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。
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.
基金
河海大学博士后基金课题
国土资源部重点基础项目!(95 0 1110 )
国土资源部百名科技人才基金资助课题
关键词
全新世
地下水
补给期
水文循环演化
演化规律
Holocene groundwater recharge period evolution of hydrologic cycle piedmont clinoplain of Taihang mountains
