In flight fragmentation reduces bomb size range and hazard during explosive volcanic eruptions

Coarse, molten fragments of low-viscosity magma (volcanic bombs) that are ejected during explosive volcanic eruptions represent a source of hazard and a record of past eruptions. After ejection, bombs tend to break up during flight, but how much this affects their dispersal is unclear. Here, we use high-speed and high-definition imaging of three recent explosive eruptions to parameterise the in-flight fragmentation of bombs. We estimate that in-flight fragmentation involves 73% of bombs coarser than ∼ 0.2 m, with bomb-to-bomb collisions and aerodynamic frictional (drag) forces being the main drivers of in-flight fragmentation, depending on eruption style. Drag force increases with increasing bomb velocity and size, selectively fragmenting the coarsest and fastest bombs, acting as a self-limiting factor for the range and energy of falling bombs. These findings pose a quantitative basis for incorporating the in-flight fragmentation processes into the interpretation of volcanic deposits and for modelling hazards from falling bombs.

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Publication Details

Journal
Scientific Reports
Published
2025-10-22
DOI
https://doi.org/10.1038/s41598-025-20900-2
Citations
2
Primary Topic
Particle Dynamics in Fluid Flows
Type
article
Field-Weighted Citation Impact
2.29

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article

In flight fragmentation reduces bomb size range and hazard during explosive volcanic eruptions

Danilo M. Palladino, Luca D’Auria, Tullio Ricci, Daniele Andronico et al.
2 citations
Scientific Reports
Particle Dynamics in Fluid Flows
2.29
article

In flight fragmentation reduces bomb size range and hazard during explosive volcanic eruptions

Danilo M. Palladino, Luca D’Auria, Tullio Ricci, Daniele Andronico, Jacopo Taddeucci, Elisabetta Del Bello, Piergiorgio Scarlato, M. A. Alatorre‐Ibargüengoitia, María Asensio‐Ramos, Clothilde Biensan
article en
2 citations

Abstract

Coarse, molten fragments of low-viscosity magma (volcanic bombs) that are ejected during explosive volcanic eruptions represent a source of hazard and a record of past eruptions. After ejection, bombs tend to break up during flight, but how much this affects their dispersal is unclear. Here, we use high-speed and high-definition imaging of three recent explosive eruptions to parameterise the in-flight fragmentation of bombs. We estimate that in-flight fragmentation involves 73% of bombs coarser than ∼ 0.2 m, with bomb-to-bomb collisions and aerodynamic frictional (drag) forces being the main drivers of in-flight fragmentation, depending on eruption style. Drag force increases with increasing bomb velocity and size, selectively fragmenting the coarsest and fastest bombs, acting as a self-limiting factor for the range and energy of falling bombs. These findings pose a quantitative basis for incorporating the in-flight fragmentation processes into the interpretation of volcanic deposits and for modelling hazards from falling bombs.

Scientific ReportsVol. 15(1)
Istituto Nazionale di Geofisica e Vulcanologia (IT), Instituto Tecnológico y de Energías Renovables (ES), Universidad de Ciencias y Artes de Chiapas (MX), Instituto Volcanológico de Canarias (ES), Sapienza University of Rome (IT)
European Commission, Ministero dell’Istruzione, dell’Università e della Ricerca, Istituto Nazionale di Geofisica e Vulcanologia, H2020 Marie Skłodowska-Curie Actions
Openalex Percentile: Top 11%
Particle Dynamics in Fluid Flows
2.29
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