毕业论文英语翻译及原文.docx
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毕业论文英语翻译及原文
ARESEARCHONDATAPROCESSINGMODELOFGPSDAM
DEFORMATIONMONITORINGNETWORK
Abstract:
ConsideringtheparticularityoftheGPSdamdeformationmonitoringnetwork,adataprocessingmodelbasedonthestationorthogonalcoordinatesystemforthree-dimensionGPSdamdeformationmonitoringnetwork,wasputforward.Also,amathematicalmodelofusingtheclusteringanalysismethodinfuzzymathematicstotesttherelativestabilityofquasi-stablepoints(ordatummarks)wassuccessfullybroughtforward.Theadjustmentmethodduringthecourseofdataprocessingwasquasi-stableadjustment.Atlast,asoftwaresystemofthree-dimensionGPSdamdeformationmonitoringnetworkwasdesignedandopenedupwiththehelpofVisualBasicLanguage.Withthreeperiodso'bservationdatafromtheGPSdeformationmonitoringnetworkofadam,anadjustmentcalculationwasdonebythesoftware.ThecalculationresultshowsthatthemathematicalmodelscanbemoresuitableforthedataprocessinginGPSdamdeformationmonitoringnetwork.
Keywords:
GPS,Damdeformationmonitoring,Quasi-stableadjustment,Clusteringanalysis1.Introduction
WGS-84coordinatesystemisgenerallyusedinGPS.Butlocalorindependentcoordinatesystemsareusuallychosenindamdeformationmonitoringnetworksfortheirsmallareas.Duringthecourseofpastdataprocessing,theadjustmentunderWGS-84coordinatesystemforindependentnetworksornetworkswithseveralfixedpointsisoftenfirstlymade.Then,thetransformationfromWGS-84coordinatesystemtolocal(orindependent)coordinatesystemsisdone.ForGPSdeformationmonitoringnetworkswithrepetitiveobservationdata,theobviouschangeofdatummarkscoordinatesunderthetwodifferentcoordinatesystemscanbebroughtbythetinydeformationofdatummarksamongdifferentperiodsofobservation.Andthegreatererrorcanbemadeduringthecoordinatetransformation.IfalocalGausscoordinatesystemischosen,theprojectiondistortionscanalsobeproducedbythetransformationitself.Forthereasonsabove,thestationorthogonalcoordinatesystemischosenasthereferencecoordinatesystemfordataprocessingofGPSdamdeformationnetworks.Andthemathematicalmodelisputforwardanddeduced.
2.Dataprocessingmodelbasedonthestationorthogonalcoordinatesystemforthree-dimensionGPSdeformationmonitoringnetworks
2.1Coordinatesystem
Thestationorthogonalcoordinatesystemisaleft-handcoordinatesystem.ItsoriginissetatoneoftheGPSmonitoringpoints.TheE(X)axispointsatthemeridianpassingtheorigin.Itisonthetangentplaneoftheorigin.Andtherightnorthistakenasforwarddirection.TheH(Z)axisisonthe
normallineofWGS-84ellipsoidatthepointandtakesoutwardasforwarddirection.TheE(Y)axisisalsoonthetangentplaneoftheoriginanduseseastforforwarddirection.
Ifthepositionvectorofthestationorthogonalcoordinatesystemorigin
rT
PoinWGS-84isexpressedaso二X0Y0Zo,accordingtothegeodeticlatitudeandIongitude(b°,L。
)'thepositionvector门inthestationorthogonalcoordinatesystemoriginofarandompointpicanbegotthroughthetranslationandrotationofitsWGS-84position
T
vectorri
「i=H(「i-ro)
(1)
Intheaboveequation,Hcanbewrittenas
-sinBoCosLo-sinBosinL。
cosBo
H=sinBocosLoo
(2)
cosBocosLocosBosinL。
sinB。
一
Ifthebaselinevectorsofthetworandompoints
piandpjinWGS-84coordinatesystemandthethestationorthogonalcoordinatesystemarewrittenas"11川''111
respectively,theexpressioncanbeeasilygainedasfollows
Artf=r/-ri=H(r-r0)-H(r-r0)=H(r'-rj
Then,therelationequationbetweenthetwobaselinevectorsisexpressed
Ar=HAr
as
TherearetwostepsintheGPSobservationdataprocessingcourse.Theyarebaselinecalculationandnetworkadjustment.ThebaselinevectorsinWGS-84canbefirstlygotusingbaselinecalculation.Secondly,thebaselinevectortransformationfromWGS-84tothestationorthogonalcoordinatesystemcanbedonewith(3).Atlast,theadjustmentofGPSdeformationmonitoringnetworksinthestationorthogonalcoordinatesystemcanbesuccessfullyfinished.
