Chapter 7 Slope Stability Part 1 [边坡稳定] 4?
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7.1 Types of slope failure [滑坡的类型] Fk aXA.JE
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The most common types of slope failure [滑坡] are illustrated in Fig.7.1. Translational slide tends to occur where an adjacent weak zone [软弱层] of soil is at a relatively shallow depth below the surface of the slope. The failure surface tends to be plane and roughly parallel to the slope. [滑动面为平面与坡面平行] :1*zr
Rotational slide is common for cohesive soil [粘性土] (e.g. clays) slope. The shape of the failure surface in section may be a circular arc or a non-circular curve. In general circular slides are associated with homogeneous soil conditions and non-circular slides are associated with non-homogeneous soil conditions. [滑动面为一曲面] K|Om5
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7.2 Methods of slope stability analysis [边坡稳定分析方法] *{Yh6{
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The stability of a slope can be analysed using one or more of the following methods: Hl/7(FJqc>
– Limit equilibrium method (equilibrium of forces) [极限平衡法] ^B|YO8.v
– Limit analysis based on plasticity (equilibrium of stresses) [极限应力分析法] q1jN]H
– Finite difference method [有限差分法] >r=6A
– Finite element method [有限元法] !8o\.uyi
Although a finite element or a finite difference method is more flexible and general, in practice, the limit equilibrium method (LEM) is used in the slope stability analysis. ZRPE-l_3:
In LEM, the soil is considered to be on the verge of failure along an assumed or a known sliding surface. [在某一假设滑动面,整个块体处于极限平衡状态] In general, the sliding surface is assumed to be a circular arc for clays or a logarithmic spiral for sands and gravels. The shear strength required to maintain a condition of limiting equilibrium is compared with the available shear strength of the soil, giving the average factor of safety along the sliding surface [安全糸数定义为抗剪力与下滑力之比]. The problem is normally considered in two dimensions. [土坡的稳定分析可简化为平面问题] MJA~jjy4
For the slope stability analysis using the LEM, two analyses are considered for each slope: my4\mi6P
– Effective Stress Analysis [有效应力分析] (ESA) which represents drained or long-term behaviour of the slope. Cohesion (c’) and angle of internal friction (’) are used in the analysis. (m/aV
– Total Stress Analysis [总应力分析] (TSA) which represents undrained or short-term behaviour of the slope. Undrained shear strength (cu) is used in the analysis. %/Bvy*X&
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7.3 Analysis of a plane translational slide 0lBat_<8
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It is assumed that the potential failure surface is parallel to the surface of the slope and is at a depth that is small compared with the length of the slope. The slope can then be considered as being of infinite length, with end effects being ignored. [假设滑动面与坡面平行, 滑动块体深度远小于边坡长度, 边坡为无限长] =E!x~S;N
The slope is inclined at angle to the horizontal and the depth of the failure plane is z, as shown in Fig.7.2. Consider a slice of soil element of width b. [坡角为, 滑动面深度z, 土条宽度为b] Assume the side forces on the soil element can be neglected in the stability analysis, ground water table is below the failure plane and the soil is cohesionless. [假设不考虑土条两边的合力,地下水位低于滑动面,无粘性土] The forces acting on the element are shown in Fig.7.2. W is weight of soil element [土条重量], T is shear force on the failure plane [平行于滑动面的下滑剪切力] and N is normal force on the failure plane [滑动面法线方向的分力]. Consider equilibrium of forces parallel to the slope surface, [边坡平行方向的静力平衡] h^Qh9G0dn
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