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Field Testing of Earth Pressures in a Large-scale Natural Loess Slope

机译:大型天然黄土边坡土压力的现场测试

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摘要

An in-situ large-scale earth pressure test was undertaken in a natural loess slope in Lanzhou, China. A 14.5-m-high natural slope was gradually cut into a vertical slope through a series of eight slope cutting work conditions. By pre-installing re-bar meters and cutting slope unloading, the real earth pressure distribution law and potential slip surface development mechanism, along with the variation of the Slope Cutting Depth (SCD), were obtained under the condition that each point in the free surface can move independently and freely. Earth pressure increases slowly at first and then decreases sharply along the Slope Excavating Depth (SED). The increase rate for 9.0 to 10.4 m is 3 to 4 times as much as the former conditions, so the self-stability height of the slope is 9.0 to 10.4 m. The unsaturated natural loess shear outlet of the slope is always located at the H/3 (where H is the natural slope height) position, so the slip surface does not pass through the bottom of the slope. The measured values of unsaturated vertical slope earth pressures are far less than the values calculated by Rankine's earth pressure theory-especially the size and position of the maximum earth pressure.
机译:在中国兰州的天然黄土边坡上进行了原位大规模土压力测试。通过一系列的八种坡度切割工作条件,将14.5米高的自然坡度逐渐切割成垂直坡度。通过预装钢筋计量仪和切割坡度卸载,在每个点自由的条件下获得了真实的土压力分布规律和潜在的滑动面发展机制,以及坡度切割深度(SCD)的变化。表面可以独立自由移动。土压力首先缓慢增加,然后沿边坡开挖深度(SED)急剧下降。 9.0至10.4 m的增加速率是前一个条件的3至4倍,因此斜坡的自稳定高度为9.0至10.4 m。斜坡的非饱和天然黄土剪切出口始终位于H / 3(其中H为天然斜坡高度)位置,因此滑移面不会穿过斜坡的底部。非饱和垂直斜坡土压力的测量值远远小于兰金土压力理论计算的值,特别是最大土压力的大小和位置。

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