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基于陆探一号SAR卫星的海州露天矿地表形变时空特征分析

Analysis of spatiotemporal characteristics of surface deformation in Haizhou Open-Pit Mine based on LT-1 SAR satellite

  • 摘要: 为掌握海州露天矿地表形变时空分布规律, 采用我国首个L波段差分干涉SAR卫星组陆探一号(LT-1), 收集了39景2023年5月至2025年1月的升轨、降轨LT-1 SAR影像, 联合采用D-InSAR、PSInSAR等技术开展矿区地表形变时空特征分析, 并结合光学遥感影像验证分析结果的可靠性。结果显示, 海州露天矿南帮沉陷最为明显, 东、西帮及中部区域也存在不稳定区域, 但形变量较南帮小;矿区面积约6.300 km2, 其中形变速率超过0.50 m/a的区域面积为0.146 km2, 约占总面积的2.3%, 形变速率在0.20 ~0.50 m/a内的区域面积为0.648 km2, 约占总面积的10.3%;LT-1 SAR数据在降轨、升轨2个观测角度下反映的变形区范围基本一致, 但形变速率的量值上差异明显, 升轨变形速率普遍低于降轨变形速率, 表明升轨敏感性较低;在南帮和东帮范围内降轨数据观测角度较优, 而西帮升轨数据观测角度较优, 结合升、降轨数据, 可完整地恢复矿区形变空间分布与过程状况。

     

    Abstract: To understand the spatiotemporal distribution patterns of surface deformation in the Haizhou Open-Pit Mine, China's first L-band differential interferometric SAR satellite constellation, LuTan-1 (LT-1), was utilized.A total of 39 ascending and descending LT-1 SAR images from May 2023 to January 2025 were collected.Techniques including D-InSAR and PSInSAR were employed to analyze the spatiotemporal characteristics of surface deformation in the mining area, with optical remote sensing images used to validate the reliability of the results.The findings reveal that the southern slope of the Haizhou Open-Pit Mine exhibits the most significant subsidence, while unstable areas also exist on the eastern and western slopes as well as the central region, though with lesser deformation magnitudes compared to the southern slope.The mining area covers approximately 6.300 km2, of which the region with a deformation rate exceeding 0.50 m/a accounts for an area of 0.146 km2, representing about 2.3% of the total area.The area with deformation ranging between 0.20 m/a and 0.50 m/a is 0.648 km2, constituting approximately 10.3% of the total area.The spatial extent of deformation detected by LT-1 SAR data is generally consistent between ascending and descending orbits, though notable differences exist in the magnitude of deformation rates, with the ascending orbit generally exhibiting lower deformation rates compared to the descending orbit, indicating its lower sensitivity.The descending orbit data provide better observational angles forthe southern and eastern slopes, while the ascending orbit data are more suitable for the western slope.By integrating data from both ascending and descending orbits, the spatial distribution and temporal evolution of deformation in the mining area can be comprehensively reconstructed.

     

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