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乌长高速金旗特大桥高陡岸坡稳定性分析研究

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贵州省乌长高速公路金旗特大桥跨越猫跳河,两岸岸坡危岩体及崩塌堆积体等不良地质条件较发育,严重影响桥梁选址及其安全.为研究该桥高陡岸坡的稳定性,该文通过空天地一体化综合勘察,查明了桥址区主要不良地质条件.结合数值分析及InSAR等技术手段,定量表征了岸坡危岩体的运动威胁范围,阐明了岸坡堆积体在内外动力作用下的稳定性及变形失稳模式.结果表明:① 桥址区不良地质主要表现为陡崖卸荷带、危岩体和崩塌堆积体,危岩体的失稳破坏模式为拉裂‒倾倒式;② W1、W3和W4危岩体失稳后的运动距离分别为65 m、57 m和320 m,影响乌当岸桥台和长顺岸桥墩;③ 乌当岸坡堆积体在天然、降雨、降雨+地震3种工况下均处于稳定状态;长顺岸坡堆积体在天然和降雨条件下较稳定,在降雨+地震工况下上部堆积体与基岩接触面处剪切塑性区完全贯通,处于不稳定状态,其失稳破坏模式为蠕滑‒拉裂式.该研究结果可为贵州省深切峡谷及陡崖地区桥梁高陡岸坡的综合勘察和稳定性分析提供参考和借鉴.
Stability Analysis of High and Steep Bank Slope of Jinqi Bridge on Wudang-Changshun Expressway
Jinqi Bridge on the Wudang-Changshun Expressway in Guizhou Province crosses the Maotiao River,and the poor geological conditions such as dangerous rock mass and collapse accumulation body on the bank slope of the river are relatively developed,which seriously affects the site selection and safety of the bridge.In order to study the stability of the high and steep bank slope of the bridge,the paper explored the main poor geological conditions in the bridge site through a comprehensive air-ground investigation.By means of numerical analysis,InSAR,and other technologies,the movement range of dangerous rock mass on the bank slope was quantitatively evaluated.The stability and deformation mode of the accumulation body on the bank slope under the action of internal and external dynamics were elucidated.The results show that:① The poor geological conditions in the bridge site are mainly cliff unloading zone,dangerous rock mass,and collapse accumulation body,and the failure mode of dangerous rock mass is pulling-toppling;② The movement distance of W1,W2,and W3 dangerous rock mass after failure is about 65 m,57 m,and 320 m,respectively,which affects the Wudangan abutment and Changshun pier;③ The accumulation body on the Wudang bank slope is very stable under normal,rainfall,and rainfall+earthquake conditions.The accumulation body on the Changshun bank slope is stable under normal and rainfall conditions.Under the rainfall+earthquake conditions,the shear plastic zone at the contact surface between the upper accumulation body and the bedrock is completely connected,and the accumulation body is in an unstable state.The failure mode is creep-pulling.The research results can provide a reference for comprehensive investigation and stability analysis of high and steep bank slopes of bridges in deep canyons and steep cliffs in Guizhou Province.

highway bridgestabilitynumerical calculationcomprehensive investigationhigh and steep bank slopedangerous rock mass

王浩

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中铁第一勘察设计院集团有限公司,陕西 西安 710043

公路桥梁 稳定性 数值计算 综合勘察 高陡岸坡 危岩体

国家自然科学基金重点资助项目国家自然科学基金资助项目

4183129042077263

2024

中外公路
长沙理工大学

中外公路

CSTPCD
影响因子:0.626
ISSN:1671-2579
年,卷(期):2024.44(4)
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