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海河流域灌溉平原区氮磷形态转化和淋失的定位研究
引用本文:戴同顺,赵忠生.海河流域灌溉平原区氮磷形态转化和淋失的定位研究[J].环境科学学报,1992,12(4):497-501.
作者姓名:戴同顺  赵忠生
作者单位:中国科学院应用生态研究所 沈阳110015 (戴同顺),中国科学院应用生态研究所 沈阳110015(赵忠生)
摘    要:对海河流域平原地区在灌溉条件下N、P形态转化和淋失进行了研究.结果表明,平原地区在灌溉条件下,干湿交替的土壤中将产生硝酸盐及少量亚硝酸盐,这些产物将随灌溉水一起向心土层渗漏,逐渐脱离生物循环进入地质大循环,造成地下水污染.

关 键 词:硝酸盐      淋失  海河流域  灌溉
收稿时间:1991/3/27 0:00:00

CASE STUDY ON THE CHEMICAL FORM CONVERSION AND LEACHING OF NITROGEN AND PHOSPHOROUS IN THE IRRIGATED PLAIN AREA OF HAIHE RIVER BASIN
Dai Tongshun and Zhao Zhongsheng.CASE STUDY ON THE CHEMICAL FORM CONVERSION AND LEACHING OF NITROGEN AND PHOSPHOROUS IN THE IRRIGATED PLAIN AREA OF HAIHE RIVER BASIN[J].Acta Scientiae Circumstantiae,1992,12(4):497-501.
Authors:Dai Tongshun and Zhao Zhongsheng
Institution:Institute of Applied Ecology, Chinese Academy of Sciences, Sheyang 110015 and Institute of Applied Ecology, Chinese Academy of Sciences, Sheyang 110015
Abstract:The N,P form conversion and leaching under the condition of irrigation in the plain area of Haihe River basin were investigated. The results show that more nitrate and less nitrite have been produced in this area when the soil is under the conditions of wet and dry alternations. These products will be leached with the irrigation water into the subsoil and gradually leave biological cycle and enter the geological cycle and causing the groundwater pollution.
Keywords:nitrate  phosphate  bio-geo-chemical cycle    
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