摘要
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。
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.
出处
《山东国土资源》
2014年第9期39-42,47,共5页
Shandong Land and Resources
基金
水利部公益性行业科研专项经费(200901076)
国家海洋局公益项目(201105020)
国家自然科学基金(40776050)
关键词
咸水入侵
水化学
超采地下水
莱州湾南岸
Salt water intrusion
water chemistry
over exploiting groundwater
