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Radon in fumarolic gases from vulcano island (Sicily, Italy)

Journal Article · · Geothermics; (United States)
In this study, Radon-222 activity was measured sporadically in fumarolic gases from the island of Vulcano (Italy) between 1978 and 1980. Rn variations in the crater fumaroles (300/sup 0/C) were found to be correlated with microseismic activity; they also correlate positively with water and negatively with the S/C1 ratio. On the basis of a geochemical model, the fumarolic gases at Vulcano are assumed to be a mixture of deep magmatic gases and fluids from shallow aquifers. Rn is carried by these fluids (an average of 500 nCi per kg of fluid). Circulating water can strip Rn from the U-rich rocks on Vulcano. At present it is impossible to determine whether microseismicity is producing composition changes, or vice versa, or whether both are the consequence of a main volcano-tectonic event.
Research Organization:
Istituto di Geocronologia e Geochimica Isotopica, CNR, Via Cardinale Maffi 36, Pisa
OSTI ID:
5047778
Journal Information:
Geothermics; (United States), Journal Name: Geothermics; (United States) Vol. 13:4; ISSN GTMCA
Country of Publication:
United States
Language:
English