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岩石类介质侵彻效应的理论研究进展

李杰 程怡豪 徐天涵 王明洋

李杰, 程怡豪, 徐天涵, 王明洋. 岩石类介质侵彻效应的理论研究进展[J]. 爆炸与冲击, 2019, 39(8): 081101. doi: 10.11883/bzycj-2019-0286
引用本文: 李杰, 程怡豪, 徐天涵, 王明洋. 岩石类介质侵彻效应的理论研究进展[J]. 爆炸与冲击, 2019, 39(8): 081101. doi: 10.11883/bzycj-2019-0286
LI Jie, CHENG Yihao, XU Tianhan, WANG Mingyang. Review on theoretical research of penetration effects into rock-like material[J]. Explosion And Shock Waves, 2019, 39(8): 081101. doi: 10.11883/bzycj-2019-0286
Citation: LI Jie, CHENG Yihao, XU Tianhan, WANG Mingyang. Review on theoretical research of penetration effects into rock-like material[J]. Explosion And Shock Waves, 2019, 39(8): 081101. doi: 10.11883/bzycj-2019-0286

岩石类介质侵彻效应的理论研究进展

doi: 10.11883/bzycj-2019-0286
基金项目: 国家自然科学基金面上项目(51679249);中国博士后基金(2018M643853)
详细信息
    作者简介:

    李 杰(1981- ),男,博士,副教授,lijierf@163.com

    通讯作者:

    程怡豪(1986- ),男,博士,讲师,05105432@163.com

  • 中图分类号: O347

Review on theoretical research of penetration effects into rock-like material

  • 摘要: 近年来,随着超高速武器的发展,侵彻效应的研究重点逐渐由高速向超高速发展。随着弹体打击速度提高,侵彻机制发生变化,并触发强烈的成坑和地冲击效应。本文综述了大速度范围内岩石类介质侵彻效应的理论研究进展,讨论了长杆弹侵彻速度的分区,介绍了岩石类介质的侵彻、成坑、地冲击效应的理论模型,并对目前研究中尚有待解决的问题和下一步的研究方向进行了展望。
  • 图  1  钢杆弹撞击铝靶机理分区[39]

    Figure  1.  Schematic of penetration of steel projectiles into aluminum targets[39]

    图  2  岩石的动力压缩曲线[50]

    Figure  2.  Dynamic compression curves of rock[50]

    图  3  侵彻速度界定及介质压缩状态

    Figure  3.  Definition the scope of penetration velocity and medium compression state

    图  4  v/cα关系曲线

    Figure  4.  Curve between v/c and α

    图  5  花岗岩侵彻实验结果(撞击速度1~2.5 km/s)[19]

    Figure  5.  Experimental results of penetration into granite targets with impact velocity from 1−2.5 km/s[19]

    图  6  变形弹计算假设[73]

    Figure  6.  Assumption of deformable projectile[73]

    图  7  不同速度侵彻后回收弹体的形态[19]

    Figure  7.  The morphology of the recovered projectiles after penetration under different velocities[19]

    图  8  基于界面压力的超高速侵彻阶段划分[74]

    Figure  8.  Phases during hypervelocity penetration based on interface pressure[74]

    图  9  弧形弹头的几何参数

    Figure  9.  Ogive-nose projectile geometry

    图  10  花岗岩侵彻深度的实验结果与理论计算结果的预测效果[32]

    Figure  10.  Comparison of calculation results with experimental results of penetration depth in granite[32]

    图  11  岩石与金属靶体超高速撞击成坑的典型外观[106, 109]

    Figure  11.  Typical appearance of craters formed by hypervelocity impact[106, 109]

    图  12  不同条件下的成坑效应

    Figure  12.  Cratering effects under different conditions

    图  13  式(41)与混凝土超高速侵彻深度实验结果的对比[114]

    Figure  13.  Comparison between Eq. (41) and experimental results of hyper-velocity penetration depth into concrete[114]

    图  14  高速弹体侵彻岩石扩孔范围计算简图[116]

    Figure  14.  Calculation diagram of cavitation induced by high-velocity projectile penetration into rocks[116]

    图  15  径向裂纹区半径计算结果与实验结果对比[32]

    Figure  15.  Comparison of crater radius between calculation results and experimental results[32]

    图  16  Z模型在不同Z值下的速度场[118]

    Figure  16.  Streamlines with different values of Z[118]

    图  17  球形弹超高速撞击下介质中压力分布[123]

    Figure  17.  Pressure distribution in medium under hypervelocity spherical projectile[123]

    图  18  峰值压力随距离衰减曲线[123]

    Figure  18.  Peak pressure decay with impact of distance[123]

    图  19  弹速3 558 m/s时实测地冲击压力时程曲线[32]

    Figure  19.  The experiment time history curve of ground shock with impact velocity 3 558 m/s[32]

    图  20  弹速3 558 m/s时按公式(50)计算的地冲击压力时程曲线[32]

    Figure  20.  the calculated time history curve of ground shock with impact velocity 3 558 m/s[32]

