杨江涛, 石振明, 张清照, 郑鸿超. 2018: 堰塞坝坝体材料力学特性的离散元方法(DEM)研究. 工程地质学报, 26(s1): 631-638. DOI: 10.13544/j.cnki.jeg.2018192
    引用本文: 杨江涛, 石振明, 张清照, 郑鸿超. 2018: 堰塞坝坝体材料力学特性的离散元方法(DEM)研究. 工程地质学报, 26(s1): 631-638. DOI: 10.13544/j.cnki.jeg.2018192
    YANG Jiangtao, SHI Zhenming, ZHANG Qingzhao, ZHENG Hongchao. 2018: DISCRETE ELEMENT METHOD (DEM) STUDY ON MECHANICAL PROPERTIES OF DAM MATERIALS. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 631-638. DOI: 10.13544/j.cnki.jeg.2018192
    Citation: YANG Jiangtao, SHI Zhenming, ZHANG Qingzhao, ZHENG Hongchao. 2018: DISCRETE ELEMENT METHOD (DEM) STUDY ON MECHANICAL PROPERTIES OF DAM MATERIALS. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 631-638. DOI: 10.13544/j.cnki.jeg.2018192

    堰塞坝坝体材料力学特性的离散元方法(DEM)研究

    DISCRETE ELEMENT METHOD (DEM) STUDY ON MECHANICAL PROPERTIES OF DAM MATERIALS

    • 摘要: 堰塞坝坝体材料的力学特性对其稳定性具有重要的影响。本文基于离散元方法(DEM),开展不同密实度及颗粒级配(细粒材料和粗粒材料)下坝体材料的直剪试验。从材料应力-应变曲线(宏观)及内部应力(微观)等信息方面,揭示坝体材料的力学特性。结果表明,宏观角度方面,随着坝体材料密实度的增大,峰值强度均有增强,粗颗粒材料尤为明显;对于不同颗粒级配的材料,细粒材料的应力-应变曲线呈现出明显的应变硬化和剪缩特性,而粗粒材料表现为应变软化和剪胀特性。微观角度方面,材料内部主应力的方向随着剪切位移的增加而逐渐发生偏移,且内部力链逐渐集中,进而内部剪切带逐渐发展。材料的颗粒级配决定了内部接触力的分布以及传递模式,粗粒材料中应力的分布主要沿骨架颗粒分布,细粒材料中为均匀分布;材料的密实度则影响材料内部颗粒间的接触形态,密实度越大越有利于颗粒间咬合力的传递,从而对内部应力及力链的大小均有不同程度增强。

       

      Abstract: The mechanical properties of the dam material have an important influence on its stability. In this study, based on the discrete element method(DEM),direct shear tests were conducted on dam materials with different densities and particle grading(fine and coarse-grained materials). From the aspects of material stress-strain curve(macro) and internal stress(micro) information, the mechanical properties of the dam material were revealed. The results show that, from the macroscopic perspective, with the increase of the density of the dam material, the peak strength is enhanced, especially for the coarse-grained material. For different grain gradation materials, the stress-strain curve of the fine-grained material shows obvious strain hardening and shear properties, while coarse-grained materials exhibit strain softening and dilatancy characteristics. From the microscopic perspective, the direction of the internal principal stress of the material gradually shifts as the shear displacement increases, the internal force chains and the internal shear zone gradually concentrateand develops. The particle size distribution of materials determines the distribution of internal contact forces and the mode of transfer. The distribution of stress in coarse-grained materials is mainly distributed along the framework particles, and is evenly distributed in fine-grained materials. The density of the materials affects the contact patterns between the particles inside the material. The greater the degree of compaction, the more conducive to the transmission of occlusal forces between particles, so that the internal stress and the strength of the chain have different degrees of enhancement.

       

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