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氮肥水平对不同土壤N2O排放的影响
摘要点击 2246  全文点击 1498    修订日期:2007-09-18
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中文关键词  N2O排放  氮肥; 稻麦轮作; 盆栽试验
英文关键词  N2O emission  N fertilizer  rice-wheat rotation period  pot experiment
作者单位
焦燕 内蒙古师范大学化学与环境科学学院呼和浩特010022 
黄耀 南京农业大学资源与环境学院, 南京210095
中国科学院大气物理研究所大气边界层物理和大气化学国家重点实验室
北京100029 
宗良纲 南京农业大学资源与环境学院 南京210095 
周权锁 南京农业大学资源与环境学院 南京210095 
Ronald L. Sass Department of Ecology and Evolutionary Biology, Rice University, Houston, TX77005-1892, USA 
中文摘要
      鉴于N2O排放量占施用氮肥量的比例即N2O排放系数还有很大不确定性,室外盆栽试验于2002~2003年选取3个供试土壤,各土壤设置对照和低、中、高氮肥水平,全年施尿素量 (以N计) 分别为334、 670和1 004 kg/hm2.结果表明,水稻生长季,各个土壤的N2O累积排放量与其对照相比的增加量在低、中、高氮肥水平间无明显差异;而小麦生长季,随氮肥施用量增加,各个土壤的N2O累积排放量与其对照相比的增加量在3种氮肥水平之间的差异显著.整个稻麦轮作系统,随氮肥用量的增加明显促进麦田N2O的排放.无论水稻或小麦生长季,对照3个土壤的N2O累积排放量并无显著差异,F土壤(江苏溧水)、G土壤(江苏涟水)和H土壤(江苏农科院)的N2O累积排放量,在水稻生长季分别为168、 127和146 mg/m2;小麦生长季,分别为134、 124和168 mg/m2.在施氮肥后,3个土壤的N2O排放量出现差异,如在中氮水平下,小麦生长季,F土壤、G土壤和H土壤N2O累积排放量分别为976、 744和626 mg/m2.稻麦轮作生长季内,在低氮与中氮2个水平下,不同土壤间N2O排放系数存在显著差异.以1个稻麦轮作周期为时间尺度,F土壤、G土壤和H土壤总的N2O排放系数分别为1.1%±0.23%、 0.75%±0.17%和1.01%±0.11%,表明不同土壤对N2O排放系数的影响不同.
英文摘要
      To investigate the effect of different urea incorporation amount in different soils on N2O emission, a pot experiment was carried in 2002-2003.Four treatments were designed as the control (without urea incorporation); low N fertilizer level(334 kg/hm2); middle N fertilizer level(670 kg/hm2); high N fertilizer level (1 004 kg/hm2). In rice growing season, compared to control, the increment of N2O emission accumulation flux of each soil has no obviously differences among three N fertilizer levels. Contrarily, in wheat-planted soils, there are remarkably differences among three N fertilizer levels. Without urea incorporation, there are no differences among N2O accumulation emission flux of three soils. During the rice growing season, N2O accumulation emission flux of F soil (jiangsu province, lishui), G soil (jiangsu province, lianshui) and H soil (jiangsu province, agriculture academy) are 168, 127 and 146 mg/m2,respectively. N2O accumulation emission flux of F soil, G soil and H soil is 134, 124 and 168 mg/m2, respectively, during wheat growing season. Incorporation of urea into different soils yielded different influence on N2O emission. For example, at middle-N fertilizer, N2O accumulation emission flux from F soil, G soil and H soil is 976, 744 and 626 mg/m2,respectively. During rice-wheat rotation period, significance differences exists among N2O emission factors of three soils, with the value of (1.1±0.23)%, (0.75±0.17%) and (1.01±0.11)%. Furthermore, under the high N fertilizer level, N2O emission factors of three soils had no significantly difference(p=0.3); while, the N2O emission factors existed difference among three soils under the low and middle N fertilizer level(F=6.25,p=0.01).

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