Item talk:Q242305
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Electrical activity during the 2006 Mount St. Augustine volcanic eruptions", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70172021", "url": "https://pubs.usgs.gov/publication/70172021" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70172021 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1126/science.1136091", "url": "https://doi.org/10.1126/science.1136091" } ], "journal": { "@type": "Periodical", "name": "Science", "volumeNumber": "315", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Science" } ], "datePublished": "2007", "dateModified": "2016-06-06", "abstract": "By using a combination of radio frequency time-of-arrival and interferometer measurements, we observed a sequence of lightning and electrical activity during one of Mount St. Augustine's eruptions. The observations indicate that the electrical activity had two modes or phases. First, there was an explosive phase in which the ejecta from the explosion appeared to be highly charged upon exiting the volcano, resulting in numerous apparently disorganized discharges and some simple lightning. The net charge exiting the volcano appears to have been positive. The second phase, which followed the most energetic explosion, produced conventional-type discharges that occurred within plume. 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