山东国土资源
山東國土資源
산동국토자원
LAND AND RESOURCES IN SHANGDONG PROVINCE
2014年
9期
39-42,47
,共5页
管清花%陈学群%张婧
管清花%陳學群%張婧
관청화%진학군%장청
咸水入侵%水化学%超采地下水%莱州湾南岸
鹹水入侵%水化學%超採地下水%萊州灣南岸
함수입침%수화학%초채지하수%래주만남안
Salt water intrusion%water chemistry%over exploiting groundwater
以莱州湾南岸潍坊北部平原地区为典型研究区，阐述了咸水体形成的成因背景与分布特征。通过水化学分析的方法，分析了潍北平原地下水水化学变化特征，及人工开采导致咸水入侵的变化，并分析了咸水入侵的主要成因。
以萊州灣南岸濰坊北部平原地區為典型研究區，闡述瞭鹹水體形成的成因揹景與分佈特徵。通過水化學分析的方法，分析瞭濰北平原地下水水化學變化特徵，及人工開採導緻鹹水入侵的變化，併分析瞭鹹水入侵的主要成因。
이래주만남안유방북부평원지구위전형연구구，천술료함수체형성적성인배경여분포특정。통과수화학분석적방법，분석료유북평원지하수수화학변화특정，급인공개채도치함수입침적변화，병분석료함수입침적주요성인。
In this paper,setting northern Weifang plain in southern Laizhou Bay as the typical research area,geo-logical background of salt water formation and distribution have been described.Through water chemistry method, characteristics of water chemistry change of underground brine and the change of saltwater instrusion caused by hu-man activities in northern Weifang plain have been analyzed.Main causes of salt water intrusion has been analyzed as well.
