• ISSN 1008-505X
  • CN 11-3996/S

双氰胺对肥料氮去向的影响依赖于土壤类型

The influence of dicyandiamide on the fate of fertilizer nitrogen depends on soil types

  • 摘要:
    目的 不同类型土壤硝化作用存在差异,研究硝化抑制剂双氰胺(DCD)对不同类型土壤中肥料氮去向和作物氮肥利用率的影响,以期为DCD在玉米氮肥管理中的应用提供理论依据。
    方法 土柱淋溶试验选择了3种典型土壤:红壤、黑土、潮土,以15N标记尿素为供试肥料,设计施用DCD和不施用DCD (施用量为尿素氮用量的10%)两个处理。在玉米播种后的第10、17、22、26、31、36、46天进行淋溶试验,收集淋溶液,用重量法测量其体积,测定淋溶液中的铵态氮和硝态氮含量。玉米在播种后57天收获,分为地上部和根部,分别测定生物量和氮含量;将土柱中的土壤混匀后,测定铵态氮和硝态氮含量,以及15N同位素丰度。
    结果 不论是否添加DCD,3种土壤的氮素淋溶随时间的动态变化趋势基本一致,铵态氮、硝态氮和全氮的淋溶主要集中在前3次,且均在第一次淋溶最高,随后快速下降至较低水平,而尿素态氮主要集中在第一次淋溶。DCD降低了3种土壤硝态氮淋溶(N 0.74~5.76 mg/kg土),对红壤的降低效果最小;增加了红壤和潮土的铵态氮淋溶,增量以潮土最多(N 2.99 mg/kg土)。DCD减少氮淋溶的效果与3种土壤的硝化作用强弱一致,即黑土>潮土>红壤。DCD降低了黑土和潮土中肥料氮的淋失率,提高了肥料氮的土壤残留率,但DCD增加了红壤的肥料氮淋失率。DCD抑制了红壤和黑土的气态氮损失,增加了潮土的气态氮损失,这可能是因为DCD导致铵态氮在潮土积累,潮土pH (8.18)较高,易产生氨挥发损失。DCD显著提高了3种土壤上玉米的氮肥利用率(增幅为3.90%~5.77%),其中以黑土提升幅度最高,但仅提高了潮土上玉米生物量。与潮土和红壤相比,黑土具有较高的玉米氮肥利用率、较低的氮淋失率和气态氮损失率。
    结论 施用DCD对玉米生长、氮肥利用率和肥料氮去向的作用效果因土壤类型而异,主要与土壤性质有关。黑土和潮土硝化作用强,施用DCD降低肥料氮的淋失率,提高肥料氮土壤残留率的效果较好,而在红壤上效果较差。施用DCD显著抑制了红壤和黑土的气态氮损失,但是却增加了潮土的气态氮损失,这可能因为潮土pH较高,DCD导致铵态氮在潮土积累而引起更多的氨挥发。

     

    Abstract:
    Objectives Given that the efficacy of DCD varies in different soils, we studied the precise efficacy of nitrification inhibitor dicyandiamide (DCD) on maize growth, fertilizer nitrogen (N) recovery efficiency, and the N fate in different soil types, to establish a theoretical foundation for the scientific application of DCD in maize N management.
    Methods A soil column leaching experiment was carried out using 15N-labeled urea. The columns were filled with one of the three soil types (red soil, black soil, and fluvo-aquic soil), and DCD was applied at 10% of the urea N application rate or omitted as a control. Water (100 mL) was added to the soil at the 10, 17, 22, 26, 31, 36, and 46 days post-sowing of maize to collect leachate for the measurement of ammonium and nitrate N. After 57 days, the maize plants were harvested to determine their yield and N content in both the aboveground parts and roots. Additionally, the ammonium- and nitrate-N content in the residual soil was measured.
    Results Regardless of DCD application, the N leaching patterns in all three soils exhibited similar temporal trends. The majority of ammonium N, nitrate N, and total N leaching occurred during the initial three leaching events, peaking during the first event and then declining rapidly thereafter. Urea N leaching was primarily concentrated in the first leaching event. DCD reduced nitrate leaching by N 0.74 to N 5.76 mg/kg soil across all three soils, with the smallest reduction observed in red soil. While DCD had no significant effect on urea leaching, it increased ammonium leaching in red and fluvo-aquic soils, with the highest increment in fluvo-aquic soil (N 2.99 mg/kg soil). The effectiveness of DCD in reducing N leaching was correlated with the soil’s nitrification capacity, following the order black soil>fluvo-aquic soil>red soil. DCD effectively minimized fertilizer N leaching and enhanced soil N retention in black and fluvo-aquic soils, but had no significant impact on red soil and even increased the fertilizer N leaching rate therein. DCD significantly inhibited gaseous N loss in red and black soils but increased it in fluvo-aquic soil. Across all three soils, DCD improved fertilizer N recovery efficiency for maize, with the greatest improvement observed in black soil. However, DCD only increased maize biomass in fluvo-aquic soil. Compared to fluvo-aquic and red soils, black soil exhibited higher maize fertilizer N recovery efficiency, lower N leaching, and lower gaseous N losses, attributed to its favorable soil conditions for optimal maize growth and minimal fertilizer N loss.
    Conclusion The effects of applying DCD on maize growth, N fertilizer use efficiency, and the fate of fertilizer N vary among soil types, primarily due to soil properties. Black soil and fluvo-aquic soil exhibit strong nitrification, so the application of DCD is more effective in reducing the leaching loss rate of fertilizer N and increasing the soil residual rate of fertilizer N, whereas its effectiveness is poorer in red soil. The application of DCD significantly inhibits gaseous N losses in red soil and black soil but increases gaseous N losses in fluvo-aquic soil. This may be attributed to the higher pH of fluvo-aquic soil, where DCD leads to the accumulation of ammonium-N, potentially causing increased ammonia volatilization.

     

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