井地密集阵列激发极化法观测系统的分析

井地密集阵列激发极化法观测系统的分析

ID:34132931

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页数:73页

时间:2019-03-04

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1、ABSTRACTBoreholeinducedpolarizationmethod(referredtoastheboreholeinducedpolarization)cantakeadvantageofthedrillingclosedetectionnexttothewellthebottomholeblindmine,comparedwiththegroundinducedpolarizationinexplorationdepthexplorationdeeporebodydeepertomakeupgroundinducedpol

2、arizationmethoddeficiencies.Theinversionmethodbyinsufficientdatalimitations,itisdifficulttomeettheprecisedetectionandcomputerautomaticinversionandimaging.Tothisend,awellsuitableforautomaticinversionimagingexcitationpolarizationobservationandforwardmodelingandinversionsystem

3、-welllandintensivearrayexcitationpolarizationjointobservationmethod,thismethodcanimprovetheapplicabilityofboreholeinducedpolarizationmethod,butalsoimprovesthedetectionaccuracyoftheorebodynexttothewell.Intheaspectof3Dborehole-groundforwardmodeling.Tointroduce3Dborehole-groun

4、dinducedpolarizationmethodnumericalsimulationalgorithmtheory.Three-dimensionalsimulationareausingradialnon-uniformsubdivisionofdiscrete,wellhead-centered,equidistantfromthesplitinthediameterdirection,splitintoeightaliquotsuniformangleof45°inthedirectionoftheringdrilling,tom

5、akesplitmethodmoreinlinewiththelawsofthewellfielddistribution,correspondingwiththissplit,wedesignfourradialsurveycenteringonthewellheadobservationdevice,effectivelysolvethecaseofthewellunknownlocationgeologicalbodyisdifficulttodetermineobservationsdirection.Weusingradiallys

6、plitthefiniteelementmethodnumericalsimulation,andthepreparationofthecorrespondingforwardsimulationprogram,webuildseveraltypicalgeologicmodelforfiniteelementsimulationtotestthereliabilityofthealgorithmandtheprogram,andunderdifferentcircumstancesabnormalresponsewereanalyzed.I

7、ntheaspectof3Dborehole-groundinversionimaging.Firstofall,thebasicprinciplesandmethodsofinversionareintroduced;Second,Weusingtheabnormalpotentialoffiniteelementmodelingmethodtocalculate,andonthisbasistoderivethepartialderivativematrix;Third,inordertoeffectivelyimprovetheaccu

8、racyoftheinversion,reducinginversionofmultiplesolutions,thesmoothnessconstraintasa

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