Carbon dioxide diffuse emission from the soil: ten years of observations at Vesuvio and Campi Flegrei (Pozzuoli), and linkages with volcanic activity |
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Authors: | D Granieri R Avino G Chiodini |
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Institution: | (1) Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Via della Faggiola, 32, 56126 Pisa, Italy;(2) Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Sezione di Napoli, via Diocleziano 328, 80124 Napoli, Italy |
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Abstract: | Carbon dioxide flux from the soil is regularly monitored in selected areas of Vesuvio and Solfatara (Campi Flegrei, Pozzuoli)
with the twofold aim of i) monitoring spatial and temporal variations of the degassing process and ii) investigating if the
surface phenomena could provide information about the processes occurring at depth. At present, the surveyed areas include
15 fixed points around the rim of Vesuvio and 71 fixed points in the floor of Solfatara crater. Soil CO2 flux has been measured since 1998, at least once a month, in both areas. In addition, two automatic permanent stations, located
at Vesuvio and Solfatara, measure the CO2 flux and some environmental parameters that can potentially influence the CO2 diffuse degassing. Series acquired by continuous stations are characterized by an annual periodicity that is related to the
typical periodicities of some meteorological parameters. Conversely, series of CO2 flux data arising from periodic measurements over the arrays of Vesuvio and Solfatara are less dependent on external factors
such as meteorological parameters, local soil properties (porosity, hydraulic conductivity) and topographic effects (high
or low ground). Therefore we argue that the long-term trend of this signal contains the “best” possible representation of
the endogenous signal related to the upflow of deep hydrothermal fluids. |
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