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Climate regulation by free water surface constructed wetlands for wastewater treatment and created riverine wetlands

机译:通过自由水面人工湿地进行废水处理和创建河流湿地来进行气候调节

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We analyzed about 150 Thomson Reuters ISI Web of Science indexed publications to estimate the role of free water surface (FWS) constructed wetlands (CWs) for wastewater treatment as well as created riverine wetlands (CRWs) in climate regulation. The meta-analysis on the relationship between the emission of greenhouse gases (GHGs), methane (CH4) and nitrous oxide (N2O) and the biophysical and design factors of the systems was based on 18 FWS CWs and 2 CRWs. The average emission values of CH4 and N2O varied greatly: between 0.15 and 5220 and from 0.03 to 34.1 mg CH4-Cm-2 h(-1), and from -0.003 to 0.65 and 0.002 to 0.28 mg N2O-N m(-2) h(-1) in FWS CWs and CRWs, respectively. We found a significant positive correlation between CH4 emission and the inflow loading of total organic carbon (TOCin), and between N2O flux and inflow total nitrogen (TN) loading. Emission factors (EF) (CH4-C/TOCin and N2O-N/TNin) were highest in the open water (without emergent vegetation) sections of CRW wetlands (on an average 32.5 and 2.0% for CH4 and N2O, respectively), while in FWS CWs and vegetated parts (transition/edge zone) of CRWs the EF values for CH4 were 16.9 and 10.6%, and for N2O were 0.13 and 0.51% correspondingly. The current global warming potential (GWP) of FWS CWs and CRWs is generally small, but their rapidly increasing number should warn wetland designers and stakeholders to better design and manage these systems. A pulsing water regime and support for macrophyte growth would help minimize both CH4 and N2O emissions. Further measurements using the eddy covariance technique will enable more accurate estimations of the long-term C balance and GWP of these wetland ecosystems. (C) 2013 Elsevier B.V. All rights reserved.
机译:我们分析了约150份汤森路透ISI Web of Science索引的出版物,以估计自由水面(FWS)人工湿地(CW)在废水处理中以及人工河湿地(CRW)在气候调节中的作用。基于18个FWS CW和2个CRW,对温室气体(GHGs),甲烷(CH4)和一氧化二氮(N2O)的排放与系统的生物物理和设计因素之间的关系进行了荟萃分析。 CH4和N2O的平均排放值变化很大:在0.15和5220之间以及从0.03到34.1 mg CH4-Cm-2 h(-1),从-0.003到0.65和0.002到0.28 mg N2O-N m(-2 )h(-1)分别在FWS CW和CRW中。我们发现CH4排放与总有机碳(TOCin)的流入负荷之间,N2O通量与流入的总氮(TN)负荷之间存在显着正相关。 CRW湿地的开阔水域(无植被出没)的排放因子(EF)(CH4-C / TOCin和N2O-N / TNin)最高(CH4和N2O分别平均为32.5和2.0%),而在FWS CW和CRW的植被部分(过渡区/边缘区)中,CH4的EF值分别为16.9和10.6%,N2O的EF值分别为0.13和0.51%。 FWS CW和CRW当前的全球变暖潜能通常很小,但是它们的数量迅速增加应该警告湿地设计者和利益相关者更好地设计和管理这些系统。脉动的水机制和对大型植物生长的支持将有助于最小化CH4和N2O排放。使用涡动协方差技术进行的进一步测量将使这些湿地生态系统的长期碳平衡和全球升温潜能值得到更准确的估计。 (C)2013 Elsevier B.V.保留所有权利。

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