A long-term simulated nitrogen deposition experiment was carried out in Ecological Locating Research Station of the Institute of Nature and Ecology of Heilongjiang Academy of Sciences, with three different treatments including low nitrogen treatment (40 kg N·hm-2·a-1), high nitrogen treatment (80 kg N·hm-2·a-1) and the control (0 kg N·hm-2·a-1). The greenhouse gas emission fluxes were measured using a static box-gas chromatography method, with environmental factors being simultaneously investigated to understand the responses of greenhouse gas emission to the nitrogen deposition in the Calamagrostis angustifolia wetland. The results showed that low and high nitrogen treatments significantly increased the greenhouse gas emission fluxes. The CO2 emission flux increased by 47.5% and 47.9%, the CH4 emission fluxes increased by 76.8% and 110.1%, and the N2O emission fluxes increased by 42.4% and 10.6% in low nitrogen treatment and high nitrogen treatment, respectively. Low nitrogen input changed the seasonal dynamics of N2O emission fluxes but had no significant effect on that of CO2 and CH4 emissions. High nitrogen treatment did not affect the seasonal dynamics of greenhouse gas emissions. Soil temperature significantly positively correlated with CO2 and CH4 emission fluxes. There was no correlation between soil temperature and N2O emission flux because the factors affecting N2O emission were complex.
利用黑龙江省科学院自然与生态研究所三江平原湿地生态定位研究站内的长期模拟氮沉降试验平台,采用静态箱-气相色谱法,设置低氮(40 kg N·hm-2·a-1)和高氮(80 kg N·hm-2·a-1)处理,以及对照(0 kg N·hm-2·a-1),测定小叶章湿地温室气体排放通量及其相关环境因子,研究三江平原小叶章湿地温室气体排放对氮沉降的响应.结果表明: 低氮和高氮输入均显著增加了温室气体的排放通量,低氮和高氮处理使CO2排放通量增加47.5%和47.9%,CH4排放通量增加76.8%和110.1%,N2O排放通量增加42.4%和10.6%.低氮输入改变了N2O排放的季节动态,但对CO2和CH4排放的季节动态没有显著影响,高氮处理对3种气体排放的季节动态均未造成影响.CO2排放通量和CH4排放通量均与土壤温度呈显著正相关,而影响N2O排放的因素较为复杂,未与土壤温度出现显著的相关关系.
Keywords: Calamagrostis angustifolia wetland; greenhouse gas; nitrogen deposition.