    表  1  冲击压缩作用下典型硬岩分区行为特征[51]

    Table  1.   Dynamic behaviors of hard rock in different ranges under shock compression[51]

    冲击压缩
    状态

    波形时间特征

    应变状态特征

    应力状态特征
    c0=1ρ0dσdε
    小扰动传播速度
    p\simfontrn
    应力波衰减特征
    冲击波速度
    特征(图2(a))
    高应力
    流体状态
    Δ=0~0.05
    冲击波特征
    εθ=0
    一维应变
    α=σrσθ1c0=Kρ0n=−2.2~3.0D>>cp
    内摩擦拟
    流体状态
    Δ=0.05~0.1
    短波特征
    εrεθ0
    受限应变
    α=σrσθ=αα0\simfontα\simfont1c0=3Kρ0(1+2α)
    介于流体与固体之间
    n=1.4~1.8Dcp
    低应力
    固体状态
    Δ>0.1
    弹塑性波特征
    εr+2εθ=0
    相容应变
    α=σrσθ=α0c0=(K+43μ)ρ0n=1.1~1.2
     注:α=1sinϕ1+sinϕϕ为介质内摩擦角;α0=υ1υυ为介质泊松比;ρ0为介质密度,K为体积模量,μ为剪切模量。
    下载: 导出CSV

    表  2  不同修正流体动力学模型中[Yp]和[Rt]值[1]

    Table  2.   The value of [Yp] and [Rt] in different models[1]

    模型[Yp][Rt]备注
    A-T[42-44]YpRtYp=HEL=σyp(1+υ)/(12υ)
    Rt=σyt[(2/3)+ln(0.57Et/σyt)]
    S-W-Z-S[78]Yp4 A4ApRt+3A4Ap8Apρtu2Ap为长杆弹截面积
    A为坑底面积,A\simfont2Ap
    R-M-M[79]YpAtApRt+AtAp2Apρtu2Ap为长杆弹截面积
    Ap为蘑菇头等效面积
    Rt=(σyt/3)[1+ln(3Et/(54v)σyt)]
    A-W[80]σyp73ln(α)σytα为靶体中塑性流动区的无量纲长度,由柱形空腔膨胀模型得到(KtGt为靶体的体积模量和剪切模量):
    (1+ρtu2σyt)Ktρtα2u2=(1+ρtα2u22Gt)Ktρtu2
    Z-H[81]Yp4D24D2pRt+βD24D2p8D2pρtu2β为动阻力系数
    L-W[73]YpSρtuUF0exp[(uUF0nUF0)2]+2ρtU2F0exp[2(uUF0nUF0)2]S为静阻力,UF0=HEL/ρt为临界侵彻速度,
    n为可调系数
    下载: 导出CSV

    表  3  地质类材料成坑效应的相似关系

    Table  3.   Similarity laws of cratering effects in geological material

    成坑参数强度控制区域重力控制区域
    VcρtVcmp=fVcs(ε)(ρpv20Yt)3ξ12(ρtρp)13ξ2+32ξ1ρtVcmp=fVcg(ε)(v20ga0)3ξ12+ξ1(ρtρp)2+ξ16ξ22+ξ1
    DcDc(ρtmp)1/3=fDcs(ε)(ρpv20Yt)ξ12(ρtρp)13ξ2+12ξ1Dc(ρtmp)1/3=fDcg(ε)(v20ga0)ξ12+ξ1(ρtρp)2+ξ16ξ23(2+ξ1)
    hh(ρtmp)1/3=fhcs(ε)(ρpv20Yt)ξ12(ρtρp)13ξ2+12ξ1h(ρtmp)1/3=fhcg(ε)(v20ga0)ξ12+ξ1(ρtρp)2+ξ16ξ23(2+ξ1)
    下载: 导出CSV

    表  4  地质类材料地冲击衰减指数n

    Table  4.   Power exponent n for attenuation of ground shock in geological material

    介质类型作用类型研究方法爆炸当量(TNT)或撞击速度n
    花岗岩化学爆炸试验拟合0.12 kg2.12
    核爆炸试验拟合4.8 kt/12.2 kt/56 kt1.6
    砂岩化学爆炸试验拟合0.1 kg2
    石灰岩化学爆炸试验拟合0.18~0.2 kg2
    撞击数值计算4~6 km/s2
    玄武岩撞击试验拟合0.6~2.7 km/s1.7±0.2
    辉长-钙长岩撞击数值计算4~45 km/s0.2~2.95
    撞击试验拟合3.9~4.6 km/s0.9~1.8
    盐岩核爆炸试验拟合1.1 kt/3.1 kt/25 kt1.6
    混凝土化学爆炸试验拟合0.12 kg1.53
    细粘土化学爆炸试验拟合0.2 kg2.6
    黏土化学爆炸试验拟合0.4 kg2.34
    下载: 导出CSV
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出版历程
  • 收稿日期:  2019-07-19
  • 修回日期:  2019-08-02
  • 刊出日期:  2019-08-01

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