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In-conduit capture of sub-micron volcanic ash particles via turbophoresis and sintering

Author

Listed:
  • Jamie I. Farquharson

    (Université de Strasbourg)

  • Hugh Tuffen

    (Lancaster University)

  • Fabian B. Wadsworth

    (Durham University)

  • Jonathan M. Castro

    (Johannes Gutenberg Universität)

  • Holly Unwin

    (Lancaster University)

  • C. Ian Schipper

    (Victoria University of Wellington)

Abstract

Ash emission in explosive silicic eruptions can have widespread impacts for human health, agriculture, infrastructure, and aviation. Estimates of the total grainsize distribution (TGSD) generated during explosive magma fragmentation underpins eruption models and ash dispersal forecasts. Conventionally, the TGSD constrained via erupted deposits is assumed to match the TGSD produced at explosive fragmentation. Here we present observations from within the vent of a recent rhyolitic eruption (Cordón Caulle, Chile, 2011–2012), demonstrating that fine (

Suggested Citation

  • Jamie I. Farquharson & Hugh Tuffen & Fabian B. Wadsworth & Jonathan M. Castro & Holly Unwin & C. Ian Schipper, 2022. "In-conduit capture of sub-micron volcanic ash particles via turbophoresis and sintering," Nature Communications, Nature, vol. 13(1), pages 1-11, December.
    • Handle: RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-32522-7
    DOI: 10.1038/s41467-022-32522-7
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    References listed on IDEAS

    as
    1. Mike Cassidy & Michael Manga & Kathy Cashman & Olivier Bachmann, 2018. "Controls on explosive-effusive volcanic eruption styles," Nature Communications, Nature, vol. 9(1), pages 1-16, December.
    2. Jonathan M. Castro & Donald B. Dingwell, 2009. "Rapid ascent of rhyolitic magma at Chaitén volcano, Chile," Nature, Nature, vol. 461(7265), pages 780-783, October.
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