2.2Adjustmentmethodandmathematicalmodel
Deformationmonitoringnetworksusuallyrequirehigherprecision.Andifseveralfixedpointsareadoptedfordatum,theobservationprecisioncanbegreatlyreduced,becausetheknowndataprecisioniso'ftesnlowerthantherequiredprecisionandthebeginningpoints'displacementca
makeannexeeffecttoobservationdataespeciallyduringthecourseofrepetitiveobservation.Sotheclassicaladjustmentmethod,whichhassomegivenpoints,isgenerallynotused.Butitisimportanttochoosethereferencepointswithstablephysicalstatusasdatumofdeformationmonitoringnetworks.Consideringtheabovetwocases,thequasi-stableadjustmentcanbeemployedtomakethemorestableunknowndata(thecoordinatesofrelativelystablepointsawayfromthedam)matchtheirstablevalues.Then,therearenodistortionofsurveyingresultandrelativelystabledatum.Andthegoaltomonitorthedeformationcanbereachedwell.TheadjustmentmodelofGPSrank-deficientnetworkscanbewrittenas
V=AX-L
T.,(4)
S(L)二阮pi
Withtheleastsquaremethod,thenormalequationisexpressedas
NX二W(5)
TT
whereNequalsAPAandWequalsaPL
Andtheequationcanbegotasfollows
R(N)=R(A)=rwhereAdenotestherank-deficientmatrixwhoserank-deficientnumberdis(n-r)」fSisasetofradicalofzerospaceN(A)andR(S)denotesd,theequationiswrittenas
AS=0(6)
Whentheinnerproductspaceisdefinedas(X,Y)=xtRYandR(R)>
d,undertheconstraintconditionXRX=min,thefollowingequationcanbegot
STRX=0(7)
With(5)and(7),thesolutionequationofweightingrank-deficient
networkscanbeexpressedas
Q亠-QhRSVRQ^
IXX
WhereQrdenotes"、R*%H
.WhenRisadiagonalmatrixanditsvalueis1or0,(8)can
becomethemodelofquasi-stableadjustment.TheSmatrixcanbegiven
accordingtotheconditionAS=0.AndtheSmatrixofGPS3-dimensionaldeformationmonitoringnetworksiswrittenas
100loo1oo-
sz=0)0010……oio⑼
ooiooioo1
2.3Mathematicalmodelofcalculatingquasistablepoints'relativestabilitywithclusteringanalysisForGPSdamdeformationmonitoringnetworks,thestabilityofdatummarksmustbefirstlytestedintheobservationdataprocessing.ThoughtherelativelystableareaischosenforbuildingdatummarkswhenGPSdamdeformationmonitoringnetworksaredesigned,thedeformationofdatummarkscancomeintobeing.Evenifthequasi-stableadjustmentmethodisused,thestabilitytestneedstobemade,too.Thequasi-stablepoints(quasi-stablepointsordatummarksindesignscheme)withmarkeddeformationshouldbeeliminated.Themathematicalmodelofcalculatingquasi-stablepoints(ordatummarks)relativestabilitywithclusteringanalysisinfuzzymathematicsisputforwardtoensurethestablequasi-stablepoints(ordatummarks)inGPSobservationdataprocessing.Onecharacteristicofquasi-stableadjustmentisthatthecorrectionvalueVofobservationdataafteradjustmentisinvariable.SotheadjustedvalueLofobservationdataisalsoinvariable.Anditisshownthatthenetworkshapeafteradjustmentisunchanged.TheobservationdataofGPSnetworksadjustmentisbaselinevectors(coordinatedifferencesin3coordinateaxisdirections).
Then,afterthequasi-stableadjustmentoftwoperiodsofobservationdata,
thedifferencesofcoordinatedifferencesoftworandomquasi-stablepointsin3coordinateaxisdirectionsbetweenthetwoperiodsare
invariable.So,thesevaluescan'tbechangedwithdifferces.cAodworkcanbefinishedonceforadotoavoidthetroubleofsomemethodscalculatingstepbystep.匸andfdenotethecoordinatedifferencesoftworandomquasi-stablepoints(iandj)aftertwoperiods'seobation
1
dataadjustment.isthediffereneeofcoordinatedifferencesbetween
(io)
twoperiods.Andequationsareasfollowsn
叭+碍
Statisticiswrittenas
=—⑴)%
1
IfthechangeoflijbetweentwoperiodsiscausedbytheaccidentalerrorofGPSobservation,itisexpressedas
心~MO,1)
Thefuzzymembershipgradeoftherelativestabilityofthetworandom
quasi-stablepoints(iandj)isdefinedas
(12)
Thatistosay,thefuzzyrelationoftherelativestabilityofquasi-stablepointsistheprobabilitydensity
valueofstandardnormaldistributionabout^.To口,itcanbedefinedas
u=0forsupplement.Itisalsoasfollows
口=于(叫)(13)
Andthefuzzyrelationofrelativestabilityofquasi-stablepointsdefinedby(12)and(13)onlysatisfies
thesymmetryofequivaleneefuzzyrelation.Thereflexivitycanbe
(14)
standardized.And「「isre-definedas
=/(0)
ThefuzzyrelationRhasmetthefirsttwoconditionsoffuzzyequivalenee
relation.ThenRisafuzzysimilarmatrix.Totransitivity,thefuzzy
similarmatrixcanbechangedtoafuzzyequivaleneematrixwiththehelpofthetransitiveclosedpackaget(R).Andthefuzzyanalysiscanbedone.
Thesortedindexparameter入ofclusteringanalysisiscomputedwiththe
statistichypothesismethod.IfthechangeofbetweentwoperiodsiscausedbytheaccidentalerrorofGPSobservation,itisexpressedas
Forthegivenconspicuouslevela,thereisacKticaWfitHue一,
thecorrespondingvalu.canbegotfrom(14).And「isthesorted
stability.Tab.1belowshowsthevaluesofaand入
TabJStatisticsonconspicuouslevelotandcriticalvalueA
a
5%
1%
O+27%
O]%
A
0.1465
0.0377
0.0111
0.0045
Obviouslyashouldbechangedinthepractice.Itiscon