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Mechanical behaviour of undisturbed diatomaceous soil

机译:未受干扰硅藻土的力学行为

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The mechanical behaviour of sedimentary marine soils containing diatoms does not follow classical trends usually found in Soil Mechanics, and evidence of geotechnical singularities of undisturbed samples are still scarce. This article presents new insights on the behaviour of natural diatomaceous soil in compression, shearing and cyclic loading, on undisturbed highly plastic diatomaceous silt from Mejillones Bay in northern Chile. Microscopic observations show that the soil contains significant amount of siliceous diatom. Isotropic compression results in high overconsolidation (OCR > 20) and high compressibility after yielding. Similarly, at low confining stress the undrained shear strength does not depend on pressure and is virtually equal to the UCS = 730 kPa. At higher stresses, a transition to frictional behaviour is observed, characterized by high variability in excess pore pressure generation during undrained triaxial shearing tests, presumably due to heterogeneous diatom layering in undisturbed soil samples. Microscopic observations indicate that high compressibility could be attributed to massive diatom breakage and disturbance of the soil microstructure. Compared to conventional data on fine soils, the cyclic behaviour of the diatomaceous soil is more brittle at low strains, with higher normalized shear modulus and lower damping at shear strains lower than 2 x 10(-1); however, it presents higher degradation at larger strains.
机译:含有硅藻的沉积海相土壤的力学行为并不遵循土壤力学中常见的经典趋势,并且未受干扰样品的岩土工程奇点的证据仍然很少。本文对天然硅藻土在智利北部梅希隆斯湾未受干扰的高塑性硅藻质淤泥的压缩、剪切和循环荷载行为提出了新的见解。显微镜观察表明,土壤中含有大量的硅质硅藻。各向同性压缩导致高过固结 (OCR > 20) 和屈服后的高压缩性。同样,在低围压下,不排水剪切强度不依赖于压力,几乎等于UCS = 730 kPa。在较高的应力下,观察到向摩擦行为的转变,其特征是在未排水的三轴剪切试验期间产生的超孔隙压力的高度可变性,这可能是由于未受干扰的土壤样品中的非均质硅藻分层。微观观察表明,高压缩性可归因于大量硅藻破碎和土壤微观结构的扰动。与常规细土数据相比,硅藻土在低应变下的循环行为更脆,在低于2 x 10(-1)%的剪切应变下具有更高的归一化剪切模量和更低的阻尼;然而,它在较大的菌株下表现出更高的降解性。

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