摘要
利用一个长达30年的水稻土长期定位试验,在保证原有定位试验继续正常开展的前提下变更部分施肥处理,得到继续施用高量有机肥(HOM)、施用常量有机肥30年后改施高量有机肥(N-H)、继续施用常量有机肥(NOM)、施用化肥30年后改施常量有机肥(C-N)、施用高量有机肥30年后改施化肥(H-C)、施用常量有机肥30年后改施化肥(N-C)、继续施用化肥(CF)等7种施肥处理,观测2013~2014年双季稻轮作周期内原有施肥和变更施肥处理后对土体N2O排放的影响。结果表明:NOM改为N-C和HOM改为H-C处理,与变更前相比,周年N2O排放的全球增温潜势估算分别提高了7.9%和4.7%,而NOM改为N-H和CF改为C-N处理,周年N2O排放的全球增温潜势估算分别降低了8.2%和4.1%。
Seven treatments were set based a 30 - year fertilization experiment in paddy soil, the original high organic mate- rial treatment ( HOM), the high organic material treatment reformed from the original normal organic material treatment ( N -H), the original normal organic material treatment (NOM), the normal organic material treatment reformed from the o- riginal chemical fertilizer treatment ( C - N ), the chemical fertilizer treatment reformed from the original high organic mate- rial treatment (H -C) and the chemical fertilizer treatment reformed from the original normal organic material treatment ( N - C) ,the original chemical fertilizer treatment (CF) ,and the N20 flux from the original and changed treatments during double rice cropping rotation cycle in 2013 -2014 was measured. The results showed that:global warming potential esti- mates of annual N20 emissions in the N - C and H - C was increased by 7. 9% and 4. 7% compared with NOM and HOM,respectively,while that in the N - H and C - N was decreased by 8.2% and 4. 1% compared with NOM and CF,respectivcly.
出处
《作物研究》
2015年第3期272-276,共5页
Crop Research
基金
国家自然科学基金(41371250)
湖南省研究生科研创新项目(CX2012B287)
关键词
红壤性水稻土
施肥
氧化亚氮
有机肥
化肥
paddy soil from red soil
fertilization
N2O
organic fertilizer
chemical fertilizer