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巴西东南部一个城市高度污染的热带沿海泻湖中的温室气体排放(一氧化碳和甲烷)及无机碳行为

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

作者信息

Cotovicz Luiz C, Ribeiro Renato P, Régis Carolina Ramos, Bernardes Marcelo, Sobrinho Rodrigo, Vidal Luciana Oliveira, Tremmel Daniel, Knoppers Bastiaan A, Abril Gwenaël

机构信息

Programa de Geoquímica, Universidade Federal Fluminense, Niterói, RJ, Brazil.

Instituto de Ciências do Mar, Universidade Federal do Ceará, Fortaleza, CE, Brazil.

出版信息

Environ Sci Pollut Res Int. 2021 Jul;28(28):38173-38192. doi: 10.1007/s11356-021-13362-2. Epub 2021 Mar 16.

Abstract

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 (CO) and methane (CH) 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 CO (pCO; up to 20,417 ppmv) and CH concentrations (up to 288,572 nmol L). 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 CH oxidation apparently consumed some CO and CH, respectively. TA concentrations showed a marked minimum at salinity of ~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 d for CO and from 2.2 to 16.5 mmol C m d for CH. This later value is among the highest documented in coastal waters. In terms of global warming potential (GWP) and CO equivalent emissions (CO-eq), the diffusive emissions of CH were higher than those of CO. 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.

摘要

沿海水域富营养化加剧,导致温室气体(GHG)浓度和向大气排放的变化,但相关记录仍然很少,特别是在热带地区。在此,我们调查了巴西东南部以城市为主的雅卡雷帕古阿泻湖复合体(JLC)中二氧化碳(CO₂)和甲烷(CH₄)的浓度及扩散通量。这个泻湖复合体接收高污染淡水,经常出现缺氧和低氧情况,且有密集的浮游植物水华。在2017年至2018年期间,进行了四次空间调查(干湿条件),在排放城市流域的河流水域以及盐度不断增加的泻湖水域进行采样。在河流中发现了强烈的氧气消耗,这与极高的CO₂分压(pCO₂;高达20,417 ppmv)和CH₄浓度(高达288,572 nmol L⁻¹)有关。这些高浓度的温室气体归因于未经处理的生活污水中有机物通过好氧和厌氧过程降解,同时产生总碱度(TA)和溶解无机碳(DIC)。在泻湖中,温室气体浓度主要因海水稀释和脱气而降低。此外,浮游植物生长和CH₄氧化显然分别消耗了一些CO₂和CH₄。与两个淡水和海洋端元相比,TA浓度在盐度约为20时出现明显最小值,表明来自低盐度区域的无机还原物种(如氨、铁和/或硫化物)发生了再氧化过程。整个泻湖的气体扩散排放量,CO₂为22至48 mmol C m⁻² d⁻¹,CH₄为2.2至16.5 mmol C m⁻² d⁻¹。后一个值是沿海水域有记录以来的最高值之一。就全球变暖潜能值(GWP)和CO₂当量排放(CO₂-eq)而言,CH₄的扩散排放量高于CO₂。这些结果突出表明,高度污染的沿海生态系统是向大气排放温室气体的热点地区,在未来全球碳预算中可能变得越来越重要。

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