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A study of bubble collapse pressure pulse waves from small scale underwater explosions near the water surface

机译:水面附近小规模水下爆炸泡沫塌陷压力脉冲的研究

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Explosive detonators have been used to study the effect of proximity of the water surface on the pressure wave generated by the collapse of an underwater explosive bubble. Transducers at four different depths recorded the pressure pulse, and a low resolution high speed video camera was used to observe the overall dynamics of the bubble. The detonators were fired at selected depths (z) within the range of 6.0-161.3 cm, corresponding to dimensionless depth (gamma) values of approximately 0.3-9.0 where gamma = z/R-max, and R-max is the maximum radius of the bubble during its first pulsation. Analysis of the recorded pressure waves was complicated by the superposition of the emitted wave with its reflection from the water surface. Despite this difficulty there was clear evidence of a dependency of the peak pressure (P-max) and impulse (I) of the emitted wave on gamma. The pressure pulse generated by the deeper events (gamma 3.4) did not appear to be strongly influenced by the water surface, exhibiting only a weak dependence on gamma. However, P-max and I decreased markedly for shallower detonations in the range gamma approximate to 1.6-2.8. Imaging results showed that this decrease was associated with migration of the bubble away from the surface during its collapse. A markedly different behaviour was observed when gamma was decreased further to 1.1. It was found that although the bubble was still repelled from the surface and I continued to decrease, P-max increased dramatically. Details of the pulse and imaging results suggested a more complex bubble collapse behaviour at this depth. For shallower values of gamma (0.6) the bubble did not collapse and appeared to breach the water surface and ingest additional gas from the atmosphere. Crown Copyright (C) 2018 Published by Elsevier Ltd. All rights reserved.
机译:炸药起爆管已被用于研究水表面附近的上通过水下爆炸的气泡破裂产生的压力波的影响。在四个不同的深度换能器记录的压力脉冲,并且使用低分辨率高速视频摄像机,观察泡沫的整体动态。雷管分别以6.0-161.3厘米的范围内选择的深度(z)的发射中,对应于无量纲深度(伽马)为约0.3-9.0值,其中的γ= Z / R-max和R-max是最大半径其第一脉动期间气泡。记录的压力波的分析通过用从水表面其反射所发射的波的叠加变得复杂。尽管这个困难有压力峰值(P-MAX)和伽马发射波的冲击(I)的依赖关系的明显证据。通过更深事件(伽马GT; 3.4)中产生的压力脉冲没有出现由水面的强烈影响,表现出只在伽马弱依赖性。然而,P-max和I显着降低为范围内的伽玛近似1.6-2.8较浅爆炸。成像结果表明,这种减少其崩溃过程中与气泡远离所述表面的迁移相关联。观察到显着不同的行为,当伽马进一步降低至1.1。结果发现,虽然泡沫仍然从表面排斥,我继续减少,P-MAX急剧增加。脉冲和成像结果的细节提出在该深度的更复杂的气泡破裂行为。伽玛(小于0.6)的较浅的值的泡沫并没有崩溃,似乎从大气违反水面和采集额外的气体。 Crown版权(c)2018由elestvier有限公司出版。保留所有权利。

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