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人类活动对安徽省淮北平原孔隙水位动态的影响
引用本文:陈伟.人类活动对安徽省淮北平原孔隙水位动态的影响[J].安徽地质,2010,20(3):229-233.
作者姓名:陈伟
作者单位:安徽省地质调查院,安徽,合肥,230001
基金项目:安徽省级地质勘查专项费项目"安徽省淮北平原地下水环境演变调查评价" 
摘    要:本文利用上世纪70年代和本世纪初的水位对比和典型孔组的水位历时变化曲线,分析安徽省淮北平原孔隙水水位动态及历史变化。结果表明:多年来持续开采地下水,改变了淮北平原孔隙水水位动态类型和不同流动系统地下水的补排关系,加剧了孔隙水水位变化的随机性;集中开采区的中深部孔隙水水位动态变化尤为显著,水位持续大幅度下降,原自流区消失,并诱发地面沉降等地质环境问题。

关 键 词:孔隙水位动态  历史变化  人类活动  淮北平原  安徽省

IMPACT OF HUMAN ACTIVITIES ON DYNAMIC PORE WATER LEVEL IN THE HUAIBEI PLAIN IN ANHUI PROVINCE
CHEN Wei.IMPACT OF HUMAN ACTIVITIES ON DYNAMIC PORE WATER LEVEL IN THE HUAIBEI PLAIN IN ANHUI PROVINCE[J].Geology of Anhui,2010,20(3):229-233.
Authors:CHEN Wei
Institution:CHEN Wei(Institute of Geological Survey of Anhui Province,Hefei,Anhui 230001,China)
Abstract:Based on water level comparison between 1970s and early this century and water level versus time curve of typical hole group,this paper analyzed dynamic and historical change in pore water level in the Huaibei plain.The results indicate that continuous exploitation of groundwater for many years past has changed dynamic type of pore water level as well as feeding-drainage relation of groundwater of different flowing systems,and intensified the randomness of change in pore water level;centralized exploitation...
Keywords:dynamic state of pore water  historical change  human activities  Huaibei plain  Anhui Province  
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