乌兰盆地地下水数值仿真模拟与可持续利用

乌兰盆地地下水数值仿真模拟与可持续利用

ID:34213095

大小:5.25 MB

页数:72页

时间:2019-03-04

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1、以上研究成果对乌兰盆地重大水源地建造、地下水资源的合理开发利用以及生态环境保护提供科学依据,为寻求西北地区一般的水资源开发利用模式积累经验。关键词:地下水,数值模拟,可持续开采阈值,乌兰盆地IIAbstractWulanislocatedateastQaidamBasin.Theclimateinthisregionissemi-aridplateaucontinentalcontinentwiththefeaturesofstrongandlong-durationevaporation,andlessandconcentratedrainfa

2、ll.Groundwateriswidelydistributedwithgoodwaterqualityandwaterstability.However,thedistributionofsurfacewaterspaceinthestudyareaisveryuneven.Also,thefreezingperiodislong.Therefore,itisurgenttofindwatersupplyschemeforgroundwaterresources.Takinggroundwaterdynamicstheoryasaguide,

3、thisthesisisaimedtoexplorethesustainableutilizationofgroundwaterinWulanbasin.Inthisstudy,numericalsimulationmethodisusedtostudytherulesoflakedegradedareaandinvestigatetheinfluenceofsurroundingecologicalenvironmentindifferentminingcase.Asaresult,thethresholdofsustainableground

4、waterexploitationandgroundwaterprotectionmeasuresareputforward.Somemajoropinionsandconclusionsobtainedfromthisstudyareshowedbelow:(1)Definingthesimulationarea.Thestudyareaissurroundedbyfourmountainsandonelake,whichareMaoniumountain,Amuneigemountain,QinghaiNanshan,Buhetemounta

5、inandChaikailake,inthedirectionofsouthwest,northwest,northandwest,respectively.Intheverticaldirection,thesurfaceisupperboundary,andthelowerboundaryisbedrock.(2)EstablishmentofWulanbasinhydrogeologicalconceptualmodel.AccordingtotheWulanbasinhydrogeological,geologicalconditions

6、andtheactualflowfieldareusedtosimplifytheboundaryconditions.Thewesternandnortheasternboundariescouldbeconceptualizedasconfiningboundaryandtherestofthebordersaretheflowboundaries.Dulanlake,KekeSaltlakeandSaltlakearetheminimumbaseleveloferosion,andthereforetheyaregeneralizedasd

7、rainageboundary.Theupperboundaryiswatertableandthelowerboundaryisthewaterimpermeableboundary.Thebasinisaintermontaneriftbasin,anditshydrogeologicalstructuremeetsthetypicalcharacteristicsofartesian;piedmontalluvialfanaquifersgenerallyaresingle-structuregravelaquifers,buttothec

8、enterofbasinalluvial-lacustrinealluvialplain,theaquifersgraduallytra

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