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  5. Non-volcanic CO2 Earth degassing: Case of Mefite d'Ansanto (southern Apennines), Italy
 
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Non-volcanic CO2 Earth degassing: Case of Mefite d'Ansanto (southern Apennines), Italy

Author(s)
Chiodini, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Granieri, D.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Avino, R.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Caliro, S.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Costa, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Minopoli, C.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Vilardo, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Language
English
Obiettivo Specifico
4.5. Studi sul degassamento naturale e sui gas petroliferi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Geophysical Research Letters  
Issue/vol(year)
/37(2010)
Publisher
American Geophysical Union
Pages (printed)
L11303
Date Issued
2010
DOI
10.1029/2010GL042858
URI
https://www.earth-prints.org/handle/2122/6050
Subjects
05. General::05.01. Computational geophysics::05.01.01. Data processing  
Subjects

Non-volcanic CO2

Mefite d'Ansanto

TWODEE-2

Abstract
Mefite d’Ansanto, southern Apennines, Italy is the largest natural emission of low temperature CO2 rich gases, from non‐volcanic environment, ever measured in
the Earth. The emission is fed by a buried reservoir, made up of permeable limestones and covered by clayey sediments.
We estimated a total gas flux of about 2000 tons per day. Under low wind conditions, the gas flows along a narrow natural channel producing a persistent gas river which has killed over a period of time people and animals. The application of a physical numerical model allowed us to define the
zones which potentially can be affected by dangerous CO2 concentration at breathing height for humans. The geometry of the Mefite gas reservoir is similar to those designed for sequestering CO2 in geological storage projects where huge amounts of CO2 should be injected in order to reduce
atmospheric CO2 concentration. The approach which we have used at Mefite to define hazardous zones for the human health can be applied also in case of large CO2 leakages from storage sites, a phenomena which, even if improbable, can not be ruled out.
Sponsors
This work was partially supported by the Research Project MIUR/PRIN2008 prot. 2008S89Y8R
References
Caliro, S., G. Chiodini, R. Moretti, R. Avino, D. Granieri, M. Russo, and
J. Fiebig (2007), The origin of the fumaroles of La Solfatara (Campi
Flegrei, south Italy), Geochim. Cosmochim. Acta, 71, 3040–3055,
doi:10.1016/j.gca.2007.04.007.
Chiodini, G., F. Frondini, and F. Ponziani (1995), Deep structures and
carbon dioxide degassing in central Italy, Geothermics, 24, 81–94.
Chiodini, G., C. Cardellini, A. Amato, E. Boschi, S. Caliro, F. Frondini,
and G. Ventura (2004), Carbon dioxide Earth degassing and seismogenesis
in central and southern Italy, Geophys. Res. Lett., 31, L07615,
doi:10.1029/2004GL019480.
Chiodini, G., M. Valenza, C. Cardellini, and A. Frigeri (2008), A New
Web‐Based Catalog of Earth Degassing Sites in Italy, Eos Trans.
AGU, 89(37), 341–342.
Cinque, A., E. Patacca, P. Scandone, and M. Tozzi (1993), Quaternary
kinematic evolution of the southern Apennines: Relationships between
surface geological features and deep lithospheric structures, Ann. Geofis.,
36(2), 249–260.
Costa, A., G. Chiodini, D. Granieri, A. Folch, R. Hankin, S. Caliro, R. Avino,
and C. Cardellini (2008), A shallow layer model for heavy gas dispersion
from natural sources: Application and hazard assessment at Caldara di
Manziana, Italy, Geochem. Geophys. Geosyst., 9, Q03002, doi:10.1029/
2007GC001762.
Del Pezzo, E., G. Lannaccone, M. Martini, and R. Scarpa (1983), The
23 November 1980 southern Italy earthquake, Bull. Seismol. Soc. Am., 73,
187–200.
Doglioni, C., S. Merlini, and G. Cantarella (1999), Foredeep geometries at
the front of the Apennines in the Ionian Sea (central Mediterranean),
Earth Planet. Sci. Lett., 168, 243–254.
Douglas, S., and R. Kessler (1990), User’s Manual for the Diagnostic Wind
Model, edited by L. Carr, Rep. 450/4‐90‐007C, Environ. Protect.
Agency, San Rafael, Calif.
Folch, A., A. Costa, and R. K. S. Hankin (2009), TWODEE‐2: A shallow
layer model for dense gas dispersion on complex topography, Comput.
Geosci., 35, 667–674, doi:10.1016/j.cageo.2007.12.017.
Frezzotti, M., L. Peccerillo, A. Panza, and G. May (2009), Carbonate metasomatism
and CO2 lithosphere‐asthenosphere degassing beneath the
western mediterranean: An integrated model arising from petrological
and geophysical data, Chem. Geol., 262(1–2), 108–120.
Gambino, N. (1991), La Mefite nella Valle d’Ansanto di Vincenzo
Maria Santoli, dopo duecento anni 1783‐1982, 424 pp., Tipografica
GraficAmodeo, Avellino, Italy.
Hankin, R., and R. Britter (1999a), TWODEE: The Health and Safety
Laboratory’s shallow layer model for heavy gas dispersion. Part 1.
Mathematical basis and physical assumptions, J. Hazard. Mater. A, 66,
211–226.
Hankin, R., and R. Britter (1999b), TWODEE: The Health and Safety
Laboratory’s shallow layer model for heavy gas dispersion. Part 2. Outline
and validation of the computational scheme, J. Hazard. Mater. A,
66, 227–237.
Hippolyte, C., J. Angelier, and F. Roure (1994), A major geodynamic
change revealed by quaternary stress pattern in the southern Apennines
(Italy), Tectonophysics, 230, 199–210.
Italiano, F., M. Martelli, G. Martinelli, and P. M. Nuccio (2000), Geochemical
evidence of melt intrusions along lithospheric faults of the southern
Apennines, Italy: Geodynamic and seismogenic implications, J. Geophys.
Res., 105, 13,569–13,578.
Kerrick, D. M. (2001), Present and past nonanthropogenic CO2 degassing
from the solid Earth, Rev. Geophys., 39, 565–585.
Mörner, N. A., and G. Etiope (2002), Carbon degassing from the lithosphere,
Global Planet. Change, 33, 185–203.
Mostardini, F., and S. Merlini (1986), Appennino centro‐meridionale.
Sezioni geologiche e proposta di modello strutturale, Mem. Soc. Geol.
Ital., 35, 177–202.
National Institute of Occupational Safety and Health (NIOSH) (1997),
Pocket guide to chemical hazard, Rep. 97‐140, Washington, D. C.
Pruess, K. (2008), On CO2 fluid flow and heat transfer behavior in the subsurface,
following leakage from a geologic storage reservoir, Environ.
Geol., 54, 1677–1686.
Sinno, R. (1969), I minerali della valle di Ansanto, Atti Accad. Sci. Fis.
Matem., 7, 219–258.
World Health Organization (WHO) (1981), Hydrogen sulphide: Environmental
health criteria, Rep. 19, Geneva.
Description
Mefite d’Ansanto, southern Apennines, Italy is the largest natural emission of low temperature CO2 rich gases, from non‐volcanic environment, ever measured in
the Earth.
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