摘要
本文通过对河北平原东部第四系深层高氟地下水水文地球化学特征分析,以地下水系统理论为指导思想,探讨了高氟地下水的分布规律及成因。
Through the analysis of hydrogeochemical features of deep groundwater of Quaternary system with high fluorine in the eastern part of Hebei plain, theregularity of distribution of high fluorine groundwater and its genesis are discussed with the aid of groundwater system theory herein.
出处
《工程勘察》
CSCD
北大核心
1993年第2期28-31,共4页
Geotechnical Investigation & Surveying