首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Effect of continued nitrogen enrichment on greenhouse gas emissions from a wetland ecosystem in the Sanjiang Plain, Northeast China: A 5 year nitrogen addition experiment
【24h】

Effect of continued nitrogen enrichment on greenhouse gas emissions from a wetland ecosystem in the Sanjiang Plain, Northeast China: A 5 year nitrogen addition experiment

机译:持续富氮对东北三江平原湿地生态系统温室气体排放的影响:一项为期五年的氮添加实验

获取原文
获取原文并翻译 | 示例
           

摘要

Mounting evidence supports that wetland ecosystems, one of the largest carbon pools on the earth, are exposed to ample nitrogen (N) additions due to atmospheric deposition or N loading from upstream agricultural fertilizer application. However, our understanding of how N enrichment affects the fluxes of greenhouse gases (GHGs) in wetlands is weak. A 5 year N addition experiment was conducted to examine the responses of CH_4 and N_2O fluxes as well as ecosystem respiration from wetlands in the Sanjiang Plain, Northeast China, through 2005 to 2009. Four levels of N addition (control, 0 kg N ha~(-1) yr~(-1); low-level, 60 kg N ha~(-1) yr ~(-1); medium-level, 120 kg N ha~(-1) yr~(-1); high-level, 240 kg N ha~(-1) yr~(-1)) were designed in this study. Overall, our results show that medium and high levels of N addition increased ecosystem respiration by 28% and 69% (P < 0.05), respectively, while low-level N addition has no effect on ecosystem respiration (P > 0.05). High-level N fertilization exerted stronger effects on ecosystem respiration in the initial year than the following years. It indicated that the effects of high-level N fertilization on CO_2 might be overestimated by short-term observations. High-level N fertilization increased N_2O emissions by 396% over the 5 years (P < 0.05), but the low- and medium-level-N addition did not exert any apparent effect on N_2O emissions (P > 0.05). N_2O emission under high-level N addition in the first and fifth years showed stronger pronounced responses to N addition compared with that from the third and fourth years, indicating the importance of long-term field observation. Over the 5 years, however, the low and medium-level N addition showed no effect on N_2O emissions. The four levels of N addition exerted no effect on CH_4 emissions (P > 0.05). Furthermore, the relationship between GHGs and soil temperature or water table depth varied among different plots and experimental time. Our findings highlighted the importance of gas species, experimental time, and the amount of fertilizer N with regard to the responses of GHG emissions to N fertilization. Key Points GHGs to N fertilization varied among N input levels and gas speciesN fertilization enhanced the temperature sensitivity of ERhigh-N stimualated SR more in the first year
机译:越来越多的证据支持,湿地生态系统是地球上最大的碳库之一,由于大气层沉积或上游农业施肥施加的氮负荷而暴露于充足的氮(N)暴露之下。但是,我们对氮的富集如何影响湿地中温室气体通量的理解很弱。进行了为期5年的氮素添加实验,研究了2005年至2009年中国东北三江平原湿地CH_4和N_2O通量的响应以及生态系统的呼吸作用。氮素添加的四个水平(对照,0 kg N ha〜 (-1)yr〜(-1);低水平,60 kg N ha〜(-1)yr〜(-1);中水平,120 kg N ha〜(-1)yr〜(-1) ;本研究设计了高水平的240 kg N ha〜(-1)yr〜(-1))。总体而言,我们的结果表明,中高水平的氮添加分别使生态系统呼吸增加28%和69%(P <0.05),而低水平的氮添加对生态系统呼吸没有影响(P> 0.05)。与后几年相比,高氮施肥在第一年对生态系统呼吸的影响更大。这表明短期观测可能高估了高氮肥对CO_2的影响。高氮施肥在5年中使N_2O排放增加了396%(P <0.05),但是低氮和中氮水平的添加对N_2O排放没有明显影响(P> 0.05)。与第三和第四年相比,在第一和第五年高氮添加下的N_2O排放显示出对氮的更明显的响应,表明了长期野外观测的重要性。然而,在过去的5年中,低和中等水平的氮添加量对N_2O排放没有影响。氮的四个添加水平对CH_4的排放没有影响(P> 0.05)。此外,温室气体与土壤温度或地下水位深度之间的关系在不同的样地和试验时间之间也不同。我们的发现突出了气体种类,实验时间和肥料氮量对温室气体排放对氮肥的响应的重要性。氮肥输入的关键因素是温室气体对氮输入水平和气体种类的影响在第一年氮肥提高了ERhigh-N刺激的SR的温度敏感性

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号