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应用生态学报 ›› 2005, Vol. 16 ›› Issue (4): 660-667.

• 研究论文 • 上一篇    下一篇

三种集约化种植体系氮素平衡及其对地下水硝酸盐含量的影响

寇长林1,2, 巨晓棠1, 张福锁1   

  1. 1. 中国农业大学资源与环境学院, 教育部植物-土壤相互作用重点实验室、农业部植物营养与养分循环重点实验室, 北京 100094;
    2. 河南省农业科学院土壤肥料研究所, 郑州 450002
  • 收稿日期:2004-04-12 修回日期:2004-10-04 出版日期:2005-04-15 发布日期:2005-04-15
  • 通讯作者: 巨晓棠,E-mail:Juxt@cau.edu.cn
  • 基金资助:
    国家自然科学基金项目(30270787,30390080)和国家"十五"科技攻关重大资助项目(2002BA516A02).

Nitrogen balance and its effects on nitrate-N concentration of groundwater in three intensive cropping systems of North China

KOU Changlin1,2, JU Xiaotang1, ZHANG Fusuo 1   

  1. 1. Key Laboratory of Plant Nutrition MOA, Key Laboratory of Plant-Soil Interactions MOE, Department of Plant Nutrition, China Agricultural University, Beijing 100094, China;
    2. Institute of Soil and Fertilizer, Henan Academy of Agricultural Sciences, Zhengzhou 450002, China
  • Received:2004-04-12 Revised:2004-10-04 Online:2005-04-15 Published:2005-04-15

摘要: 选取中国北方3种重要的集约化种植体系小麦玉米轮作、大棚蔬菜和果园,研究了3种体系年度氮素输入输出关系、土壤硝酸盐的累积、不同体系地下水硝态氮含量的动态变化.结果表明,大棚蔬菜年度化肥氮、有机肥氮、灌水带入的氮和总氮输入量分别为135.8、1881、402和36.56kg·hm-2,分别为小麦玉米田的25、37.5、83.8和5.8倍,为果园的2.1、10.4、6.82和4.2倍.不同系统降水输入的氮在142~189kg·hm-2之间.3个体系氮输出量分别为280、329和121kg·hm-2.氮素年度盈余分别为349、332.7和74.6kg·hm-2.0~90cm土层硝态氮累积量分别为22.1~2.75、1173和613kg·hm-2,90~180cm土层硝态氮累积量分别为2.13~2.42、10.32和976kg·hm-2.在0~180cm剖面中,小麦玉米田各层土壤硝态氮处于相对均一分布,大棚蔬菜以表层最高,30cm以下各层也远高于大田,果园土壤硝态氮累积随土壤深度而增加.3种体系均表现出硝酸盐的明显淋洗.大棚蔬菜区浅井地下水硝态氮含量99%超过了10mg·L-1.而大棚深井和果园浅井超标率均为5%,小麦玉米深井为1%.大棚蔬菜区地下水硝态氮含量与井深呈指数函数降低关系.

关键词: 集约化种植体系, 氮素平衡, 土壤硝酸盐累积, 地下水, 硝酸盐污染

Abstract: Selecting three main intensive cropping systems of North China,i.e,wheat-maize rotation,plastic greenhouse vegetable,and apple orchard as test objectives,this paper studied their nitrogen (N) budget,soil nitrate-N accumulation,and year-round dynamics of groundwater nitrate-N concentration.The results showed that in plastic greenhouse vegetable cropping system,the annual N input from chemical fertilizers,manure,and irrigation was 1 358,1 881 and 402 kg·hm-2,being 2.5,37.5 and 83.8 folds of the corresponding items in wheat-maize cropping system,and 2.1,10.4 and 68.2 folds in orchard,respectively,and its total N input amounted to 3 656 kg·hm-2,being 5.8 times of the wheat-maize cropping system,and 4.2 times of the orchard.The wet deposition N in the three cropping systems ranged from 14.2 kg·hm-2 to 18.9 kg·hm-2.The N output by wheat-maize,greenhouse vegetable and orchard was 280,329 and 121 kg·hm-2,the N surplus was 349,3 327 and 746 kg·hm-2,and the remained nitrate-N after harvest amounted to 221~275,1 173 and 613 kg·hm-2 in 0~90 cm soil layer,and 213~242,1 032 and 976 kg·hm-2 in 90~180 cm soil layer,respectively.Crop field had a comparatively even distribution of nitrate N in its 0~180 cm soil profile,and a sharp increase of nitrate N throughout the soil profile were found in both greenhouse vegetable and orchard fields.There was an evident nitrate leaching in all three cropping systems.The groundwater in shallow well (<15 m) was severely contaminated in greenhouse vegetable area,with the nitrate-N concentration in 99% of the samples exceeding the maximum permissible limit for drinking water (10 mg·L-1),while 5% of the samples in deep well in vegetable area and in shallow well in orchard and 1% of the samples in deep well in wheat-maize field were exceeded the limit.The nitrate-N concentration exponentially decreased with well depth (m) in greenhouse vegetable area.

Key words: Intensive cropping systems, Nitrogen budget, Nitrate accumulation in soil, Groundwater, Nitrate contamination

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