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Analyzing the differences of brackish-water in the Badain Lake by geophysical exploration method

查看全文 作  者:SONG Hong-[1]wei;MU Hai-[1]dong;XIA [2]Fan 高影响力作者 机构地区:[1]The Institute of Hydrogeology and Environmental Geology,CAGS,Shijiazhuang 050061,China;[2]Hebei Provincial of Academy of Environmental Sciences,Shijiazhuang 050031,China高影响力机构 出  处:《Journal of Groundwater Science and Engineering》索引2018年第6卷第3期,共6页高影响力期刊 基  金:supported by A 1/250 000 Hydrogeological Survey in the Badain Jaran Desert(G201610-3) 摘  要:BadainJ aran Desert of Inner Mongolia is arid and rainless all the year around,with much more evaporation than rainfall.But the special groundwater recharge mechanism contributes to the generation of several lakes of different sizes that have never not dried up for years,among which there are many freshwater lakes.As the research object in this paper,East Badain Lake and West Badain Lake in the southeast of the desert,which are less than 50m away from each other,show the considerable difference in mineralization.In fact,one is a freshwater lake,but the other is a brackish-water lake.Considering the underground aquifer structure of BadainJ aran Desert and the special formation structure the particularity of the stratigraphic structure around Badain Lake,the author uses AMT(audio magneto telluric)method and ultra-high density resistivity method to analyze the difference in mineralization of East Badain Lake and West Badain Lake from the perspective of geophysical prospecting methods. 关 键 词:AMT Badain Jaran DESERT Super density electrical method GEOPHYSICS
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