• ISSN 1008-505X
  • CN 11-3996/S
陈明昌, 张强, 杨晋玲, 潘大丰, 张藕珠. 田间土壤氮素形态转化模拟模型的研究[J]. 植物营养与肥料学报, 1996, 2(3): 261-269. DOI: 10.11674/zwyf.1996.0312
引用本文: 陈明昌, 张强, 杨晋玲, 潘大丰, 张藕珠. 田间土壤氮素形态转化模拟模型的研究[J]. 植物营养与肥料学报, 1996, 2(3): 261-269. DOI: 10.11674/zwyf.1996.0312
Chen Mingchang Zhang Qiang Yang Jinling Pan Dafeng Zhang Ouzhu, . SIMULATION MODEL AND ITS APPLICATION OF NITROGEN BEHAVIOR AND CYCLING UNDER FIELD CONDITIONS[J]. Journal of Plant Nutrition and Fertilizers, 1996, 2(3): 261-269. DOI: 10.11674/zwyf.1996.0312
Citation: Chen Mingchang Zhang Qiang Yang Jinling Pan Dafeng Zhang Ouzhu, . SIMULATION MODEL AND ITS APPLICATION OF NITROGEN BEHAVIOR AND CYCLING UNDER FIELD CONDITIONS[J]. Journal of Plant Nutrition and Fertilizers, 1996, 2(3): 261-269. DOI: 10.11674/zwyf.1996.0312

田间土壤氮素形态转化模拟模型的研究

SIMULATION MODEL AND ITS APPLICATION OF NITROGEN BEHAVIOR AND CYCLING UNDER FIELD CONDITIONS

  • 摘要: 本文重点讨论了田间条件下土壤氮素形态转化计算机模拟模型的基本结构。该模型是在借鉴国内外较成功模型的基础上,通过修正和重新组装而提出的。所涉及的主要氮素行为有:矿化、固定、反硝化、硝态氮的径流和淋洗等。通过三年的冬小麦田间试验对该模型的验证结果表明,冬小麦收获时经济产量、子粒氮含量、土壤含水量、地上部累积干物质量、冬小麦一大豆轮作周期内0~90cm土层硝态氮含量和冬小麦生育期体内氮浓度的模拟结果与实际田间测定结果之间没有明显差异。所建立的田间土壤氮素形态转化计算机模型基本适合我国北干旱和半干旱地区石灰性土壤,这对今后研究氮素在土壤作物环境中的转移和氮肥的合理施用具有重要的意义。

     

    Abstract: A simulation model of nitrogen behavior and cycling in soil-plant systems was discussed. This model was developed based on the home and foreign successful models of nitrogen behavior in soil-plant systems, and amended and repackaged for fitting in with the local specific conditions. Some processes of nitrogen were included such as mineralization/immobilization, denitrification, nitrate loss in surface runoff, and nitrate leaching in this model. It was validated by using the results of field trials on winter wheat for three years. There was agreement within the measured and simulated values of grain dry weight, %N in the grain, nitrate and water in 0-90cm depth of soils, total biomass and %N in the above ground parts of plant. Research results indicated that the simulation model can be used to predicting the nitrogen behavior of calcareous soils in arid and semiarid area of china.

     

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