摘要
由于地下水电导率与矿化度之间存在相关关系,在地下水资源调查时,可以通过现场实测地下水电导率的方式估测地下水矿化度。为探求两者间的相关性,通过对鲁北平原区地下水矿化度与电导率测试数据的统计分析,发现在矿化度≤3g/L的情况下,电导率与矿化度存在较好的线性关系,而且不同的阴离子水化学类型线性关系式不相同。
Due to relationship between groundwater conctuctlvlty ana salinity, aurmg me perloa of the groundwater resource investigation, by the way of field measurement of groundwater salinity, groundwa-ter conductivity can be estimated. In order to find the correlation between the two parts, through statisti-cal analysis on groundwater salinity and conductivity test data of Lubei plain in Shandong province, it is found that under the condition of salinity ≤ 3g / L, there is a good relationship between conductivity and salinity linear, and different types of linear anionic water chemistry relationships are not the same.
出处
《山东国土资源》
2013年第9期57-60,64,共5页
Shandong Land and Resources
关键词
电导率
矿化度
线性关系
鲁北平原
Conductivity
salinity
linear relationship
Lubei plain in Shandong province
