Patrones de distribución temporal de algunas variables físicas y químicas en el embalse Paso Bonito, Cienfuegos, Cuba

A study is presented on the pH, redox potential (Eh), dissolved oxygen (DO), and temperature (T) in the Paso Bonito reservoir, used as a source of drinking water supply for the Cienfuegos City. This reservoir has its basin located mainly in a mountain area, affected by the organic, physical, and res...

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Detalhes bibliográficos
Autores: Betancourt, Carmen, Suárez, Roberto, Toledo, Liliana
Tipo de documento: artigo
Data de publicação:2009
País:España
Recursos:Universitat Autònoma de Barcelona
Repositório:Dipòsit Digital de Documents de la UAB
Idioma:espanhol
OAI Identifier:oai:ddd.uab.cat:40120
Acesso em linha:https://ddd.uab.cat/record/40120
Access Level:Acceso aberto
Palavra-chave:Temperatura
Ph
Potencial redox
Oxígen dissolt
Estratificació tèrmica
Oxígeno disuelto
Estratifcación térmica
Temperature
Redox potential
Dissolved oxygen
Thermal stratification
Descrição
Resumo:A study is presented on the pH, redox potential (Eh), dissolved oxygen (DO), and temperature (T) in the Paso Bonito reservoir, used as a source of drinking water supply for the Cienfuegos City. This reservoir has its basin located mainly in a mountain area, affected by the organic, physical, and residue pollution from an old pyrite mine. From September 2006 through November 2007 samples were collected at meter intervals from the surface to bottom near water withdrawal site. The reservoir was polymictic during wet summers, and monomictic during dry summers. During thermal stratification it had a clinograde oxygen distribution pattern, a pH between 7.0 and 8.1 and a negative hypolimnetic Eh during thermal stratification. We derived an empiric model relating Eh, DO and T. The correlations between the studied indicators were also determined. These results will facilitate the interpretation of highly complex phenomena such as the release of nutrients, metals, and organic matter from the sediments.