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Experimental study of the shear strength of soil from the Heifangtai Platform of the Loess Plateau of China

机译:黄土高原黑坊台平台土抗剪强度试验研究

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Purpose Loess landslides induced by irrigation are common geological disasters in the Loess Plateau, China. Long-term watering decreases the matric suction and soil strength of loess, thus causing the frequent occurrence of landslides. Therefore, studying the strength characteristics of unsaturated loess is of great significance for knowing how such landslides occur and, a step further, preventing them. Materials and methods Undisturbed loess samples in Heifangtai Platform were collected to measure their soil water characteristic curves (SWCC) and a series of direct shear tests and triaxial shear tests were carried out with unsaturated loess. Moreover, the strength characteristics of the loess were discussed. Results and discussion The results showed that in the direct shear test, the cohesion (c) increased linearly with increasing matric suction whereas the suction internal friction angle (phi(b)) was approximately constant. In the triaxial shear test, c increased nonlinearly with increasing matric suction. The value of phi(b) was a constant when matric suction was 0-100 kPa, but decreased as matric suction increased within the range of 100-200 kPa. The effective stress parameter (chi) lay in the range from 0.5 to 0.8. When the matric suction was small, the shear strength calculated by Lu's suction theory was almost the same as that obtained by Fredlund's theory. With the increase of matric suction, the shear strength calculated by Fredlund's theory gradually outperformed that of Lu's suction theory. The shear strength calculated by the curve of moisture desorption was slightly larger than that of moisture absorption. Conclusions The variation trends of strength parameters with matric suction under the two tests were similar. The effective internal friction angles obtained by the triaxial shear test are slightly larger than those by the direct shear test. The suction internal friction angle (phi(b)) was approximately a constant and smaller than phi '. The phi(b) obtained by the direct shear test was slightly larger than that obtained by the triaxial test. Lu's theory can be used to evaluate the stability of unsaturated soils on some loess slopes with high soil moisture content.
机译:目的黄土高原灌溉引起的滑坡是黄土高原地区常见的地质灾害。长期浇水会降低黄土的基质吸力和土壤强度,从而引起滑坡的频繁发生。因此,研究非饱和黄土的强度特性对于了解这种滑坡是如何发生以及进一步防止滑坡的发生具有重要意义。材料和方法收集黑坊台平台原状黄土样品,测量其土壤水分特征曲线(SWCC),并用非饱和黄土进行一系列直接剪切试验和三轴剪切试验。此外,还讨论了黄土的强度特性。结果与讨论结果表明,在直接剪切试验中,内聚力(c)随基质吸力的增加而线性增加,而吸力内摩擦角(phi(b))大致恒定。在三轴剪切试验中,c随着基质吸力的增加而非线性增加。 phi(b)的值在基质吸力为0-100 kPa时是恒定的,但在基质吸力在100-200 kPa范围内增加时降低。有效应力参数(chi)在0.5到0.8的范围内。当基质吸力较小时,由卢的吸力理论计算的剪切强度几乎与由弗雷德伦德理论获得的剪切强度相同。随着基质吸力的增加,由弗雷德伦德理论计算出的抗剪强度逐渐超过了鲁氏吸力理论。由水分解吸曲线计算出的剪切强度略大于水分吸收曲线。结论在两个试验中,强度参数随基质吸力的变化趋势相似。通过三轴剪切试验获得的有效内摩擦角略大于通过直接剪切试验获得的有效内摩擦角。吸入内摩擦角(phi(b))大致恒定,小于phi'。通过直接剪切试验获得的phi(b)稍大于通过三轴试验获得的phi(b)。鲁的理论可以用来评价某些高含水量黄土边坡上非饱和土的稳定性。

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