@Article{AlmeidaHRABBGHJLPCRSR:2019:LiEfLa,
author = "Almeida, Rafael M. and Hamilton, Stephen K. and Rosi, Emma J. and
Arantes J{\'u}nior, Jo{\~a}o Durval and Barros, Nathan and
Boemer, Gina and Gripp, Anderson and Huszar, Vera L. M. and
Junger, Pedro C. and Lima, Michele and Pacheco, Felipe Siqueira
and Carvalho, Dario and Reisinger, Alexander and Silva, L{\'u}cia
H. S. and Roland, F{\'a}bio",
affiliation = "{Universidade Federal de Juiz de Fora (UFJF)} and {Cary Institute
of Ecosystem Studies} and {Cary Institute of Ecosystem Studies}
and {Ecology and Environment do Brasil Ltda} and {Universidade
Federal de Juiz de Fora (UFJF)} and {Ecology and Environment do
Brasil Ltda} and {Universidade Federal do Rio de Janeiro (UFRJ)}
and {Universidade Federal do Rio de Janeiro (UFRJ)} and
{Universidade Federal de S{\~a}o Carlos (UFSCar)} and {Ecology
and Environment do Brasil Ltda} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Santo Ant{\^o}nio Energia} and
{University of Florida} and {Universidade Federal do Rio de
Janeiro (UFRJ)} and {Universidade Federal de Juiz de Fora
(UFJF)}",
title = "Limnological efects of a large Amazonian run-of-river dam on the
main river and drowned tributary valleys",
journal = "Scientific Reports",
year = "2019",
volume = "9",
number = "1",
pages = "e16846",
month = "Dec.",
abstract = "Run-of-river dams are often considered to have lower environmental
impacts than storage dams due to their smaller reservoirs and low
potential for fow alteration. However, this has been questioned
for projects recently built on large rivers around the world. Two
of the worlds largest run-of-river damsSanto Ant{\^o}nio and
Jirauwere recently constructed on the Madeira River, a major
tributary to the Amazon River in Brazil. Here we evaluate the
efects of the creation of the Santo Ant{\^o}nio dam on the water
chemistry and thermal structure of the Madeira River mainstem and
back-fooded valleys of tributaries within the reservoir inundated
area. In contrast to the mainstem river, some back-fooded
tributaries periodically developed thermal stratifcation, which is
associated with higher water residence times. Additionally,
biochemical oxygen demand, partial pressure of CO2, and organic
carbon all increased in the tributary valleys inundated by the
reservoir, possibly due to increased input of allochthonous
organic matter and its subsequent mineralization upon
back-foodinga common feature of newly fooded impoundments. The
mainstem did not show detectable dam-related changes in water
chemistry and thermal structure. Although the majority of the
reservoir area maintained riverine conditions, the lateral valleys
formed upon back-foodingcorresponding to ~30% of the Santo
Ant{\^o}nio reservoir areadeveloped lake-like conditions akin to
a typical reservoir of a storage dam.",
doi = "10.1038/s41598-019-53060-1",
url = "http://dx.doi.org/10.1038/s41598-019-53060-1",
issn = "2045-2322",
language = "en",
targetfile = "almeida_limnological.pdf",
urlaccessdate = "28 abr. 2024"
}