguaje:Español
Publicado: Centro de Ecología Aplicada del Litoral (Consejo Nacional de Investigaciones Científicas y Técnicas - Universidad Nacional de Nordeste) 2024
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Acceso en línea:https://revistas.unne.edu.ar/index.php/eco/article/view/7358
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spelling I48-R154-article-73582024-02-16T12:40:27Z Contribution to the limnological knowledge of the Bermejo river in its lower course Contribución al conocimiento limnológico del Río Bermejo en su tramo inferior Bonetto, Argentino A. Zalocar, Yolanda Pedrozo, Fernando L. Bonetto, Carlos Conocimiento limnológico Río Bermejo Puerto Velaz The main limnological features of the Bermejo river have been recorded at Puerto Velaz, 30 kilometers upstream the river mouth.The most stricking feature of the Bermejo river is an extremely high rate of suspended solid. The low water transparency limited the phytoplankton growth. Therefore phytoplankton density and primary production were undetectable during the flood period, reaching a máximum of 170 ind/ml and 30 mgC/m2/d respectively during the low water period. Diatoms (Melosira) and Chlorophytes (Scenedesmus) were dominant.The suspended solid concentration reached a máximum of 9,500 mg/1 in the summer flood, during the studied period. The dissolved oxygen was always near saturation. Chemical oxygen demand and water transparency were very low. Conductivity ranged from 850 uS/cm to 310 /uS/cm. Centro de Ecología Aplicada del Litoral (Consejo Nacional de Investigaciones Científicas y Técnicas - Universidad Nacional de Nordeste) 2024-02-15 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículo revisado por pares application/pdf https://revistas.unne.edu.ar/index.php/eco/article/view/7358 10.30972/eco.11217358 Ecosur; 1984: vol. 11, nos. 21-22; 61-74 0325-108X spa https://revistas.unne.edu.ar/index.php/eco/article/view/7358/6791
institution Universidad Nacional del Nordeste
institution_str I-48
repository_str R-154
container_title_str Revistas UNNE - Universidad Nacional del Noroeste (UNNE)
language Español
format Artículo revista
topic Conocimiento limnológico
Río Bermejo
Puerto Velaz
spellingShingle Conocimiento limnológico
Río Bermejo
Puerto Velaz
Bonetto, Argentino A.
Zalocar, Yolanda
Pedrozo, Fernando L.
Bonetto, Carlos
Contribution to the limnological knowledge of the Bermejo river in its lower course
topic_facet Conocimiento limnológico
Río Bermejo
Puerto Velaz
author Bonetto, Argentino A.
Zalocar, Yolanda
Pedrozo, Fernando L.
Bonetto, Carlos
author_facet Bonetto, Argentino A.
Zalocar, Yolanda
Pedrozo, Fernando L.
Bonetto, Carlos
author_sort Bonetto, Argentino A.
title Contribution to the limnological knowledge of the Bermejo river in its lower course
title_short Contribution to the limnological knowledge of the Bermejo river in its lower course
title_full Contribution to the limnological knowledge of the Bermejo river in its lower course
title_fullStr Contribution to the limnological knowledge of the Bermejo river in its lower course
title_full_unstemmed Contribution to the limnological knowledge of the Bermejo river in its lower course
title_sort contribution to the limnological knowledge of the bermejo river in its lower course
description The main limnological features of the Bermejo river have been recorded at Puerto Velaz, 30 kilometers upstream the river mouth.The most stricking feature of the Bermejo river is an extremely high rate of suspended solid. The low water transparency limited the phytoplankton growth. Therefore phytoplankton density and primary production were undetectable during the flood period, reaching a máximum of 170 ind/ml and 30 mgC/m2/d respectively during the low water period. Diatoms (Melosira) and Chlorophytes (Scenedesmus) were dominant.The suspended solid concentration reached a máximum of 9,500 mg/1 in the summer flood, during the studied period. The dissolved oxygen was always near saturation. Chemical oxygen demand and water transparency were very low. Conductivity ranged from 850 uS/cm to 310 /uS/cm.
publisher Centro de Ecología Aplicada del Litoral (Consejo Nacional de Investigaciones Científicas y Técnicas - Universidad Nacional de Nordeste)
publishDate 2024
url https://revistas.unne.edu.ar/index.php/eco/article/view/7358
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