不同沟灌方式下玉米根区矿物氮迁移动态研究

Transfer of mineral nitrogen in maize root zone soil under different furrow irrigation modes

  • 摘要: 为探索交替隔沟灌溉下玉米根区矿物氮分布规律, 通过遮雨棚内微区试验, 研究了常规沟灌、交替隔沟灌和固定隔沟灌3 种沟灌方式对玉米根区硝态氮、铵态氮迁移的影响。结果表明: 交替隔沟灌溉根区硝态氮等值线和常规沟灌相似, 沟内硝态氮含量基本沿垄的中心对称分布。固定隔沟灌溉的湿润沟内硝态氮含量小于干燥沟, 施氮后非灌水沟硝态氮保持较高水平。收获时交替隔沟灌溉的根区硝态氮残留量比常规灌溉略高。与硝态氮分布相比, 铵态氮在根区土壤中的含量很小, 3 种沟灌方式在沟和垄中的铵态氮含量没有明显差异。

     

    Abstract: The objective of this study was to explore the distribution of mineral nitrogen in maize root zone soils under alternative furrow irrigation. To that end, micro-field rain-shield experiments were conducted to determine the effects of three different furrow irrigation modes conventional furrow irrigation (CFI), alternative furrow irrigation (AFI) and fixed furrow irrigation (FFI) on NO3--N and NH4+-N transfer in maize root zone soils. Results showed that NO3--N content in AFI root zone soils was similar to that in CFI. Also NO3--N in furrow profile occurred along centre line ridge symmetry. Under FFI, NO3--N content in wet furrow was less than that in dry furrow. The content in dry furrow steadily increased after fertilization. At harvest, NO3--N residue in AFI was slightly higher than that in CFI. Compared with NO3--N, NH4+-N content was very little. There was no significant difference in furrow and ridge in terms of NO3--N and NH4+-N content.

     

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