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贵州省旱田土壤N2O释放及其环境影响因素
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中文关键词  N2O  释放通量  旱田土壤  影响因素
英文关键词  N2O,flux, upland soils,controlling factors.
作者单位
徐文彬 中国科学院地球化学研究所环境地球化学国家重点实验室,贵阳550002 
洪业汤 浙江大学环境与资源化学研究所,杭州310027 
陈旭晖 贵州省农业科学院土壤肥料研究所,贵阳550006 
王羽 浙江大学环境与资源化学研究所,杭州310027 
中文摘要
      以贵州省的玉米-油菜轮作田、大豆-冬小麦轮作和休耕地为研究对象,采用密闭箱-气相色谱法,对整个轮作期的土壤N2O释放进行观测,初步研究我国亚热带旱田的N2O释放特征.实验研究结果表明,3试验田N2O释放通量具有相同的规律性日变化形式,秋收作物达通量极大值的时间比越冬作物滞后2h~3h,气温是控制N2O通量日变化的主要环境因子:3试验田N2O释放通量(以N2O中的N计)分别在9.81~433.11,4.00~180.41和9.74~282.00μg·m-2·h-1,高于我国水田和北方旱田的N2O释放通量;进一步分析表明,3试验田N2O释放通量具有相同的季节变化模式,N2O 释放峰受降雨事件的直接影响,N2O通量与降雨量和土壤湿度间有显著的正相关性,而与温度的关系不明显
英文摘要
      Three fields including a corn rape rotation field,a soybean winter wheat rotation field and a fallow land were chosen as study plots to measure N2O flux from soils using close chamber GC method during crop rotation,the purpose of this research was to study the characteristics of N2O flux.The results indicated the shapes of N2O diurnal variation were similar between above three fields,the time which N2O flux reached the highest was 2 or 3 hours later from corn and soybean fields than from rape and winter wheat fields,and air temperature was the key factor influencing the diurnal variation of N2O flux.The ranges of N2O flux(as N in N2O)from above three fields were 9.81~433.11,4.00~180.41 and 9.74~282.00μg·m-2 ·h-1 respectively,they were higher than fluxes from upland soils in North China.Furthermore,the seasonal variation characteristics of N2O flux from above three fields were homologous,N2O flux pulses were produced and driven by rainfall events directly,the relativity between N2O flux and precipitation and soil's moisture were positive remarkably,but the relativity was not important between N2O flux and temperature.

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