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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Spatio-temporal variations of GHG emissions from surface water of Xiangxi River in Three Gorges Reservoir region, China
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Spatio-temporal variations of GHG emissions from surface water of Xiangxi River in Three Gorges Reservoir region, China

机译:三峡库区湘西河地表水温室气体排放的时空变化

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Damming has exerted far-reaching and profound impacts on ecological functions in river ecosystems. However, the "damming effects" on greenhouse gases (GHG) emissions from tributaries of reservoirs in subtropical region were largely overlooked. In this study, we assessed the GHG fluxes (CH4, CO2 and N2O) from air-water interface and the related factors in Xiangxi River of Three Gorges Reservoir (TGR) region over one year. The annual average fluxes of CH4, CO2 and N2O from Xiangxi River were 0.13 +/- 0.11 mg m(-2) h(-1), 16.01 +/- 23.21 mg m(-2) h(-1) and 21.57 +/- 12.75 mg m(-2) h(-1), respectively, which were significantly lower than those from tropical rivers or lakes. The GHG fluxes showed strong seasonal dynamics: CH4 was consistently released to the atmosphere and was more in summer than the other seasons. CO2 was absorbed from the atmosphere in spring, but was emitted the most in winter. N2O flux was higher in cold season than in warm season. Additionally, CH4 emission showed obvious spatial variations that decreased gradually from shallow to deep water-level areas. Correlation analysis demonstrated that CH4 emission was negatively correlated with water depth and air-water temperature difference, and positively with air temperature. CO2 flux was negatively related to chlorophyll a (Chl. a) and N2O flux was negatively correlated with dissolved oxygen (DO). The present study will deepen our understanding of Three Gorges Dam (TGD) construction impacts on GHG emissions in the tributaries, and help us to better estimate GHG emissions for TGR. (C) 2015 Elsevier B.V. All rights reserved.
机译:大坝建设对河流生态系统的生态功能产生了深远的影响。然而,亚热带地区水库支流对温室气体(GHG)排放的“筑坝效应”在很大程度上被忽略了。在这项研究中,我们评估了三峡水库(TGR)地区湘西河气水界面的温室气体通量(CH4,CO2和N2O)以及一年以上的相关因素。湘西河CH4,CO2和N2O的年平均通量分别为0.13 +/- 0.11 mg m(-2)h(-1),16.01 +/- 23.21 mg m(-2)h(-1)和21.57 +分别为12.75 mg m(-2)h(-1),明显低于热带河流或湖泊中的水。温室气体通量表现出强烈的季节动态:CH4持续释放到大气中,夏季比其他季节更多。春季从大气中吸收了二氧化碳,而冬季则排放最多。在寒冷季节,N2O通量高于温暖季节。此外,CH4排放显示出明显的空间变化,从浅水区到深水位区域逐渐减小。相关分析表明,CH4的排放与水深和气水温差呈负相关,与气温呈正相关。 CO2通量与叶绿素a(Chl。a)负相关,N2O通量与溶解氧(DO)负相关。本研究将加深我们对三峡大坝(TGD)建设对支流GHG排放的影响的理解,并有助于我们更好地估算TGR的GHG排放。 (C)2015 Elsevier B.V.保留所有权利。

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