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dc.rights.licenseopenen_US
dc.contributor.authorPACHECO, Felipe Siqueira
dc.contributor.authorSOARES, M. C. S.
dc.contributor.authorASSIREU, Arcilan T.
dc.contributor.authorCURTARELLI, Marcelo Pedroso
dc.contributor.authorROLAND, F.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorABRIL, Gwenaël
dc.contributor.authorSTECH, José Luiz
dc.contributor.authorALVALÁ, P. C.
dc.contributor.authorOMETTO, J. P.
dc.date.accessioned2024-06-03T09:17:52Z
dc.date.available2024-06-03T09:17:52Z
dc.date.issued2015-01-09
dc.identifier.issn1726-4170en_US
dc.identifier.urihttp://www.biogeosciences.net/12/147/2015/bg-12-147-2015.html
dc.identifier.urioai:crossref.org:10.5194/bg-12-147-2015
dc.identifier.uriorcid:0000-0002-4221-1039:10.5194/bg-12-147-2015
dc.identifier.uriftcopernicus:oai:publications.copernicus.org:bg2448
dc.identifier.urioai:researchgate.net:270587454
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200213
dc.description.abstractEnAbstract. Abundant research has been devoted to understanding the complexity of the biogeochemical and physical processes that are responsible for greenhouse gas (GHG) emissions from hydropower reservoirs. These systems may have spatially complex and heterogeneous GHG emissions due to flooded biomass, river inflows, primary production and dam operation. In this study, we investigated the relationships between the water–air CO2 fluxes and the phytoplanktonic biomass in the Funil Reservoir, which is an old, stratified tropical reservoir that exhibits intense phytoplankton blooms and a low partial pressure of CO2 (pCO2). Our results indicated that the seasonal and spatial variability of chlorophyll concentrations (Chl) and pCO2 in the Funil Reservoir are related more to changes in the river inflow over the year than to environmental factors such as air temperature and solar radiation. Field data and hydro\\-dynamic simulations revealed that river inflow contributes to increased heterogeneity during the dry season due to variations in the reservoir retention time and river temperature. Contradictory conclusions could be drawn if only temporal data collected near the dam were considered without spatial data to represent CO2 fluxes throughout the reservoir. During periods of high retention, the average CO2 fluxes were 10.3 mmol m−2 d−1 based on temporal data near the dam versus −7.2 mmol m−2 d−1 with spatial data from along the reservoir surface. In this case, the use of solely temporal data to calculate CO2 fluxes results in the reservoir acting as a CO2 source rather than a sink. This finding suggests that the lack of spatial data in reservoir C budget calculations can affect regional and global estimates. Our results support the idea that the Funil Reservoir is a dynamic system where the hydrodynamics represented by changes in the river inflow and retention time are potentially a more important force driving both the Chl and pCO2 spatial variability than the in-system ecological factors.
dc.language.isoENen_US
dc.sourcecrossref
dc.sourceorcid
dc.sourcebase
dc.sourceresearchgate
dc.title.enThe effects of river inflow and retention time on the spatial heterogeneity of chlorophyll and water–air CO2 fluxes in a tropical hydropower reservoir
dc.typeArticle de revueen_US
dc.identifier.doi10.5194/bg-12-147-2015en_US
bordeaux.journalBiogeosciencesen_US
bordeaux.page147-162en_US
bordeaux.volume12en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
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dc.rights.ccCC BYen_US
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