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应用生态学报 ›› 1997, Vol. 8 ›› Issue (1): 49-54.

• 研究论文 • 上一篇    下一篇

田间非饱和流条件下土壤硝态氮运移的模拟

崔剑波, 庄季屏   

  1. 中国科学院沈阳应用生态研究所, 沈阳 110015
  • 收稿日期:1996-10-15 修回日期:1996-11-18 出版日期:1997-01-25 发布日期:1997-01-25
  • 基金资助:

    国家“九五”科技攻关项目

Soil NO3--N transport under field unsaturated flow condition——a simulation study

Cui Jianbo, Zhuang Jiping   

  1. Institute of Applied Ecology, Academia Sinica, Shenyang 110015
  • Received:1996-10-15 Revised:1996-11-18 Online:1997-01-25 Published:1997-01-25

摘要: 运用马尔可夫过程的理论,建立了土壤非饱和流条件下,模拟硝态氮通过土层运移的随机模型.模型把时间可变系统假设为由紧密相连的时间均质情况相接而成,使得运用马尔可夫过程成为可能,在给定土壤水流量及汇源项转移强度的土壤层次中,给出了硝态氮溶质的统计分布.模型将随机过程与确定性过程相结合,在计算各土层间的转移概率时考虑了硝态氮的作物吸收、淋洗、硝化和反硝化等主要过程,并用相关函数修正N素转化关系.在褐土农田土壤非饱和流条件下,用微区试验对该模型运行效果进行了验证,结果显示模拟计算值与实测值之间吻合性较好,说明模型可以用于相似类型区,预测和评价土壤-作物系统中硝态氮溶质的运移行为.

关键词: 田间条件, 土壤非饱和流, 硝态氮, 溶质运移, 细根分解, 马尾松, 养分

Abstract: Based on the theory of Markov Process, a stochastic model is established to simulate the interlayer transport of NO3--N in a cinnamon soil with unsaturated water flow. This model converts the temporally variable system into a system closely resembles the time homogeneous case, and makes Markov Process model applicable. The probability distribution of NO3--N is given for each soil layer under a given soil water flow and a given transport intensity of source and sink. In calculating the transport probability from one soil layer to another one, the main processes of NO3--N uptake and its leaching, nitrification and denitrification are considered, and the relationship between N transformations is calibrated with correlation function. Amicro plot experiment on NO3--N transport is installed to verify the results obtained from simulation study, which shows a satisfactory agreement between measured and simulated results, indicading that the model can be used in similar areas to predict and evaluate the behavior of NO3--N transport in soil crop system.

Key words: Field condition, Unsaturated soil waterflow, Nitrate nitrogen, Solute transport, fine root decomposition, Pinus massoniana, nutrient