潍坊咸-卤水入侵引起的地下水化学成分变化及其对环境的影响  

CHEMICAL COMPOSITION VARIATION IN GROUNDWATER CAUSED BY SALT BRINE WATER INTRUSION AND ITS AFFECTION TO ENVIRONMENT IN WEIFANG AREA

作　　者：张永祥[1] 薛禹群[1] 陈鸿汉[2] 

机构地区：[1]南京大学地球科学系 [2]长春地质学院水文地质与工程地质系

出　　处：《环境科学学报》1997年第3期295-301,共7页Acta Scientiae Circumstantiae

基　　金：国家自然科学基金

摘　　要：阐述了莱州湾南岸潍坊地区咸卤水入侵的发展，入侵过程中地下水中宏量组分和微量元素的分布和变化特征，以及地下水化学成分变化引起的水质恶化。Salt brine water intrusion in southern coastal area of Laizhou Bay, Weifang District was studied. The distribution and variation of major components and minor elements in groundwater were studied. The environment problems caused by salt brine water intrusion, such as degeneration of groundwater quality, soil salinization and deterioration of ecological were illustrated.

关 键 词：潍坊地区 咸-卤水 化学成分 环境影响 地下水 

分 类 号：P641.12[天文地球—地质矿产勘探] X828[天文地球—地质学]