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首页> 外文期刊>Archives of Hydro-engineering and Environmental Mechanics >Geotechnical Parameters of Alluvial Soils from in-situ Tests
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Geotechnical Parameters of Alluvial Soils from in-situ Tests

机译:冲积土的土工参数现场试验

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摘要

The article concentrates on the identification of geotechnical parameters of alluvial soil represented by silts found near Poznan and Elblag. Strength and deformation parameters of the subsoil tested were identified by the CPTU (static penetration) and SDMT (dilatometric) methods, as well as by the vane test (VT). Geotechnical parameters of the subsoil were analysed with a view to using the soil as an earth construction material and as a foundation for buildings constructed on the grounds tested. The article includes an analysis of the overconsolidation process of the soil tested and a formula for the identification of the overconsolidation ratio OCR. Equation 9 reflects the relation between the undrained shear strength and plasticity of the silts analyzed and the OCR value. The analysis resulted in the determination of the N_(kt) coefficient, which might be used to identify the undrained shear strength of both sediments tested. On the basis of a detailed analysis of changes in terms of the constrained oedomet-ric modulus M_0, the relations between the said modulus, the liquidity index and the OCR value were identified. Mayne's formula (1995) was used to determine the M_0 modulus from the CPTU test. The usefulness of the sediments found near Poznari as an earth construction material was analysed after their structure had been destroyed and compacted with a Proctor apparatus. In cases of samples characterised by different water content and soil particle density, the analysis of changes in terms of cohesion and the internal friction angle proved that these parameters are influenced by the soil phase composition (Fig. 18 and 19). On the basis of the tests, it was concluded that the most desirable shear strength parameters are achieved when the silt is compacted below the optimum water content.
机译:本文着重于以波兹南和埃尔伯拉格附近发现的淤泥为代表的冲积土的岩土工程参数的识别。通过CPTU(静态穿透)和SDMT(膨胀法)以及叶片测试(VT)来确定被测地下土的强度和变形参数。分析了地下土壤的岩土工程参数,以期将土壤用作土方建筑材料并作为在测试地面上建造的建筑物的基础。该文章包括对所测试土壤的超固结过程的分析,以及用于确定超固结率OCR的公式。公式9反映了所分析的粉土的不排水剪切强度和可塑性与OCR值之间的关系。分析结果确定了N_(kt)系数,该系数可用于确定两种测试沉积物的不排水剪切强度。在对约束弹性模量M_0方面的变化进行详细分析的基础上,确定了所述弹性模量,流动性指数和OCR值之间的关系。 Mayne公式(1995)用于根据CPTU测试确定M_0模量。在用Proctor装置破坏并压实沉积物结构之后,分析了在Poznari附近发现的沉积物作为土建材料的有用性。如果样品的含水量和土壤颗粒密度不同,则对内聚力和内摩擦角变化的分析表明,这些参数受土壤相组成的影响(图18和19)。根据试验得出的结论是,当淤泥压实在最佳含水量以下时,可获得最理想的剪切强度参数。

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