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Centrifugal Model Testing for Deformations in High-Filling Foundation of Loess in a Gully

机译:沟壑区黄土高填土变形的离心模型试验

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A major problem of concern in high-filling engineering is settlement deformations in filling foundation. Such deformations are affected by many factors. In this study, a large-scale centrifugal model test was carried out to study the deformation of high-filling foundation of loess in a gully area, under the conditions of natural water content and rising groundwater respectively. The treatment technology between the original mountain slope and the filling body was also investigated. It was found that the settlement deformations of the high-filling foundation mainly occurred under the condition of increasing centrifugal acceleration. The settlement rate also increased in this process, and the final settlement increased with filling thickness. When the groundwater in the filling body rose, additional settlement in the filling foundation occurred which readily leads to foundation destabilization. Improving the compactness had a significant effect on reducing this additional settlement. Adopting a stepped treatment method to overlap the original mountain slope, the filling body helped to decrease the settlement of the filling foundation above the joint. However, it was not conducive to controlling the settlement of the adjacent filling body. The slope of the original mountain should be taken into account in the design of the overlapping method. For the overlapping region between the filling body and the original rock mass, permeable materials should be installed in the joint which can be compacted to form a permeable zone, which in turn could connect to a drainage pipeline laid at the bottom of the gully. The bedrock fissure water is then efficiently drained and the water infiltrating into the filling body reduced. This could help to avoid a large amount of additional settlement and is beneficial to the foundation’s stability after construction.
机译:高填方工程中的一个主要问题是填方地基中的沉降变形。这种变形受许多因素影响。本研究进行了大型离心模型​​试验,研究了自然含水量和地下水上升条件下黄土沟壑区高填土基础的变形。还研究了原始山坡与填土之间的处理技术。研究发现,高填方地基的沉降变形主要发生在离心加速度增加的条件下。在此过程中沉降速度也有所提高,最终沉降随着填充厚度的增加而增加。当填充体内的地下水上升时,填充基础中发生了额外的沉降,这很容易导致基础不稳定。改善紧密度对减少这种额外的沉降有重大影响。采用阶梯式处理方法以覆盖原始的山坡,填充体有助于减少填充物在接缝上方的沉降。但是,这不利于控制相邻填充物的沉降。在重叠法的设计中应考虑原始山的坡度。对于填充体与原始岩体之间的重叠区域,应在节缝中安装可渗透材料,可将其压实以形成可渗透区,进而可连接至位于沟渠底部的排水管道。然后,基岩裂隙水被有效地排出,并且渗入填充体的水减少了。这样可以避免大量的额外沉降,并且有利于基础在施工后的稳定性。

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