Sentinel-1A京津冀平原区2016—2018年地面沉降InSAR监测

doi:10.6046/zrzyyg.2020341

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摘要

京津冀地区是我国地面沉降发展最迅速,影响面积最大的地区。地面沉降已成为京津冀协同发展中不容忽视的地质问题。文章利用多时相合成孔径雷达干涉测量(multi-temporal interferometric synthetic aperture Radar,MT-InSAR)技术对2016年1月—2018年10月覆盖京津冀地区的多轨Sentinel-1A数据进行处理,经水准数据验证和相邻轨道数据结果交叉验证后,对多轨SAR数据结果进行融合获取了京津冀平原2016—2018年间的地面沉降结果。InSAR监测结果表明,监测时段内京津冀平原最大沉降速率达164 mm/a,研究区内地面沉降分布广泛,且空间分布不均。对京津冀地区地面沉降时空变化特征进行分析发现,2016—2018年间唐山—秦皇岛地区地面沉降呈不断加剧趋势; 其余地区地面沉降发展较为稳定。研究表明了InSAR技术在大区域地面沉降监测中的可靠性,研究结果为区域沉降防治提供重要依据,为京津冀特大城市群建设提供科学保障。

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	史珉
	宫辉力
	陈蓓蓓
	高明亮
	张舜康

关键词 ：地面沉降, 京津冀平原区, InSAR, Sentinel-1A

Abstract：

The land subsidence in the Beijing-Tianjin-Hebei (BTH) region has developed the most rapidly and affects the largest area in China and it has become an unnegligible geological problem in the coordinated development of the BTH region. In this study, the multi-track Sentinel-1A data from January 2016 to October 2018 that cover the whole BTH plain was processed using the multi-temporal InSAR (MT-InSAR) technique. After the verification using leveling data and the cross-validation using the data from adjacent tracks, the land subsidence in the BTH region during 2016—2018 were obtained by integrating multi-track SAR data results. The InSAR monitoring results show that the maximum subsidence rate in the BTH region reached 164 mm/a and the land subsidence was widely and unevenly distributed in space in the study area during the monitoring period. According to the analysis of the spatial-temporal change characteristics of the land subsidence in the BTH region, the land subsidence showed an increasing trend in the Tangshan-Qinhuangdao area but stably developed in the remaining areas in the BTH region during 2016—2018. This paper demonstrates that the reliability of the InSAR technique in the monitoring of land subsidence in large regions. The results of this study will provide an important basis for the prevention and mitigation of regional subsidence and will provide a scientific guarantee for the construction of the BTH urban agglomeration.

Key words： land subsidence Beijing-Tianjin-Hebei plain InSAR Sentinel-1A

收稿日期: 2020-10-28 出版日期: 2021-12-23

ZTFLH:

TP79

基金资助:国家自然科学基金重点项目“京津冀典型区地下空间演化与地面沉降响应机理研究”(41930109/D010702);国家自然科学基金面上项目“南水进京背景下地面沉降演化机理”(41771455/D010702);北京卓越青年科学家项目(BJJWZYJH01201910028032);北京市优秀人才青年拔尖项目和北京市自然基金面上项目“新水情背景下京津高铁沿线地面沉降演化机制及调控方法”(8182013)

作者简介: 史珉(1989-),女,博士研究生,主要从事地面沉降演化机理方面的研究。Email: Minshi_cnu@126.com。

引用本文:

史珉, 宫辉力, 陈蓓蓓, 高明亮, 张舜康. Sentinel-1A京津冀平原区2016—2018年地面沉降InSAR监测[J]. 自然资源遥感, 2021, 33(4): 55-63.
SHI Min, GONG Huili, CHEN Beibei, GAO Mingliang, ZHANG Shunkang. Monitoring of land subsidence in Beijing-Tianjin-Hebei plain during 2016—2018 based on InSAR and Sentinel-1A data. Remote Sensing for Natural Resources, 2021, 33(4): 55-63.

链接本文:

https://www.gtzyyg.com/CN/10.6046/zrzyyg.2020341 或 https://www.gtzyyg.com/CN/Y2021/V33/I4/55

Fig.1 研究区概况示意图

Tab.1 Sentinel-1A影像信息

Fig.2 2016—2018年京津冀平原区PS-InSAR地表形变速率

Fig.3 2016—2018年各年度InSAR平均形变速率

Fig.4 剖面时间序列InSAR形变速率结果

Fig.5 研究区内沉降特征点对应时序特征

Fig.6 InSAR结果与水准测量结果精度验证

Tab.2 InSAR所得形变信息与水准测量结果比对

Fig.7 多轨SAR影像形变速率交叉验证结果

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