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背河洼地土壤水盐动态研究
引用本文:裴钟源,刘君阁.背河洼地土壤水盐动态研究[J].郑州大学学报(工学版),1994(2).
作者姓名:裴钟源  刘君阁
作者单位:郑州工学院水环系
摘    要:本文通过盐分传感器对背河洼地土壤水盐动态进行实地、定点、定时测定,获得地下水位与地下水矿化度和土壤合盐量的季节性变化规律,以及地下水矿化度与电导率的相关性,r=0.955,y=0.0011x+0.24。对该地区的农业生产持续地发展具有一定的指导作用。

关 键 词:土壤水盐动态,地下水矿化度,相关性,电导率

Study of salt-water Dynamic Regime in Soil on Low Ground of Back River
Pci Zhongyuan.Study of salt-water Dynamic Regime in Soil on Low Ground of Back River[J].Journal of Zhengzhou University: Eng Sci,1994(2).
Authors:Pci Zhongyuan
Affiliation:Zhengzhou Institute of Technology
Abstract:In this article,by using saltsensing unit on the spot,pinpont and at regular time to determine the salt-water dynamic regime in the soil low ground of back river.Law of seasonal change is obtianed that the water table and mineralization degree of ground water and soil's salinity,so are the correlation between the mineralization of ground water and the conductivity. there are certaiuly directive function for the development of the agroproduction in these regions.
Keywords:salt-water dynamic regime in soli  mineralization degree of ground water  correlation  conductivity
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