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[河套灌区春小麦与萝卜复种系统中硝态氮动态变化]

[NO3(-)-N dynamics in a spring wheat and radish multiple-crop system in the Hetao Irrigation District].

作者信息

Feng Zhao-zhong, Wang Xiao-ke, Feng Zong-wei

机构信息

State Key Laboratory of Systems Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, China.

出版信息

Huan Jing Ke Xue. 2006 Jun;27(6):1223-8.

Abstract

The NO3(-)-N dynamics of the soil, soil solution and groundwater were studied under spring wheat and radish multiple-crop system in Hetao Irrigation District over two years. A strong tendency of NO3(-)-N to move from upper layer to deeper layer could be observed and soil NO3(-)-N was increased at the layer of 100 approximately 150cm. NO3(-)-N concentration of soil solution at the depth of 70 and 120 cm was significantly higher than that at the depth of 30 cm, especially in the radish growth season. NO3(-)-N leaching amount was correlated with deep percolation at both different crop growth seasons and different years and it accounted for higher than 30% of total N input across two years. In the fertilizer plot, the concentration of NO3(-)-N in groundwater was far higher than that in the non-fertilizer plot, and 65.5% samples were over the safe standard of WHO (11.3mg/L) in the fertilizer plot. The topsoil NO3(-)-N content was markedly decreased during the two years multiple-crop system. However, NO3(-)-N leaching was inevitable in the near future due to a large amount of residual NO3(-)-N in the middle and deeper soil profiles.

摘要

在两年时间里,对河套灌区春小麦和萝卜复种系统下土壤、土壤溶液及地下水的硝态氮动态变化进行了研究。可以观察到硝态氮有从上层向深层移动的强烈趋势,且在100至150厘米土层土壤硝态氮有所增加。70厘米和120厘米深度土壤溶液中的硝态氮浓度显著高于30厘米深度处,尤其是在萝卜生长季节。不同作物生长季节和不同年份的硝态氮淋溶量均与深层渗漏相关,且两年间其占总氮输入量的比例均高于30%。在施肥地块,地下水中硝态氮浓度远高于未施肥地块,施肥地块65.5%的样品超过了世界卫生组织的安全标准(11.3毫克/升)。在两年的复种系统中,表层土壤硝态氮含量显著下降。然而,由于中深层土壤剖面中存在大量残留硝态氮,在不久的将来硝态氮淋溶仍不可避免。

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