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Growth and potential collapse of the lava dome in Unzen volcano and the estimation on block-and-ash flows

机译:熔岩圆顶的增长和潜在崩溃,在Unzen火山中的估算和块和灰度流动

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Heisei lava dome was formed in Unzen volcano over the period from 1991 to 1995. The recent continuous observations have shown that the lava dome is still growing, which is a threat for the life of the nearby residents. How to estimate the range of collapse and potential block-and-ash flows is an urgent problem. Airborne laser scanning method is briefly introduced. We presented a division to separate the lava dome with 10 potential collapsed blocks and set some measuring points to observe the elevation change in each block. By analyzing the elevation decrease from 2003 to 2014, the potential collapsed blocks that experienced obvious changes were identified. With the evaluation of elevation changes by airborne laser data, the buried terrain of dome was reconstructed. The results show that the whole lava dome from lobe 1 to 11 may collapse, and the potential maximum volume of collapsed part is 1.46 x 10(7) m(3). If the collapsed part forms block-and-ash flow, the flow will arrive at the seaside in approximately 7 minutes according to the result of simulation. The flow could travel approximately 8.5 km, and the average velocity is approximately 20 m/s.
机译:1991年至1995年,海茜熔岩穹顶于1991年至1995年在愈合火山形成。最近的持续观察结果表明,熔岩圆顶仍在增长,这是对附近居民生活的威胁。如何估计崩溃范围和潜在的块和灰分流动是一个紧迫的问题。简要介绍了机载激光扫描方法。我们提出了一个分部,将Lava圆顶分开10个潜在的折叠块,并设置一些测量点以观察每个块的高度变化。通过分析从2003年到2014年的高程减少,确定了经历明显变化的潜在折叠块。随着空中激光数据的升高变化的评价,重建了圆顶的埋地地形。结果表明,来自叶片1至11的整个熔岩圆顶可能崩溃,折叠部分的潜在最大体积为1.46×10(7)m(3)。如果折叠部分形成块和灰分流,则根据模拟结果,流量将在大约7分钟内到达海滨。流动可以行进约8.5 km,平均速度约为20米/秒。

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