Zhu Ren-Bin, Sun Li-Guang, Zhao San-Ping, Xie Zhou-Qing, Liu Xiao-Dong, Yin Xue-Bin
Institute of Polar Environment, University of Science and Technology of China, Hefei 230026, China.
J Environ Sci (China). 2005;17(4):551-6.
The preliminary measurements of nitrous oxide fluxes from the ornithogenic soils on tropical Xi-sha atoll were made using a closed chamber technique for the first time. N2O fluxes from the ornithogenic soils ranged from 1.8 to 40.3 microg/(m2 x h) on Dong Island and 3.2 to 20.4 microg/(m2 x h) on Yongxing Island and their flux averaged 11.0 microg/(m2 x h) and 8.3 microg/(m2 x h), respectively. N2O fluxes from two wetland sites in salt marsh of Dong Island were approximately one order of magnitude lower than those from the ornithogenic soils and averaged 2.1 microg/(m2 x h) and 2.4 microg/(m2 x h). The diurnal variation cycle in the fluxes was obtained at the observation sites; the N2O flux increased with the increase in soil temperature. The sudden increase in soil moisture greatly stimulated N2O emission from the ornithogenic soils on Dong Island due to the heavy rainfall. The undisturbed soils showed the lower N2O fluxes and the average was 4.8 microg/(m2 x h) and the soils via the reclamation showed the higher N2O fluxes and the average was 16.6 microg/(m2 x h) on Yongxing Island, suggesting that the changes of land use have an important effect on N2O fluxes from the ornithogenic soils. In addition, the N2O fluxes at the different sites showed high spatial variations. The fluxes were positively correlated with the concentrations of NO3-, PO4(3-) and Mn in the soils. The negative correlation between the fluxes and total S concentration in the ornithogenic soils was also found for the first time. Coastal soils or sediments constitute an important source of global atmospheric N2O and the increases in nitrogen loading from seabird guanos will lead to significant increases in the flux of this atmospherically active gas.
首次采用密闭箱技术对热带西沙环礁鸟粪土的氧化亚氮通量进行了初步测量。东岛鸟粪土的N2O通量范围为1.8至40.3微克/(平方米·小时),永兴岛为3.2至20.4微克/(平方米·小时),其通量平均分别为11.0微克/(平方米·小时)和8.3微克/(平方米·小时)。东岛盐沼两个湿地站点的N2O通量比鸟粪土的通量低约一个数量级,平均为2.1微克/(平方米·小时)和2.4微克/(平方米·小时)。在观测站点获得了通量的日变化周期;N2O通量随土壤温度升高而增加。由于暴雨,土壤湿度的突然增加极大地刺激了东岛鸟粪土的N2O排放。在永兴岛,未扰动土壤的N2O通量较低,平均为4.8微克/(平方米·小时),而垦殖后的土壤N2O通量较高,平均为16.6微克/(平方米·小时),这表明土地利用变化对鸟粪土的N2O通量有重要影响。此外,不同站点的N2O通量存在高度的空间变异性。通量与土壤中NO3-、PO4(3-)和Mn的浓度呈正相关。首次发现鸟粪土通量与总硫浓度之间存在负相关。沿海土壤或沉积物是全球大气N2O的重要来源,海鸟鸟粪中氮负荷的增加将导致这种大气活性气体通量的显著增加。