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王子元, 莫品强, 胡静, 赵子露, 肖琼. 颗粒材料堆积体的基底压力分布试验研究[J]. 岩土工程学报, 2024, 46(S1): 158-163. DOI: 10.11779/CJGE2024S10020
引用本文: 王子元, 莫品强, 胡静, 赵子露, 肖琼. 颗粒材料堆积体的基底压力分布试验研究[J]. 岩土工程学报, 2024, 46(S1): 158-163. DOI: 10.11779/CJGE2024S10020
WANG Ziyuan, MO Pinqiang, HU Jing, ZHAO Zilu, XIAO Qiong. Experimental study on base pressure distribution of accumulations of granular materials[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(S1): 158-163. DOI: 10.11779/CJGE2024S10020
Citation: WANG Ziyuan, MO Pinqiang, HU Jing, ZHAO Zilu, XIAO Qiong. Experimental study on base pressure distribution of accumulations of granular materials[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(S1): 158-163. DOI: 10.11779/CJGE2024S10020

颗粒材料堆积体的基底压力分布试验研究

Experimental study on base pressure distribution of accumulations of granular materials

  • 摘要: 针对颗粒材料堆积体的压力下降问题,研究了点沉积法下不同漏斗高度、颗粒粒径和颗粒形状对基底压力分布的影响。结果显示,基底压力下降现象与内部应力拱有关,且与漏斗高度、颗粒粒径和颗粒形状相关。随着堆积体质量的增加,应力拱稳定性增强,应力凹陷比趋于稳定。漏斗高度距堆顶距离越大,测得的基底压力越大,应力凹陷程度越小。堆积体应力凹陷比随颗粒粒径的增加,呈现先增加后减少的趋势,并在粒径0.6~1.18 mm的堆积体中出现了应力集中现象。随着堆积体质量的增加,标准砂试样的应力凹陷比先增加后减小,而散煤则是一致下降。

     

    Abstract: Addressing the issue of pressure reduction in accumulations of granular materials, the impact of varying funnel heights, particle sizes and particle shapes on the distribution of base pressure is investigated utilizing the point deposition method. The results show that the phenomenon of base pressure reduction is intricately linked to the formation of internal stress arches and influenced by the factors such as the height of the funnel, granulometry of the particles, and morphological characteristics of the granules. With the increase of the accumulations, there is an enhancement in the stability of the stress arches, leading to a convergence towards a steady state of the stress depression ratio. The base pressure measured increases with the increase of the vertical distance from the funnel to the apex of the accumulations, resulting in a decrease of the stress depression. The stress depression ratio within the accumulations exhibits a trend of the initial increase followed by a decrease as the particle size escalates, with a notable occurrence of stress concentration in the accumulations comprised of particles ranging from 0.6 to 1.18 mm in diameter. With the increase in the mass of the accumulations, the stress depression ratio for the standard sand samples initially increases and then decreases, whereas for the loose coal particles, a consistent decline is observed.

     

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