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Conduit dynamics and post-explosion degassing on Stromboli:a combined UV camera and 1 numerical modelling treatment

机译:Stromboli上的管道动力学和爆炸后脱气:UV相机和1个数值建模处理的组合

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摘要

Recent gas flux measurements have shown that strombolian explosions are often followed by periods of elevated flux, or ‘gas codas’, with durations of order a minute. Here, we present UV camera data from 200 events recorded at Stromboli volcano to constrain the nature of these codas for the first time, providing estimates for combined explosion plus coda SO2 masses of ≈ 18 – 225 kg. Numerical simulations of gas slug ascent show that substantial proportions of the initial gas mass can be distributed into a train of ‘daughter bubbles’ released from the base of the slug, which we suggest, generate the codas, on bursting at the surface. This process could also cause transitioning of slugs into cap bubbles, significantly reducing explosivity. This study is the first attempt to combine high temporal resolution gas flux data with numerical simulations of conduit gas flow to investigate volcanic degassing dynamics.
机译:最近的气体通量测量表明,爆发爆炸后通常会出现通量升高或“汽水汽化”的时期,持续时间约为一分钟。在这里,我们首次展示了在Stromboli火山记录的200次事件的紫外线照相机数据,以首次限制这些尾气的性质,从而提供了组合爆炸加尾气SO2的总质量≈18 – 225 kg的估计值。气团上升的数值模拟表明,大部分初始气体质量可以分配到从团根底部释放的“女儿气泡”序列中,我们建议在气泡破裂时会生成尾气。此过程还可能导致团块转变为帽状气泡,从而大大降低爆炸性。这项研究是首次尝试将高时间分辨率的气体通量数据与导管气体流动的数值模拟相结合,以研究火山岩的脱气动力学。

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