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在具有回震的有限厚度流体层中对里希特迈尔-梅什科夫不稳定性的数值研究
Linfei Li1, Tai Jin2, Liyong Zou3
1State Key Laboratory of Clean Energy Utilization, <a href="https://ror.org/00a2xv884">Zhejiang University</a>, Hangzhou 310027, People's Republic of China.
Physical review. E
|June 22, 2024
概括
这项研究从数值上研究了冲击诱导的流体层演变以及在再冲击波下里希特迈尔-梅什科夫不稳定性. 更薄的层和特定的阶段条件改变了尖峰/泡的发展和混合宽度的增长.
科学领域:
- 流体动力学 流体动力学
- 计算物理 计算物理
- 不稳定的现象 不稳定的现象
背景情况:
- 里希特迈尔-梅什科夫不稳定性 (RMI) 在各种物理过程中至关重要.
- 了解反震波下的RMI对于预测复杂的流体行为至关重要.
- 之前的研究往往简化了条件,需要详细的数值调查.
研究的目的:
- 为了数值地研究冲击诱导的流体层进化.
- 为了揭示RMI在重震波效应下的潜在机制.
- 分析像振幅扰动,流体层厚度和相位等初始参数对重震流体层演变的影响.
主要方法:
- 冲击诱导的流体层演变的数值模拟.
- 参数研究涉及六种不同的初始流体层配置.
- 分析接口形态,混合宽度增长和振幅扰动.
主要成果:
- 接口合在较薄的流体层中得到加强,抑制尖峰和泡的发展.
- 外相条件导致喷气出现,而在相条件产生气泡.
- 混合宽度表现出线性和非线性生长阶段,受到震荡波的抑制,并在相位逆转期间轻微减弱.
- 幅度的增长与理论预测一致,但由于挤压和拉伸效应,在非常晚的阶段会有分歧.
结论:
- 流体层厚度和初始阶段在重震下显著影响RMI动态.
- 该研究提供了有关RMI演变的机制的见解,包括喷气和泡形成.
- 数字结果验证了振幅增长的理论模型,突出了后期的偏差.
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