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Bubble size distributions in a convecting layer - art. no. 1784

机译:对流层中的气泡尺寸分布-艺术。没有。 1784年

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1] We have conducted a series of laboratory experiments to explore the bubble size distribution coupled with convection in a magma chamber. Boiling liquid heated from below exhibits two types of convection pattern depending on the viscosity. When the viscosity is sufficiently high, bubbles are distributed uniformly in the liquid, and the bubble size distribution becomes the power law type for large bubbles and exponential distribution for small bubbles. On the other hand, when the viscosity is low, bubbles are separated from the liquid layer, making a foam, and their size distribution is exponential for large bubbles and unimodal for small bubbles. These experimental results suggest that the bubble size distribution is determined whether the viscous drag of the magma is sufficiently high to trap bubbles. [References: 15
机译:1]我们进行了一系列实验室实验,以探索岩浆室内的气泡尺寸分布以及对流。从下方加热的沸腾液根据粘度表现出两种对流模式。当粘度足够高时,气泡在液体中均匀地分布,并且气泡尺寸分布对于大气泡变成幂律类型,而对于小气泡变成指数分布。另一方面,当粘度低时,气泡从液体层分离,形成泡沫,并且对于大气泡其尺寸分布是指数的,对于小气泡是单峰的。这些实验结果表明,确定气泡大小分布是确定岩浆的粘性阻力是否足够高以捕获气泡。 [参考:15

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