摘要
LabexperimentandmathematicalsimulationModularthreedimensionalfinitedifferencegroundwater(MODFLOW)wereperformedinasoiltanktosimulatethehydrogeochemicalinteractionbetweenlakeandtypicalunconfinedaquifer.Resultsshowthatthevelocitydecreasesexponentiallywiththetransectdistanceonseepageface.Themaximalvelocityoccursatthetoppointofseepageface.Theobliquityofseepagefacehasagreatinfluenceonthemaximumanddistributionofseepagevelocity.Withtheincreaseoftheobliquityofseepageface,themaximalvelocitydecreasesquicklyandthevelocitydistributionbecomesmuchmoreeven.Mostofgroundwaterflowandpollutantfluxdischargesthroughanarrowportionnearthetopofseepageface.Theflowandmassconcentratedinthenarrowportionincreasewiththedecreaseoftheobliquityofseepageface.Thesewillbenefittodesignareasonableandeconomicalscenariotomanagelakeshoreandtocontrolthepollutionoflakewaternearlakeshore.
出版日期
2007年06月16日(中国Betway体育网页登陆平台首次上网日期,不代表论文的发表时间)