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Impact of climate on the vertical water column structure of Lajes Reservoir (Brazil): A tropical reservoir case
Author(s) -
Branco Christina W.C.,
KozlowskySuzuki Betina,
SousaFilho Izidro F.,
Guarino Alcides W.S.,
Rocha Rinaldo J.
Publication year - 2009
Publication title -
lakes and reservoirs: research and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.296
H-Index - 39
eISSN - 1440-1770
pISSN - 1320-5331
DOI - 10.1111/j.1440-1770.2009.00403.x
Subject(s) - water column , hypolimnion , stratification (seeds) , environmental science , thermal stratification , water quality , hydrology (agriculture) , tributary , thermocline , bottom water , anoxic waters , geology , oceanography , nutrient , geography , eutrophication , ecology , seed dormancy , botany , germination , geotechnical engineering , cartography , dormancy , biology
Ribeirão das Lajes Reservoir was constructed in 1905 for energy production, and is now used as a domestic water supply for about 1 million people. The reservoir was considered as being general monomictic, exhibiting water column mixing in the winter. Water column mixing, however, did not occur in the deepest parts of the reservoir in the warm year of 2005. Nevertheless, the long stratification period leads to an anoxic, nutrient‐rich hypolimnion that exhibits poor water quality in the deepest part. The meteorological events of cold front passages in the reservoir region were not able to disrupt the water column stability, or affect its water quality for domestic supply. Maintenance of thermal stratification over most of the year was likely because of the low influence of wind, long water retention time, and the input of cold water from the tributary and from rain directly draining into the metalimnion.