Role of volatiles in highly explosive basaltic eruptions

Giuseppe La Spina, Fabio Arzilli, Mike Burton, Margherita Polacci, Amanda Clarke

Research output: Contribution to journalArticlepeer-review

Abstract

Water and carbon dioxide are the most abundant volatile components in terrestrial magmas. As they exsolve into magmatic vapour, they promote magma buoyancy, accelerating ascent and modulating eruptive dynamics. It is commonly thought that an increase in pre-eruptive volatile content produces an increase in eruption intensity. Using a conduit model for basaltic eruptions, covering the upper 6 km of conduit, we show that for the same chamber conditions mass eruption rate is not affected by CO2 content, whereas an increase in H2O up to 10 wt.% produces an increase in eruption rate of an order of magnitude. It is only when CO2 is injected 26 in the magma reservoir from an external source that the resulting pressurization will generate a strong increase in eruption rate. Results also show that ascent velocity and fragmentation depth are strongly affected by pre-eruptive volatile contents demonstrating a link between volatile content and eruptive style.
Original languageEnglish
JournalCommunications Earth & Environment
Publication statusAccepted/In press - 16 Jun 2022

Fingerprint

Dive into the research topics of 'Role of volatiles in highly explosive basaltic eruptions'. Together they form a unique fingerprint.

Cite this