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基于小基线集时序干涉雷达分析武汉中心城区地表沉降时空特征
引用本文:周吕,鲁金金,文学霖,章迪,王成,杨飞.基于小基线集时序干涉雷达分析武汉中心城区地表沉降时空特征[J].科学技术与工程,2021,21(1):40-46.
作者姓名:周吕  鲁金金  文学霖  章迪  王成  杨飞
作者单位:桂林理工大学测绘地理信息学院,桂林541004;桂林理工大学博文管理学院,桂林541004;桂林理工大学测绘地理信息学院,桂林541004;武汉大学测绘学院,武汉430079;广西壮族自治区自然资源调查监测院,南宁530023;桂林理工大学测绘地理信息学院,桂林541004;武汉大学测绘学院,武汉430079
基金项目:广西自然科学基金资助项目(2018GXNSFBA050006),武汉市科技计划项目(2019010702011314),2018年广西高校中青年教师基础能力提升项目(2018KY0851),广西科技计划项目(桂科AD19110107),国家自然科学基金(41604019),广西空间信息与测绘重点实验室资助课题(19-050-11-01)。
摘    要:利用2015—2016年期间获取的15景Sentinel-1A TOPS SAR影像,采用小基线集时序干涉雷达(interferometric syn-thetic aperture radar,InSAR)分析方法,研究了武汉中心城区的地表沉降特征,分析并建立了该地区地表沉降与城市建设、降雨量和长江水位变化等因素的关系.采用32个水准点数据验证了基于Sentinel-1A反演的地表沉降结果,精度为5.82 mm/a.研究区域内不均沉降明显,其地表沉降速率范围为-81.5~18.2 mm/a,且探测到的最大沉降速率位于后湖地区;地表沉降时间序列呈伴随有明显季节变化的非线性沉降.地表沉降与影响因子的对比分析表明,沉降漏斗与工程建设施工区位置分布具有较高的空间相关性;地表沉降中的季节性变化与水位变化和降雨量有关;研究区域地表沉降主要由人为活动、土层压缩性以及地下水过度开采等造成.研究结果给出了武汉中心城区地表沉降时空特征和地表沉降与其影响因子之间的相互关系.

关 键 词:时序干涉雷达  地表沉降  水位变化  时空特征
收稿时间:2019/12/31 0:00:00
修稿时间:2020/9/17 0:00:00

Spatial-temporal Characteristics Analysis of Surface Subsidence in Central Urban Areas of Wuhan Based on Small Baseline Subset Interferometric SAR
ZHOU Lü,LU Jin-jin,WEN Xue-lin,ZHANG Di,WANG Cheng,YANG Fei.Spatial-temporal Characteristics Analysis of Surface Subsidence in Central Urban Areas of Wuhan Based on Small Baseline Subset Interferometric SAR[J].Science Technology and Engineering,2021,21(1):40-46.
Authors:ZHOU Lü  LU Jin-jin  WEN Xue-lin  ZHANG Di  WANG Cheng  YANG Fei
Institution:College of Geomatics and Geoinformation, Guilin University of Technology;School of Geodesy and Geomatics, Wuhan University;Guangxi Institute of Natural Resources Survey and Monitoring
Abstract:In this paper, surface subsidence characteristics in central urban areas of Wuhan was investigated using 15 Sentinel-1A Terrain Observation with Progressive Scans (TOPS) SAR images acquired from 2015 to 2016 with the Small Baseline Subset Interferometric SAR (SBAS InSAR) analysis method. The correlations between surface subsidence and urban construction, precipitation, and water level changes in Yangtze River in the study area were analyzed and established. The inversion surface subsidence results based on Sentinel-1A were validated by 32 leveling points at an accuracy of 5.82 mm/year. Prominent uneven subsidence patterns were identified in the study area. Specifically, surface subsidence rates ranged from ?81.5 mm/year to 18.2 mm/year, and maximum subsidence rate was detected in Houhu areas. Surface subsidence time series presented nonlinear subsidence with pronounced seasonal variations. Comparative analysis of surface subsidence and influencing factors indicated a relatively high spatial correlation between locations of subsidence bowl and those of engineering construction. Seasonal variations in subsidence were correlated with water level changes and precipitation. Surface subsidence in the study area was mainly attributed to anthropogenic activities, compressibility of soil layer, and groundwater overexploitation. The spatial-temporal characteristics of surface subsidence and the relationship between surface subsidence and influencing factors in central urban areas of Wuhan were given in the results of this study.
Keywords:Time-series  InSAR  surface  subsidence  water  level changes  spatial-temporal  characteristics
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