首页|基于SBAS-InSAR的城市地面沉降特征及其与易涝点关系分析

基于SBAS-InSAR的城市地面沉降特征及其与易涝点关系分析

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在全球气候变化背景下极端暴雨事件频发,很多城市出现严重内涝,造成人民生命财产巨大损失。为分析沿海城市地面沉降与内涝之间的联系,以广州市南沙区为例,选择2017-2023年20景哨兵1号影像为数据源,利用SBAS-InSAR技术分析地面沉降特征,对地面易涝点时序沉降量与降水量、积水深度、积水持续时间等进行相关性分析。结果表明:①南沙区平均沉降速率为1。363 mm/a,沉降区域主要位于河流沿岸、施工区域、围垦区域,6 a平均累计沉降量为-10。05 mm,沉降剧烈区域有扩大趋势;②区域季节强降水可以在一定程度上缓解地面沉降,下沉或平稳类易涝点沉降时序过程与降水量的季节变化同步,且降水量季节性越明显,下沉趋势越平缓;③城市化进程和自然地理条件共同作用于地表形变,南沙区强降雨引发的易涝点主要包括局部低地,立交桥底、地铁隧道口,以及排水管道系统设置不合理或超过排泄能力等3种类型。针对各易涝点地表形变时间演变特征和积水影响程度,分别溯源其内涝诱发原因,为进一步提出防治对策措施提供了参考。
Urban Land Subsidence Characteristics and Their Relationship with Locations Liable to Waterlogging Based on SBAS-InSAR
Under the background of global climate change,extreme rainstorm events occur frequently,and many cities have suffered from serious waterlogging,resulting in huge losses of people's lives and property.In order to analyze the relationship between urban land subsidence and waterlogging in coastal cities,this paper took Nansha District of Guangzhou as an example and selected 20 scenes of Sentinel-1 images from 2017 to 2023 as data sources.SBAS-InSAR technology was used to analyze land subsidence characteristics,and the correlation between the temporal subsidence of land waterlogging points and precipitation,water depth,and waterlogging duration was analyzed.The results show that:① the average subsidence rate in Nansha District is 1.363 mm/a,and the subsidence area is mainly located in the river bank,construction area,and reclamation area.The average cumulative subsidence within six years is-10.05 mm,and the area with severe subsidence tends to expand.② Regional seasonal heavy precipitation can alleviate land subsidence to a certain extent.The temporal subsidence process of sinking or stationary waterlogging points is synchronized with the seasonal variation of precipitation,and more obvious seasonal precipitation indicates a more gentle subsidence trend.③The urbanization process and natural geographical conditions work together on the surface deformation.The waterlogging points caused by heavy rainfall in Nansha District mainly include local lowlands,overpass bottom,subway tunnel entrance,the unreasonable layout of the drainage pipeline system,or waterlogging that exceeds drainage capacity.According to the temporal evolution characteristics of surface deformation and the influence degree of water accumulation in each waterlogging point,the causes of waterlogging were traced respectively,which provided a reference for further prevention and control measures.

Sentinel 1SBAS-InSARtemporal deformationwater depthprecipitation

刘桓语、吴臻、余煌浩、陈广成、肖洋、李匡、李彬权

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河海大学水文水资源学院,江苏 南京 210098

广州市南沙区水务局,广东 广州 510640

河海大学水利部水循环与水动力系统重点实验室,江苏 南京 210024

中国水利水电科学研究院,北京 100038

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哨兵1号 SBAS-InSAR 时序形变 积水深度 降水量

2025

人民珠江
水利部珠江水利委员会

人民珠江

影响因子:0.406
ISSN:1001-9235
年,卷(期):2025.46(1)