双氰胺对设施蔬菜地N2O和CO2排放的影响及其驱动因素

Effects of dicyandiamide on N2O and CO2 emissions and the underlying driving factors in greenhouse vegetable fields

  • 摘要: 设施蔬菜种植因过量氮肥投入加剧了土壤碳氮迁移转化, 驱动N2O和CO2等温室气体产生和排放, 影响全球气候变化。施用硝化抑制剂作为减缓氮转化损失和温室气体排放的重要措施被广泛应用。为探究硝化抑制剂双氰胺(DCD)施用对设施蔬菜地N2O和CO2排放的影响及其关键驱动因素, 本研究通过湖南省长沙农业与环境监测站的设施蔬菜种植定位试验, 设置施用常规化学氮肥(CK)和化学氮肥配施DCD两种处理, 定期监测蔬菜全生育期N2O和CO2排放通量及土壤理化性质。研究结果表明, 与CK处理相比, DCD施用显著降低了蔬菜种植初期(0~53 d) N2O排放通量(P<0.05), 但在后期(54~163 d)两处理无显著差异; DCD处理的全生育期N2O累积排放量为0.94 kg(N)∙hm−2, 比CK处理显著降低了21.67% (P<0.05)。与N2O排放不同, DCD施用对CO2排放通量及其累积排放量累积排放量DCD处理为1 778.79 kg(C)∙hm−2, CK处理为1 731.02 kg(C)∙hm−2均无显著影响显著。在全生育期内, DCD施用对设施蔬菜地土壤温度和充水孔隙度(WFPS)无显著影响, 但显著增加了土壤铵态氮(NH4+-N)含量(P<0.05), 降低了硝态氮(NO3-N)含量(P<0.05)。随机森林结果显示, 土壤WFPS、NH4+-N和NO3-N含量及温度是设施蔬菜地N2O排放通量季节性波动的主要控制因素, 解释了其变异的27%; CO2排放季节性动态与土壤温度显著正相关(R2=0.51, P<0.05)。回归分析结果也表明, N2O排放通量与NH4+-N和NO3-N含量显著正相关(P<0.05), 说明DCD施用通过抑制硝化过程减少NO3-N积累, 降低N2O排放。本研究阐明了DCD在施用初期通过减少NO3-N含量降低了N2O排放, 而对CO2排放过程无显著影响。DCD在施用初期通过调控氮素形态减缓N2O排放, 为设施农业温室气体减排提供理论依据。

     

    Abstract: Excessive nitrogen fertilizer inputs in greenhouse vegetable field intensify soil carbon and nitrogen migration and transformation, and drive the production and emissions of greenhouse gases nitrous oxide (N2O) and carbon dioxide (CO2), thus contributing to global climate change. Nitrification inhibitors (such as dicyandiamide, DCD) are widely utilized as a crucial measure to alleviate nitrogen losses and greenhouse gas emissions. Herein, a experiment was conducted out at the Changsha Agricultural and Environmental Monitoring Station in Hunan Province to explore the impacts of DCD on N2O and CO2 emissions and their key environmental drivers in greenhouse vegetable field located at the Changsha Agricultural and Environmental Monitoring Station in Hunan Province. Two treatments were established, conventional chemical nitrogen fertilization (CK) and chemical nitrogen fertilization combined with dicyandiamide (DCD), Throughout the entire growth period of vegetables, the emission fluxes of N2O and CO2, as well as soil physicochemical properties, were monitored regularly. The results showed that compared with the CK treatment, DCD application significantly reduced N2O flux during the early stage of vegetable planting (0–53 days)(P<0.05). but there was no significant difference between the two treatments during the later stage (54–163 days). The overall cumulative N2O emission during the whole growth period under the DCD treatment was 0.94 kg (N)·hm−2, which was significantly 21.67% lower than that under the CK treatment (P < 0.05). Different from N2O emission, DCD application had no significant effect on the CO2 fluxes and its cumulative emission the cumulative emissions were 1,778.79 and 1,731.02 kg(C)∙hm−2 under the DCD and CK treatment, respectively. Throughout the entire growth period, the DCD application did not significantly alter soil temperature and water-filled pore space (WFPS) in greenhouse vegetable fields, but significantly increased soil ammonium nitrogen (NH4+-N) content (P < 0.05) and decreasing soil nitrate nitrogen (NO3-N) content (P < 0.05) . Random forest results showed that soil WFPS, NH4+-N, NO3-N and temperature were the main controlling factors for the seasonal fluctuation of N2O fluxes in greenhouse vegetable fields, explaining 27% of its variation. The seasonal dynamics of CO2 emissions had a significant positive correlation with soil temperature (R2=0.51,P < 0.05) .Regression analysis also indicated that the N2O fluxes were significantly positively correlated with both NH4+-N and NO3-N contents (P < 0.05) , suggesting that DCD application reduced N2O emissions by inhibiting the nitrification process and thus decreasing NO3-N accumulation This study clarified that DCD reduced N2O emissions in the early stage of application by decreasing NO3-N content, while having no significant effect on the CO2 fluxes. DCD mitigates N2O emission by regulating nitrogen forms in the early stage of application, providing a theoretical basis for greenhouse gas emission reduction in facility agriculture.

     

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