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Instituto de Investigação
em Vulcanologia e Avaliação de Riscos
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Painéis ► em encontros internacionais

 

Referência Bibliográfica


VIVEIROS, F.; CARDELLINI, C.; FERREIRA, T.; CALIRO, S.; CHIODINI, G.; SILVA, C.; PEDONE, M.; ANDRADE, C.; ZANON, V.; HIPÓLITO, A.R. (2015) - CO2 degassing zones in various volcanic systems of the Azores archipelago (Portugal) – continuous and discrete measurements. Deep Carbon Observatory – Second International Science Meeting, 26 a 28 de Março, Munique, Alemanha.

Resumo


​CO2 is one of the most abundant volcanic gases and is released not only during eruptive periods, but also during quiescent periods of activity. 
This is the case of the various CO2 emissions found in the Azores archipelago volcanic systems. In fact, and even if the last volcanic eruption occurred in 1998-2001, nowadays various secondary manifestations of volcanism are found on the islands and high amounts of hydrothermal/volcanic CO2 are emitted, mainly through fumaroles and soil diffuse degassing areas. 
​Furnas volcano (São Miguel Island) shows high CO2 emission, estimated to be about 1200 t d-1accounting with the contribution of the fumaroles, springs, lake and soil diffuse degassing areas. Soil diffuse degassing represents 90% of the total emission. More than 1010 t d-1 shows hydrothermal origin.
At Terceira Island, where a project grant in the scope of the DECADE initiative was developed in 2014, the CO2 emission was estimated to be 3 t d-1 from an area with about 24700 m2, and the presence of hydrothermal CO2 was essentially associated with the area surrounding the only fumarolic ground of the island.
Carbon isotopic data (δ13CCO2) o​f the sampled gases (soil fluxes, fumaroles and fluid inclusions) were used to discriminate different origins (biogenic vs. hydrothermal) for the CO2.
A permanent network of seven soil CO2 flux stations is also installed in the archipelago and time series show significant daily and seasonal variations related mainly with meteorological variables.

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