中文摘要：

作用在脆性结构材料表面的高能量密度脉冲会以冲击波的形式传播进入材料内部，导致压缩破坏和功能失效．通过设计并引入微孔洞，显著增强了脆性材料冲击下的塑性变形能力，从而使脆性结构材料可以有效地吸收耗散冲击波能量，并抑制冲击诱导裂纹的扩展贯通．建立格点一弹簧模型并用于模拟研究致密和多孔脆性材料在高能量密度脉冲加载下的冲击塑性机理、能量吸收耗散过程和裂纹扩展过程．冲击波压缩下孔洞塌缩，导致体积收缩变形和滑移以及转动变形，使得多孔脆性材料表现出显著的冲击塑性．对致密样品、气孔率5％和10％的多孔样品吸能能力的计算表明，多孔脆性材料吸收耗散高能量密度脉冲的能力远优于致密脆性材料．在短脉冲加载下，相较于遭受整体破坏的致密脆性材料，多孔脆性材料以增加局部区域的损伤程度为代价，阻止了严重的冲击破坏扩展贯通整个样品，避免了材料的整体功能失效．

英文摘要：

The high energy density pulse input into brittle structural materials will propagate as a shock wave. It induces compression fracture and function failure. In this work, voids are introduced to significantly enhance the shock plastic deformability of brittle structural materials, so that brittle structural materials can effectively absorb the shock wave energy, and restrain the propagation of shock-induced cracks. A lattice-spring model is established to investigate the mechanism of shock plastic, and the processes of energy absorbing and crack expanding in porous brittle materials. The shock wave inside porous brittle material splits into an elastic wave and a deformation wave. The deformation wave is similar to the plastic wave in ductile metal, however, its deformation mechanism is of volume shrinkage induced by voids collapse, and slippage and rotation deformation of scattered tiny scraps comminuted by shear cracks. We calculate the shock wave energy based on particle velocities and longitudinal stresses on nine interfaces of the modeled brittle sample, and further obtain the absorbed energy density. The absorbed energy density curve is composed of two stages： the absorbing stage and the saturation stage. The absorbing stage corresponds to the deformation wave, and the saturation stage corresponds to the shock equilibrium state （Hugoniot state）. The energy absorb abilities of the dense sample and porous samples with 5% and 10% porosities are compared based on calculation results. It shows that the ability of the porous brittle material to absorb high energy density pulse is much higher than that of the dense brittle material. The ability of porous brittle materials to restrain the propagation of the shock fracture is also explored. The goal of this design is to freeze the propagation of the shock fracture in the middle of the brittle sample, so that the other parts of the sample keep nearly intact during the shock. Inside the protected area, the designed functions of brittle materials can be accomplishe