• ISSN 1008-505X
  • CN 11-3996/S
薛晓辉, 郝明德. 旱作地区长期小麦连作和苜蓿连作土壤剖面的矿质氮研究[J]. 植物营养与肥料学报, 2010, 16(3): 620-625. DOI: 10.11674/zwyf.2010.0315
引用本文: 薛晓辉, 郝明德. 旱作地区长期小麦连作和苜蓿连作土壤剖面的矿质氮研究[J]. 植物营养与肥料学报, 2010, 16(3): 620-625. DOI: 10.11674/zwyf.2010.0315
XUE Xiao-hui, HAO Ming-de. Mineral nitrogen in soil profiles under long-term wheat cultivation and alfalfa continuous cropping in the dry farming area[J]. Journal of Plant Nutrition and Fertilizers, 2010, 16(3): 620-625. DOI: 10.11674/zwyf.2010.0315
Citation: XUE Xiao-hui, HAO Ming-de. Mineral nitrogen in soil profiles under long-term wheat cultivation and alfalfa continuous cropping in the dry farming area[J]. Journal of Plant Nutrition and Fertilizers, 2010, 16(3): 620-625. DOI: 10.11674/zwyf.2010.0315

旱作地区长期小麦连作和苜蓿连作土壤剖面的矿质氮研究

Mineral nitrogen in soil profiles under long-term wheat cultivation and alfalfa continuous cropping in the dry farming area

  • 摘要: 对不同施肥条件下23年小麦连作地和苜蓿连作地土壤矿质氮分布和累积进行研究,探讨种植浅根系和深根系植物对硝态氮淋溶的影响。结果表明,不施肥(CK)和单施磷(P)肥,小麦和苜蓿连作地土壤硝态氮主要集中在0—60 cm土层,0—60 cm土层以下硝态氮含量变化稳定并小于2 mg/kg。氮肥、磷肥和有机肥配施(NPM)时,小麦连作地土壤硝态氮累积在20—100 cm和140—320 cm土层,年累积速率可达42.12 kg/(hm2 ·a); 苜蓿连作土壤硝态氮主要集中在0—60 cm土层,仅在200—300 cm土层出现轻微累积,年累积速率仅为1.01 kg/(hm2·a)。在不施肥和单施磷肥下,种植小麦或苜蓿对土壤硝态氮残留量影响不显著,而氮、磷和有机肥配施时,小麦连作地土壤硝态氮残留量迅速增加,并与不施肥、单施磷肥处理有显著差异; 苜蓿连作地土壤硝态氮残留量虽有少量增加,但与不施肥、单施磷肥处理无显著差异。不施肥、单施磷肥和氮、磷和有机肥配施,小麦连作、苜蓿连作地土壤剖面铵态氮含量主要在10—20 mg/kg之间波动,在土壤剖面无明显的累积现象,铵态氮残留量受施肥和作物种类的影响不显著。

     

    Abstract: The distribution and accumulation of soil mineral N in soil profiles under different fertilization after 23-year wheat cultivation and alfalfa continuous cropping were studied, and as well as the effects of nitrate leaching in wheat cultivation and alfalfa continuous cropping. The results show that NO-3-N is centralized in 0-60 cm soil layer in the CK and P treatments after 23-year wheat cultivation and alfalfa continuous cropping, and the content of NO-3-N is less than 2 mg/kg below 60 cm-deep of soil profiles. Lots of NO-3-N are accumulated in 20-100 and 140-320 cm soil layers after 23-year wheat continuous cropping under the NPM treatments, and the accumulation rate of NO-3-N can reach to 42.12 kg/(ha·a). While, NO-3-N is centralized in 0-60 cm soil layer and is slightly accumulated in 200-300 cm soil layer after 23-year alfalfa continuous cropping under the NPM treatments, and the accumulation rate of NO-3-N is about 1.01 kg/(ha·a). In terms of residual NO-3-N rate in soil, it is not affected by wheat or alfalfa cultivation under no fertilization or P fertilization alone. However, the residual NO-3-N rate in 0-400 cm soil layer is increased under the NPM fertilization after 23-year wheat continuous cropping, and the differences of the residual NO-3-N rates are significant between the NPM treatment and the treatments CK and P. The residual NO-3-N rate is increased slightly under the NPM fertilization in the alfalfa fields, and the differences of NO-3-N accumulation are not significant between the NPM and CK, P treatments. The NH+4-N contents are about 10-20 mg/kg in all soil layers after 23-year wheat and alfalfa continuous cropping, and the phenomenon of NH+4-N accumulation is not found in soil profiles. Therefore, the residual NH+4-N rates are not affected significantly by the fertilization and cropping.

     

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