Yu Junbao, Liu Jingshuang, Wang Jinda, Sun Weidong, Patrick William H, Meixner Franz X
Key Lab of Wetland Ecology and Environment, Northeast Institute of Geography and Agricultural Ecology, Chinese Academy of Sciences, 3195 Weishan Road, Changchun, 130012, China.
Environ Manage. 2007 Oct;40(4):613-22. doi: 10.1007/s00267-006-0349-9. Epub 2007 Jul 27.
Here we report N(2)O emission results for freshwater marshes isolated from human activities at the Sanjiang Experimental Station of Marsh Wetland Ecology in northeastern China. These results are important for us to understand N(2)O emission in natural processes in undisturbed freshwater marsh. Two adjacent plots of Deyeuxia angustifolia freshwater marsh with different water regimes, i.e., seasonally waterlogged (SW) and not- waterlogged (NW), were chosen for gas sampling, and soil and biomass studies. Emissions of N(2)O from NW plots were obviously higher than from the SW plots. Daily maximum N(2)O flux was observed at 13 o'clock and the seasonal maximum occurred in end July to early August. The annual average N(2)O emissions from the NW marsh were 4.45 microg m(-2) h(-1) in 2002 and 6.85 microg m(-2) h(-1) in 2003 during growing season. The SW marsh was overall a sink for N(2)O with corresponding annual emissions of -1.00 microg m(-2) h(-1) for 2002 and -0.76 microg m(-2) h(-1) for 2003. There were significant correlations between N(2)O fluxes and temperatures of both air and 5-cm-depth soil. The range of soil redox potential 200-400 mV appeared to be optimum for N(2)O flux. Besides temperature and plant biomass, the freeze-thaw process is also an important factor for N(2)O emission burst. Our results show that the freshwater marsh isolated from human activity in northeastern China is not a major source of N(2)O.
在此,我们报告了在中国东北沼泽湿地生态系统三江实验站开展的、与人类活动隔绝的淡水沼泽中一氧化二氮(N₂O)排放的研究结果。这些结果对于我们理解未受干扰的淡水沼泽自然过程中的N₂O排放具有重要意义。我们选取了两块相邻的狭叶甜茅淡水沼泽样地,它们具有不同的水分状况,即季节性淹水(SW)和非淹水(NW),用于气体采样、土壤及生物量研究。NW样地的N₂O排放量明显高于SW样地。每日N₂O通量最大值出现在13时,季节性最大值出现在7月底至8月初。2002年生长季期间,NW沼泽的年平均N₂O排放量为4.45微克·米⁻²·小时⁻¹,2003年为6.85微克·米⁻²·小时⁻¹。SW沼泽总体上是N₂O的汇,2002年和2003年相应的年排放量分别为-1.00微克·米⁻²·小时⁻¹和-0.76微克·米⁻²·小时⁻¹。N₂O通量与空气温度和5厘米深度土壤温度之间存在显著相关性。200 - 400毫伏的土壤氧化还原电位范围似乎最有利于N₂O通量。除了温度和植物生物量外,冻融过程也是N₂O排放激增的一个重要因素。我们的结果表明,中国东北与人类活动隔绝的淡水沼泽并非N₂O的主要排放源。