Bisson M, Spinetti C, Gianardi R, Strehlow K, De Beni E, Landi P
Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Pisa, Pisa, Italy.
Istituto Nazionale di Geofisica e Vulcanologia - ONT, Rome, Italy.
Sci Rep. 2023 Aug 18;13(1):13465. doi: 10.1038/s41598-023-39600-w.
A detailed mapping of volcanic ballistic projectiles emplaced in a defined area, represents the starting point to derive preparatory data in hazard and risk studies of ballistics phenomena. Considering as case study the 3rd July 2019 paroxysmal eruption occurred at Stromboli volcano, we map and analyse at very high spatial resolution (8 cm) the distribution of the ballistic spatter clasts emplaced on the E flank of the volcano. The resulting map identifies and reproduces as geospatial polygon elements 152,228 spatter clasts with areal dimensions from 0.03 to 4.23 m. Dispersed on 0.407 km, the spatters cover an area of 29,000 m corresponding to an erupted products volume from 2.3 to 7.0 × 10 m, calculated here for the first time. Spatial analyses indicate that the area mostly affected by the clasts emplacement is between N67.5 and N135 directions, identifying a preferential deposition between N112.50 and N123.75 directions. The clasts size distribution rapidly decreases with the size increase, highlighting a nearly constant ratio small/large clasts regardless the distance from the vent. Finally, additional investigations reveal that clasts dispersion parameters decrease progressively with the distance from the vent only along one direction (N67.5), highlighting how the morphology influences the deposition and remobilisation of mapped ballistics.
对特定区域内放置的火山抛射物进行详细测绘,是在弹道现象的灾害和风险研究中获取预备数据的起点。以2019年7月3日斯特龙博利火山发生的阵发性喷发为例,我们以非常高的空间分辨率(8厘米)绘制并分析了放置在火山东侧的弹道飞溅碎屑的分布情况。生成的地图将152,228个飞溅碎屑识别并再现为地理空间多边形元素,其面积尺寸从0.03至4.23平方米不等。这些碎屑散布在0.407千米的范围内,覆盖面积为29,000平方米,对应于此首次计算得出的2.3至7.0×10立方米的喷发产物体积。空间分析表明,受碎屑放置影响最大的区域在N67.5和N135方向之间,确定了在N112.50和N123.75方向之间的优先沉积。碎屑尺寸分布随尺寸增大而迅速减小,突出显示了无论距离喷口多远,小/大碎屑的比例几乎恒定。最后,进一步的调查显示,碎屑散布参数仅沿一个方向(N67.5)随距喷口距离的增加而逐渐减小,突出了地形对已测绘弹道的沉积和再移动的影响。