A theoretical model of the explosive fragmentation of vesicular magma

Recent experimental work has shown that, when a vertical column of rock under large pressure is suddenly depressurized, the column can 'explode' in a structured and repeatable way. The observations show that a sequence of horizontal fractures forms from the top down, and the resulting bloc...

Description complète

Détails bibliographiques
Auteurs principaux: Fowler, A, Scheu, B, Lee, W, McGuinness, M
Format: Journal article
Langue:English
Publié: 2010
_version_ 1826283970954788864
author Fowler, A
Scheu, B
Lee, W
McGuinness, M
author_facet Fowler, A
Scheu, B
Lee, W
McGuinness, M
author_sort Fowler, A
collection OXFORD
description Recent experimental work has shown that, when a vertical column of rock under large pressure is suddenly depressurized, the column can 'explode' in a structured and repeatable way. The observations show that a sequence of horizontal fractures forms from the top down, and the resulting blocks are lifted off and ejected. The blocks can suffer secondary internal fractures. This experiment provides a framework for understanding the way in which catastrophic explosion can occur, and is motivated by the corresponding phenomenon of magmatic explosion during Vulcanian eruptions. We build a theoretical model to describe these results, and show that it is capable of describing both the primary sequence of fracturing and the secondary intrablock fracturing. The model allows us to suggest a practical criterion for when such explosions occur: firstly, the initial confining pressure must exceed the yield stress of the rock, and, secondly, the diffusion of the gas by porous flow must be sufficiently slow that a large excess pore pressure is built up. This will be the case if the rock permeability is small enough. © 2010 The Royal Society.
first_indexed 2024-03-07T01:06:50Z
format Journal article
id oxford-uuid:8ba3650b-5f9f-456e-8bfb-5af11821767c
institution University of Oxford
language English
last_indexed 2024-03-07T01:06:50Z
publishDate 2010
record_format dspace
spelling oxford-uuid:8ba3650b-5f9f-456e-8bfb-5af11821767c2022-03-26T22:39:17ZA theoretical model of the explosive fragmentation of vesicular magmaJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:8ba3650b-5f9f-456e-8bfb-5af11821767cEnglishSymplectic Elements at Oxford2010Fowler, AScheu, BLee, WMcGuinness, MRecent experimental work has shown that, when a vertical column of rock under large pressure is suddenly depressurized, the column can 'explode' in a structured and repeatable way. The observations show that a sequence of horizontal fractures forms from the top down, and the resulting blocks are lifted off and ejected. The blocks can suffer secondary internal fractures. This experiment provides a framework for understanding the way in which catastrophic explosion can occur, and is motivated by the corresponding phenomenon of magmatic explosion during Vulcanian eruptions. We build a theoretical model to describe these results, and show that it is capable of describing both the primary sequence of fracturing and the secondary intrablock fracturing. The model allows us to suggest a practical criterion for when such explosions occur: firstly, the initial confining pressure must exceed the yield stress of the rock, and, secondly, the diffusion of the gas by porous flow must be sufficiently slow that a large excess pore pressure is built up. This will be the case if the rock permeability is small enough. © 2010 The Royal Society.
spellingShingle Fowler, A
Scheu, B
Lee, W
McGuinness, M
A theoretical model of the explosive fragmentation of vesicular magma
title A theoretical model of the explosive fragmentation of vesicular magma
title_full A theoretical model of the explosive fragmentation of vesicular magma
title_fullStr A theoretical model of the explosive fragmentation of vesicular magma
title_full_unstemmed A theoretical model of the explosive fragmentation of vesicular magma
title_short A theoretical model of the explosive fragmentation of vesicular magma
title_sort theoretical model of the explosive fragmentation of vesicular magma
work_keys_str_mv AT fowlera atheoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT scheub atheoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT leew atheoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT mcguinnessm atheoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT fowlera theoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT scheub theoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT leew theoreticalmodeloftheexplosivefragmentationofvesicularmagma
AT mcguinnessm theoreticalmodeloftheexplosivefragmentationofvesicularmagma