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基于SBAS-InSARR技术的离层注浆结束后地表沉降监测与分析

Monitoring and analysis of surface subsidence after separation grouting based on SBAS-InSARR technology

  • 摘要: 为揭示注浆结束后矿区地表沉降的长期演化特征及其形成原因, 采用小基线集合成孔径雷达干涉测量(SBAS-InSARR)技术, 对2023–10–02—2025–05–12期间的45景Sentinel-1 A升轨影像数据进行时序处理, 反演了研究区地表沉降信息。研究结果表明: 注浆结束后工作面区域内年平均沉降速率主要分布在10~40 mm/a, 占监测点的84%以上, 区域地表变形总体受控, 但局部区域仍存在明显沉降; 地表沉降随时间持续增加而沉降速率逐渐减缓, 呈现典型残余沉降特征, Kelvin蠕变模型能够较好地刻画其时序演化过程。通过对比分析注浆结束后与未注浆情况下的地表沉降特征发现, 实施离层注浆后, 地表沉降衰减更快, 且最终残余沉降值相对较小。进一步结合体积守恒模型分析表明, 注浆量是影响注浆结束后地表残余沉降的重要因素, 注浆量较大的区域离层与裂隙充填更充分, 覆岩体系残余可压缩空间较小, 其对应的地表残余沉降小于注浆量较小的区域。通过与水准测量数据对比验证, SBAS-InSARR技术反演结果与实测沉降趋势一致, 均方根误差(RMSE)为7.4 mm, 平均差值为5.3 mm, 表明该技术用于注浆结束后地表沉降监测具有较高的可靠性。

     

    Abstract: In order to reveal the long-term evolution characteristics and causes of surface subsidence in the mining area after grouting, the small baseline synthetic aperture radar interferometry technology was used to process the time series of 45 Sentinel-1 A ascending image data from October 2, 2023 to May 12, 2025, and the surface subsidence information in the study area was inverted. The results show that the annual average subsidence rate in the working face area after grouting is mainly distributed in the range of 10-40 mm/a, accounting for more than 84% of the monitoring points, indicating that surface deformation in the area is generally controlled, although obvious subsidence still occurs in some local areas; surface subsidence increases continuously with time while the subsidence rate gradually slows down, exhibiting typical residual subsidence characteristics, which can be well described by the Kelvin creep model. By comparing and analyzing the characteristics of surface subsidence after grouting and non-grouting conditions, it is found that after the implementation of separation grouting, the surface subsidence decays faster, and the final residual subsidence value is relatively small. Further analysis combined with the volume conservation model shows that, it can be seen that the grouting volume is an important factor affecting residual surface subsidence after grouting, areas with larger grouting volumes are more fully filled with separations and fractures, the residual compressible space of the overburden system is smaller, and the corresponding residual surface subsidence is lower than that in areas with smaller grouting volumes. Through comparison and validation with leveling measurement data, the surface subsidence results retrieved by the SBAS-InSARR technique are consistent with the measured subsidence trends, with a root mean square error of 7.4 mm and an average difference of 5.3 mm, indicating that this technique has high reliability for monitoring surface subsidence after the completion of grouting.

     

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