山西省汾河灌区地下水系统分析  

Systematic Analysis on Groundwater of Fenhe River Irrigation District of Shanxi Province

作　　者：白彦飞[1] 孙磊[1] 

机构地区：[1]水利部山西水利水电勘测设计研究院,山西太原030024

出　　处：《地下水》2003年第2期65-67,共3页Ground water

摘　　要：本文运用有关地下水系统理论 ,对山西省汾河灌区地下水资源作系统分析。灌区水资源系统由地表水系统与地下水系统构成。地下水系统具有双层含水结构 :浅层潜水——承压水系统和中层承压水系统。由于含水系统本身特点及人工开采影响 ,浅层水对中层地下水垂直越流补给。地下水属松散孔隙水。地下水运动以垂向为主 。This paper has made systematic analysis on groundwater resources in Fenhe River Irrigation District Shanxi Province by applied the relevant systematic analysis theory of groundwater. Water resources systems of irrigation district are composed with surface water system and groundwater system. Groundwater systems have shallow phreatic water-confined water system and medium layer confined water system. Owing to its native feature and the influence by artificial exploitation, the shallow groundwater is vertical cross-flow supplement to medium layer groundwater. Groundwater belong to loose pore water, the groundwater mainly is vertical movement and horizontal movement subsidiary.

关 键 词：山西 地下水系统 汾河灌区 双层含水结构 浅层潜水 承压水系统 中层承压水系统 地下水资源 水利调查 地下水运动 

分 类 号：TV211.12[水利工程—水文学及水资源] P641.2[天文地球—地质矿产勘探]