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Modelling temperature distributions and radon emission at Stromboli Volcano using a non-extensive statistical approach

✍ Scribed by G Gervino; C Cigolini; A Lavagno; C Marino; P Prati; L Pruiti; G Zangari


Publisher
Elsevier Science
Year
2004
Tongue
English
Weight
272 KB
Volume
340
Category
Article
ISSN
0378-4371

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✦ Synopsis


Studying the hydrothermal features in a volcanic ÿeld is an important step in understanding eruption mechanisms as well as volcanically induced earthquakes. These processes can occur cyclically in a volcanic systems and could be explained by modern thermo-uidodynamics theory. A computer model has been performed on the basis of ÿeld measurements. Radon emission are strictly correlated with magma degassing, the local temperature gradient, rock porosities and permeabilities. Anomalies in radon emissions at the surface can provide critical informations about the geothermal system and about the distribution of fracture networks in the volcanic structure. We therefore describe radon migration from the magma column and from the magma chamber in terms of a bi-dimensional model, in order to explain relative radon peak emissions by using a non-extensive statistical approach. The results of the model, compared with the collected ÿeld data, are hereby presented and discussed.