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Fig. 7 | Earth, Planets and Space

Fig. 7

From: Influence of permeability on the hydrothermal system at Vulcano Island (Italy): inferences from numerical simulations

Fig. 7

Simulated surface temperature from January 2001 to April 2005. The values of the conduit permeability, the CO2 flow rate, and its percentage in the mixture are reported over time. An increase in the permeability and in the flow rate and percentage of CO2 are simulated in the linear trend period and in the heating phase from 6 November 2004 to 13 January 2005, while a decrease in the permeability and in the content and percentage of CO2 are simulated in the cooling phase which affects the period 14 January 2005–30 April 2005 (Tables 3, 4). The temperature measurements are extrapolated from Diliberto (2011)

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