Double ceramic sphere's sympathetic implosions triggered by local impacts

IF 11.8 1区 工程技术 Q1 ENGINEERING, MARINE Journal of Ocean Engineering and Science Pub Date : 2025-02-01 DOI:10.1016/j.joes.2023.04.001
Yandong Hu, Yifan Zhao, Min Zhao, Miaolin Feng
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Abstract

Due to sophistications in experimental studies, the implosions in chain reaction, also named as sympathetic implosions, demand numerical models to understand the phenomena caused by various impacts to the primary sphere. We developed a 3D air-solid-water model considering the influence of brittle sphere failures of two alumina spheres to simulate the outbreak of the sympathetic implosion in the seawater of 114 MPa. According to the triggering mode, two cases of simultaneous implosions and five cases of sympathetic implosions of a double-sphere were numerically studied. We found that the induced fracture of the secondary sphere happened before the outbreak of the positive pressure wave, i.e., the induced fracture is caused by the uneven pressure around the sphere lower than the hydrostatic pressure. To our knowledge, the present paper is the first report on the early fracture of the secondary solid sphere in sympathetic implosions. With various triggering modes of the primary sphere, the secondary fractures are all induced at the proximal side and extend to the other side. The formed ring-shaped implosion cores are caused by individual fracture mode. The shifting of the two implosion cores eventually affects the pressure pulses at a position. A higher or similar values of the secondary pulse are found closely related to the double sphere's fracture modes, i.e., related to the triggering modes of the local impacts. This work help to estimate the damage of the sympathetic implosion to the surroundings, and prevent further implosions by understanding spatial superposition of a series of pulses.
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双陶瓷球的内爆是由局部撞击引起的
由于实验研究的复杂性,连锁反应中的内爆也被称为交感内爆,需要数值模型来理解各种对初级球体的冲击所引起的现象。建立了考虑两个氧化铝球脆性破坏影响的三维气固水模型,模拟了114 MPa海水中交感内爆的爆发。根据触发方式,对两种双球同步内爆和五种交感内爆进行了数值研究。我们发现二次球的诱导破裂发生在正压力波爆发之前,即诱导破裂是由于球周围压力低于静水压力的不均匀造成的。据我们所知,本文是关于交感内爆次生实心球早期骨折的第一篇报道。在原生球的多种触发方式下,次生裂缝均在近端诱发,并向另一侧延伸。环形内爆岩心的形成是由单个断裂模式引起的。两个内爆芯的移动最终会影响某一位置的压力脉冲。发现二次脉冲的较高或相近值与双球断裂模式密切相关,即与局部冲击触发模式密切相关。这项工作有助于估计交感神经内爆对周围环境的损害,并通过了解一系列脉冲的空间叠加来防止进一步的内爆。
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来源期刊
CiteScore
11.50
自引率
19.70%
发文量
224
审稿时长
29 days
期刊介绍: The Journal of Ocean Engineering and Science (JOES) serves as a platform for disseminating original research and advancements in the realm of ocean engineering and science. JOES encourages the submission of papers covering various aspects of ocean engineering and science.
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