• ISSN 1008-505X
  • CN 11-3996/S

长期施用不同有机肥对黄泥田土壤团聚体氮矿化的调控效应

Regulation of soil aggregate nitrogen mineralization by long-term application of various organic fertilizers in yellow muddy fields

  • 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和0.25~2 mm土壤团聚体,然后以原状土和两种团聚体为材料,进行161天的间歇淹水密闭培养试验,测定各粒级团聚体的有机氮矿化量、矿化速率和矿化势。
    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天后,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>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团聚体的矿化速率常数比>2 mm团聚体高58.7%~71.2% (NPKS除外)。总体而言,>2 mm团聚体的矿化势高于0.25~2 mm团聚体,而矿化速率常数相反。各粒级团聚体的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团聚体的氮矿化累积量和矿化势与容重呈显著负相关。
    结论 >2 mm团聚体决定土壤氮供应容量,0.25~2 mm土壤团聚体主要影响土壤氮供应强度。长期施用牛粪或秸秆与化肥配施均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。牛粪与化肥配施还可提高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,牛粪和化肥配施是协调低产黄泥田土壤氮素供应潜力和强度的有效措施。

     

    Abstract:
    Objectives Organic nitrogen mineralization process plays a crucial role in derterming soil nitrogen supply capacity and crop nitrogen use efficiency. We investigated the effect of commonly used organic fertilizer sources on nitrogen mineralization in soil aggregates of yellow mud fields, aiming to reveal their regulatory mechanisms on soil nitrogen supply.
    Methods Soil samples were collected from a 36 years long-term experiment in a yellow mud field. The treatments included: no fertilization control (CK), application of chemical fertilizer alone (NPK), chemical fertilizer plus cow manure (NPKM), and chemical fertilizer plus full rice straw return (NPKS). The wet sieving method was used to separate soil aggregate in sizes of >2 mm and 0.25−2 mm. Then the aggregates were incubated in darkness for 161 days. During incubation, total N, available N, microbial biomass nitrogen content were analyzed periodically.
    Results Compared with CK, the NPK, NPKM and NPKS treatments increased cumulative nitrogen mineralization by 10.7%–58.3% in bulk soil, 7.1%–49.4% in >2 mm aggregates, and 36.6%–50.1% in 0.25–2 mm aggregates. The cumulative nitrogen mineralization in bulk soils and >2 mm aggregates under NPKM and NPKS treatments were significantly higher than that under NPK treatment, and the nitrogen mineralization potential were significantly higher under NPKM and NPKS treatments than that under CK and NPK treatment. The nitrogen mineralization potentials in >2 mm aggregates under each fertilization treatment were significantly higher than that in 0.25−2 mm aggregates, but the mineralization rate constant showed the opposite trend, except under NPKS treatment. 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 the soil nitrogen pool, and that in 0.25−2 mm aggregates influences soil nitrogen supply capacity. Long-term combined application of chemical fertilizers with cow 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 increasing nitrogen pools and microbial activity, with cow manure showing stronger effects than straw. Cow manure also shows effects on steep up the mineralization rate of 0.25−2 mm aggregates, showing higher nitrogen supply capacity than straw. So cow manure and chemical fertilizer is more effective in regulating the accumulation and supply potential of soil nitrogen in the low-fertility yellow-mud field.

     

/

返回文章
返回