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Bubble growth during decompression of magma: experimental and theoretical investigation

机译:岩浆减压过程中气泡的生长:实验和理论研究

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A model of bubble growth during decompression of supersaturated melt was developed in order to explore the conditions for preservation of gas overpressure in bubbles or for maintaining supersaturation of the melt. The model accounts for the interplay of three dynamic processes: decompression rate of the magma, deformation of the viscous melt around the growing bubble, and diffusion of volatiles into the bubble. Generally, these processes are coupled and the evolution of bubble radius and gas pressure is solved numerically. For a better understanding of the physics of the processes, we developed some analytical solutions under simplifying assumptions for cases where growth is controlled by viscous resistance, diffusion or linear decompression rate. We show that the solutions are a function of time and two dimensionless numbers, which are the ratios of either the diffusive or viscous time scales over the decompression time scale. The conditions for each growth regime are provided as a function of the two governing dimensionless parameters. Analytical calculations for some specific cases compare well with numerical simulations and experimental results on bubble growth during decompression of hydrated silicic melts. The model solutions, including the division to the growth regimes as function of the two parameters, provide a fast tool for estimation of the state of erupting magma in terms of gas overpressure, supersaturation and gas volume fraction. The model results are in agreement with the conditions of Plinian explosive eruption (e.g. Mount St. Helens, 18 May 1980), where high gas overpressure is expected. The conditions of effusion of lava domes with sudden onset of explosive activity are also in agreement with the model predictions, mostly in equilibrium degassing and partly in overpressure conditions. We show that in a situation of quasi-static diffusion during decompression the diffusive influx depends on the diffusivity away from the bubble, insensitive to the diffusivity profile.
机译:为了探索保持气泡中气体超压或保持熔体过饱和的条件,开发了一种在过饱和熔体减压过程中气泡生长的模型。该模型说明了三个动态过程的相互作用:岩浆的减压速度,正在生长的气泡周围的粘性熔体变形以及挥发物向气泡中的扩散。通常,这些过程是耦合的,并且数值计算了气泡半径和气压的变化。为了更好地了解过程的物理原理,我们在简化假设下针对粘性阻力,扩散或线性减压速率控制生长的情况,开发了一些分析解决方案。我们表明,解是时间和两个无量纲数的函数,这是扩散时间尺度或粘性时间尺度在减压时间尺度上的比率。根据两个控制的无量纲参数提供每种生长方式的条件。在某些特定情况下的分析计算结果与水合硅质熔体减压过程中气泡生长的数值模拟和实验结果相吻合。这些模型解决方案,包括根据两个参数对生长方式进行划分,为根据气体超压,过饱和度和气体体积分数估算岩浆喷发状态提供了一种快速工具。模型结果与普林尼亚爆发性喷发的条件(例如,圣海伦斯山,1980年5月18日)的条件相符,在该条件下预计会有很高的气体超压。突然爆发爆炸活动的熔岩穹顶的渗出条件也与模型预测一致,主要是在平衡脱气中,部分在超压条件下。我们表明,在减压过程中的准静态扩散情况下,扩散涌入取决于远离气泡的扩散率,对扩散率曲线不敏感。

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