祁生文, 李永超, 宋帅华, 等. 2022. 青藏高原工程地质稳定性分区及工程扰动灾害分布浅析[J]. 工程地质学报, 30(3): 599-608. doi: 10.13544/j.cnki.jeg.2022-0172.
    引用本文: 祁生文, 李永超, 宋帅华, 等. 2022. 青藏高原工程地质稳定性分区及工程扰动灾害分布浅析[J]. 工程地质学报, 30(3): 599-608. doi: 10.13544/j.cnki.jeg.2022-0172.
    Qi Shengwen, Li Yongchao, Song Shuaihua, et al. 2022. Regionalization of engineering geological stability and distribution of engineering disturbance disasters in Tibetan Plateau[J]. Journal of Engineering Geology, 30(3): 599-608. doi: 10.13544/j.cnki.jeg.2022-0172.
    Citation: Qi Shengwen, Li Yongchao, Song Shuaihua, et al. 2022. Regionalization of engineering geological stability and distribution of engineering disturbance disasters in Tibetan Plateau[J]. Journal of Engineering Geology, 30(3): 599-608. doi: 10.13544/j.cnki.jeg.2022-0172.

    青藏高原工程地质稳定性分区及工程扰动灾害分布浅析

    REGIONALIZATION OF ENGINEERING GEOLOGICAL STABILITY AND DISTRIBUTION OF ENGINEERING DISTURBANCE DISASTERS IN TIBETAN PLATEAU

    • 摘要: 随着我国西部大开发等国家战略部署的相继实施以及某交通线路等重大工程的逐渐上马,青藏高原上的工程活动日趋增多。受快速隆升影响,高原内构造运动活跃,工程地质条件复杂,合理的场址选择成为制约重大工程安全建设与运营的关键。本文利用模糊数学方法选取全新世活动断裂及地形地貌作为评价因子,基于最大隶属度准则,对青藏高原全区工程地质稳定性进行分级。结果显示全区工程地质稳定性为差、较差、一般、较好和好的区域面积占比分别为:22.48%、18.01%、28.79%、22.72%和8.00%。对青藏高原全区的重大工程及其扰动灾害进行解译,共识别出重大工程铁路、公路、水电站、矿山等2176处;重大工程扰动灾害6562处,主要分布在工程地质稳定性为差和较差的区域,占比约69.66%。初步分析表明工程地质稳定性分区结果对青藏高原重大工程建设选址具有重要指导意义,自然灾害高发地段与工程扰动灾害有较高重合度。切坡扰动灾害主要发生在滑坡路段、厚层崩坡积路段以及强卸荷坡段,而水库诱发灾害主要类型表现为滑坡复活以及松散堆积物中的滑塌,并且随着蓄水年限增加灾害数量迅速减少。

       

      Abstract: The successive implementation of national strategic deployments(e.g., the Western Development) and the gradual launch of some giant engineering(e.g., Sichuan-Tibet Railway) have been increasing the engineering activities on the Tibetan Plateau. Affected by rapid uplift, the tectonic movement in the plateau is active and the engineering geological conditions are complex. Reasonable site selection becomes the key for safe construction and operation of giant engineering. In this paper, the distance from the Holocene active fault and the relief amplitude are selected as evaluation factors, and the membership method is used to classify the engineering geological stability of the Tibetan Plateau. The results show that the whole region can be divided into five zones based on the engineering geological stability, namely poor, relatively poor, medium, relatively good and good. And the corresponding proportions in the regional land area are 22.48%, 18.01%, 28.79%, 22.72% and 8.00%, respectively. By interpreting the giant engineering and their disturbance disasters in the Tibetan Plateau, a total of 2176 giant engineering projects(e.g., railways, highways, hydropower stations, mines) are identified. And 6562 disturbance disasters are identified and mainly distributed in the poor and relatively poor zones. They take accounts of 69.66% in the total. Preliminary analysis shows that the result of engineering geological stability zoning has great significance for guiding the site selection of giant engineering in the Tibetan Plateau. Engineering disturbance disasters mainly occur in the high occurrence areas of nature disasters. The slope-cutting disturbance disasters mainly occur in the areas where landslides, thick colluvial slopes and strong unloading slopes exist. The main types of reservoir-induced disasters are landslide revival and slump in loose deposits, and the number of these disasters decreases rapidly after water storage.

       

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