弹体超高速侵彻石灰岩靶体地冲击的数值模拟研究

张山豹 孔祥振 方秦 洪建

张山豹, 孔祥振, 方秦, 洪建. 弹体超高速侵彻石灰岩靶体地冲击的数值模拟研究[J]. 爆炸与冲击, 2022, 42(1): 013302. doi: 10.11883/bzycj-2021-0007
引用本文: 张山豹, 孔祥振, 方秦, 洪建. 弹体超高速侵彻石灰岩靶体地冲击的数值模拟研究[J]. 爆炸与冲击, 2022, 42(1): 013302. doi: 10.11883/bzycj-2021-0007
ZHANG Shanbao, KONG Xiangzhen, FANG Qin, HONG Jian. Numerical simulation on ground shock waves induced by hypervelocity penetration of a projectile into a limestone target[J]. Explosion And Shock Waves, 2022, 42(1): 013302. doi: 10.11883/bzycj-2021-0007
Citation: ZHANG Shanbao, KONG Xiangzhen, FANG Qin, HONG Jian. Numerical simulation on ground shock waves induced by hypervelocity penetration of a projectile into a limestone target[J]. Explosion And Shock Waves, 2022, 42(1): 013302. doi: 10.11883/bzycj-2021-0007

弹体超高速侵彻石灰岩靶体地冲击的数值模拟研究

doi: 10.11883/bzycj-2021-0007
基金项目: 国家自然科学基金(51808550);中国博士后科学基金(2020M671296)
详细信息
    作者简介:

    张山豹(1996- ),男,博士研究生,thzhangs@126.com

    通讯作者:

    孔祥振(1988- ),男,博士,副教授,ouckxz@163.com

  • 中图分类号: O385

Numerical simulation on ground shock waves induced by hypervelocity penetration of a projectile into a limestone target

  • 摘要: 为探究超高速动能武器的对地破坏效应及其影响因素,采用数值模拟方法对弹体超高速侵彻的地冲击规律进行了研究。首先,基于石灰岩静动态力学性能实验数据对材料模型参数进行了标定,并对已有弹体大范围着速侵彻石灰岩靶体进行了模拟,验证了所采用材料模型和数值模拟方法的合理性。随后,开展了钨合金长杆弹超高速侵彻石灰岩靶体的数值模拟,细致分析了地冲击传播的现象和机理:弹体超高速侵彻靶体时,弹靶交界面处会产生瞬时高压,并以应力波的形式在靶体中传播,对靶体内部造成破坏,且当弹体初速度高于3.0 km/s时,地冲击显著增强。最后,进一步研究了不同弹靶参数对地冲击的影响,发现从相对深度来看,弹体参数(弹体长径比、密度)对地冲击规律影响不大;而靶体特征特别是孔隙率对地冲击传播具有较大影响。
  • 图  1  最大强度面模型与实验数据的拟合

    Figure  1.  Fitting of the maximum strength surface model to the experimental data

    图  2  石灰岩应力-应变曲线的数值模拟结果与实验数据的对比

    Figure  2.  Comparison of stress-strain curves of limestone between experimental data and numerical simulation

    图  3  石灰岩动态强度增强因子随应变率的变化曲线

    Figure  3.  Changes of the dynamic increase factors with strain rate for limestone

    图  4  石灰岩状态方程曲线与实验数据的拟合

    Figure  4.  Equation of state of limestone fitted to experimental data

    图  5  数值模拟的侵彻深度与实验数据的对比

    Figure  5.  Simulated depths of penetration at different initial projectile velocities compared with experimental data

    图  6  应力波造成的靶体破坏分区

    Figure  6.  Damage regions of the target caused by stress waves

    图  7  数值模拟得到不同撞击速度下的的侵彻深度

    Figure  7.  Simulated depths of penetration at different initial projectile velocities

    图  8  超高速侵彻过程中的破坏现象及压力波传播

    Figure  8.  Damage and pressure wave propagation in the target during hypervelocity penetration

    图  9  不同深度的应力时程曲线

    Figure  9.  Time histories of stress waves at different depths

    图  10  不同弹体初速度下应力峰值随深度的变化趋势

    Figure  10.  Change of peak stress with depth at different initial projectile velocities

    图  11  侵彻深度与弹体长径比的关系(弹径不变)

    Figure  11.  Depth of penetration versus length-to-diameter ratio at a constant projectile diameter

    图  12  弹体长径比对地冲击的影响

    Figure  12.  Effect of length-to-diameter ratio on ground shock wave

    图  13  弹体密度对地冲击的影响

    Figure  13.  Effects of projectile density on ground shock wave

    图  14  不同孔隙率岩石材料的状态方程

    Figure  14.  Equations of state for limestones with different porosities

    图  15  靶体孔隙率对地冲击的影响

    Figure  15.  Effect of target porosity on ground shock wave

    表  1  石灰岩的强度模型参数

    Table  1.   Parameters of the strength surface models for limestone

    最大强度面残余强度面屈服强度面损伤参数
    a1a2a3a1ya2yλm
    0.8770.0220.800.8900.0463×10−5
    下载: 导出CSV

    表  2  石灰岩的动态强度增强因子参数

    Table  2.   Parameters for dynamic increase factors of limestone

    动态强度增强因子FmWxSWy
    DIFC 91.81.25.0
    DIFT101.61.65.5
    下载: 导出CSV

    表  3  石灰岩的状态方程参数

    Table  3.   Equation of state parameters for limestone

    pcrush/MPaplock/GPanA1/GPaA2/GPaA3/GPa
    1001.44322.53–175.0495.0
    下载: 导出CSV

    表  4  不同弹体密度情况下的侵彻深度

    Table  4.   Depths of penetration at different projectile densities

    材料ρs/(kg∙m−3ρs/ρt1/2hp/m
    27851.102.58
    78301.854.69
    170002.736.20
    下载: 导出CSV
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出版历程
  • 收稿日期:  2021-01-06
  • 录用日期:  2021-11-22
  • 修回日期:  2021-03-08
  • 网络出版日期:  2021-12-06
  • 刊出日期:  2022-01-20

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