论文标题
微重力中二氧化碳饱和水中气泡云的生长
Growth of a bubble cloud in CO2-saturated water in microgravity
论文作者
论文摘要
浸入气体饱和液体中的密集气泡云的扩散驱动的生长是一个问题,可以在几种现代技术中找到应用,例如溶剂交换微反应器,纳米技术或泡沫材料的生产。但是,在地球的重力条件下,只有由于浮力的作用,即重力效应的作用,才能在非常有限的时间内观察到这些动力学。在这里,我们介绍了在微重力条件下在CO $ _2 $ _2 $启用水中生长的密集气泡云的时间演变的实验观察结果。我们报告存在三种制度的存在,其中气泡云表现出不同的增长率。在短时间内,每个气泡在爱泼斯坦(Epstein)方程式之后独立生长。后来,气泡开始相互互动,随着它们争夺可用的CO $ _2 $,它们的增长率会降低。发生这种情况时,增长率会减慢。这发生在较早的范围内,气泡就越深。最终,长期以来,只有果壳上的那些泡沫继续增长。这些机制可以通过数学模型进行定性描述,其中每个单独的气泡在点质量下沉的存在下都会生长。尽管该模型仅对稀释气泡云有效,但其预测与实验观察结果一致,即使我们观察到的气泡云相当密集。
The diffusion-driven growth of a dense cloud of bubbles immersed in a gas-supersaturated liquid is a problem that finds applications in several modern technologies such as solvent-exchange micro-reactors, nanotechnology or the manufacturing of foamy materials. However, under Earth's gravity conditions, these dynamics can only be observed for a very limited time if the cloud is not attached to a surface, due to the action of buoyancy, i.e. of gravity effects. Here, we present experimental observations of the time evolution of dense bubble clouds growing in CO$_2$-supersaturated water in microgravity conditions. We report the existence of three regimes where the bubble cloud exhibits different growth rates. At short times, each bubble grows independently following the Epstein--Plesset equation. Later on, bubbles start to interact with each other and their growth rate diminishes as they compete for the available CO$_2$. When this happens, the growth rate slows down. This occurs earlier the deeper the bubble is in the cloud. Finally, at long times, only those bubbles on the husk continue growing. These regimes may be qualitatively described by a mathematical model where each individual bubble grows in the presence of a constellation of point mass sinks. Despite the model being only valid for dilute bubble clouds, its predictions are consistent with the experimental observations, even though the bubble clouds we observe are rather dense.