Articles | Volume 8, issue 2
Solid Earth, 8, 561–581, 2017
https://doi.org/10.5194/se-8-561-2017
Solid Earth, 8, 561–581, 2017
https://doi.org/10.5194/se-8-561-2017

Research article 27 Apr 2017

Research article | 27 Apr 2017

Inelastic compaction and permeability evolution in volcanic rock

Jamie I. Farquharson et al.

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Cited articles

Adelinet, M., Fortin, J., Schubnel, A. and Guéguen, Y.: Deformation modes in an Icelandic basalt: from brittle failure to localized deformation bands, J. Volcanol. Geoth. Res., 255, 15–25, 2013.
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Short summary
In volcanic rock, permeability is the property that tells us how efficiently fluids such as gas or water can travel through cracks and frozen bubbles in the rock (its porosity) and is important in the context of volcanic activity. This study addresses how permeability evolves under a range of mechanical experimental conditions. We show that with a small amount of porosity loss (compaction), permeability can increase. However, with more compaction, permeability can decrease significantly.