Volcano Blog by Tom Pering
  • Blog
  • UV Cameras
  • Publications
  • Slug Calculator
  • About Me

Another year, another EGU! #EGU16

15/4/2016

 
Picture
Another year, and another EGU, my third so far. Again, I am looking forward to a couple of days of sciencey goodness. This year I am trying to do EGU on a budget, which is not an easy task! Perhaps I shall blog a few tips afterwards. I shall be attending volcanic sessions on Monday and Tuesday and will blog about some of the fascinating science that is presented during oral sessions and posters. Looking forward to seeing new and familiar faces!

I will be presenting on "Gas Emissions and Slug Dynamics" on Tuesday at 11 am. I will be talking about work conducted comparing UV camera measurements of a large number of events at Stromboli and computational simulations of slug flow. My abstract is below:

Abstract: We present UV camera data for 200 strombolian and hornito degassing events at Stromboli during June and July 2014. This data was processed to calculate SO2 masses for each event. In addition to calculating SO2 masses of the slugs which generate these events we also observe periods of elevated flux following events, termed the gas coda, lasting ≈ 30 – 180 s, which we also calculate SO2masses for. This provided a range of explosive plus coda SO2 masses of ≈ 18 – 225 kg. In combination with 3D fluid numerical simulations of slug flow we begin to probe a possible generation mechanism for the observed gas codas. The simulations show that ‘daughter bubbles’ are produced from the base of ascending slugs, which result in gas mass loss rates from the slugs of between ≈ 1.2 – 14.2 kg s−1 . Nf , the dimensionless inverse viscosity number, can be used to characterise the form of a slug wake, and hence when mass loss through daughter bubble production may occur. However, the observed daughter bubble behaviour occurs at lower levels of Nf than predicted by previous mm- to cm-scale studies and suggests that extra physics (e.g. surface tension), beyond that included in Nf , may be needed to parameterise daughter bubble production. We suggest that daughter bubbles could play a role in modulating explosivity of strombolian eruptions as a potential causal mechanism for gas coda production.​

Comments are closed.
    Volcano Blog Logo

    RSS Feed

    Share this page

    Archives

    July 2023
    August 2022
    May 2022
    January 2021
    February 2020
    December 2019
    November 2019
    April 2019
    January 2019
    May 2018
    April 2018
    March 2018
    February 2018
    January 2018
    October 2017
    August 2017
    June 2017
    January 2017
    October 2016
    July 2016
    June 2016
    May 2016
    April 2016
    January 2016
    December 2015
    July 2015
    June 2015
    May 2015
    April 2015
    March 2015
    January 2015
    December 2014
    August 2014
    July 2014
    June 2014
    May 2014
    April 2014
    January 2014
    November 2013
    October 2013
    September 2013
    August 2013
    July 2013
    June 2013
    May 2013
    April 2013
    March 2013
    February 2013
    January 2013
    December 2012
    November 2012
    October 2012
    September 2012
    August 2012
    July 2012
    May 2012
    April 2012
    March 2012
    February 2012
    December 2011
    November 2011
    October 2011
    September 2011
    July 2011
    June 2011
    May 2011
    April 2011
    March 2011

An informative blog for anyone interested about all things volcano related!
  • Blog
  • UV Cameras
  • Publications
  • Slug Calculator
  • About Me