Many explosive volcanic eruptions produce underexpanded starting gas-particle jets. The dynamics of the accompanying pyroclast ejection can be affected by several parameters, including magma texture, gas overpressure, erupted volume and geometry. With respect to the latter, volcanic craters and vents are often highly asymmetrical. Here, we experimentally evaluate the effect of vent asymmetry on gas expansion behaviour and gas jet dynamics directly above the vent. The vent geometries chosen for this study are based on field observations. The novel element of the vent geometry investigated herein is an inclined exit plane (5, 15, 30° slant angle) in combination with cylindrical and diverging inner geometries. In a vertical setup, these modifi...
International audienceExplosive volcanic eruptions produce high-velocity turbulent jets that can for...
Plinian air‐fall deposits and ignimbrites are the principal products of explosive eruptions of high ...
The eruption style of silicic magmas is affected by the loss of gas (outgassing) during ascent. We i...
Many explosive volcanic eruptions produce underexpanded starting gas-particle jets. The dynamics of ...
Predicting the onset, style and duration of explosive volcanic eruptions remains a great challenge. ...
We present a model of fountain collapse for small-scale (Soufrière-type) explosive eruptions that re...
International audienceThick lava flows that are a feature of many volcanic fields on the Earth and V...
Turbulent volcanic jets are produced by highly-energetic explosive eruptions and may form buoyant pl...
International audienceTurbulent volcanic jets are produced by highly-energetic explosive eruptions a...
AbstractWe present three‐dimensional numerical simulations of eruption clouds from circular to linea...
Pyroclast ejection during explosive volcanic eruptions occurs under highly dynamic conditions invol...
The spatial distribution of eruptive vents around volcanoes can be complex and evolve as a volcano g...
AbstractPyroclast ejection during explosive volcanic eruptions occurs under highly dynamic condition...
International audienceEfficient turbulent entrainment causes otherwise dense volcanic jets to rise h...
International audienceExplosive volcanic eruptions produce high-velocity turbulent jets that can for...
Plinian air‐fall deposits and ignimbrites are the principal products of explosive eruptions of high ...
The eruption style of silicic magmas is affected by the loss of gas (outgassing) during ascent. We i...
Many explosive volcanic eruptions produce underexpanded starting gas-particle jets. The dynamics of ...
Predicting the onset, style and duration of explosive volcanic eruptions remains a great challenge. ...
We present a model of fountain collapse for small-scale (Soufrière-type) explosive eruptions that re...
International audienceThick lava flows that are a feature of many volcanic fields on the Earth and V...
Turbulent volcanic jets are produced by highly-energetic explosive eruptions and may form buoyant pl...
International audienceTurbulent volcanic jets are produced by highly-energetic explosive eruptions a...
AbstractWe present three‐dimensional numerical simulations of eruption clouds from circular to linea...
Pyroclast ejection during explosive volcanic eruptions occurs under highly dynamic conditions invol...
The spatial distribution of eruptive vents around volcanoes can be complex and evolve as a volcano g...
AbstractPyroclast ejection during explosive volcanic eruptions occurs under highly dynamic condition...
International audienceEfficient turbulent entrainment causes otherwise dense volcanic jets to rise h...
International audienceExplosive volcanic eruptions produce high-velocity turbulent jets that can for...
Plinian air‐fall deposits and ignimbrites are the principal products of explosive eruptions of high ...
The eruption style of silicic magmas is affected by the loss of gas (outgassing) during ascent. We i...