Tian Lin-Lin, Zhu Bo, Wang Tao, Zhao Yuan, Dong Hong-Wei, Ren Guang-Qian, Hu Lei
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China.
Key Laboratory of Mountain Surface Processes and Ecological Regulation, Chinese Academy of Sciences, Chengdu 610041, China.
Huan Jing Ke Xue. 2017 May 8;38(5):2074-2083. doi: 10.13227/j.hjkx.201611163.
Agricultural headwater ditches, the important locations for retaining and transforming nitrogen derived from the adjacent farmlands, have been regarded as the potential source of nitrous oxide (NO) emission. In this study, NO emissions from a typical agricultural ditch in the Hilly Area of Central Sichuan Basin, were observed by closed static chamber-GC technique during the maize season (rainy season), from June to the end of September. During the study period, cumulative NO emissions in the sediment-water interface without vegetation (NV) and the ditch ecosystem with natural vegetation (V) were 0.07 and 0.43 kg·hm, respectively. Meanwhile, the mean NO flux from the agricultural headwater ditch ecosystem[14.7 μg·(m·h)] was comparable to the magnitude of direct NO flux from the maize cropland in this region. Nitrate concentration in the overlying water could be the main factor governing NO emission from the ditch, especially in the rainy season. The existence of vegetation increased the indirect NO emission factor (V:0.05% .NV:0.01%). The indirect NO emission factor from this field investigation was much lower than the default value proposed by the Intergovernmental Panel on Climate Change (IPCC, 2006) for assessing indirect agricultural NO emissions. More attention should be paid to measurements to reduce uncertainty of NO estimation calculated by only applying the default value for emission factor from the IPCC.
农业上游沟渠是截留和转化来自相邻农田氮素的重要场所,一直被视为氧化亚氮(N₂O)排放的潜在源。本研究在四川盆地中部丘陵区的一个典型农业沟渠,于玉米季(雨季,6月至9月底)采用密闭静态箱 - 气相色谱技术观测了N₂O排放。研究期间,无植被的沉积物 - 水界面(NV)和有天然植被的沟渠生态系统(V)的累积N₂O排放量分别为0.07和0.43 kg·hm⁻²。同时,农业上游沟渠生态系统的平均N₂O通量[14.7 μg·(m²·h)⁻¹]与该地区玉米农田的直接N₂O通量量级相当。上覆水中的硝酸盐浓度可能是控制沟渠N₂O排放的主要因素,尤其是在雨季。植被的存在增加了间接N₂O排放因子(V:0.05%,NV:0.01%)。本次田间调查的间接N₂O排放因子远低于政府间气候变化专门委员会(IPCC,2006)提出的用于评估农业间接N₂O排放的默认值。应更加关注测量,以减少仅应用IPCC排放因子默认值计算N₂O排放量时的不确定性。