利用Sentinel-1 SAR干涉测量法监测巴西累西腓市的地面沉降

A. M. Ruiz-Armenteros, W. Souza, J. Cabral
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摘要

世界上地面沉降的主要原因之一是开采超过含水层系统再生能力的地下水。然而,河口地区的快速城市增长也可能促进这一现象的发展。巴西东北部城市累西腓就是一个例子。城市建在由几条河流组成的河口平原上(Capibaribe, Beberibe, Tejipió),这些河流的形成是由于潮湿地区和红树林的占领。近几十年来,由于地下水资源的过度抽取,一些地方深层含水层的压力水平下降了100多米。这些因素在累西腓的存在可能导致地面沉降。为了检测这种现象,采用了持续散射干涉合成孔径雷达(PSInSAR)技术。该数据集由2016年9月至2021年4月期间135张Sentinel-1A干涉宽(IW)单视复合体(SLC)图像组成。图像是在下降轨道和VV偏振下获得的。PSInSAR分析结果显示,累西腓有几个地区的地面沉降速度接近-15 mm/年。土壤沉降主要发生在西部大的新建区域,北部小的新建区域。由于地下水的开采,南部地区发生了轻微的病例。确定这些地面沉降区有助于研究城市排水系统,以避免出现水浸地点,并有助于采取缓解措施,以适当利用地下水资源。
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Monitoring of land subsidence in the city of Recife/Brazil using Sentinel-1 SAR interferometry
One of the main causes of land subsidence in the world is the exploitation of groundwater above the regeneration capacity of the aquifer systems. However, the rapid urban growth in estuarine areas can also contribute to the development of this phenomenon. An example of this occurs in the city of Recife, northeastern Brazil. The municipality is built on an estuarine plain composed of several rivers (Capibaribe, Beberibe, Tejipió), which formation results from the occupation of humid areas and mangroves. In recent decades, the excessive removal of water resources from the subsoil has caused the reduction of more than 100 meters of the deep aquifer piezometric level in some places. The presence of these factors in Recife may contribute to land subsidence. To detect this phenomenon, the Persistent Scatterer Interferometric Synthetic Aperture Radar (PSInSAR) technique was used. The dataset consisted of 135 Sentinel-1A Interferometric Wide (IW) Single Look Complex (SLC) images from September 2016 to April 2021. The images were acquired in descending orbits and VV polarization. The results of the PSInSAR analysis reveal that in Recife there are several areas of land subsidence with a rate close to -15 mm/year. The main occurrence of soil settlement is observed in large recently built areas in the west zone, and small areas in the north zone. Minor cases occur in the southern zone due to the exploitation of groundwater. The identification of these land subsidence areas can help in the study of urban drainage to avoid flooding sites and in the adoption of mitigating measures for the suitable use of underground water resources.
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