基于InSAR评估地下水位回升对太原市地面沉降的影响
Land subsidence caused by groundwater level recovery in Taiyuan City
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摘要: 过去几十年中,太原市地下水的过度开采导致地下水位大幅下降,造成严重的地面沉降。近年来,太原市大力实施严格的地下水资源管理措施和“引黄入晋”引水工程项目,极大地缓解了地下水超采现状,地下水位逐步回升。因此,需要科学评估地下水位回升对地面沉降的影响效应。研究利用ENVISAT 2003—2010年和Sentinel-1 2017—2021年2个时间段的合成孔径雷达(synthetic aperture Radar,SAR)数据,基于永久散射体干涉测量技术(persistent scatterer interferometric SAR,PS-InSAR)提取太原市2个时段的地面沉降信息,以此比较不同历史时段地面沉降的演变情况,并结合太原市地下水开采量、“引黄入晋”引水量以及地下水位数据进行对比分析。结果表明: 太原市地面沉降得到极大缓解,城区已由地面沉降转为地面抬升; 在沉降最为严重的小店区,地面沉降面积增大,但整体地面沉降速率减弱,沉降中心发生南移; 太原地面沉降减缓甚至地面抬升的主要原因是地下水开采量的逐年减少和引水工程导致的地下水位持续回升。研究成果可以为太原市地下水位回升条件下地面沉降精细化防控和地下水管理提供科学依据。Abstract: Over the past few decades, excessive groundwater exploitation has led to a significant decrease in the groundwater level and serious land subsidence in Taiyuan City. In recent years, Taiyuan has vigorously implemented strict groundwater management measures and the project of water diversion into Shanxi from the Yellow River, substantially alleviating groundwater overexploitation and gradually recovering groundwater levels in the city. Therefore, it is necessary to scientifically assess the effect of groundwater level revovery on land subsidence. Based on 2003—2010 synthetic aperture radar (SAR) data from ENVISAT and 2017—2021 SAR data from Sentinel-1, this study extracted the land subsidence information of Taiyuan City of both periods using persistent scatterer interferometric SAR (PS-INSAR). Accordingly, this study compared and analyzed the temporal evolution of land subsidence during the two periods by combining the groundwater extraction volumes, water volumes diverted from the water diversion project, and data on groundwater levels. The results show that the land subsidence in Taiyuan City has been significantly mitigated, with the urban area having shifted from subsidence to uplift. In the Xiaodian area, which underwent the most serious land subsidence, the subsidence area expanded. Nevertheless, the overall land subsidence rate decreased, and the subsidence center has moved southward. The main cause for the slowdown of the land subsidence and even the land uplift in Taiyuan is the continuous groundwater level recovery attributed to the reduced groundwater exploitation and the water diversion project. The results of this study provide a scientific basis for fine-scale land subsidence prevention and groundwater management in Taiyuan City under conditions of groundwater level recovery.
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