摘要
采用静态箱(暗箱)-气相色谱法对潮棕壤不同施肥处理的稻田N2O排放进行了原位观测,同时测定了整个生长季0cm^10cm、10cm^20cm耕层土壤中NO3--N、NH4+-N含量的动态变化。结果表明:植物—土壤系统为大气N2O的源。不同耕层土壤NO3--N含量在整个生长季的变化呈“两头高中间低”的形式:在水稻生长前期和收割前后较高,在生长中期含量很低;而NH4+-N含量在水稻成熟以前较高,进入成熟期以后含量急剧降低。氮肥施用可增加稻田N2O排放的总量和耕层土壤(0 cm^20cm)NH4+-N含量;对NO3--N含量则无明显影响。图3,参16。
A field experiment was conducted to evaluated N2O fluxes from rice paddy fields using static chamber-gas chromatographic techniques. At the same time, the contents of NO3^- - N, NH4^+ - N in the different depth soil (0cm - 10 cm, 10cm - 20 cm) were measured respectively.The results were as follows: in the growing season, the soil-plant system is the source of atmospheric N2O,The variation of NO3^- - N eontents in different depth appear very regular: it is higher in early rice paddy growing stage, harvest period , and lower in middle rice paddy growing stage.The NH4^+ - N contents is higher before rice paddy mature , but it reduced sharply after rice paddy matured.Application of nitrogen fertilization enhanced N2O total fluxes from paddy rice and NH4^+ - N contents in soils, but its effect on NO3^- - N contents (0 cm - 20cm) in soil is not remarkable.
出处
《农业系统科学与综合研究》
CSCD
2006年第2期139-142,共4页
System Sciemces and Comprehensive Studies In Agriculture
基金
国家自然科学基金重点项目(40331014)
中国科学院创新专题(KZ-CX-SW-01-01B-13)
中国科学院沈阳生态实验站基金资助项目(SYZ0302)
关键词
氮肥
无机氮素
N2O
稻田
土壤
nitrogen fertilization: inorganic nitrogen
nitrous oxide
rice pad