CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 9
Presentation Time: 9:00 AM-6:00 PM

CORRELATING VOLCANIC SO2 EMISSION-RATES, SEISMICITY, AND ERUPTIVE PROCESSES


DUFFY, Ashley P., Department of Geology & Astronomy, West Chester University of Pennsylvania, Merion Science Center 207, West Chester, PA 19383, AD627215@wcupa.edu

Volcanic emissions of sulfur dioxide (SO2) were first observed and recorded in the late 1960’s, and have since been used as a valuable tool in tracking changes in volcanic activity. This data review compares correlations between SO2 emission-rates, seismicity and eruptive processes of the active volcanoes Kilauea (USA), Mount Etna (Italy), Mount St. Helens (USA), Popocatépetl (Mexico), Masaya (Nicaragua), Soufrière Hills (Montserrat), Galeras (Colombia), and Karymsky (Kamchatka, Russia). This review combines published data and results, from observatories and institutions around the world, in order to examine the eruptive styles of these volcanoes and their relationship to trends of eruptive processes, precursory and syn-eruptive seismicity and SO2 emission-rates. Publications and data sets dating back from 1979 and through to the present were analyzed and classified to both quantitatively and qualitatively reveal correlations between published findings of the volcanoes under investigation.

A variety of SO2 emission-rate measurement systems were used at each of the sites of volcanic activity. The COSPEC and other miniature UV-spectrometer systems which used the DOAS method for analyzing spectral data were utilized based on the frequency of eruptive activity and accessibility to the volcanic plume. Preliminary results have shown that SO2 emission-rates positively correlate with seismic activity, before, during, and after eruptive episodes. This can be seen in cases such as those of the 1991-1993 eruptions of Galeras volcano (Colombia) that reveal the long-term decreases in SO2 flux associated with long-period seismicity. Other positive correlations between volcanic processes, such as ash blasts and increased lava extrusion rates, and SO2 emission-rates have been observed at several of the volcanoes examined in this review. Published interpretations as to the cause of the observed correlations between SO2 flux and seismic/volcanic activity are included in this presentation.

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