摘要在三角形坡面递减的外荷载作用下,带岩架的边坡应力状态的变化

Zh. Bayalieva, B. Zhumabaev
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引用次数: 0

摘要

吉尔吉斯共和国的国土面积为1985,000平方公里。山脉和山坡占全国面积的94%以上。因此,在山区,山坡在山坡的不同高度,从几百米到4-5公里,都被用来进行各种类型的人类经济活动。研究的对象是山坡的边缘,它们是经济活动所必需的,位于斜坡的不同高度。研究的对象是在重力和构造力的作用下,山体陡坡附近岩体的初始和变化的应力-应变状态。本研究的目的是建立数学模型,计算山腰陡坡附近岩体的应力-应变状态,以校核在减小三角坡荷载作用下的边界条件。研究的目的是利用Kolosov-Muskhelishvili方法求解平衡微分方程,建立岩体各点的应力分布规律。岩架要么是自然形成的,要么是人类在技术上创造的,并与山坡在不同高度的不同倾斜角度相匹配。为了评价岩架带结构体在滑坡过程中的稳定性和安全性,有必要仔细研究岩体的应力-应变状态。为了研究岩体的应力状态,主要采用了以下几种方法:卸载法、有限元法、有限差分法以及采用保角映射的版本[Gulnara]中的Kolosov-Muskhelishvili的解析方法。因此,为了研究边坡岩架带岩体的状态,有必要建立边坡岩架岩体应力-应变状态的解析模型,该模型将岩架与边坡的共轭区、岩架的可能高度、体荷载和面荷载的影响综合考虑在一个单一的解析模型中。在这种情况下,作者考虑了在重力、水平构造力和外部分布荷载共同作用下形成的具有对称陡坡的山体在自然条件下的应力状态为三角形纯态的问题。利用Kolosov-Muskhelishvili方法和MATNCAD软件环境解决了该问题。计算的结果是,创建了具有岩架的山坡块体中的应力分布模式,其中分别考虑了重力和水平构造力的作用。为了检查边界条件与一个递减三角形图的载荷,计算应力的轮廓附近的轮廓点的轮廓部分的一部分。以应力等值线的形式给出了各应力分量的初始应力状态分布规律。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CHANGES IN THE STRESS STATE OF A MOUNTAIN SLOPE WITH A Ledge UNDER THE ACTION OF AN EXTERNAL LOAD WITH A DECREASING TRIANGULAR EPUR
The Kyrgyz Republic covers an area of – 198,5 thousand km2. Mountains and mountain slopes occupy more than 94 % of the country. For this reason, in mountainous areas, mountain slopes are used for conducting various types of human economic activity ledges at different heights of the mountain slope, from hundreds of meters to 4–5 km. The object of the study is the ledges of the mountain slope, which are necessary for economic activity, located at different heights of the slope. The subject of the study is the initial and changed stress-strain state of the massif near the scarp of the mountain slope from the action of gravitational and tectonic forces. The aim of the study is to create a mathematical model and calculate the stress-strain state of the massif near the scarps of the mountainside to check the boundary conditions with the load of a decreasing triangular epure. The objective of the study is to establish the laws of stress distribution in each point of the massif by solving the differential equation of equilibrium using the Kolosov-Muskhelishvili method. Ledges are formed either by nature or created by man, technogenically, and are mated with the mountain slope at a different angle of inclination at different heights of the slope. To assess the stability and safety from landslide processes of structures located in the ledge zone, it becomes necessary to carefully study the stress-strain state of the massifs. To study the stress state of a rock mass, the following main methods have been used: the unloading method, the finite element method, the finite difference method, as well as the analytical methods of Kolosov-Muskhelishvili in the version where the conformal mapping is used [Gulnara]. Thus, to study the state of massifs in the zone of ledges of the mountain slope, it is necessary to create an analytical model of the stress-strain state of massifs of ledges of the mountain slope, in which the zones of conjugation of the ledge and the mountain slope, the possible heights of the ledge, the effect of volumetric and surface loads would be taken into account in a single analytical model. In this case, the authors consider the problem when the stress state of a mountain massif with a symmetrical scarp in natural conditions, which is formed under the combined action of gravitational, horizontal tectonic forces and external distributed loads with a triangular epure. The problem is solved using the Kolosov-Muskhelishvili method and the MATNCAD software environment. As a result of the calculations, the patterns of stress distribution in the massifs of the mountain slope with a ledge have been created, where the actions of gravitational, horizontal tectonic forces were taken into account each separately. To check the boundary conditions with a load with a decreasing triangular diagram, the stresses are calculated for the contour points in the vicinity of the loaded section of the contour. The patterns of distribution of the initial stress state of the slope mass with ledges are presented for each stress component in the form of stress isolines.
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