基于时序 InSAR 的北京地表形变监测与沉降机制分析

Jinghui Wang, Ziyan Luo, Lv Zhou, Xinyi Li, Cheng Wang, Dongming Qin
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摘要

摘要本文利用覆盖北京的 43 幅 Sentinel-1A 图像数据集,获取了研究区域 2022 年 1 月至 2023 年 10 月的地表形变时间序列信息。结合降水和城市建设分析了地面沉降的成因。主要研究成果如下(1) 在北京市朝阳区东部(沉降区 A)、北京市通州区西北部(沉降区 B)和与北京相邻的河北省燕郊镇(沉降区 B)发现了三个明显的沉降区。沉降区 A 和 B 呈分散分布,最大地面沉降速率超过 -30 毫米/年。相比之下,沉降区 C 的沉降呈漏斗状,大部分地区的地面沉降速率超过-25 毫米/年,最大速率达到-45 毫米/年。(2)降水对研究区地表变形影响显著,降水与地面沉降之间存在较强的相关性,相关值分别为 0.77、0.77 和 0.74。(3)城市建设对地面沉降有一定影响,但不同地区影响程度不同。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Surface Deformation Monitoring and Subsidence Mechanism Analysis in Beijing based on Time-series InSAR
Abstract. This article uses 43 Sentinel-1A image datasets covering Beijing to obtain time series surface deformation information in the study area from January 2022 to October 2023. It analyzes the causes of land subsidence by integrating precipitation and urban construction. The main research results are as follows: (1) Three distinct subsidence areas are identified in the eastern part of Chaoyang District in Beijing (Subsidence Area A), the northwestern part of Tongzhou District in Beijing (Subsidence Area B), and Yanjiao Town in Hebei Province (Subsidence Area B), which is adjacent to Beijing. Subsidence Areas A and B exhibit a dispersed pattern, with maximum land subsidence rates exceeding −30 mm/year. In contrast, Subsidence Areas C displays a funnel-shaped subsidence, where the majority of areas experience land subsidence rates exceeding −25 mm/year, with a maximum rate reaching −45 mm/year. (2) Precipitation has a significant impact on surface deformation in the study area, and there is a strong correlation between precipitation and land subsidence, with correlation values of 0.77, 0.77, and 0.74, respectively. (3) Urban construction has a certain impact on land subsidence, but the degree of impact varies in different regions.
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