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Influence of grain size distribution of inclusions on the mechanical behaviours of track-bed materials

机译:夹杂物粒度分布对路基材料力学行为的影响

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摘要

In French conventional railway track-bed, an interlayer was created, mainly from the interpenetration of ballast and subgrade. Field investigation showed that the ballast content decreases over depth. In addition, depending on the locations, the grain size distribution of ballast grains can be quite different, defining different values of coefficient of uniformity, C-u. In this study, triaxial tests were carried out on the interlayer soil with three C-u values and five volumetric inclusion contents, f(v). X-ray micro computed tomography scans were also conducted on representative samples to visualise the corresponding inclusion distributions. Results show that: (a) at all three C-u values, two soil fabrics can be identified, namely grain-grain contact structure for large inclusion contents (f(v) = 35% and 45%) and fine-fine contact structure for small inclusion contents (f(v) = 5%, 10% and 20%), and the characteristic volumetric inclusion content f(v-cha) separating these two categories was larger for smaller C-u since in this case fewer inclusion contacts were expected to be developed at a given f(v); (b) for the grain-grain contact structure, a smaller C-u caused larger maximum deviator stress q(max), larger friction angle, larger Poisson ratio and more dilatancy due to the involvement of more large grains at smaller C-u; (c) for the fine-fine contact structure, an opposite trend was observed: the smaller the C-u, the smaller the q(max), the friction angle, the Poisson ratio and the dilatancy owing to a smaller quantity of inclusion grains; (d) the change patterns of Young's modulus and cohesion with increasing C-u were the same for the two soil fabrics - Young's modulus and cohesion decreased with the increase of C-u.
机译:在法国传统的铁路路基中,主要是通过压载物和路基的相互渗透而创建的夹层。现场调查表明,压载物含量随着深度的增加而降低。另外,根据位置,压载颗粒的粒度分布可能会非常不同,从而定义了均匀系数C-u的不同值。在这项研究中,在具有三个C-u值和五个体积夹杂物含量f(v)的夹层土壤上进行了三轴试验。还对代表性样品进行了X射线计算机断层扫描,以可视化相应的夹杂物分布。结果表明:(a)在所有三个Cu值下,都可以识别出两种土壤织物,即夹杂物含量较大时的颗粒-谷物接触结构(f(v)= 35%和45%)和较小的细密接触结构。夹杂物含量(f(v)= 5%,10%和20%),并且对于较小的Cu,分离这两个类别的特征体积夹杂物含量f(v-cha)较大,因为在这种情况下,预期的夹杂物接触较少在给定的f(v)下发展; (b)对于晶粒-晶粒接触结构,较小的C-u会导致较大的最大偏斜应力q(max),较大的摩擦角,较大的泊松比和更大的膨胀率,这是因为在较小的C-u处会包含更多的较大晶粒; (c)对于细微接触结构,观察到相反的趋势:由于夹杂物颗粒的数量较少,C-u越小,q(max),摩擦角,泊松比和膨胀率越小; (d)两种土壤织物的杨氏模量和内聚力随C-u的增加而变化的模式相同-杨氏模量和内聚力随C-u的增加而降低。

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