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Preliminary studies on nitrous oxide emissions from the ornithogenic soils on Xi-sha atoll, South China Sea

机译:南海西沙环礁鸟类群落土壤一氧化二氮排放的初步研究

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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. N_2O fluxes from the ornithogenic soils ranged from 1.8 to 40.3 mu g/(m~2 -h) on Dong Island and 3.2 to 20.4 mu g/(m~2-h) on Yongxing Island and their flux averaged 11.0 mu g/(m~2 centre dot h) and 8.3 mu g/(m~2 centre dot h), respectively. N_2O 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 mu g/(m~2 centre dot h) and 2,4 mu g/(m~2 centre dot h). The diurnal variation cycle in the fluxes was obtained at the observation sites; the N_2O flux increased with the increase in soil temperature. The sudden increase in soil moisture greatly stimulated N_2O emission from the ornithogenic soils on Dong Island due to the heavy rainfall. The undisturbed soils showed the lower N_2O fluxes and the average was 4.8 mu g/(m~2 centre dot h) and the soils via the reclamation showed the higher N2O fluxes and the average was 16.6 mu g/(m~2 centre h) on Yongxing Island, suggesting that the changes of land use have an important effect on N_2O fluxes from the ornithogenic soils. In addition, the N_2O fluxes at the different sites showed high spatial variations. The fluxes were positively correlated with the concentrations of NO_3~-. PO~(3-)_4 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 N_2O and the increases in nitrogen loading from seabird guanos will lead to significant increases in the flux of this atmospherically active gas.
机译:首次使用密闭室技术对热带西沙环礁鸟类群落土壤中的一氧化二氮通量进行了初步测量。鸟类群落土壤中N_2O的通量在董岛上为1.8至40.3μg /(m〜2-h),在永兴岛上为3.2至20.4μg /(m〜2-h),平均通量为11.0μg /( m〜2中心点h)和8.3μg /(m〜2中心点h)。东岛盐沼两个湿地的N_2O通量比鸟类生土的N_2O通量低约一个数量级,平均通量为2.1μg /(m〜2中心点h)和2,4μg /(m〜2中心点h)。在观测点获得了通量的日变化周期。 N_2O通量随着土壤温度的升高而增加。由于暴雨,土壤水分的突然增加极大地刺激了东岛鸟类群落土壤中N_2O的排放。未扰动土壤的N_2O通量较低,平均为4.8μg /(m〜2中心点h),经复垦的土壤N2O通量较高,平均为16.6μg/(m〜2中心点h)在永兴岛上,表明土地利用的变化对鸟类生土中N_2O通量有重要影响。另外,不同部位的N_2O通量表现出较大的空间变化。通量与NO_3〜-的浓度呈正相关。土壤中的PO〜(3-)_ 4和Mn。还首次发现了鸟类生土中通量与总S浓度之间的负相关。沿海土壤或沉积物是全球大气N_2O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的通量显着增加。

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