成像雷达遥感地质灾害应用
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摘要
概述了合成孔径雷达技术的发展状况,对合成孔径雷达成像机理及特征做了简要介绍。结合SAR技术的发展阶段,简述了成像雷达遥感地质研究的技术理论,总结了国内外应用研究现状。同时对新兴起的新型成像雷达技术(极化雷达、干涉雷达)及其发展趋势也做了简单描述,重点突出了新型成像雷达技术在地质地震研究中的应用。最后提出了新型成像雷达技术在目前研究中存在的问题及对当前研究的改进措施,展望了他们未来的发展趋势。
Development situation of synthetic aperture radar(SAR) technology was sketched and imaging mechanism and characteristics of SAR was introduced briefly.Combining technological development stage,the technical theory of SAR remote sensing geological research was described and its actual research state at home and abroad was summarized.The new imaging radar technology(polarimetric SAR,interferometric SAR) and its application to geological research was highlighted Also some problems of this new technology in geological research and related improvements were pointed out.The new radar imaging technology playing a very important role in geological studies was full recognized,and their future development trends were looked forward to.
Development situation of synthetic aperture radar(SAR) technology was sketched and imaging mechanism and characteristics of SAR was introduced briefly.Combining technological development stage,the technical theory of SAR remote sensing geological research was described and its actual research state at home and abroad was summarized.The new imaging radar technology(polarimetric SAR,interferometric SAR) and its application to geological research was highlighted Also some problems of this new technology in geological research and related improvements were pointed out.The new radar imaging technology playing a very important role in geological studies was full recognized,and their future development trends were looked forward to.
引文
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[25]Stramondo S,Bozzano F,Marra F,et al.Subsidence induced by urbanisation in the city of Rome detected by advanced InSAR technique andgeotechnical investigations[J].Remote Sensing of Environment,2008,112:3160-3172.
[26]Massonnet D,Briole P,Arnand A.Deflation of Mount Etna monitored by space-borne radar interferometry[J].Nature,1995,375:567-570.
[27]Dzurisin D,Lisowski M,Wicks C W,et al.Geodetic observations and modeling of magmatic inflation at the Three Sisters volcanic center,centralOregon Cascade Range,USA[J].Journal of Volcanology and Geothermal Research,2006,150:35-54.
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[29]Hole J K,Bromley C J,Stevens N F,et al.Subsidence in the geothermal fields of the Taupo Volcanic Zone,New Zealand from 1996 to 2005measured by InSAR[J].Journal of Volcanology and Geothermal Research,2007,166:125-146.
[30]Ruch J,Anderssohn J,Walter TR,et al.Caldera-scale inflation of the Lazufre volcanic area,South America:Evidence from InSAR[J].Jour-nal of Volcanology and Geothermal Research,2008,174:337-344.
[31]Massonnet D,Feigl K,Rossi M,et al.Radar Interferomic mapping of deformation in the year after the Landers Earthquake[J].Nature,1994,369:227-230.
[32]Ohkura H.Application of SAR data to monitoring earth surface changes and displacement[J].Advances in Space Research,1998,21:485-492.
[33]Pedersen R,Jonsson S,rnadottir T,et al.Fault slip distribution of two June 2000 MW6.5 earthquakes in South Iceland estimated from joint in-version of InSAR and GPS measurements[J].Earth and Planetary Science Letters,2003,213:487-502.
[34]Funning G J,Barke R MD,Lamb S H,et al.The 1998 Aiquile,Bolivia earthquake:Aseismically active fault revealed with InSAR[J].Earthand Planetary Science Letters,2005,232:39-49.
[35]Wang H,Xu C J,Ge L L.Coseismic deformation and slip distribution of the 1997 Mw7.5 Manyi,Tibet,earthquake from InSAR measurements[J].Journal of Geodynamics,2007,44:200-212.
[36]Zhang L,Wu J C,Ge LL,et al.Determining fault slip distribution of the Chi-Chi Taiwan earthquake with GPS and InSAR data using triangu-lar dislocation elements[J].Journal of Geodynamics,2008,45:163-168.
