压缩性
离散元法
材料科学
压缩(物理)
各向异性
粒子(生态学)
球体
范德瓦尔斯力
接触力
机械
岩土工程
接触角
复合材料
经典力学
地质学
物理
光学
海洋学
量子力学
分子
天文
作者
Pei Wang,Zhen‐Yu Yin,Pierre‐Yves Hicher,Yu‐Jun Cui
摘要
Abstract In order to clarify the micro‐mechanics of clay during compression, the behavior of clay subjected to one‐dimensional compression is investigated at the particle scale using discrete element method (DEM). The flaky clay particles in the simulation are approximated by clumps made of spheres. A new contact model is implemented to account for the double‐layer repulsive force, the van der Waals attractive force and the mechanical contact force. The effect of sphere arrangement in the particle clump is discussed. The DEM model is validated against experimental observations in terms of macroscopic compressibility, particle dip angle as well as the over consolidated behavior. The e ‐log σ v curve shows a concave‐to‐linear shape. The evolution of dip angle of clay particles indicates that particles tend to have an anisotropy with a preferential orientation towards horizontal direction. The increase of preconsolidation pressure decreases the initial compressibility due to the increase the number of mechanical contacts. The evolution of average coordination and sphere‐sphere contact shows that the majority of mechanical contacts are generated before the compressive stress reaches 100 kPa. Evolution of soil fabric is presented and discussed.
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