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利用环境示踪剂估算滹沱河冲洪积扇地下水天然补给
引用本文:刘君,陈宗宇,张兆吉,费宇红,张凤娥,陈京生,王昭.利用环境示踪剂估算滹沱河冲洪积扇地下水天然补给[J].地质科技情报,2009,28(6).
作者姓名:刘君  陈宗宇  张兆吉  费宇红  张凤娥  陈京生  王昭
作者单位:中国地质科学院水文地质环境地质研究所,石家庄,050061
基金项目:国家自然科学基金项目(40472125);;中国地质调查局地质调查项目(1212010734411)
摘    要:包气带是降水补给地下水的一个主要环节,是了解补给变化的地质信息载体。以滹沱河冲洪积扇河北省正定试验场包气带剖面为研究对象,利用环境示踪剂(氚和氯)方法,估算了该区地下水近三十多年来的天然补给强度。研究结果表明:近30年来天然降水平均补给强度约为0.089m/a,在天然条件下该区降水垂直运移速度约为0.6m/a,其变化趋势主要受降水量变化影响,并表现出一定的滞后性。

关 键 词:华北平原  包气带剖面  环境示踪剂  补给强度  

Estimation of Natural Groundwater Recharge in the Hutuo River Alluvial-Proluvial Fan Using Environmental Tracers
LIU Jun,CHEN Zong-yu,ZHANG Zhao-ji,FEI Yu-hong,ZHANG Feng-e,CHEN Jing-sheng,WANG Zhao.Estimation of Natural Groundwater Recharge in the Hutuo River Alluvial-Proluvial Fan Using Environmental Tracers[J].Geological Science and Technology Information,2009,28(6).
Authors:LIU Jun  CHEN Zong-yu  ZHANG Zhao-ji  FEI Yu-hong  ZHANG Feng-e  CHEN Jing-sheng  WANG Zhao
Institution:Institute of Hydrogeology and Environmental Geology;Chinese Academy ofGeological Sciences;Shijiazhuang 050061;China
Abstract:Estimation of groundwater recharge is one of the important scientific issues for sustainable development and management of water resources.However,the large spatial and temporal variation makes it difficult to measure directly the groundwater recharge rate and hence it is very difficult to reconstruct the groundwater recharge history and estimate the changes of recharge rate.Unsaturated zone,as a link between precipitation and groundwater recharge,may contain information about recharge.This paper discusses ...
Keywords:North China Plain  unsaturated zone profile  environmental tracer  recharge rate  
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