利用PS-DInSAR和SBAS方法监测天津市地面沉降

H. Fan, K. Deng, C. Zhu, Jiqun Xue
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引用次数: 0

摘要

由于地下水的过度开采,天津市地面沉降日益严重。一些研究人员试图使用D-InSAR技术来监测该地区的下沉情况。但是,D-InSAR存在时空基线去相关和大气影响等问题。为了获得高精度的长时间序列地表形变,SAR影像集监测地表沉降已成为研究热点。PSDInSAR (Persistent Scatterers-DInSAR)和SBAS (Small Baseline Sets)是利用SAR图像监测地面沉降的两种经典方法。前者根据基线阈值选择一幅图像作为主图像,后者根据基线阈值选择多幅图像作为主图像。利用18幅ERS影像和SRTM DEM资料,采用上述两种方法获得了天津市1992 ~ 1998年的地面沉降。PS- dinsar和SBAS分别鉴定出18906和42041个PS点。平均最大沉降速度分别为16.4 mm/a和24.2 mm/a。虽然数值不同,但各点的分布和沉降规律基本一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Monitoring land subsidence by PS-DInSAR and SBAS methods in Tianjin City
Because of groundwater over-exploitation, the land subsidence of Tianjin city has become more and more serious. Some researchers tried to use D-InSAR technique to monitor the subsidence of this area. However, D-InSAR has some problems such as space and time baseline decorrelation and atmospheric influence. In order to obtain long time series land deformation with high accuracy, SAR image set to monitor land subsidence has become a research focus. PSDInSAR (Persistent Scatterers-DInSAR) and SBAS (Small Baseline Sets) are two classical methods to monitor land subsidence by SAR images. The former chooses one image as the master and the latter chooses several images as the masters according to the threshold of baselines. Using eighteen ERS images and SRTM DEM data the land subsidence of Tianjin city from 1992 to 1998 was obtained by two methods mentioned. 18906 and 42041 PS points were identified respectively by PS-DInSAR and SBAS. While, 16.4 mm/a and 24.2 mm/a of the mean maximal subsidence velocities were obtained respectively. Although they are different in values, the distributions and subsidence laws of points are nearly same.
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