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首页> 外文期刊>Journal of geophysics and engineering >Site characterization and evaluation of the stability of the Yesilyurt Landslide (Trabzon, NE Turkey) using back analysis method
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Site characterization and evaluation of the stability of the Yesilyurt Landslide (Trabzon, NE Turkey) using back analysis method

机译:使用后分析方法的现场表征和yesily山体滑坡稳定性的评价(Trabzon,Ne Turkey)

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The aim of this study was to determine the soil profile of the Yesilyurt Landslide Area (NE Turkey) and to investigate the stability of the landslide area after the excavation planned by back analysis for support design. For these purposes, after the 1/1000 scaled engineering geological map was prepared, seismic refraction, electrical resistivity tomography and ground penetrating radar measurements were performed on different profiles to understand vertical and horizontal homogeneity of the landslide materials and undisturbed/disturbed soil samples were obtained from the test pits to determine the geotechnical properties of the soil. The results of the geophysical measurements showed that the landslide material was composed of two different soil zones. While the maximum thickness of the upper zone is 2.5, the thickness of the lower zone is about 5 m. The depth of dasidic rock mass is about 7 m. Residual cohesions of the soil samples obtained upper and lower zones were determined as 38 kPa and 44 kPa, and their residual friction angles were determined as 18 degrees and 15 degrees respectively. Unit weight values of the soil samples obtained from both zones were 16.9 kN m(-3). The data obtained from laboratory tests showed that the landslide material is a uniform lithology. The geophysical measurements indicate that the wave velocity and resistivity values of these profiles differ from each other due to groundwater at a depth of 2.5 m. Limit equilibrium analysis were carried out with Slide v5.0 software using data obtained from the field measurements and laboratory tests to evaluate current and supported cases of the studied area. Because the safety factor of the slope obtained from the LE analyses is 0.99 and the studied soil environment is considered as unstable, the reliable and economical reinforcement was suggested using the retaining wall. The back-analysis method was evaluated to ensure the stability for a 1.5 safety factor and finally the lateral active forces
机译:本研究的目的是确定尤艾尔特滑坡区域(NE TURKEY)的土壤剖面,并在挖掘后的挖土机面积探讨促进后的脱井区分析,以进行支持设计。出于这些目的,在制备1/1000缩放的工程地质图之后,在不同的轮廓上进行地震折射,电阻率断层扫描和地面穿透雷达测量,以了解滑坡材料的垂直和水平均匀性,并获得未受干扰/扰动的土壤样品从测试坑中确定土壤的岩土性质。地球物理测量结果表明,滑坡材料由两种不同的土壤区组成。虽然上部区域的最大厚度为2.5,但下部区域的厚度约为5米。 dasidic岩体的深度约为7米。将上下区域获得的土壤样品的残留内聚为38kPa和44kPa,分别测定其残余摩擦角度为18度和15度。从两个区域获得的土壤样品的单位重量值为16.9kN m(-3)。从实验室测试中获得的数据表明滑坡材料是均匀的岩性。地球物理测量表明,由于地下水的深度为2.5米,这些曲线的波速和电阻率值彼此不同。使用从现场测量和实验室测试中获得的数据进行限制平衡分析,使用从现场测量和实验室测试获得的数据来评估所研究区域的电流和支持的情况。因为从Le分析中获得的斜率的安全系数为0.99,所研究的土壤环境被认为是不稳定的,所以使用挡土墙建议可靠和经济的加强。评估后分析方法以确保1.5安全系数的稳定性,最后是横向活动力

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