摘要
鉴于氯离子在地下水中的分布很广,因此,探究地下水环境氯离子含量时空动态演化规律具有重要意义。研究发现,上海市地下水环境Cl-含量年际演化幅度比较大,且呈现规律性的二次曲线或三次曲线,各个含水层之间的变化呈显著性差异。从其垂直方向分布看,氯离子平均含量由高到低依次为第二承压含水层,第五承压含水层,潜水含水层,第四承压含水层和第三承压含水层。
There is a wide distribution of Chloride Ion in groundwater, so it is of great significance to probe into the temporal and spatial dynamic evolution of Chloride content in groundwater environment. The results showed there existed a relevantly great change in the annual content of Chloride Ion in the groundwater of Shanghai City, presenting a regular quadric curve or cubic curve. Furthermore, the change in each aquifer presented a significant difference. From the perspective of its vertical distribution, the average content of Chloride Ion from height to lowness in turn was the second confined aquifer, the fifth confined aquifer, the unconfined aquifer, the fourth and the third confined aquifer.
出处
《山东农业大学学报(自然科学版)》
CSCD
2015年第6期892-897,共6页
Journal of Shandong Agricultural University:Natural Science Edition
基金
上海市重点学科建设项目(B604)
关键词
上海市
地下水环境
氯离子含量
时空动态演化
Shanghai City
groundwater environment
Chloride Ion content
temporal and spatial dynamic evolution