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作 者:丛康林[1,2] 岳建平 董超[1] 方云波[3] Cong Kanglin;Yue Jianping;Dong Chao;Fang Yunbo(School of Information Science and Engineering,Shandong Agricultural University,Taian 271018,China;School of Earth Sciences and Engineering,Hohai University,Nanjing 211100,China;Shanghai Weichen Geomatics Technology Co.,Ltd.,Shanghai 200001,China)
机构地区:[1]山东农业大学信息科学与工程学院,山东泰安271018 [2]河海大学地球科学与工程学院,江苏南京211100 [3]上海卫宸测绘科技有限公司,上海200001
出 处:《矿山测量》2020年第6期1-5,共5页Mine Surveying
基 金:国家重点研发计划(2018YFC1508603)。
摘 要:针对新汶矿区,采用SBAS-StaMPS方法对2016~2020年48景Sentinel-1A影像进行时序分析,反演了4年的地表形变过程,提取了8个采煤区地表时序沉降量,最大沉降量达180 mm,最大沉降速率为44.49 mm/a,沉降区中心表现出匀速型、阶梯型和加速型三种趋势。结果表明SBASStaMPS方法能够有效应用于多植被覆盖的采矿沉陷区识别与监测,可作为矿区地表形变监测分析的有效手段。Time series analysis on 48 scenes of Sentinel-1 A images was analyzed by the SBAS-StaMPS method from 2016 to 2020 in Xinwen mining area.Surface deformation process was inverted for 4 years.The time series of surface subsidence was obtained in 8 coal mining areas.Maximum settlement was 180 mm,and the maximum deformation rate was 44.49 mm and acceleration.Results showed that the SBAS-StaMPS method could be effectively applied to the identification and monitoring of mining subsidence areas with a large amount of vegetation cover,providing the effective method for monitoring and analysis of surface deformation in mining areas.
关 键 词:StaMPS-MTI SBAS 矿区形变 沉降速率 新汶
分 类 号:P237[天文地球—摄影测量与遥感] TD325[天文地球—测绘科学与技术]
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