[2]Koopmans B N,Forero R G.Airborne SAR and Landsat MSS as complementary information source for geological hazard mapping[J].ISPRS Jour-nal of Photogrammetry and Remote Sensing,1993,48:28-37.
[3]Kaupp V H,Gaddis L R,Mouginis-Mark P J,et al.Preliminary analyses of SIR-B radar data for recent Hawaii lava flows[J].Remote Sens-ing of Environment,1986,20:283-290.
[4]Yesou H,Besnus Y,Rolet J,et al.Merging Seasat and SPOTimagery for the study of geological structures in a temperate agricultural region[J].Remote Sensing of Environment,1993,43:265-279.
[5]Guo Huadong,Liao Jingjuan,Wang Changlin,et al.Use of multifrequency,multipolarization shuttle imaging radar for volcano mapping in theKunlun Mountains of Western China[J].Remote Sensing of Environment,1997,59:364-374.
[6]Abdallah E D,Khattab G A,Asif Khan M.Detection of sand-covered geologic features in the Arabian Peninsula using SIR-C/X-SAR data[J].Remote Sensing of Environment,1997,59:375-382.
[7]Stramondo S,Saroli M,Tolomei C,et al.Surface movements in Bologna(Po Plain-Italy)detected by multitemporal DInSAR[J].Remote Sens-ing of Environment,2007,110:304-316.
[8]Liu G X,Ding X L,Li Z L,et al.Pre-and co-seismic ground deformations of the 1999 Chi-Chi,Taiwan earthquake,measured with SARinterferometry[J].Computers&Geosciences,2004,30:333-343.
[9]Tomiyama N,Koike K,Omura M.Detection of topographic changes associated with volcanic activities of Mt.Hossho using D-InSAR[J].Ad-vances in Space Research,2004,33:279-283.
[10]Tizzani P,Berardino P,Casu F,et al.Surface deformation of Long Valley caldera and Mono Basin,California,investigated with the SBAS-In-SAR approach[J].Remote Sensing of Environment,2007,108:277-289.
[11]Rowland S K,Smith G A,Mouginis-Mark P J.Preliminary ERS-1 observations of Alaskan and Aleutian volcanoes[J].Remote Sensing of En-vironment,1994,48:358-369.
[12]Kervyn F.Modelling topography with SAR interferometry:illustrations of a favourable and less favourable environment[J].Computers&Geosci-ences,2001,27:1039-1050.
[13]Thurmond A K,Abdelsalam MG,Thurmond J B.Optical-radar-DEMremote sensing data integration for geological mapping in the Afar De-pression,Ethiopia[J].Journal of African Earth Sciences,2006,44:119-134.
[14]Kusky TM,Ramadan TM.Structural controls on Neoproterozoic mineralization in the South Eastern Desert,Egypt:an integrated field,LandsatTM,and SIR-C/X SAR approach[J].Journal of African Earth Sciences,2002,35:107-121.
[15]Mering C,Huaman-Rodrigo D,Chorowicz J,et al.Newdata on the geodynamics of southern Peru fromcomputerized analysis of SPOTand SARERS-1 images[J].Tectonophysics,1996,259:153-169.
[16]Raharimahefa T,Kusky TM.Structural and remote sensing studies of the southern Betsimisaraka Suture,Madagascar[J].Gondwana Research,2006,10:186-197.
[17]McCauley J F,Schaber G G,Breed C S,et al.Subsurface valleys and geoarcheology of the Eastern Sahara revealed by shuttle radar[J].Science,1982,218:1004-1020.
[18]Schaber G G,McCauley J F,Breed C S.The use of multifrequency and polarimetric SIR-C/X-SAR data in geologic studies of Bir Safsaf,E-gypt[J].Remote Sensing of Environment,1997,59:337-363.
