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兵工学报 ›› 2024, Vol. 45 ›› Issue (10): 3371-3384.doi: 10.12382/bgxb.2024.0420

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速度对射弹垂直破冰入水空泡流动特性的影响

黄振贵1,*(), 王浩1, 蔡晓伟2, 刘想炎1, 陈志华1, 秦健1, 郝戌龙1   

  1. 1 南京理工大学 瞬态物理全国重点实验室, 江苏 南京 210094
    2 中国船舶科学研究中心 水动力学重点实验室, 江苏 无锡 214082

Influence of Velocity on the Cavity Flow Characteristics of Vertical Ice-breaking Water Entry of a Projectile

HUANG Zhengui1,*(), WANG Hao1, CAI Xiaowei2, LIU Xiangyan1, CHEN Zhihua1, QIN Jian1, HAO Xulong1   

  1. 1 National Key Laboratory of Transient Physics, Nanjing University of Science and Technology, Nanjing 210094, Jiangsu, China
    2 National Key Laboratory of Hydrodynamics, China Ship Scientific Research Center, Wuxi 214082, Jiangsu, China
  • Received:2024-05-30 Online:2024-10-28

摘要:

探究冰层对高速射弹入水过程的影响机理对发展适用于冰区海域的先进跨介质武器具有重要指导意义。基于耦合欧拉-拉格朗日(Coupled Euler-Lagrange, CEL)方法对圆柱射弹以不同初速度垂直高速破冰入水过程进行研究。研究结果表明:射弹初速度较低时(50m/s),撞击所形成的冰孔尺寸较小,严重阻碍了外界气体涌入,空泡扩张发展受阻,导致提前发生颈缩,且不再出现无冰时的表面闭合现象,空泡更快发生深闭合;射弹初速较高时(≥100m/s),撞击所形成的冰孔尺寸较大,外界空气能够持续涌入,延迟空泡闭合,冰层与无冰的空泡尺度差异随初速增加而减小;随着入水速度增加,碎冰对气流干扰程度加剧,增强了空泡内部流场的非线性和湍流特性;射弹在无冰环境入水受力峰值为同速度下破冰入水(冰厚为二分之一射弹直径)的70%。当速度达到 150m/s 时,破冰入水过程中的弹体头部会发生微弱塑性应变,在设计新型冰区跨介质武器时,应着重提高射弹头部结构强度。

关键词: 高速入水, 空泡演化, 结构响应, 冰层, 裂纹扩展

Abstract:

Exploring the influence mechanism of ice sheet on the water-entry process of a high-speed projectile is of great significance for the development of advanced trans-media weapons suitable for ice-water areas. The processes of vertical ice-breaking water-entry of a high-speed cylindrical projectile at different initial velocities are studied based on the coupled Euler-Lagrange (CEL) method. The findings indicate that, when the initial velocity of projectile is relatively low (50m/s), the size of ice hole formed by impact is relatively small to severely hinder the influx of external gas, and the expansion and development of cavity are obstructed, leading to the premature neckingand early closure of cavity. Besides, there is no longer a surface closure phenomenon as no ice, and the deep closure of cavity occurs faster. When the velocity of projectile is higher (≥100 m/s), the size of ice hole formed by impact is larger, allowing a continuous influx of external air and delaying the closure of cavity. The difference in scale between the ice sheet and the ice-free cavity decreases with the increase in initial velocity. Additionally, as the initial velocity of projectile increases, the interference of crushed ice on the airflow intensifies, thus enhancing the nonlinear and turbulent characteristics of flow field within the cavity. It is worth noting that the peak force of projectile entering water in an ice-free environment is 70% of that of ice-breaking water-entry (the ice thickness is half of the diameter of projectile) at the same speed. At a speed of 150m/s, a weak plastic strain occurs at the projectile head during the ice-breaking water-entry process, which should be emphasized to improve the structural strength of projectile head when designing new types of trans-media weapons used in ice-water areas.

Key words: high-speed water-entry, cavity evolution, structural response, ice sheet, crack propagation

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