School of Resource and Environmental Sciences, Wuhan University, Wuhan 430079, China.
Key Laboratory of Geographic Information System, Ministry of Education, Wuhan University, Wuhan 430079, China.
Sensors (Basel). 2019 Feb 12;19(3):743. doi: 10.3390/s19030743.
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.
武汉市是中国中部最大的城市,由于其快速的城市建设,近年来一直存在地面沉降问题。然而,长期、大范围的地面沉降监测仍存在不足。沉降的原因还需要进一步研究,如自然条件和人类活动。我们使用小基线子集(SBAS)干涉合成孔径雷达(InSAR)方法和 2015 年至 2018 年期间获取的高分辨率 RADARSAT-2 图像来推导出沉降。SBAS-InSAR 结果通过 56 个水准基准点进行验证,其中记录了两次高程读数。研究了两种自然因素(碳酸盐岩和软土)和三种人为因素(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,检测到四个主要沉降区,沉降速率在-51.56 毫米/年至 27.80 毫米/年之间,平均为-0.03 毫米/年。超过 83.81%的持久散射(PS)点获得的标准偏差小于-6 毫米/年,并且 SBAS-InSAR 方法和水准数据之间的差异小于 5 毫米/年。因此,我们得出结论,使用 Radarsat-2 数据的 SBAS-InSAR 方法可用于可靠地长期监测武汉市大面积的地面沉降。此外,地面沉降是自然条件和人类活动共同作用的结果。自然条件为沉降提供了基础,使沉降成为可能。人类活动是驱动因素,使沉降发生。此外,沉降信息可用于灾害预防、城市规划和水文建模。