[19]Blumberg D G,Neta T,Margalit N,et al.Mapping exposed and buried drainage systems using remote sensing in the Negev Desert,Israel[J].Geomorphology,2004,61:239-250.
[20]郭华东,刘浩,王心源,等.航天成像雷达对阿拉善高原次地表古水系探测与古环境分析[J].中国科学(D辑),2000,30(1):88-95.
[21]Blumberg D G.Remote Sensing of Desert Dune Forms by Polarimetric Synthetic Aperture Radar(SAR)[J].Remote Sensing of Environment,1998,65:204-216.
[22]Colesanti C,Ferretti A,Prati C,et al.Monitoring landslides and tectonic motions with the Permanent Scatterers Technique[J].Engineering Ge-ology,2003,68:3-14.
[23]Meisina C,Zucca F,Fossati D,Ceriani M,et al.Ground deformation monitoring by using the Permanent Scatterers Technique:The example ofthe Oltrepo Pavese(Lombardia,Italy)[J].Engineering Geology,2006,88:240-259.
[24]Tomas R,Marquez Y,Lopez-Sanchez J M,et al.Mapping ground subsidence induced by aquifer overexploitation using advanced DifferentialSAR Interferometry:Vega Media of the Segura River(SE Spain)case study[J].Remote Sensing of Environment,2005,98:269-283.
[25]Stramondo S,Bozzano F,Marra F,et al.Subsidence induced by urbanisation in the city of Rome detected by advanced InSAR technique andgeotechnical investigations[J].Remote Sensing of Environment,2008,112:3160-3172.
[26]Massonnet D,Briole P,Arnand A.Deflation of Mount Etna monitored by space-borne radar interferometry[J].Nature,1995,375:567-570.
[27]Dzurisin D,Lisowski M,Wicks C W,et al.Geodetic observations and modeling of magmatic inflation at the Three Sisters volcanic center,centralOregon Cascade Range,USA[J].Journal of Volcanology and Geothermal Research,2006,150:35-54.
[28]Tizzani P,Berardino P,Casu F,et al.Surface deformation of Long Valley caldera and Mono Basin,California,investigated with the SBAS-In-SAR approach[J].Remote Sensing of Environment,2007,108:277-289.
[29]Hole J K,Bromley C J,Stevens N F,et al.Subsidence in the geothermal fields of the Taupo Volcanic Zone,New Zealand from 1996 to 2005measured by InSAR[J].Journal of Volcanology and Geothermal Research,2007,166:125-146.
[30]Ruch J,Anderssohn J,Walter TR,et al.Caldera-scale inflation of the Lazufre volcanic area,South America:Evidence from InSAR[J].Jour-nal of Volcanology and Geothermal Research,2008,174:337-344.
[31]Massonnet D,Feigl K,Rossi M,et al.Radar Interferomic mapping of deformation in the year after the Landers Earthquake[J].Nature,1994,369:227-230.
[32]Ohkura H.Application of SAR data to monitoring earth surface changes and displacement[J].Advances in Space Research,1998,21:485-492.
[33]Pedersen R,Jonsson S,rnadottir T,et al.Fault slip distribution of two June 2000 MW6.5 earthquakes in South Iceland estimated from joint in-version of InSAR and GPS measurements[J].Earth and Planetary Science Letters,2003,213:487-502.
[34]Funning G J,Barke R MD,Lamb S H,et al.The 1998 Aiquile,Bolivia earthquake:Aseismically active fault revealed with InSAR[J].Earthand Planetary Science Letters,2005,232:39-49.
[35]Wang H,Xu C J,Ge L L.Coseismic deformation and slip distribution of the 1997 Mw7.5 Manyi,Tibet,earthquake from InSAR measurements[J].Journal of Geodynamics,2007,44:200-212.
[36]Zhang L,Wu J C,Ge LL,et al.Determining fault slip distribution of the Chi-Chi Taiwan earthquake with GPS and InSAR data using triangu-lar dislocation elements[J].Journal of Geodynamics,2008,45:163-168.
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