论文标题
在氢/空气混合物中的传播爆炸波与水喷水云之间的相互作用
Interactions between a propagating detonation wave and water spray cloud in hydrogen/air mixture
论文作者
论文摘要
抑制氢爆炸对于意识到其广泛的应用至关重要,并且由于许多优势,细水喷雾是一种理想的缓解剂。在这项工作中,对传播氢/爆炸波与圆形水云之间的相互作用进行了数值研究。使用二维配置,应用了涉及双向气流耦合的Eulerian-Lagrangian方法。考虑了不同的液滴(直径,浓度)和云(直径)特性。我们的结果表明,液滴的大小,浓度和云半径对爆炸波的峰值压力轨迹具有重大影响。与云相互作用后,爆炸波显示了三种传播模式,包括扰动的繁殖,背风重新定义和爆炸灭绝。从气体和液滴数量的不稳定的演变中分析了背风重定位。云内部的折射爆炸波被解耦,并且比云外部的爆炸波更慢。爆炸的重新发射来自局部热点,这是由于上下衍射引爆的冲击而引起的。由于两种流体的有效密度差异,爆炸波越过云层并观察到多相界面不稳定时,水滴的瓦解会进行。此外,当我们考虑各种水云大小时,会观察到爆炸灭绝。当爆炸经过云时,峰值压力轨迹迅速褪色,并且在冲击聚焦区域中没有局部自动签名。还研究了在灭绝过程中受到冲击区域的热化学结构的进化。此外,考虑各种液滴浓度和云半径的参数研究。
Inhibition of hydrogen explosion is crucial to realize its wide applications and fine water spray is an ideal mitigant due to numerous advantages. In this work, interactions between a propagating hydrogen/air detonation wave and circular water cloud are numerically studied. Eulerian-Lagrangian method involving two-way gas-droplets coupling is applied, with a two-dimensional configuration. Different droplet (diameter, concentration) and cloud (diameter) properties are considered. Our results show that droplet size, concentration and cloud radius have significant effects on peak pressure trajectory of the detonation wave. After interacting with cloud, the detonation wave exhibits three propagation modes, including perturbed propagation, leeward re-detonation, and detonation extinction. Leeward re-detonation is analyzed from unsteady evolutions of gas and liquid droplet quantities. The refracted detonation wave inside the cloud is decoupled and propagates more slowly than the one outside the cloud. The detonation re-initiation is from a local hot spot, caused by shock focusing from upper and lower diffracted detonations. Disintegration of water droplets proceeds when the detonation wave crosses the cloud and multiphase interfacial instability is observed due to the difference in effective density of the two fluids. Furthermore, detonation extinction is observed when we consider various water cloud size. It is featured by quickly fading peak pressure trajectories when the detonation passes the cloud, and no local autoignition occurs in the shock focusing area. Evolutions of thermochemical structures from the shocked area in an extinction process are also studied. Moreover, parametric studies considering various droplet concentrations and cloud radii are performed.