测绘通报 ›› 2025, Vol. 0 ›› Issue (2): 77-82.doi: 10.13474/j.cnki.11-2246.2025.0214

• 学术研究 • 上一篇    下一篇

基于坡向约束的高寒矿区边坡InSAR三维形变分析

沈显名1, 李素敏1,2, 郭军3, 毛嘉骐1, 严胜航1, 戴祚敏1, 彭翔1   

  1. 1. 昆明理工大学国土资源工程学院, 云南 昆明 650093;
    2. 云南省高校高原山区空间信息测绘技术应用工程研究中心, 云南 昆明 650093;
    3. 玉溪大红山矿业有限公司, 云南 玉溪 653100
  • 收稿日期:2024-06-11 发布日期:2025-03-03
  • 通讯作者: 李素敏。E-mail:153064487@qq.com
  • 作者简介:沈显名(1999—),男,硕士,研究方向为InSAR三维形变监测。E-mail:2896677849@qq.com
  • 基金资助:
    国家自然科学基金(52364020;42161067);云南省基础研究计划(202301AT070463)

Slope constraint-based 3D InSAR deformation analysis in alpine mining areas

SHEN Xianming1, LI Sumin1,2, GUO Jun3, MAO Jiaqi1, YAN Shenghang1, DAI Zuomin1, PENG Xiang1   

  1. 1. Faculty of Land and Resources Engineering, Kunming University of Science and Technology, Kunming 650093, China;
    2. Surveying and Mapping Geo-Technology Research Center on Plateau Mountains of Yunnan Higher Education, Kunming 650093, China;
    3. Yuxi Dahongshan Mining Co., Ltd., Yuxi 653100, China
  • Received:2024-06-11 Published:2025-03-03

摘要: 高寒矿区边坡地质环境脆弱,冻胀融沉作用下矿区边坡稳定性易发生破坏。为获取高寒矿区反复冻融下精确的三维形变特征,根据重力作用下边坡物质向最大地形落差方向发生滑移的特点,本文选取西藏某矿区边坡为研究对象,以坡向约束为先验条件,联合SBAS-InSAR构建三维形变模型。结果显示:该矿区两年多内东西向最大累计沉降量为-78 mm,垂直向最大累计沉降量为-38 mm,南北向最大累计沉降量为-25 mm,主要形变发生在采场下方,露天采场较为稳定;通过截取矿区剖面线对滑移边坡进行时空演化分析发现,位移随深度的增加逐渐减小,冻胀融沉仅发生在活动层表面;三维形变分析发现,温度变化引起的冻胀融沉和集中降水对边坡在垂直向和东西向形变影响较大,南北向变化相对较小。本文计算结果较为可靠,该探索为高寒矿区的大尺度遥感边坡监测提供了一定的参考价值。

关键词: 高寒矿区边坡, 坡向约束, SBAS-InSAR, 三维形变, 冻胀融沉

Abstract: The geological environment of the high-altitude cold mine slope is fragile,and the stability of the mine slope is easy to be destroyed under the action of frost,swelling,thawing and sinking.In order to obtain accurate 3D deformation characteristics under the condition of repeated freezing and thawing in high-altitude cold mines,and according to the features of slope materials sliding to the direction of maximum topographic drop under the action of gravity,this paper selects a certain slope in Jiama mine area in Tibet as the research object,takes slope direction constraint as prior condition,and constructs the 3D deformation model by jointing SBAS-InSAR.The results show that within more than two years the maximum cumulative sinking amount of the mine in east-west direction is -78 mm,the maximum cumulative sinking amount in vertical direction is -38 mm,and the maximum cumulative sinking amount in north-south direction is -25 mm.The main deformation occurs below the mining area,and the open-pit mining area is relatively stable.Through cutting out the mine profile line to analyse time-space evolution of sliding slope,it can be found that displacement gradually decreases with depth increase,and frost,swelling,thawing and sinking only occur on the surface of active layer.3D deformation analyses show that frost,swelling,thawing,and sinking and concentrated rainfall induced by temperature change have greater influence on the deformation of the slope in vertical and east-west directions,while the influence in north-south direction is relatively small.The calculation results of this paper are reliable,which provides some reference value for large-scale remote sensing slope monitoring in high-altitude cold mine areas.

Key words: slope of alpine mining area, aspect constraints, SBAS-InSAR, 3D deformation, frost heave and thawing

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