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Mechanical Analysis of Buckling Failure of Bedding Rock Slopes

机译:顺层岩质边坡屈曲破坏的力学分析

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摘要

As a typical model of steep-tilt or moderate-tilt bedding rock slopes, buckling failure differs greatly from tensile or shear failure. The mechanical characteristic of buckling failure is analyzed, and the geo-mechanics model of buckling failure is put forward. The process of buckling failure includes three phases: slope terrane creep deformation, the lower of slope terrane bend deformation, and terrane structure collapse. Using pressure bar failure theory, a formulation for calculating critical load of buckling failure is developed, which shows that critical load decreases with bend length increasing. The relationship between critical slope length and bend length is analyzed. It is indicated that critical slope length decreases with bend length increasing, and that critical slope length reaches minimal value while critical load is zero. The minimal slope length can be considered as a limit value while analyzing buckling failure of bedding slope, and its calculation equation is developed.
机译:作为陡倾或中倾顺层岩石坡度的典型模型,屈曲破坏与拉伸或剪切破坏有很大不同。分析了屈曲破坏的力学特性,提出了屈曲破坏的力学模型。屈曲破坏的过程包括三个阶段:斜坡地体蠕变变形,斜坡地体弯曲变形的下部和地形结构塌陷。利用压杆破坏理论,提出了一种计算屈曲破坏临界载荷的公式,该公式表明临界载荷随着弯曲长度的增加而减小。分析了临界斜率长度与弯曲长度之间的关系。结果表明,临界边坡长度随弯曲长度的增加而减小,临界边坡长度在临界载荷为零时达到最小值。在分析顺层边坡屈曲破坏时,可以将最小边坡长度作为极限值,并建立了计算公式。

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