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中国黄土区土壤剖面中的硝酸盐与饮水的硝酸盐污染

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摘要 20年来,中国施用氮肥大大地增加了作物产量。但在陕西米脂县川道地区由于大量施用氮肥,导致饮水中的硝态氮含量已达到不可接受的程度。本项研究揭示,在川道地土壤水中硝态氮含量非常高,而在丘陵顶部和坡地上的土壤水中硝态氮含量比较低。在200~400cm土层中,川台地为272kg/hm^2,川滩地为172kg/hm^2。该区土壤剖面中水分入渗深度每年约为2m左右。假如在200cm深度以下的硝酸盐作物根系不能吸收,那么在土壤剖面中每年每公顷在川台地和川滩地上将要淋失的氮肥即分别相当于损失148美元和94美元。
出处 《人类环境杂志》 1998年第6期441-443,共3页
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参考文献10

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  • 10First submitted 14 August 1996.Accepted for publication after revision 17 January 1997. 被引量:1

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