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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7449

Authors: Bai, L.*
Baker, D. R.*
Polacci, M.*
Hill, R. J.*
Title: In-situ degassing study on crystal-bearing Stromboli basaltic magmas: Implications for Stromboli explosions
Title of journal: Geophysical Research Letters
Series/Report no.: /38(2011)
Publisher: American Geophysical Union
Issue Date: 7-Sep-2011
DOI: 10.1029/2011GL048540
URL: http://www.agu.org/pubs/crossref/2011/2011GL048540.shtml
Keywords: Experimental volcanism
Stromboli
degassing
crystal-bearing magmas
Abstract: Three-dimensional crystal and bubble sizes and distributions in experimentally produced vesicular crystal-bearing Stromboli basalts and natural scoria were studied with X-ray microtomography (μCT) at high (1.85 μm) and low (5.46–9.0 μm) resolution. The permeabilities from lattice Boltzmann (LB) simulations and experimental measurements are about 1–2 orders of magnitude higher than in aphyric Stromboli basalts at porosity 31.6–55.3%. We propose that the higher permeability in crystal-bearing samples results in highly efficient degassing in shallow, highly porphyritc (HP) magma as opposed to the deeper, aphyric (LP) magma. In paroxysmal explosions, the LP magma flows up in a cylindrical conduit due to the density and viscosity difference between the two magmas. This type of convection can cause the LP magma with exsolved gas to be efficiently transferred through the overlying HP magma, potentially resulting in the more-violent paroxysmal explosions.
Appears in Collections:04.08.05. Volcanic rocks
04.08.02. Experimental volcanism
Papers Published / Papers in press

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