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全新世以来太行山前倾斜平原地下水演化规律
引用本文:张光辉,费宇红,聂振龙,李惠娣.全新世以来太行山前倾斜平原地下水演化规律[J].地球学报,2000,21(2):121-127.
作者姓名:张光辉  费宇红  聂振龙  李惠娣
作者单位:国土资源部环境地质开放研究实验室,石家庄;中国地质科学院水文地质工程地质研究所,河北正定;中国地质科学院水文地质工程地质研究所,河北正定;中国地质科学院水文地质工程地质研究所,河北正定
基金项目:河海大学博士后基金课题,国土资源部重点基础项目(9501110 ),国土资源部百名科技人才基金资助课题
摘    要:全新世以来太行山前倾斜平原地下水形成、演变与区域水文循环演化的周期性密切相关。在 8.0~ 3 .5kaB .P.期间为主要补给期 ,地下水获取了充足补给 ,奠定了现今地下水系统的基础。

关 键 词:全新世    地下水    补给期    水文循环演化    太行山前倾斜平原

The Evolution Regularity of Groundwater in Piedmont Clinoplain of Taihang Mountains since Holocene
ZHANG Huang-hui,FEI Yu-hong,NIE Zhen-long and LI Hui-di.The Evolution Regularity of Groundwater in Piedmont Clinoplain of Taihang Mountains since Holocene[J].Acta Geoscientia Sinica,2000,21(2):121-127.
Authors:ZHANG Huang-hui  FEI Yu-hong  NIE Zhen-long and LI Hui-di
Institution:Open Laboratory of Environmental Geology, MGMR, Zhengding, Heibei;Institute of Hydrogeology and Environmental Geology, CAGS, Zhengding, Hebei;Institute of Hydrogeology and Environmental Geology, CAGS, Zhengding, Hebei;Institute of Hydrogeology and Environmental Geology, CAGS, Zhengding, Hebei
Abstract:The formation and the evolution of regional groundwater have been closely related to periodic hydrological cycle in piedmont clinoplain of Taihang mountains since Holocene.The main recharge period of groundwater was 8.0 to 3.5 ka B.P.,during which the recharge of groundwater was sufficient.This lay the foundation of present groundwater system.
Keywords:Holocene  groundwater  recharge period  evolution of hydrologic cycle  piedmont clinoplain of Taihang mountains
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