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Monitoring Land Subsidence in Wuhan City (China) using the SBAS-InSAR Method with Radarsat-2 Imagery Data

机译:利用SBAS-InSAR方法和Radarsat-2影像数据监测武汉市的地面沉降

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摘要

Wuhan city is the biggest city in central China and has suffered subsidence problems in recent years because of its rapid urban construction. However, longtime and wide range monitoring of land subsidence is lacking. The causes of subsidence also require further study, such as natural conditions and human activities. We use small baseline subset (SBAS) interferometric synthetic aperture radar (InSAR) method and high-resolution RADARSAT-2 images acquired between 2015 and 2018 to derive subsidence. The SBAS-InSAR results are validated by 56 leveling benchmarks where two readings of elevation were recorded. Two natural factors (carbonate rock and soft soils) and three human factors (groundwater exploitation, subway excavation and urban construction) are investigated for their relationships with land subsidence. Results show that four major areas of subsidence are detected and the subsidence rate varies from −51.56 to 27.80 millimeters per year (mm/yr) with an average of −0.03 mm/yr. More than 83.81% of persistent scattered (PS) points obtain a standard deviation of less than −6 mm/yr, and the difference between SBAS-InSAR method and leveling data is less than 5 mm/yr. Thus, we conclude that SBAS-InSAR method with Radarsat-2 data is reliable for longtime monitoring of land subsidence covering a large area in Wuhan city. In addition, land subsidence is caused by a combination of natural conditions and human activities. Natural conditions provide a basis for subsidence and make subsidence possible. Human activities are driving factors and make subsidence happen. Moreover, subsidence information could be used in disaster prevention, urban planning, and hydrological modeling.
机译:武汉市是中国中部最大的城市,由于其快速的城市建设,近年来遭受了沉降问题。但是,缺乏对地面沉降的长期和广泛监测。沉陷的原因还需要进一步研究,例如自然条件和人类活动。我们使用小型基线子集(SBAS)干涉合成孔径雷达(InSAR)方法和2015年至2018年之间获取的高分辨率RADARSAT-2图像来得出沉降。 SBAS-InSAR结果通过56个水平基准进行了验证,其中记录了两次海拔读数。研究了两个自然因素(碳酸盐岩和软土)和三个人为因素(地下水开采,地铁开挖和城市建设)与地面沉降的关系。结果表明,发现了四个主要沉降区域,沉降速率从每年-51.56到27.80毫米(mm / yr)不等,平均为-0.03 mm / yr。超过83.81%的持久性散射(PS)点获得的标准偏差小于-6 mm / yr,并且SBAS-InSAR方法与水准测量数据之间的差小于5 mm / yr。因此,我们得出结论,利用Radarsat-2数据的SBAS-InSAR方法对于武汉市大面积土地沉降的长期监测是可靠的。此外,地面沉降是自然条件和人类活动共同造成的。自然条件为沉降提供了基础,并使沉降成为可能。人类活动是驱动因素并使沉降发生。此外,沉陷信息可用于防灾,城市规划和水文建模。

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