doi10.3969/j.issn.1672-6073.2014.04.015·27420148D-InSAR11121.1001012.100037D-InSAR、、、、。SBAS-DInSAR6D-InSAR。D-InSAR。D-InSARSBAS-DInSARP225U231.1A1672-6073201404-0062-051。、、、2013-09-222014-03-12985122935@qq.com、。。。、12、、、、。、、。GPS、、、。、、、。1D-InSARGPS、。1D-InSAR、、、、、、、26D-InSAR1D-InSARGPS、GPSD-InSAR、、、、、、、、、。。6D-InSARD-InSAR。2D-InSARD-InSARtopo、flat、atm。20D-InSAR41D-InSAR“”、“”、“”2PS、StaMPS、IPTA、STUN3SBAS、CPTA4PSSBASESD。D-InSAR。SBAS-DInSARD-InSAR。SBAS-DInSAR、。SBASSAR。SARSAR。。。。。SBAS-DInSAR1。1SBAS-DInSARt0…tnNSARMN/2≤M≤NN-1/2。tA、tBSARjtB>tAxΔφjx≈tBx-tAx=4πλdtBx-dtAx1λSARdtBxdtAxt0LOSdt0x=0tBxtAxdtBxdtAxNA=Δ2NSARΔMAM×N136·27420148261SAR+1-10。M≥NAN=A#ΔA#=ATA-1AT33DEM、。1SAR。ATA。LAN-L+1N≤M。SBASSVD。AM×NA=USVT4UM×NAATu1VN×NATAViSM×NAATλi。M>NARAATRM-R0。AA+A+=∑Ri=11λ槡iviui5^=A+δ。、。36、、、、29km19—2。620083—4。120094—56。6。32008—20096。32008—2009526ENVISATSARSRTM490mDEM116°10'32.6″~116°47'14.5″39°40'31.5″~40°07'55.8″20036—20108。SBAS-DInSARSBAS2007—2008、2008—20092007—200964~6。4SBAS-DInSAR2007—2008SBAS-DInSARSBAS-DInSAR27。46D-InSAR5SBAS-DInSAR2008—20096SBAS-DInSAR2007—200922008—2009SBAS-DInSARmmSBAS-DInSAR-2.7-2.90.2-0.7-0.3-0.3-3.0-0.6-2.4-2.71.5-4.2-3.32.2-5.5-3.32.4-5.8-0.74.1-4.80.72.6-1.9-0.73.8-4.5-0.36.2-6.6-0.38.5-8.82.03.9-1.9-2.30.3-2.6-18.0-13.6-4.4-32.0-28.0-4.0-100.0-84.9-15.1-85.0-87.32.3-62.0-55.9-6.1-79.3-87.58.127-15.1mm。6372008—2009SBAS-DInSARENVISATASAR30mSARSBAS-DInSAR。4、。D-InSAR、GPSSBAS-DInSARSBAS-DInSAR61D-InSARSBAS-DInSAR2ENVISATASAR6RADARSAT-2、TerraSAR-XCOSMO-SkyMed1、3、5m3D-InSARD-InSAR。1.PSInSARD.2009.2.D-InSARD.2008.56·274201483.InSARD.2010.4..SBAS-InSARJ.20102282-895.SBAS_InSARD.2012.6.InSARD.2011.7.SBAS-InSARD.2011.8CasuF.ThesmallBaselinesubsettechniqueperformanceassessmentandnewdevelopmentsforsurfacedeformationanalysisofveryextendedareasD.200952-55.9BerardinoPFornaroGLanariRSANSOSTIE.AnewalgorithmforsurfacedeformationmonitoringbasedonsmallbaselinedifferentialSARinterferogramsIEEETransactJ.GeoscienceandRemoteSensing200240112375-2383.10LRiccardoCFrancescoMMariarosariaetcAnoverviewofthesmallbaselinesubsetalgorithmADInSARtechniqueforsurfacedeformationanalysispureandappliedgeophysicsJ.PureApplGeophys.2007164637-661.D-InSARTechnologyAppliedintheFieldofDeformationMonitoringinUrbanRailTransitLiuYunming1MaQuanming1ChenDayong1XuYuming21.BeijingUrbanConstructionExploration&SurveyingInstituteBeijing1001012.BeijingMTRConstructionAdministrationCorporationBeijing100037AbstractD-InSARtechnologyisanewtypeofspacegeodetictechniques,characterizedbyitsall-day,all-weather,andwiderangeobservationabilitytoobtainhigh-precision,high-resolution,andlarge-scalesurfacedeformationwithoutrequiringgroundcontrolpoints.Therefore,D-InSARtechnologywasintroducedintourbanrailtransitfordeformationmonitoring.ExperimentofusingSBAS-DInSARtechnologyandprecisionlevelingtechnologywascarriedouttomonitorthegroundsubsidencealongBeijingmetroline6;thecomparisonshowsthatthetestdataofD-InSARisinaccordancewiththedatatestbyprecisiontechnology.SpecificengineeringapplicationsofD-InSARtechnologyinthedeformationmonitoringofurbanrailtransitprojectswerediscussed.ItisfeasibletoapplyD-InSARtechnologyfordeformationmonitoringinurbanrailtransit.Keywordsurbanrailtransit;differentialInSAR;SmallBaselineSubsetDifferentialInSAR;deformationmonitoring;715。3。200m。20161。、。·16。http//news.xinhuanet.com/world2014-07-1637110。。72、、、、、。。http//.jt.dl.gov.cn2014-07-0313771313。、、、。、。、“”。。http//.ccmetro.com2014-07-0766