numerical simulation and prediction of mine water a case study in dangtu county of anhui province

numerical simulation and prediction of mine water a case study in dangtu county of anhui province

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时间:2019-01-09

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1、NumericalSimulationandPredictionofMineWaterACaseStudyinDangtuCountyofAnhuiProvince  【Abstract】Inthispaper,theregionalgroundwaterflowsysteminZhongJiuironorewasgeneralizedintothree-dimensionalunsteadygroundwaterflowsystemswithhomogeneous,isotropicandnoboundarylimits.ThesoftwareofVisua

2、lMODFLOWwasusedtosimulateandpredictthegushingprocess.theconclusionwasthatthecalibratedparameterswerereasonableandthepredictedvaluecansatisfythedemandoftheconsumptionofmining.  【Keywords】ZhongJiuironore,Hydrogeologicalconditions,VisualMODFLOW,Numericalsimulation,Waterinflowpredicting

3、.  Numericalmethodincludesfoursteps:hydrogeologicalmodelconceptualization,buildingmathematicalmodel,modelcalibration,minewaterinflowpredictingect.  1TheEstablishmentoftheHydrogeologicalConceptualModel  Themineareawasinwater-bearingmediumthathasnoobviouswaterboundary,therearemanyclea

4、rdifferencesamongdifferentwater-bearingrockgroupsoreventhesameones,buttherearestillsomehydraulicconnections.So,theanisotropyaquifermediumthat6above-370metersinminingareawasidentifiedastheflowfield,whichisisotropicandhasnoconfinedboundary.  Inordertoreflectthegeologicfeature,theaquif

5、ersweregeneralizedinto10layers.Thesimulatedrangewas143km2aroundthemine.Theboundarywasgeneralizedasgeneralheadboundaryandthesimulationareawasregardedasheterogeneousisotropic.ThegroundwaterflowwasdefinedastransientflowthatobeytheDarcy'slaw.  2TheDeterminationofInitialConditions  Thein

6、itialflowfieldwasdrawnbasedonthedateofthewaterlevelindecember2009,Thetenaquifergroupshaddifferentinitialflowfieldsbecauseoftheminordifferencesamongthemandtheminorgroundwaterexploitationquantities.  3MathematicalModelofGroundwaterFlow  3.1Discretization  Inspace,accordingtogeological

7、structurecharacteristics,hydrauliccharacteristics,flowfieldcharacteristics,simulationaccuracyandtheboundarycondition,twogroupsoforthogonalgridby11kmx13kmwhichareparalleltoxaxisandyaxisdividedthestudyareainto14300activecellswhichrepresenttheactualplanararea.  Intime,thesimulationtime

8、was7thdecember2009t

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