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Optimizing Non-Invasive Techniques for Surface and Sub-Surface Soil Characterizations for a Slope in Lebanon

机译:黎巴嫩坡面非表层土壤特性的非侵入性技术优化

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This work aims to be an initial investigation to the use of geophysical and limited geotechnical data to obtain soil and stratigraphy characterization. This approach is essential for developing countries where geotechnical data is typically scarce and expensive. This type of consolidation was used on a study area in Lebanon that consists of a failed slope. A consolidation of data from surface wave measurements, electrical resistivity, and in-situ data was carried out where each gave a part of the description of the site. The surface wave measurements revealed that the seismic bedrock depth was not reached in the range of measurements carried out for this study. Soil was revealed to be mostly clayey sand. Geostatistical analysis results showed that spatial variability of soil properties in both vertical and horizontal directions could be achieved from the electrical resistivity measurements. For this study area, it was shown that 9 m and 4 m were the sizes of the essential spatial structures in the data in the horizontal and vertical directions respectively. Another finding of interest was a second order trend in the resistivity data in both the horizontal and vertical directions that can be due to the decrease in resistivity with depth due to soil compression. All in all, the slope has been better understood with the merging of data and the aspects that require further investigation have been clearly depicted.
机译:这项工作旨在对利用地球物理和有限的岩土数据获取土壤和地层特征进行初步调查。对于通常缺乏岩土数据且价格昂贵的发展中国家而言,这种方法至关重要。这种类型的加固用于黎巴嫩的一个研究区,该研究区由一个失败的斜坡组成。对表面波测量,电阻率和原位数据的数据进行了合并,每个数据都给出了该站点描述的一部分。地表波测量表明,在本研究进行的测量范围内未达到地震基岩深度。结果表明,土壤主要是黏土。地统计分析结果表明,通过电阻率测量可以实现土壤性质在垂直和水平方向的空间变异性。对于该研究区域,表明在水平和垂直方向上,数据中基本空间结构的大小分别为9 m和4 m。另一个有趣的发现是电阻率数据在水平和垂直方向上的二阶趋势,这可能是由于土壤压缩导致电阻率随深度而降低。总而言之,通过合并数据可以更好地理解坡度,并且已经清楚地描绘了需要进一步研究的方面。

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