Greenhouse gas emissions (CO2 and CH4) and inorganic carbon behavior in an urban highly polluted tropical coastal lagoon (SE, Brazil)

被引:26
|
作者
Cotovicz, Luiz C., Jr. [1 ,2 ]
Ribeiro, Renato P. [3 ]
Regis, Carolina Ramos [1 ]
Bernardes, Marcelo [1 ]
Sobrinho, Rodrigo [1 ]
Vidal, Luciana Oliveira [4 ]
Tremmel, Daniel [1 ]
Knoppers, Bastiaan A. [1 ]
Abril, Gwenael [1 ,5 ]
机构
[1] Univ Fed Fluminense, Programa Geoquim, Niteroi, RJ, Brazil
[2] Univ Fed Ceara, Inst Ciencias Mar, Fortaleza, CE, Brazil
[3] Inst Fed Educ Ciencia & Tecnol Rio de Janeiro IFR, Ctr Expt Monitoramento & Mitigacao Ambiental CEMM, Nilopolis, RJ, Brazil
[4] Univ Estadual Norte Fluminense, Ctr Biociencias & Biotecnol, Lab Ciencias Ambientais, Campos Dos Goytacazes, RJ, Brazil
[5] Museum Natl Hist Nat, Biol Organismes & Ecosyst Aquat BOREA, CNRS, UMR 7208,IRD,SU,UCN,UA, Paris, France
关键词
Carbon dioxide; Methane; Carbonate chemistry; Coastal eutrophication; Environment pollution; Coastal lagoons; RIO-DE-JANEIRO; GUANABARA BAY; ALKALINITY GENERATION; SEASONAL VARIABILITY; METHANE OXIDATION; RIVER ESTUARY; FRESH-WATER; DIOXIDE; FLUXES; EUTROPHICATION;
D O I
10.1007/s11356-021-13362-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Increasing eutrophication of coastal waters generates disturbances in greenhouse gas (GHG) concentrations and emissions to the atmosphere that are still poorly documented, particularly in the tropics. Here, we investigated the concentrations and diffusive fluxes of carbon dioxide (CO2) and methane (CH4) in the urban-dominated Jacarepagua Lagoon Complex (JLC) in Southeastern Brazil. This lagoonal complex receives highly polluted freshwater and shows frequent occurrences of anoxia and hypoxia and dense phytoplankton blooms. Between 2017 and 2018, four spatial surveys were performed (dry and wet conditions), with sampling in the river waters that drain the urban watershed and in the lagoon waters with increasing salinities. Strong oxygen depletion was found in the rivers, associated with extremely high values of partial pressure of CO2 (pCO(2); up to 20,417 ppmv) and CH4 concentrations (up to 288,572 nmol L-1). These high GHG concentrations are attributed to organic matter degradation from untreated domestic effluents mediated by aerobic and anaerobic processes, with concomitant production of total alkalinity (TA) and dissolved inorganic carbon (DIC). In the lagoon, GHG concentrations decreased mainly due to dilution with seawater and degassing. In addition, the phytoplankton growth and CH4 oxidation apparently consumed some CO2 and CH4, respectively. TA concentrations showed a marked minimum at salinity of similar to 20 compared to the two freshwater and marine end members, indicating processes of re-oxidation of inorganic reduced species from the low-salinity region, such as ammonia, iron, and/or sulfides. Diffusive emissions of gases from the entire lagoon ranged from 22 to 48 mmol C m(-2) d(-1) for CO2 and from 2.2 to 16.5 mmol C m(-2) d(-1) for CH4. This later value is among the highest documented in coastal waters. In terms of global warming potential (GWP) and CO2 equivalent emissions (CO2-eq), the diffusive emissions of CH4 were higher than those of CO2. These results highlight that highly polluted coastal ecosystems are hotspots of GHG emissions to the atmosphere, which may become increasingly significant in future global carbon budgets.
引用
收藏
页码:38173 / 38192
页数:20
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