Identifying Soft Soils using Pore-Pressure Parameters: A Machine Learning Approach

Jeniffer Viegas, António Gallardo, Lucas Bottaro, Rodrigo Marinaro
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Abstract

- The cone penetration test (CPT) is a widely used method for identifying soil profiles and estimating soil parameters. Numerous correlations have been established to facilitate geo-characterization of soils based on CPT data. However, caution must be exercised when applying these correlations and laboratory tests should be used to validate them. Tropical residual soils are highly variable, even for seemingly similar samples, which can make it difficult for project designers to accurately characterize them. The present work focuses on a case study where the goal was to distinguish and characterize two soft soils existent on the foundation of a tailings dam in the southwest of Brazil. The construction of the dam is still ongoing, and its foundation belongs to a complex geological environment with soft soils that can reach N SPT blows as low as its own weight. The geological survey identifies two horizons of residual soil of dolomitic phyllite: soft and very soft. However, spatially distinguishing this material regarding its consistence has shown to be a challenging task. Since they differ essentially on the degree of weathering, most parameters for both materials are quite similar, and from laboratory tests, the parameter that helps differentiate these soils is the pore pressure Skempton parameter at failure – A f . Based on these findings, it can be inferred that the pore-pressure parameter Bq in CPT represents the excess pore-pressure during the test, whereas Af describes the excess pore-pressure at failure during triaxial tests. Despite the lack of a currently established theoretical correlation between the two parameters, they can offer valuable insight into the soil's response to rapid loading. Notably, both measures have proven to be effective in distinguishing between residual soils, even though they are distinct measures. In this study, the B q and A f parameters are employed to classify soils using an unsupervised learning method, specifically the K-means algorithm. The resulting clusters exhibit strong agreement with borehole profiles near the CPT locations.
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利用孔隙压力参数识别软土:一种机器学习方法
-锥贯试验(CPT)是一种广泛使用的识别土壤剖面和估计土壤参数的方法。已经建立了许多相关性,以促进基于CPT数据的土壤地理特征。但是,在应用这些相关性时必须谨慎,并应使用实验室测试来验证它们。热带残余土壤是高度可变的,即使是看似相似的样品,这可能使项目设计者难以准确地描述它们。本文以巴西西南部某尾矿坝地基上的两种软土为研究对象,对其特征进行了分析。大坝的建设仍在进行中,其基础属于复杂的地质环境,软土可以达到nspt,低至自重。地质调查确定了白云岩千层残土的软层和极软层两个层位。然而,在空间上区分这种材料的一致性是一项具有挑战性的任务。由于它们在风化程度上存在本质上的差异,因此两种材料的大多数参数非常相似,并且从实验室测试中,有助于区分这两种土壤的参数是破坏时的孔隙压力Skempton参数- A f。由此可以推断,CPT中孔隙压力参数Bq代表试验过程中的超孔隙压力,Af代表三轴试验中破坏时的超孔隙压力。尽管目前这两个参数之间缺乏建立的理论相关性,但它们可以为土壤对快速加载的响应提供有价值的见解。值得注意的是,这两种措施已被证明在区分残余土壤方面是有效的,即使它们是不同的措施。本研究采用无监督学习方法,即K-means算法,利用B q和A f参数对土壤进行分类。所得到的簇与CPT位置附近的井眼剖面非常吻合。
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