A shallow‐layer model for heavy gas dispersion from natural sources: Application and hazard assessment at Caldara di Manziana, Italy
Identifieur interne : 000128 ( Main/Exploration ); précédent : 000127; suivant : 000129A shallow‐layer model for heavy gas dispersion from natural sources: Application and hazard assessment at Caldara di Manziana, Italy
Auteurs : A. Costa [Italie] ; G. Chiodini [Italie] ; D. Granieri [Italie] ; A. Folch [Italie] ; R. K. S. Hankin [Royaume-Uni] ; S. Caliro [Italie] ; R. Avino [Italie] ; C. Cardellini [Italie]Source :
- Geochemistry, Geophysics, Geosystems [ 1525-2027 ] ; 2008-03.
Descripteurs français
- Wicri :
- topic : Conditions atmosphériques, Géochimie, Géophysique, Simulation.
English descriptors
- KwdEn :
- Atmospheric conditions, Average value, Britter, Caldara, Caliro, Calm ambient, Carbon balance, Carbon dioxide, Cardellini, Central italy, Chiodini, Cloud depth, Complex topography, Computational, Computational domain, Computational geophysics, Computational model, Concentration maps, Continuous releases, Costa, Crater, Crater floor, Dangerous conditions, Degassing, Different time slices, Diffuse emission, Dioxide, Dispersion, Dispersion figure, Dispersion model, Earth degassing, February, Flow behavior, Flow rates, Flux measurements, Folch, Forest canopy, Fossa crater, Friction velocity, Frondini, Further details, Geochemistry, Geochemistry geophysics geosystems, Geophys, Geophysics, Geosystems, Granieri, Hankin, Hazard assessment, Health hazard, High order scheme, Horseshoe lake, Input data, Instantaneous releases, Istituto nazionale, Lake nyos, Layer model, Major hazard risk assessment, Mammoth mountain, Manziana, Mater, Meteorological, Meteorological conditions, Meteorological data, Meteorological station, Model applications, National institute, Natural sources, Nighttime duration, Open path, Order scheme, Plume, Regional aquifers, Rogie, Shallow layer model, Shallow layer simulation, Simulation, Southern italy, Temporal evolution, Terrain elevation, Time evolution, Time span, Transport model, Vadose zone, Volcanic unrest, Volcanol, Water column, Water pool, Water pools, White dots, Wind conditions, Wind direction, Wind speed.
- Teeft :
- Atmospheric conditions, Average value, Britter, Caldara, Caliro, Calm ambient, Carbon balance, Carbon dioxide, Cardellini, Central italy, Chiodini, Cloud depth, Complex topography, Computational, Computational domain, Computational geophysics, Computational model, Concentration maps, Continuous releases, