基于多源遥感数据的白龙江黑多古滑坡体变形特征、破坏模式及其影响因素分析

    DEFORMATION CHARACTERISTICS AND FAILURE MODE OF HEIDUO ANCIENT LANDSLIDE DEPOSITS IN BAILONG RIVER, AND ITS IMPACT FACTOR ANALYSIS BASED ON MULTI-SOURCE REMOTE SENSING DATA

    • 摘要: 古滑坡堆积体复活往往导致位于滑坡堆积体之上或者之下的居民房屋、道路、输电线塔等建构筑物发生严重毁损破坏。该复活致灾过程同时也是古滑坡堆积体裂缝生成扩展、结构解体、滑动破坏的渐进变形和时空效应过程。基于2007~2021年共6期多源高清卫星遥感数据和无人机影像,测量滑坡裂缝相对位移量并计算位移速率,本文研究了白龙江流域上游黑多村古滑坡堆积体的变形特征和裂缝空间展布形式,分析了其破坏模式和影响因素。研究表明:(1)古滑坡堆积体沿基覆界面发生慢速滑动,周缘裂缝贯通圈闭,内部鼓胀裂缝发育并导致滑坡体局部解体;(2)古滑坡堆积体两侧边界的相对位移量均表现为上部大于下部,呈现典型的推移式滑坡的渐进变形特征;(3)古滑坡堆积体顺边界剪切裂缝发生右向偏转运动,造成右侧边界裂缝相对位移量和位移速率小于左侧边界对应值;(4)古滑坡堆积体年位移速率与年降雨量呈现较好的正相关关系,同时也受到2008年汶川MS8.0地震的远程效应和公路切坡扰动的影响。这表明基于多源多期高清遥感数据的变形测量是进行古滑坡体灾前变形探测和预测的有效技术手段,可为白龙江流域大量慢速滑坡变形监测提供有益参考。

       

      Abstract: The revival of ancient landslide deposits often leads to serious damage of residential buildings,roads,power transmission towers,and other structures located above or below the landslide deposits. It is also a process of progressive deformation and spatio-temporal effect of crack generation and expansion,structure disintegration,and sliding failure of ancient landslide deposits. Based on six periods of multi-source high-resolution satellite remote sensing data and UAV images from 2007 to 2021,the relative displacement along landslide cracks was measured and the slip rate was calculated. In this paper,the deformation characteristics and crack spatio-temporal distribution of the ancient landslide deposits in Heiduo Village,in the upper reaches of the Bailong River Basin,were studied,and the failure modes and influencing factors were analyzed. The results show that:(1)the ancient landslide deposits are sliding slowly along the interface between the lower bedrock and the upper deposit,the marginal cracks have completely connected with close-up,and the internal swelling cracks develop and lead to the partial disintegration of the landslide body; (2)The relative displacements in the upper part of the ancient landslide deposit are larger than those in the lower part at both margins,showing the progressive deformation characteristics of a typical push-type landslide; (3)The ancient landslide deposit moves toward the right along the marginal cracks,resulting in the relative displacement and slip rate at the right part being larger than the corresponding values at the left part; (4)The annual slip rate of ancient landslide deposits is positively correlated with the annual rainfall and is also affected by the remote effect of the 2008 Wenchuan MS8.0 earthquake and the disturbance of road-slope cutting. It shows that deformation measurement based on multi-source and multi-period high-resolution remote sensing data is an effective technique for detecting and predicting the deformation of ancient landslides and could provide helpful reference for other slow-moving landslides in the Bailong River.

       

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