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Analysis of the railway heave induced by soil swelling at a site in southern France

机译:法国南部某地点土壤膨胀引起的铁路沉陷分析

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In order to better understand the heave observed on the railway roadbed of the French high-speed train (TGV) at Chabrillan in southern France, the swelling behaviour of the involved expansive clayey marl taken from the site by coring was investigated. The aim the study is to analyse the part of heave induced by the soil swelling. First, the swell potential was determined by flooding the soil specimen in an oedometer under its in-situ overburden stress. On the other hand, in order to assess the swell induced by the excavation undertaken during the construction of the railway, a second method was applied. The soil was first loaded to its in situ overburden stress existing before the excavation. It was then flooded and unloaded to its current overburden stress (after the excavation). The swell induced by this unloading was considered. Finally, the experimental results obtained were analyzed, together with the results from other laboratory tests performed previously and the data collected from the field monitoring. This study allowed estimating the heave induced by soil swelling. Subsequently, the part of the heave due to landslide could be estimated which corresponds to the difference between the monitored heave and the swelling heave.
机译:为了更好地了解法国南部Chabrillan的法国高速列车(TGV)的铁路路基上的沉沉,对取自现场的相关膨胀黏土泥岩的取芯行为进行了研究。研究的目的是分析土壤膨胀引起的隆起部分。首先,通过在土体表上的原地上覆应力作用下将土壤标本淹没来确定膨胀势。另一方面,为了评估在铁路建设过程中进行的开挖引起的膨胀,采用了第二种方法。在开挖之前,首先将土壤加载到原位覆盖应力。然后将其淹没并卸载至当前的上覆应力(开挖后)。考虑了这种卸载引起的膨胀。最后,对获得的实验结果以及先前进行的其他实验室测试的结果以及从现场监测中收集的数据进行分析。这项研究可以估算土壤膨胀引起的起伏。随后,可以估计由于滑坡而导致的起伏部分,它对应于所监测的起伏和膨胀起伏之间的差异。

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