• ISSN 1008-505X
  • CN 11-3996/S

长期施用不同有机肥调节黄泥田土壤团聚体氮矿化的效应

Effects of different organic fertilizers on regulating nitrogen mineralization of soil aggregates in yellow-mud paddy field

  • 摘要:
    目的 有机氮矿化过程对土壤供氮和作物氮素利用至关重要。黄泥田是南方重要的中低产水稻土类型,其氮素供应特征直接影响水稻产量。本研究旨在揭示施肥管理对土壤氮素供应的调控机制,为优化施肥策略提供科学依据。
    方法 以黄泥田36年长期定位试验耕层土壤为研究对象,采集其中不施肥(CK)、单施化肥(NPK)、化肥+牛粪(NPKM)、化肥+全量稻秸还田(NPKS)4个处理小区的耕层土壤样品,采用湿筛法筛选>2 mm和0.25—2 mm土壤团聚体,然后以原状土和两个团聚体为材料进行间歇淹水密闭培养实验,测定分析各粒级团聚体中有机氮的矿化量、矿化速率和矿化势,共培养161天。
    结果 与CK相比,NPK、NPKM和NPKS处理增加了各粒级团聚体的氮矿化累积量,培养161 d后,各施肥处理的原状土、>2 mm团聚体、0.25—2 mm团聚体氮矿化累积量分别增加了10.7%~58.3%、7.1%~49.4%和36.6%~50.1%。NPKM和NPKS处理的原状土和>2 mm团聚体的氮矿化累积量显著高于NPK处理,氮矿化势显著高于CK和NPK处理。各施肥处理的>2 mm团聚体的有机氮矿化势比0.25—2 mm团聚体提高30.6%~244.8%;0.25—2 mm团聚体矿化速率常数比>2 mm团聚体提高58.7%~71.2% (NPKS除外)。总体而言,>2 mm团聚体矿化势高于0.25—2 mm团聚体,而矿化速率常数相反。各粒级团聚体氮矿化累积量和矿化势与全氮、碱解氮、有机碳、微生物量氮呈显著正相关,原状土和>2 mm团聚体氮矿化累积量和矿化势与容重呈显著负相关。
    结论 >2 mm团聚体氮决定土壤氮的供应容量,0.25—2 mm土壤团聚体主要影响土壤氮的供应强度。牛粪、秸秆与化肥长期配施军可有效提升大团聚体氮库和微生物活性,显著提升黄泥田土壤氮矿化潜力,其中施用牛粪效果优于秸秆还田。牛粪与化肥配合还可促进0.25—2 mm团聚体有机碳的矿化速率,提升土壤的供氮能力,因此,牛粪和化肥配合更有效地协调低产黄泥田土壤的氮素供应潜力和供应强度。

     

    Abstract:
    Objective Organic nitrogen mineralization process plays crutial role in derterming soil nitrogen supply capacity and crop nitrogen use efficiency. We investigated the effect of common used organic fertilizer sources on the nitrogen mineralization of soil aggregates in yellow mud field, aiming to reveal the regulation mechanism of them on regulating soil nitrogen supply.
    Methods The soil samples were collected from the plots subjected to a 36 years of positioning experiment in a yellow mud field. The treatments included: no fertilization control (CK), single application of chemical fertilizer (NPK), chemical fertilizer plus cow dung (NPKM), and chemical fertilizer plus total rice straw returning (NPKS). The wet screening method was used to screen soil aggregate in sizes of >2 mm and 0.25−2 mm. Then the aggregates were incubated in darkness for 161 days, during which the total N, available N, microbial mass nitrogen content were analyzed regularly.
    Results Compared with CK, all the NPK, NPKM and NPKS treatments increased the cumulative nitrogen mineralization of soil, the increments in the bulk soil, >2 aggregates, and 0.25−2 mm aggregates by were 10.7%−58.3%, 7.1%−49.4%, and 36.6%−50.1%, respectively. The cumulative nitrogen mineralization of bulk soils and >2 mm aggregates in NPKM and NPKS treatments were significantly higher than that of NPK treatment, and the nitrogen mineralization potential were significantly higher than that under CK and NPK treatment. The nitrogen mineralization potential of >2 mm aggregates under each fertilization treatment was significantly higher than that of 0.25-2 mm aggregates, but the mineralization rate constant, except for NPKS treatment, was the opposite. The nitrogen mineralization accumulation and mineralization potential of all aggregates were positively correlated with total N, alkali-hydrolyzed N, organic carbon and microbial biomass nitrogen (P<0.05), while the nitrogen mineralization accumulation and mineralization potential of undisturbed soil and >2 mm aggregates were negatively correlated with bulk density (P<0.05).
    Conclusions Organic nitrogen in >2 mm aggregates is pivotal to soil nitrogen pool, and that in 0.25−2 mm aggregates influences soil nitrogen supply capacity. Long-term combined application of chemical fertilizers with caw manure and straw could significantly enhance the nitrogen mineralization potential of both >2 mm and 0.25−2 mm aggregates in yellow-mud paddy soil by increased nitrogen pools and microbial activity, with cattle manure being more effective than straw. Caw manure also shows effects on steep up the mineralization rate of 0.25−2 mm aggregates, showing higher nitrogen supply capacity than straw. So caw manure and chemical fertilizer is more effective in regulating the accumulation and supply potential of soil nitrogen in the low fertility yellow-mud field.

     

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