Earth-prints repository, logo   DSpace

About DSpace Software
|earth-prints home page | roma library | bologna library | catania library | milano library | napoli library | palermo library
Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7415

Authors: Carapezza, M. L.*
Barberi, F.*
Ranaldi, M.*
Ricci, T.*
Tarchini, L.*
Title: Diffuse CO2 soil degassing and CO2 and H2S air concentration and related hazard at Vulcano Island (Aeolian arc, Italy).
Title of journal: Journal of Volcanology and Geothermal Research
Series/Report no.: 3-4/207(2011)
Publisher: elsevier
Issue Date: 2011
DOI: 10.1016/j.jvolgeores.2011.06.010
URL: http://www.sciencedirect.com/science/article/pii/S0377027311001764
Keywords: Vulcano Island
diffuse degassing
Abstract: La Fossa crater on Vulcano Island is quiescent since 1890. Periodically it undergoes “crises” characterized by marked increase of temperature (T), gas output and concentration of magmatic components in the crater fumaroles (T may exceed 600 °C). During these crises, which so far did not lead to any eruptive reactivation, the diffuse CO2 soil degassing also increases and in December 2005 an anomalous CO2 flux of 1350 tons/day was estimated by 1588 measurements over a surface of 1.66 km2 extending from La Fossa crater to the inhabited zone of Vulcano Porto. The crater area and two other anomalously degassing sites (Levante Beach and Palizzi) have been periodically investigated from December 2004 to August 2010 for diffuse CO2 soil flux. They show a marked variation with time of the degassing rate, with synchronous maxima in December 2005. Carbon dioxide soil flux and environmental parameters have been also continuously monitored for over one year by an automatic station at Vulcano Porto. In order to assess the hazard of the endogenous gas emissions, CO2 and H2S air concentrations have been measured by Tunable Diode Laser profiles near the fumaroles of the crater rim and of the Levante Beach area, where also the viscous gas flux has been estimated. In addition, CO2 air concentration has been measured both indoor and outdoor in an inhabited sector of Vulcano Porto. Results show that in some sites usually frequented by tourists there is a dangerous H2S air concentration and CO2 exceeds the hazardous thresholds in some Vulcano houses. These zones should be immediately monitored for gas hazard should a new crisis arise.
Appears in Collections:04.04.12. Fluid Geochemistry
Papers Published / Papers in press

Files in This Item:

File Description SizeFormatVisibility
vulcano carapezza et al 2011 JVGR 2.pdfmain article3.95 MBAdobe PDFView/Open
12 2011 JVGR Vulcano.pdf3.3 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.


Share this record
Del.icio.us

Citeulike

Connotea

Facebook

Stumble it!

reddit


 

Valid XHTML 1.0! ICT Support, development & maintenance are provided by CINECA. Powered on DSpace Software. CINECA