Atmospheric 210Po anomaly as a precursor of volcano eruptions

Details Atmospheric 210Po anomaly as a precursor of volcano eruptions Atmospheric 210Po anomaly as a precursor of volcano eruptions

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002georl..29e..14s&link_type=abstract

Geophysical Research Letters, Volume 29, Issue 5, pp. 14-1, CiteID 1070, DOI 10.1029/2001GL013856

Mathematics

Logic

2

Exploration Geophysics: Radioactivity Methods, Atmospheric Composition And Structure: Volcanic Effects (8409), Oceanography: Biological And Chemical: Aerosols (0305), Volcanology: Eruption Monitoring (7280)

Scientific paper

Due to its high volatility, 210Po can be effectively released from active volcanoes prior to their explosions. A continuous record of the fallout rate of 210Po versus that of 210Pb in northern Taiwan reveals that most of the 210Po was derived from pre-eruption gas emission of Philippines'Mayon volcano in the past two years. From this observation we suggest that, if a global network can be properly designed, it may be possible to employ 210Po anomaly as a precursor of volcano eruptions worldwide.

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