Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10360
AuthorsDi Martino, R. M. R.* 
Capasso, G.* 
Camarda, M.* 
TitleSpatial domain analysis of carbon dioxide from soils on Vulcano Island: Implications for CO2 output evaluation
Issue Date28-Sep-2016
Series/Report no./444(2016)
DOI10.1016/j.chemgeo.2016.09.037
URIhttp://hdl.handle.net/2122/10360
KeywordsCarbon dioxide
CO2 flux
CO2 soil degassing
CO2 isotope composition
Volcano monitoring
Vulcano Island (Aeolian Islands)
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.01. Gases 
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques 
05. General::05.02. Data dissemination::05.02.01. Geochemical data 
AbstractThe carbon dioxide emissions of volcanoes have been targeted as effective contributors of CO2 to the atmosphere. However, different sources can be effective and active at the same time in the generation and release of CO2 in volcanic zones. Since isotopic fingerprinting of CO2 allows the precise identification of different sources, coupling carbon isotope and CO2 flux measurements enables the evaluation of the mass contribution of each source to the carbon dioxide emissions. This paper accounts for the first extensive spatial analysis of coupled measurements of carbon isotopologues of CO2 in the soil gases and CO2 fluxes discharged by soils on Vulcano Island. An innovative method has been designed, tested and fine-tuned in the laboratory to measure δ13C(CO2) values directly in field using a new type of laser-based isotopologues analyzer, namely a DeltaRay™ (Thermo Fisher Scientific). The method can be used to determine the carbon isotope composition across the full range of CO2 concentrations in the soil gases (0 – 100 vol%). These data have been combined with measurements of the CO2 contents in the soil gases to distinguish CO2 from deep origins from CO2 of biogenic origin in the inhabited area of Vulcano Porto. The method of evaluating the amount of deep-origin CO2 in the soil gases is widely applicable in volcanic and geothermal zones for evaluation and monitoring purposes for both gas and volcanic hazards.
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