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A general model for welding of ash particles in volcanic systems validated using in situ X-ray tomography

Wadsworth, Fabian B.; Vasseur, Jérémie; Schauroth, Jenny; Llewellin, Edward W.; Dobson, Katherine J.; Havard, Tegan; Scheu, Bettina; von Aulock, Felix W.; Gardner, James E.; Dingwell, Donald B.; Hess, Kai-Uwe; Colombier, Mathieu; Marone, Federica; Tuffen, Hugh; Heap, Michael J.

A general model for welding of ash particles in volcanic systems validated using in situ X-ray tomography Thumbnail


Authors

Jérémie Vasseur

Jenny Schauroth

Edward W. Llewellin

Katherine J. Dobson

Tegan Havard

Bettina Scheu

Felix W. von Aulock

James E. Gardner

Donald B. Dingwell

Kai-Uwe Hess

Mathieu Colombier

Federica Marone

Hugh Tuffen

Michael J. Heap



Abstract

Welding occurs during transport and deposition of volcanic particles in diverse settings, including pyroclastic density currents, volcanic conduits, and jet engines. Welding rate influences hazard-relevant processes, and is sensitive to water concentration in the melt. We characterize welding of fragments of crystal-free, water-supersaturated rhyolitic glass at high temperature using in-situ synchrotron-source X-ray tomography. Continuous measurement of evolving porosity and pore-space geometry reveals that porosity decays to a percolation threshold of 1–3 vol.%, at which bubbles become isolated and welding ceases. We develop a new mathematical model for this process that combines sintering and water diffusion, which fits experimental data without requiring empirically-adjusted parameters. A key advance is that the model is valid for systems in which welding is driven by confining pressure, surface tension, or a combination of the two. We use the model to constrain welding timescales in a wide range of volcanic settings. We find that volcanic systems span the regime divide between capillary welding in which surface tension is important, and pressure welding in which confining pressure is important. Our model predicts that welding timescales in nature span seconds to years and that this is dominantly dependent on the particle viscosity or the evolution of this viscosity during particle degassing. We provide user-friendly tools, written in Python™ and in Excel®, to solve for the evolution of porosity and dissolved water concentration during welding for user-defined initial conditions.

Citation

Wadsworth, F. B., Vasseur, J., Schauroth, J., Llewellin, E. W., Dobson, K. J., Havard, T., …Heap, M. J. (2019). A general model for welding of ash particles in volcanic systems validated using in situ X-ray tomography. Earth and Planetary Science Letters, 525, Article 115726. https://doi.org/10.1016/j.epsl.2019.115726

Journal Article Type Article
Acceptance Date Jul 21, 2019
Online Publication Date Aug 19, 2019
Publication Date Nov 30, 2019
Deposit Date Aug 30, 2019
Publicly Available Date Mar 28, 2024
Journal Earth and Planetary Science Letters
Print ISSN 0012-821X
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 525
Article Number 115726
DOI https://doi.org/10.1016/j.epsl.2019.115726

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