基于分子动力学模拟的蒙脱石水化与力学行为研究

    Study on hydration and mechanical behavior of montmorillonite based on molecular dynamics simulations

    • 摘要: 通过分子动力学模拟研究了蒙脱石的水化膨胀及力学性能演变规律,揭示了含水率对其结构稳定性和力学各向异性的影响规律。结果表明,随含水率增加,蒙脱石层间距扩大。水分子的存在会减弱范德华力并增强静电作用,导致晶体膨胀。水分子分布从低含水率下的集中吸附逐渐转变为高含水率下的多层均匀分布。模拟的层间距结果与试验数据一致,验证了该方法的可靠性。研究发现蒙脱石力学行为表现出明显的各向异性:XY方向呈脆性破坏,而Z方向具有更高韧性。含水率的增加显著削弱了力学性能,特别在XY方向表现为明显的应变集中与剪切破坏。Si―Ob、Al―Ob、Al―Oh和Oh―Ho键的断裂与重组主导了力学响应过程。拉伸时Si―Ob键最易断裂,压缩时则表现为键断裂与重组的协同作用,尤其在Z方向压缩下层间结构重组最为显著。

       

      Abstract: This study investigates the hydration swelling of montmorillonite and the evolution of its mechanical properties through molecular dynamics simulations, revealing the influence of water content on structural stability and mechanical anisotropy. The results show that as water content increases, the basal spacing of montmorillonite expands. The infiltration of water molecules weakens van der Waals forces and enhances electrostatic interactions, leading to crystal swelling. Water molecule distribution transitions from concentrated adsorption at low water content to multi-layer uniform distribution at high water content. The simulation results are consistent with experimental data, confirming the reliability of the method. It is found that montmorillonite exhibits significant anisotropy in mechanical behavior: X and Y directions show brittle failure, while the Z direction demonstrates higher toughness. Increased water content notably weakens mechanical properties, particularly manifesting as strain concentration and shear failure in X and Y directions. Microscopic analysis reveals that the breaking and reformation of Si―Ob, Al―Ob, Al―Oh, and Oh―Ho bonds dominate the mechanical response process. During tension, Si―Ob bonds are most prone to breakage, while during compression, a synergistic effect of bond breaking and reformation occurs, with interlayer structural reorganization being particularly significant under Z-direction compression.

       

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