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Mapping and interpreting of subsidence in West Tianjin with high spatiotemporal x-band persistent scatterer SAR interferometry

机译:高时空x波段持续散射SAR干涉仪在津西沉降的制图与解释

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Ground subsidence in West Tianjin area is explored by means of the persistent scatterer (PS) networking interferometric synthetic aperture radar (PSNInSAR) technique. The pivotal algorithm of the PSNInSAR is briefly represented and the computation is based on 15 high spatiotemporal resolution (HSTR) TerraSAR-X (TX) SAR images acquired between Mar., 2009 and Jan., 2010. The PS subsidence velocity map shows the maximum subsidence velocity as high as 56 to 68 mm/yr, implying that the study area is an active zone for ground deformation. The hydrogeological conditions in the area are examined to explore the mechanism of the uneven subsidence caused by excessive exploitation of groundwater. The derived subsidence measurements are validated with the in situ data taken by the optical leveling at 9 benchmarks, which implies the HSTR PSNInSAR with short radar wavelength (3.1 cm for TX) can reach an accuracy of millimeter (±4.09 mm/yr in our work). The results demonstrate that the HSTR PSNInSAR is of great advantage to detect subsidence and can help to reveal the spatial evolution of the subsidence phenomenon. Advisably, based on the results above and the chief parameters of the radar sensor, the predominance and limitations of the high spatiotemporal TX SAR interferometry in subsidence detecting are discussed.
机译:通过持续散射(PS)网络干涉式合成孔径雷达(PSNInSAR)技术探索了天津西部地区的地面沉降。简要介绍了PSNInSAR的关键算法,其计算基于2009年3月至2010年1月之间采集的15张高时空分辨率(HSTR)TerraSAR-X(TX)SAR图像。PS沉降速度图显示了最大沉降速度高达56到68 mm / yr,这意味着研究区域是地面变形的活跃区域。研究了该地区的水文地质条件,以探讨由于过度开采地下水引起的沉降不均的机理。得出的沉陷测量值已通过光学水准仪在9个基准点处获得的原位数据进行了验证,这意味着短雷达波长(TX为3.1 cm)的HSTR PSNInSAR可以达到毫米的精度(在我们的工作中为±4.09 mm / yr )。结果表明,HSTR PSNInSAR在探测沉降方面具有很大的优势,可以帮助揭示沉降现象的空间演化。明智的是,基于以上结果和雷达传感器的主要参数,讨论了高时空TX SAR干涉仪在沉降检测中的优势和局限性。

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