中国农业科学 ›› 2009, Vol. 42 ›› Issue (3): 918-925 .doi: 10.3864/j.issn.0578-1752.2009.03.021

• 土壤肥料·节水灌溉·农业生态环境 • 上一篇    下一篇

小麦氮磷肥长期配施对土壤硝态氮淋溶的影响

  

  1. 中国科学院水土保持与生态环境研究中心
  • 收稿日期:2008-06-02 修回日期:2008-06-25 出版日期:2009-03-10 发布日期:2009-03-10
  • 通讯作者: 郝明德

Nitrate-N Leaching in 23-Year Winter Wheat Field Combined with Application of Nitrogen and Phosphorus

  

  1. 中国科学院水土保持与生态环境研究中心
  • Received:2008-06-02 Revised:2008-06-25 Online:2009-03-10 Published:2009-03-10
  • Contact: HAO Ming-de

摘要:

【目的】利用长期肥料定位试验,监测旱地农田土壤硝态氮的淋溶动向,研究施肥量与硝态氮累积量之间的关系,为科学施肥提供参考。【方法】在试验小区0~300 cm土壤剖面中,每20 cm深度取一个土样,1 mol?L-1 KCl浸提后以AA3连续流动分析仪测定硝态氮含量。【结果】单施氮肥土壤硝态氮累积峰出现在80~100 cm土层和300 cm以下土层,当施氮量达到180 kg?hm-2?a-1时,0~300 cm土层硝态氮累积总量相当于8年的施氮量。单施磷肥对土壤硝态氮分布无影响;氮、磷肥配施时,施氮量增加硝态氮累积量显著增加,配施磷肥后可以减少硝态氮累积量,且施氮量越大减少的越多。过量施用氮肥,即使配施磷肥,硝态氮也能发生淋溶并在100~120 cm和240~260 cm土层附近累积;二次多项式回归能够较好地反映氮、磷施用量与土壤硝态氮累积量之间的关系。【结论】长期过量施用氮肥,导致硝态氮大量淋溶并形成两个累积峰,科学合理地配施磷肥可以减少硝态氮淋失;旱地麦田长期施用最大产量施肥量,可能导致硝态氮大量累积在土壤深层。

关键词: 长期施肥, 硝态氮淋溶, 旱地, 氮,

Abstract:

【Objective】 To provide a reference for scientific fertilization in the dry-land,present study on the changing trend of NO3--N leaching and the relationship between NO3--N accumulation and fertilizer rates in the farmland ecosystem based on data of the long-term fertilizer experiment. 【Method】Soil samples were collected per 20 cm in 0-300 cm soil layer, after being extracted with 1 mol?L-1 KCl, the NO3--N concentration in soil was analyzed with AA3 automated flow injection analyzer. 【Result】 When N fertilizer was applied alone, the accumulation peaks of NO3--N occurred in 80-100 cm and below 300 cm soil layer. If the annual rate of N reached 180 kg hm-2, total NO3--N accumulation amount in 0-300 cm soil layer was 8 times the amount of annual N application. When P fertilizer was applied alone, it had no significant effect on NO3--N distribution. NO3--N accumulation amount in the soil enhanced significantly with increasing N application rates. When N and P fertilizer was applied in combination, the application of P fertilizer alleviated NO3--N leaching and the positive effect increased with increasing N application rates. When N rates were excessive, even combined with P fertilizer, NO3--N penetrated into deep soil layer and accumulation peaks were found in 100-120 cm and 240-260 cm soil layers. Quadratic polynomial regression equation could reflect the relationship between NO3--N accumulation and N, P fertilizer rates. 【Conclusion】 When N fertilizer was applied excessively for 23 years, NO3--N penetrated largely into deep soil layer and two accumulation peaks were observed. However, NO3--N leaching could be mitigated by combined application of nitrogen and phosphorus. Long-term fertilizers application at rates for maximum yield would result in a great amount of NO3--N accumulation in deep soil layer in dry-land wheat field.

Key words: long-term fertilizer application, NO3--N leaching, dry-land, nitrogen, phosphorus