Award Abstract # 0751776
Collaborative Research: Strombolian eruptions, magma degassing, and hydrothermal discharge at an active submarine arc volcano

NSF Org: OCE
Division Of Ocean Sciences
Recipient: OREGON STATE UNIVERSITY
Initial Amendment Date: February 11, 2009
Latest Amendment Date: October 13, 2009
Award Number: 0751776
Award Instrument: Continuing Grant
Program Manager: Barbara Ransom
bransom@nsf.gov
 (703)292-7792
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: February 1, 2009
End Date: January 31, 2012 (Estimated)
Total Intended Award Amount: $330,304.00
Total Awarded Amount to Date: $390,304.00
Funds Obligated to Date: FY 2009 = $220,342.00
FY 2010 = $169,962.00
History of Investigator:
  • William Chadwick (Principal Investigator)
    bill.chadwick@oregonstate.edu
  • Robert Dziak (Co-Principal Investigator)
Recipient Sponsored Research Office: Oregon State University
1500 SW JEFFERSON AVE
CORVALLIS
OR  US  97331-8655
(541)737-4933
Sponsor Congressional District: 04
Primary Place of Performance: Oregon State University Marine Science Center
Newport
OR  US  97365-5296
Primary Place of Performance
Congressional District:
04
Unique Entity Identifier (UEI): MZ4DYXE1SL98
Parent UEI:
NSF Program(s): Marine Geology and Geophysics
Primary Program Source: 01000910DB NSF RESEARCH & RELATED ACTIVIT
01001011DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 162000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

In April 2006, extraordinary observations of a deep-sea explosive (Strombolian) volcanic eruption were made at NW Rota-1, a submarine volcano in the Mariana arc of the western Pacific. This research funds a return to the volcano to collect observational and analytical data and its subsequent on-shore data analysis and interpretation. Instruments including hydrophones, chemical sensors, current meters, and plume sensing devices will be deployed at the eruption site for one year. During the cruises, visual observations will made. A time-series collection of lava, gas and fluids at the active volcanic vent will also take place. Vent fluids and biological specimens from local hydrothermal vent sites will also be sampled. In terms of scientific impact, the research provides an opportunity to learn about volcanological process that have been impossible to study directly until now. Owing to the high viscosity of water, compared to air, closer and more specific observation and sampling of a Strombolian eruption can take place at Rota 1 than can be accomplished in subaerial settings. As a result, this work reveals critical proceses that help unravel eruptive mechanism of a highly destructive type of explosive volcanism. Broader impacts include public outreach via the media. The work also involves inter-Agency participation, an interdisciplinary inter-institutional collaboration, and the training a graduate student.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Butterfield, DA; Nakamura, K; Takano, B; Lilley, MD; Lupton, JE; Resing, JA; Roe, KK "High SO2 flux, sulfur accumulation, and gas fractionation at an erupting submarine volcano" GEOLOGY , v.39 , 2011 , p.803 View record at Web of Science 10.1130/G31901.
Chadwick, WW; Embley, RW; Baker, ET; Resing, JA; Lupton, JE; Cashman, KV; Dziak, RP; Tunnicliffe, V; Butterfield, DA; Tamura, Y "Northwest Rota-1 Seamount" OCEANOGRAPHY , v.23 , 2010 , p.182 View record at Web of Science
Chadwick, W. W., Jr., R. P. Dziak, J. H. Haxel, R. W. Embley, and H. Matsumoto "Submarine landslide triggered by volcanic eruption recorded by in-situ hydrophone" Geology , v.40 , 2012 , p.51 doi:10.1130/G32495.1
Huber, J. A., H. V. Cantin, S. M. Huse, D. B. M. Welch, M. L. Sogin, and D. A. Butterfield "Isolated communities of Epsilonproteobacteria in hydrothermal vent fluids of the Mariana Arc seamounts" FEMS Microb. Ecol. , v.73 , 2010 , p.538 DOI:10.1111/j.1574-6941.2010.00910.x

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