沙特, 罗勇, 雷坤超, 田芳, 王新惠. 0: 基于分布式光纤传感技术的北京宋庄地面沉降和地裂缝综合监测. 地质通报. DOI: 10.12097/gbc.2023.09.003
    引用本文: 沙特, 罗勇, 雷坤超, 田芳, 王新惠. 0: 基于分布式光纤传感技术的北京宋庄地面沉降和地裂缝综合监测. 地质通报. DOI: 10.12097/gbc.2023.09.003
    Te SHA, Yong LUO, Kunchao LEI, Fang TIAN, Xinhui WANG. 0: Comprehensive Monitoring of Land Subsidence and Ground Fissures in Songzhuang, Beijing Based on Distributed Optical Fiber Sensing Technology. Geological Bulletin of China. DOI: 10.12097/gbc.2023.09.003
    Citation: Te SHA, Yong LUO, Kunchao LEI, Fang TIAN, Xinhui WANG. 0: Comprehensive Monitoring of Land Subsidence and Ground Fissures in Songzhuang, Beijing Based on Distributed Optical Fiber Sensing Technology. Geological Bulletin of China. DOI: 10.12097/gbc.2023.09.003

    基于分布式光纤传感技术的北京宋庄地面沉降和地裂缝综合监测

    Comprehensive Monitoring of Land Subsidence and Ground Fissures in Songzhuang, Beijing Based on Distributed Optical Fiber Sensing Technology

    • 摘要: 针对地面沉降及地裂缝,传统点式监测技术手段难以实现地质体变形的连续监测,且无法通过地面沉降、地裂缝的综合监测定量分析两者之间的关系。基于钻孔全断面分布式光纤监测技术实现了地面沉降和地裂缝同步监测,根据监测结果对宋庄地区地下水-地面沉降-地裂缝之间的关系进行了分析。监测结果表明:北京宋庄地面沉降主要受到地下水开采影响,含水砂层抽水发生压缩变形,地裂缝两侧均存在明显的地面沉降,且差异沉降显著;差异沉降量和地裂缝变形量均持续增大,但增大速率放缓。地面沉降、地裂缝同步监测结果表明,该地区地裂缝发育主要受地层差异沉降影响。

       

      Abstract: For land subsidence and ground fissures, it is difficult for traditional point measurement to realize monitoring of the deformation of the strata, and the relationship between land subsidence and ground fissures cannot be quantitatively analyzed through comprehensive monitoring. Based on the full-section optical fiber monitoring technology of borehole and distributed optical fiber monitoring technology, this paper realized the synchronous monitoring of land subsidence and ground fissures. Based on the monitoring results, the relationship between groundwater, land subsidence and ground fissures in Songzhuang is analyzed .The monitoring results show that the land subsidence in Songzhuang is mainly affected by groundwater exploitation. The pumping of the water-bearing sand layer is compressed and the land subsidence is obvious on both sides of the ground fissures, and uneven subsidence is obvious on both sides of the ground fissures. Both the uneven subsidence and ground fissures deformation increase continuously, but the increase rate slows down. The synchronous monitoring results of land subsidence and ground fissures show that the development of ground fissures in this area is mainly affected by the differential subsidence of strata. 

       

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