基于InSAR和热点分析技术的黄土高原地质灾害隐患识别

    DETECTION OF POTENTIAL GEOLOGICAL HAZARD IN LOESS PLATEAU BASED ON INSAR AND HOTSPOT ANALYSIS TECHNOLOGIES

    • 摘要: 黄土高原面积约64万km2,受到自然和人为因素的影响,近年来地质灾害呈现多发频发趋势,严重威胁了人民的生命财产安全。对黄土高原开展地质灾害隐患早期识别和动态监测,对当地防灾减灾具有重要意义。目前已开展的工作多集中于黄土高原局部范围内单一灾种的研究,缺乏全局尺度上多灾种的调查和分析。基于此,本文采用短基线干涉测量(SBAS-InSAR)技术,对覆盖整个黄土高原的1994景Sentinel-1A数据进行处理,得到了黄土高原2019年1月1日至2021年3月31日的年平均形变速率以及时间序列结果。采用热点分析技术提取了有效形变区域,在此基础上借助光学影像,采用人工目视判读的方法,识别出黄土高原3240处地质灾害隐患点,其中采矿沉陷1920处,地面沉降593处,滑坡727处。对灾害隐患点的空间分布规律及原因进行分析,得出采矿沉陷区域基本为煤炭资源分布区域,其与地层岩性具有较好的一致性,主要沿着地层岩性走向分布;地面沉降主要分布于城市区域,地下水开采和人类工程建设是主要驱动因素;地层岩性、人类活动、河流等都会对黄土高原滑坡的发育产生一定的影响,滑坡灾害点的分布与高程、坡度、坡向也存在一定的相关性,滑坡灾害点在高程1500~3000 m,坡度10°~30°,坡向北、东北、东、东南方向上分布较多。

       

      Abstract: The Loess Plateau with an area of about 640,000 km2 has experienced and is experiencing the severe geological hazards due to the complex natural condition and intensive human activities,threatening the safety of people's lives and property. It is urgent to detect and monitor the potential geological hazards in the Loess Plateau with purpose of preventing and mitigating the disasters. However,the existed studies focused on the isolated disaster investigation over the small-scale region,and there was a lack of multi disasters investigations over the whole Loess Plateau. In this context,we used the SBAS-InSAR technology to process 1994 Sentinel-1A images,and obtained the annual deformation rate and time series deformation spanning from January 1,2019 to March 31,2021 over the whole Loess Plateau. Then,we employed the hot spot analysis technology to extract the effective deformation area. On this basis,with the help of optical images and manual visual interpretation,a total of 3240 potential geological hazards in the Loess Plateau were identified,including 1920 mining sinkholes,593 subsiding regions and 727 landslides. After that,we analyzed the spatial distribution laws and causes of detected geological hazards,and concluded that the mining sinkholes distribute along the regions with rich coal resources,and had a good consistency with the lithology of the stratum. The subsiding regions mainly concentrates in the cities,where the over-exploitation of groundwater and intensive human activities were conducted in the last few decades. For the landslides,they are correlated with the stratigraphic lithology,human activities and rivers. The results show that the detected landslides are located in the elevation of 1500~3000 m,the slope of 10°~30°,and the slope aspect of the north,northeast,east and southeast directions.

       

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