• ISSN 1008-505X
  • CN 11-3996/S
曹良元, 张磊, 蒋先军, 苏海锋, 石杰, 李楠. 长期垄作免耕对不同大小土壤团聚体中几种氮素形态分布的影响[J]. 植物营养与肥料学报, 2009, 15(4): 824-830. DOI: 10.11674/zwyf.2009.0413
引用本文: 曹良元, 张磊, 蒋先军, 苏海锋, 石杰, 李楠. 长期垄作免耕对不同大小土壤团聚体中几种氮素形态分布的影响[J]. 植物营养与肥料学报, 2009, 15(4): 824-830. DOI: 10.11674/zwyf.2009.0413
CAO Liang-yuan, ZHANG Lei, JIANG Xian-jun, SU Hai-feng, SHI Jie, LI Nan. Effects of long-term ridge tillage on distributions of different nitrogen forms of soil water stable aggregates[J]. Journal of Plant Nutrition and Fertilizers, 2009, 15(4): 824-830. DOI: 10.11674/zwyf.2009.0413
Citation: CAO Liang-yuan, ZHANG Lei, JIANG Xian-jun, SU Hai-feng, SHI Jie, LI Nan. Effects of long-term ridge tillage on distributions of different nitrogen forms of soil water stable aggregates[J]. Journal of Plant Nutrition and Fertilizers, 2009, 15(4): 824-830. DOI: 10.11674/zwyf.2009.0413

长期垄作免耕对不同大小土壤团聚体中几种氮素形态分布的影响

Effects of long-term ridge tillage on distributions of different nitrogen forms of soil water stable aggregates

  • 摘要: 在西南大学国家紫色土肥力定位监测点,研究了长期(18年)垄作免耕和常规轮作两种耕作方式下,不同大小土壤团聚体中几种形态氮素含量及脲酶活性分布模式。结果表明,两种轮作方式下全氮、微生物体氮、NO3--N含量及脲酶活性在水稳性土壤团聚体中具有相似的分布模式。全氮和微生物体氮含量主要分布在 0.25 mm粒级的大团聚体中,其次是0.25~0.053 mm粒级的微团聚体中,粉砂与粘粒组分(0.053 mm)中分布最少;2.0~0.25 mm粒级团聚体中脲酶活性最高,0.25~0.053 mm的微团聚体中脲酶活性最低;NH4+-N和NO3-N在2.0 mm粒级团聚体中的含量均比其它粒级高。垄作免耕下各级团聚体中全氮、微生物体氮、NO3--N含量及脲酶活性均高于常规轮作。其中,2.0~0.25 mm粒级团聚体中的全氮含量高23.1%;2.0 mm粒级团聚体中NO3--N含量高26.7%。表明垄作免耕下各团聚体中全氮、微生物氮含量及脲酶活性显著高于常规轮作,但氮素含量及脲酶活性在不同粒径大小的土壤水稳性团聚体中的分布模式决定于土壤结构体本身,耕作方式的影响不显著。

     

    Abstract: Soil aggregates are the most important structures, and different sizes of aggregates have different functions in maintaining, supplying and transforming nutrients. A 18-year long-term field experiment was carried out to study distributions of nitrogen forms and urease activities of soil aggregates under conventional tillage (CT) and ridge tillage (RT) practices. The results show that there are similar distribution patterns of total nitrogen, microbial nitrogen, NO3--N and urease activities in soil water stable aggregates under CT and RT. Total nitrogen and microbial nitrogen are mainly distributed in soil aggregate whose size is large than 0.25 mm, followed by those in the 0.25–0.053 mm aggregate, and those in the silt and clay component (0.053 mm) are the least. Urease activities are the highest in the size of 2.0–0.25 mm aggregate, and are the least in the size of 0.25–0.053 mm aggregate. NH4+-N and NO3--N concentrations are the highest in the size of larger than 2.0 mm aggregate. Total nitrogen, microbial nitrogen, NO3--N and urease activities under RT are higher than those under CT. For instance, total nitrogen concentration within 2.0–0.25 mm aggregate under RT is 23.1% higher than that under CT, NO3--N in the size of larger than 2.0 mm aggregate is 26.7% higher under RT than that under CT. In conclusion, total nitrogen, microbial itrogen concentrations and rease activities in different sizes of aggregates under RT are significantly higher than those under CT, the distribution patterns of nitrogen concentrations and urease activities are dependent on the structures of aggregates, while tillage methods had no significant effects on them.

     

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