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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8373

Authors: Del Bello, E.*
Llewellin, E. W.*
Taddeucci, J.*
Scarlato, P.*
Lane, S.*
Title: An analytical model for gas overpressure in slug-driven explosions: Insights into Strombolian volcanic eruptions
Title of journal: Journal of geophysical research - solid earth
Series/Report no.: /117(2012)
Publisher: American Geophysical Union
Issue Date: 10-Feb-2012
DOI: 10.1029/2011JB008747
Keywords: Stromboli
Taylor bubble
basaltic volcanoes
falling film
gas slug
Abstract: Strombolian eruptions, common at basaltic volcanoes, are mildly explosive events that are driven by a large bubble of magmatic gas (a slug) rising up the conduit and bursting at the surface. Gas overpressure within the bursting slug governs explosion dynamics and vigor and is the main factor controlling associated acoustic and seismic signals. We present a theoretical investigation of slug overpressure based on magma-static and geometric considerations and develop a set of equations that can be used to calculate the overpressure in a slug when it bursts, slug length at burst, and the depth at which the burst process begins. We find that burst overpressure is controlled by two dimensionless parameters: V′, which represents the amount of gas in the slug, and A′, which represents the thickness of the film of magma that falls around the rising slug. Burst overpressure increases nonlinearly as V′ and A′ increase. We consider two eruptive scenarios: (1) the “standard model,” in which magma remains confined to the vent during slug expansion, and (2) the “overflow model,” in which slug expansion is associated with lava effusion, as occasionally observed in the field. We find that slug overpressure is higher for the overflow model by a factor of 1.2–2.4. Applying our model to typical Strombolian eruptions at Stromboli, we find that the transition from passive degassing to explosive bursting occurs for slugs with volume >24–230 m3, depending on magma viscosity and conduit diameter, and that at burst, a typical Strombolian slug (with a volume of 100–1000 m3) has an internal gas pressure of 1–5 bars and a length of 13–120 m. We compare model predictions with field data from Stromboli for low-energy “puffers,” mildly explosive Strombolian eruptions, and the violently explosive 5 April 2003 paroxysm. We find that model predictions are consistent with field observations across this broad spectrum of eruptive styles, suggesting a common slug-driven mechanism; we propose that paroxysms are driven by unusually large slugs (large V′).
Appears in Collections:04.08.99. General or miscellaneous
Papers Published / Papers in press
04.08.03. Magmas
04.08.02. Experimental volcanism

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