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The importance of grain size and shape in controlling the dispersion of the Vedde cryptotephra

Research output: Contribution to journalArticle

Original languageEnglish
Pages (from-to)175-185
Number of pages11
JournalJournal of Quaternary Science
Volume35
Issue number1-2
Early online date25 Nov 2019
DOIs
DateAccepted/In press - 17 Sep 2019
DateE-pub ahead of print - 25 Nov 2019
DatePublished (current) - 29 Jan 2020

Abstract

Volcanic ash is dispersed in the atmosphere according to meteorology and particle properties, including size and shape. However, the multiple definitions of size and shape for non‐spherical particles affect our ability to use physical particle properties to understand tephra transport. Moreover, although particles <100µm are often excluded from operational ash dispersion model setups, ash in tephra deposits <1000 km from source can exceed 100µm. Here we measure the shape and size of samples of Vedde ash from Iceland, an exceptionally widespread tephra layer in Europe, collected in Iceland and Norway. Using X‐ray computed tomography and optical microscopy, we show that distal ash is more anisotropic than proximate ash, suggesting that shape exerts an important control on tephra dispersion. Shape also impacts particle size measurements. Particle long axis, a parameter often reported by tephrochronologists, is on average 2.4x greater than geometric size, used by dispersion modellers. By using geometric size and quantifying shape, we can explain the transport of Vedde ash particles <190µm more than 1200 km from source. We define a set of best practices for measuring the size and shape of cryptotephra shards and discuss the benefits and limitations of using physical particle properties to understand cryptotephra transport.

    Research areas

  • volcanic ash, dispersion modelling, cryptotephra deposits, particle shapes, settling velocity

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    Rights statement: This is the final published version of the article (version of record). It first appeared online via Wiley at https://onlinelibrary.wiley.com/doi/full/10.1002/jqs.3152 . Please refer to any applicable terms of use of the publisher.

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