黄河上游灌区稻田N2O排放特征
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宁夏职业技术学院,中国农业科学院 农业环境与可持续发展研究所,中国农业科学院农业环境与可持续发展研究所 北京,中国农业科学院农业环境与可持续发展研究所 北京,中国农业科学院农业环境与可持续发展研究所 北京,中国农业科学院农业环境与可持续发展研究所,中国农业科学院农业环境与可持续发展研究所,中国农业科学院农业环境与可持续发展研究所,中国农业科学院农业环境与可持续发展研究所

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中国-欧盟科技合作项目(S2010GR0977); 国家科技重大专项资助(No.2009ZX07212-004)


The feature of N2O emission from a paddy field in irrigation area of the Yellow River
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Ningxia Vocational and Technical College,Institute of Environment and Sustainable Development in Agriculture, CAAS Beijing,Institute of Environment and Sustainable Development in Agriculture, CAAS Beijing,,,,,

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    摘要:

    黄河上游灌区稻田高产区过量施肥现象十分突出,氮肥过量施用引起土壤氮素盈余,导致N2O排放量增大,由此引起的温室效应引起广泛关注。采用静态箱-气相色谱法研究黄河上游灌区稻田不同施肥处理下N2O排放特征。试验设置5个施肥处理,包括常规氮肥300 kg/hm2下单施尿素和有机肥配施2个处理,分别用N300和N300-OM代表;优化氮肥240 kg/hm2下单施尿素和有机肥配施2个处理,分别用N240和N240-OM代表;对照不施氮肥用N0代表。试验结果得出,灌区水稻生长季稻田土壤N2O排放主要集中在水稻分蘖前及水稻生长的中后期,稻田氮肥施用、灌水及土壤温度的变化对N2O排放通量影响较大,不同处理水稻各生育阶段N2O累积排放量与稻田土壤耕层NO-3-N含量动态变化显著相关。稻田N2O排放不是黄河上游灌区稻田氮素损失的主要途径,但灌区稻田N2O排放的增温潜势较大;稻田氮肥过量施用会显著增加N2O排放量,在相同氮素水平下,有机肥配施会显著增加稻田土壤N2O的排放量(P<0.01)。优化施氮能有效减少灌区稻田水稻生长季N2O排放量。稻田不同处理的水稻整个生长季土壤N2O排放总量为2.69-3.87 kg/hm2,肥料氮通过N2O排放损失的百分率仅为0.43%-0.64%。在灌区习惯灌水和高氮肥300 kg/hm2时,N300-OM处理的稻田N2O排放量达3.87 kg/hm2,在100 a时间尺度上的全球增温潜势(GWPs)为20.76×107 kg CO2/hm2;优化施氮240 kg/hm2水平下,N240和N240-OM处理的N2O累计排放量较N300-OM处理,分别降低了1.18 kg/hm2和0.57 kg/hm2,在100 a尺度上每年由稻田N2O排放引起的GWPs分别降低了6.33×107 kg CO2/hm2和3.06×107 kg CO2/hm2

    Abstract:

    Input of nitrogen (N) is essential for high crop yields, but excessive application of N fertilizer increased the loss of gaseous nitrogen. Gaseous loss of N is a main way of nitrogen loss in the paddy fields of the irrigation area. The static chamber-gas chromatograph method was used to measure the N2O emission from the paddy field. The five N treatments of field experiment were conducted, including two treatments of the conventional N application rate (300 kg/hm2), i.e the application of only urea (N300) and the application of the organic fertilizer (manure) with the urea nitrogen (N300-OM); two treatments of the optimized N application rate (240 kg/hm2), i.e, the application of only urea (N240) and the application of the organic fertilizer (manure) with the urea nitrogen (N240-OM), and no N fertilizer application plot (CK).
    The results showed that N2O emissions mainly occurred before the tiller stage or at the pre- and late- rice growth stages, and more N2O emissions were measured after rice planting and irrigation. At different nitrogen levels, the total amount of N2O emissions during the whole rice growing season varied among 2.69-3.87kg/hm2, and the loss of fertilizer N due to N2O emissions was only 0.43%-0.64%. N2O emissions from the paddy field is not an important way of nitrogen loss at the Yellow River irrigation area, but the warming potential through N2O emissions in the irrigation area is not neglectable. Excessive application of nitrogen fertilizer in the paddy field significantly increased N2O emissions, and at the same level of nitrogen application, organic fertilizer amendment increased N2O emissions from the paddy soil (P<0.01). Optimization of nitrogen application in the irrigated paddy field during the rice growing season reduced N2O emissions. With the conventional irrigation practice, N2O emissions from paddy fields in N300-OM treatment reached 3.87kg/hm2. In the scales of 100a, the global warming potentials (GWPs) were 20.76×107 kg CO2/hm2. Optimization of N application in the irrigated paddy field during the rice growing season reduced N2O emissions. Compared with N300-OM treatment, cumulative N2O emissions in N240 and N240-OM treatments decreased by 1.18 kg/hm2 and 0.57 kg/hm2, respectively. In the scales of 100a, GWPs caused by N2O emissions in the paddy field decreased 6.33×107 kg CO2/hm2 and 3.06×107 kg CO2/hm2, respectively.

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张惠,杨正礼,罗良国,张晴雯,易军,杨世琦,陈媛媛,王明.黄河上游灌区稻田N2O排放特征.生态学报,2011,31(21):6606~6615

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