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首页> 外文期刊>Global change biology >Ecosystem-atmosphere exchange of CH and NO and ecosystem respiration in wetlands in the Sanjiang Plain, Northeastern China
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Ecosystem-atmosphere exchange of CH and NO and ecosystem respiration in wetlands in the Sanjiang Plain, Northeastern China

机译:三江平原湿地CH,NO生态系统-大气交换与生态系统呼吸

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摘要

Natural wetlands are critically important to global change because of their role in modulating atmospheric concentrations of CO, CH, and NO. One 4-year continuous observation was conducted to examine the exchanges of CH and NO between three wetland ecosystems and the atmosphere as well as the ecosystem respiration in the Sanjiang Plain in Northeastern China. From 2002 to 2005, the mean annual budgets of CH and NO, and ecosystem respiration were 39.40 pl 6.99 g C mpo yrp#, 0.124 pl 0.05 g N mpo yrp#, and 513.55 pl 8.58 g C mpo yrp# for permanently inundated wetland; 4.36 pl 1.79 g C mpo yrp#, 0.11 pl 0.12 g N mpo yrp#, and 880.50 pl 71.72 g C mpo yrp# for seasonally inundated wetland; and 0.21 pl 0.1 g C mpo yrp#, 0.28 pl 0.11 g N mpo yrp#, and 1212.83 pl 191.98 g C mpo yrp# for shrub swamp. The substantial interannual variation of gas fluxes was due to the significant climatic variability which underscores the importance of long-term continuous observations. The apparent seasonal pattern of gas emissions associated with a significant relationship of gas fluxes to air temperature implied the potential effect of global warming on greenhouse gas emissions from natural wetlands. The budgets of CH and NO fluxes and ecosystem respiration were highly variable among three wetland types, which suggest the uncertainties in previous studies in which all kinds of natural wetlands were treated as one or two functional types. New classification of global natural wetlands in more detailed level is highly expected.
机译:天然湿地对全球变化至关重要,因为它们在调节大气中的CO,CH和NO浓度中发挥了作用。连续进行了为期4年的观察,以研究中国东北三江平原三个湿地生态系统与大气之间的CH和NO交换以及大气和生态系统的呼吸作用。从2002年到2005年,CH和NO和生态系统呼吸的年平均预算分别为39.40 pl 6.99 g C mpo yrp#,0.124 pl 0.05 g N mpo yrp#和513.55 pl 8.58 g C mpo yrp#。对于季节性淹没的湿地,为4.36 pl 1.79 g C mpo yrp#,0.11 pl 0.12 g N mpo yrp#和880.50 pl 71.72 g C mpo yrp#。用于灌木沼泽的0.21 pl 0.1 g C mpo yrp#,0.28 pl 0.11 g N mpo yrp#和1212.83 pl 191.98 g C mpo yrp#。气体通量的年际变化很大是由于明显的气候变化,这突显了长期连续观测的重要性。气体排放的明显季节性模式与气体通量与气温的显着关系有关,这暗示着全球变暖对自然湿地温室气体排放的潜在影响。在三种湿地类型中,CH,NO通量和生态系统呼吸的预算变化很大,这表明以前的研究存在不确定性,在这些研究中,各种天然湿地都被视为一种或两种功能类型。高度期望对全球自然湿地进行更详细的分类。

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