Carbon dioxide diffuse emission from the soil: ten years of observations at Vesuvio and Campi Flegrei (Pozzuoli), and linkages with volcanic activity

2009 ◽  
Vol 72 (1) ◽  
pp. 103-118 ◽  
Author(s):  
D. Granieri ◽  
R. Avino ◽  
G. Chiodini
1948 ◽  
Vol 17 (51) ◽  
pp. 97-103 ◽  
Author(s):  
P. O'R. Smiley

Few places in the world can possess more historical associations than the small stretch of country that reaches from Naples west-ward to the shores of the Tyrrhenian Sea. It is known as the ‘Campi Flegrei’, ‘the Burning Fields’, on account of the volcanic activity that has characterized it from the earliest times, and which the recent eruption of Vesuvius shows to be still a formidable feature of the neighbour-hood. In a space of some fifty square miles it contains names which have become the commonplaces of history and legend—Baia, Cuma, Pozzuoli, Averno—places associated for ever with a thousand famous and infamous men—Nero, Ovid, St. Paul, Hannibal, Augustus, Gregory the Great, Totila, Petrarch, Garibaldi. But for many it will be best remembered and most eagerly studied as the scene of the sixth book of the Aeneid; for the story of the Trojan hero's descent to the regions of the dead, while it is one of the greatest pieces of imaginative writing in existence, has a solid foundation in reality. Not only its atmosphere but also its topography can be recaptured to this day in the ‘Campi Flegrei’ a few miles from Naples.That Virgil was well acquainted with this district is beyond doubt, even without the evidence of the sixth book of the Aeneid. The Georgics were written at Naples; and the poet, as friend and admirer of Augustus, must have spent many days among the emperor’s favourite haunts, examinig the famous landmarks and whatching the progress of the great engineering programmes that were being carried out in the Gulf of Pozzuoli.


Science ◽  
1979 ◽  
Vol 204 (4398) ◽  
pp. 1195-1196 ◽  
Author(s):  
D. M. THOMAS ◽  
J. J. NAUGHTON

Nukleonika ◽  
2016 ◽  
Vol 61 (3) ◽  
pp. 245-249
Author(s):  
Erzsébet Sóki ◽  
István Csige

Abstract The final product of a post-volcanic activity is the exhalation of low-temperature (<100°C) gases containing mostly carbon dioxide. The phenomenon is called mofettes, which are often used for therapeutic treatments in the form of dry CO2 spas. Along its pathway to the surface, the deep origin gas also intakes different radon isotopes from the rocks and soils; therefore, the risks associated with radon exposures should also be a concern. In this work, we have found that the 222Rn activity concentration in the mofette gas of Mátraderecske is particularly high; it is in the order of 200 kBq·m−3. However, owing to the carefully designed flow pattern of mofette gas and fresh air, the radon level is about 1 kBq·m−3 at the breath level of the staff, accompanying the treatment, which is the radon reference level for workers in Hungary. We have also found that in this dry spa, radon is a good tracer of CO2; therefore, it can be used to monitor the CO2 distribution in the treatment pools.


Author(s):  
John Parnell ◽  
Kirsty Macleod ◽  
Malcolm J. Hole

ABSTRACTLower Devonian volcanic rocks in the northern British Isles, especially Scotland, show extensive evidence for contemporaneous subaerial weathering. Basalt and andesite lavas were altered to red iron oxides, commonly accompanied by calcite. Measurement of carbonate contents in 104 samples over a region of 100,000 km2 show an average of 13% calcite. Weighted for outcrop thickness, this represents an estimated 7.3×1016 moles CO2, extracted from surface waters and ultimately the atmosphere. The time frame for this drawdown is difficult to constrain, but complete weathering of a one-metre unit over 1000 years would involve CO2 consumption comparable with the highest rates determined in modern basaltic watersheds. These data demonstrate that volcanic activity can be a major sink, as well as a source for CO2, and provide a data set for modelling of CO2 flux during episodes of volcanic activity in the geological record. The high capacity of the Devonian lavas for CO2 drawdown emphasises the potential of basalts for CO2 sequestration.


2019 ◽  
Vol 52 ◽  
pp. 1-8 ◽  
Author(s):  
Mariarosaria Falanga ◽  
Enza De Lauro ◽  
Simona Petrosino ◽  
Salvatore De Martino

Abstract. We study oscillations recorded at Stromboli and Campi Flegrei by different sensors: seismometers, strainmeters and tiltmeters. We examine both the high-frequency (>0.5 Hz) portion of the spectrum and very long period signals up to tidal scales. In this context, seismicity and deformation are investigated on different time scales (from minutes to days/years) in order to identify the basic elements of their interaction, whose understanding should provide new insights on the predictive models. In this work, the strict relation of tides and volcanic processes is shown. At Stromboli, indeed the transition from the stationary phase to the non-stationary phase seems to have a tidal precursor that is related to the duration of the crisis. The subsequent volcanic activity is interpreted as the response of the volcano to restore the equilibrium condition. The moveout from equilibrium produces, first, variations in the standard statistics of explosions, then leads to effusive stage and to a pressure drop in the shallow feeding system. That process induces the nucleation of a gas bubble and the excitation of low frequencies. Campi Flegrei seismicity shows a correlation between the diurnal solar solid tide and the energy released by the long period signals, indicating that the whole mechanism is modulated on a tidal scale. In other words, in the case of Stromboli, a departure from the equilibrium state is marked by solid tide variations in a certain frequency band. On the other hand, at Campi Flegrei diurnal to annual solid tides modulate an increase of volcanic activity.


2015 ◽  
Vol 304 ◽  
pp. 294-303 ◽  
Author(s):  
Giovanni Chiodini ◽  
Carlo Cardellini ◽  
María Clara Lamberti ◽  
Mariano Agusto ◽  
Alberto Caselli ◽  
...  

2001 ◽  
Vol 28 (22) ◽  
pp. 4275-4278 ◽  
Author(s):  
José M. L. Salazar ◽  
Pedro A. Hernández ◽  
Nemesio M. Pérez ◽  
Gladys Melián ◽  
Julio Álvarez ◽  
...  

Eos ◽  
2020 ◽  
Vol 101 ◽  
Author(s):  
Kate Wheeling

Researchers find that a pulse of volcanic activity spanning several hundred years released as much carbon dioxide into the atmosphere as anthropogenic emissions projections for the 21st century.


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