James E. Gardner
Bubble Formation in Magma
Gardner, James E.; Wadsworth, Fabian B.; Carley, Tamara L.; Llewellin, Edward W.; Kusumaatmaja, Halim; Sahagian, Dork
Authors
Dr Fabian Wadsworth fabian.b.wadsworth@durham.ac.uk
Associate Professor
Tamara L. Carley
Professor Edward Llewellin ed.llewellin@durham.ac.uk
Professor
Halim Kusumaatmaja halim.kusumaatmaja@durham.ac.uk
Visiting Professor
Dork Sahagian
Abstract
Volcanic eruptions are driven by bubbles that form when volatile species exsolve from magma. The conditions under which bubbles form depend mainly on magma composition, volatile concentration, presence of crystals, and magma decompression rate. These are all predicated on the mechanism by which volatiles exsolve from the melt to form bubbles. We critically review the known or inferred mechanisms of bubble formation in magmas: homogeneous nucleation, heterogeneous nucleation on crystal surfaces, and spontaneous phase separation (spinodal decomposition). We propose a general approach for calculating bubble nucleation rates as the sum of the contributions from homogeneous and heterogeneous nucleation, suggesting that nucleation may not be limited to a single mechanism prior to eruption. We identify three major challenges in which further experimental, analytical, and theoretical work is required to permit the development of a general model for bubble formation under natural eruption conditions. ▪ We review the mechanisms of bubble formation in magma and summarize the conditions under which the various mechanisms are understood to operate. ▪ Bubble formation mechanisms may evolve throughout magma ascent as conditions change such that bubbles may form simultaneously and sequentially via more than one mechanism. ▪ Contributions from both homogeneous nucleation and heterogeneous nucleation on multiphase crystal phases can be captured via a single equation. ▪ Future work should focus on constraining macroscopic surface tension, characterizing the microphysics, and developing a general framework for modeling bubble formation, via all mechanisms, over natural magma ascent pathways.
Citation
Gardner, J. E., Wadsworth, F. B., Carley, T. L., Llewellin, E. W., Kusumaatmaja, H., & Sahagian, D. (2023). Bubble Formation in Magma. Annual Review of Earth and Planetary Sciences, 51(1), 131-154. https://doi.org/10.1146/annurev-earth-031621-080308
Journal Article Type | Article |
---|---|
Online Publication Date | May 31, 2023 |
Publication Date | 2023 |
Deposit Date | Jun 5, 2023 |
Publicly Available Date | Jun 5, 2023 |
Journal | Annual Review of Earth and Planetary Sciences |
Print ISSN | 0084-6597 |
Electronic ISSN | 1545-4495 |
Publisher | Annual Reviews |
Peer Reviewed | Peer Reviewed |
Volume | 51 |
Issue | 1 |
Pages | 131-154 |
DOI | https://doi.org/10.1146/annurev-earth-031621-080308 |
Public URL | https://durham-repository.worktribe.com/output/1172905 |
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Copyright Statement
Copyright © 2023 by the author(s). This work is licensed under a Creative Commons Attribution 4.0 International License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. See credit lines of images or other third-party material in this article for license information
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