@Article{PachecoSACRASAO:2014:RiInRe,
author = "Pacheco, Felipe Siqueira and Soares, M. C. S. and Assireu, Arcilan
Trevenzoli and Curtarelli, Marcelo Pedroso and Roland, F. and
Abril, G. and Stech, Jos{\'e} Luiz and Alval{\'a}, Plinio Carlos
and Ometto, Jean Pierre Henry Balbaud",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {} and {} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "River inflow and retention time affecting spatial heterogeneity of
chlorophyll and water-air CO2 fluxes in a tropical hydropower
reservoir",
journal = "Biogeosciences Discussions",
year = "2014",
volume = "11",
number = "6",
pages = "8531--8568",
keywords = "tropical reservoirs, river inflow, retention time, carbon dioxide
flux.",
abstract = "Much research has been devoted to understanding the complexity of
biogeochemical and physical processes responsible for the
greenhouse gas (GHG) emissions from hydropower reservoirs. Spatial
complexity and heterogeneity of GHG emission may be observed in
these systems because it is dependent on flooded biomass, river
inflow, primary production and dam operation. In this study, we
investigate the relationships between waterair CO2 fluxes and
phytoplanktonic biomass in Funil Reservoir, an old and stratified
tropical reservoir, where intense phytoplankton blooms and low
partial pressure of CO2 (pCO2) are observed. Our results showed
that Funil Reservoir sea sonal and spatial variability of
chlorophyll concentration (Chl) and pCO2 is more related to
changes in river inflow over the year than environmental factor
such as air temperature and solar radiation. Field data and
hydrodynamic simulations reveal that the river inflow contributes
to increased heterogeneity in dry season due to the variation of
reservoir retention time and river temperature. Contradictory
conclusion can be drawn if temporal data collected only near the
dam is considered instead of spatial data to represent CO2 fluxes
in whole reservoir. The average CO2 fluxes was \−17.6 and
22.1 mmolm\−2 d\−2 considering data collected near
the dam and spatial data, respectively, in periods of low
retention time. In this case, the lack of spatial information can
change completely the role of Funil Reservoir regarding GHG
emissions. Our results support the idea that Funil Reservoir is a
dynamic system where the hydrodynamics represented by changes in
river inflow and retention time is potentially more important
force driving both Chl and pCO2 spatial variability than in-system
ecological factors.",
doi = "10.5194/bgd-11-8531-2014",
url = "http://dx.doi.org/10.5194/bgd-11-8531-2014",
issn = "1810-6277",
label = "lattes: 2691497637313274 7 PachecoSACRASAO:2014:RiInRe",
language = "en",
targetfile = "bgd-11-8531-2014.pdf",
url = "http://www.biogeosciences-discuss.net/11/8531/2014/bgd-11-8531-2014.html",
urlaccessdate = "26 abr. 2024"
}