Gas-Pyroclast Motions in Volcanic Conduits During Strombolian Eruptions, in Light of Shock Tube Experiments

Salvatore, Valentino; Cigala, Valeria; Taddeucci, Jacopo; Arciniega-Ceballos, Alejandra; Pena Fernandez, Juan Jose; Alatorre-Ibarguengoitia, Miguel Angel; Gaudin, Damien; Palladino, Danilo M.; Kueppers, Ulrich und Scarlato, Piergiorgio (2020): Gas-Pyroclast Motions in Volcanic Conduits During Strombolian Eruptions, in Light of Shock Tube Experiments. In: Journal of Geophysical Research-Solid Earth, Bd. 125, Nr. 4, e2019JB019182

Abstract

In a Strombolian volcanic eruption, bursting of a pressurized gas pocket accelerates a mixture of gas and pyroclasts along a conduit and out of a vent. While mixture ejection at the vent is the subject of direct geophysical measurements, and a key to eruption understanding, the dynamics of how the mixture moves in the conduit are not observable and only partly understood. Here, we use analog, transparent shock tube experiments to study the dynamics of gas and particles under fast gas decompression in a vertical tube. Maximum particle exit velocity increases linearly with increasing energy (pressure times volume) of the pressurized gas and, subordinately, with decreasing particle size and depth in the tube. Particles, initially at rest, are at first accelerated and dispersed in the conduit by the expanding gas. When the gas decelerates or even reverses its motion due to pressure changes in the tube, the particles, moving under their inertia, are then decelerated by the gas drag. Deceleration lasts longer for lower initial gas energy and for deeper particle starting position. Experiments and eruptions share two key vent ejection features: (1) particles exit the vent already decelerating, and (2) the exit velocity of the particles decays over time following the same nonlinear law. Friction with slower or even backflowing gas likely causes pyroclast deceleration in volcanic conduits during Strombolian explosions. Pyroclast deceleration, in turn, affects their exit velocity at the vent, as well as estimates of the explosion source depth based on temporal changes in exit velocity. Plain Language Summary Strombolian explosions are relatively small but frequent explosive volcanic eruptions that attract both scientists and tourists and represent a good test ground for new theories and a source of hazard for visitors. The explosions, driven by the release of large pockets of pressurized gas in the magma, eject gas and magma fragments (volcanic ash, lapilli, and blocks) from a vent, but how these components move before reaching the vent is still unclear. We reproduce Strombolian explosions using a shock tube. The lower part of the tube is filled with pressurized gas. The upper part is at ambient conditions and contains volcanic particles. When opening a diaphragm separating the two parts, a shock wave pressurizes the upper tube, the gas and particles are ejected, and we track their motion. The particles are first accelerated by the expanding gas at a velocity that depends on the gas pressure and volume and then decelerate because the gas slows down first while the particles move faster due to inertia. Current observations at volcanoes suggest that the same process probably occurs during Strombolian explosions. Studying how particles move in volcanic conduits is important for understanding the hazards they may pose and the depths from which they come.

• Dokumententyp: Zeitschriftenartikel
• Fakultät: Geowissenschaften > Department für Geo- und Umweltwissenschaften
• Themengebiete: 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie
• ISSN: 2169-9313
• Sprache: Englisch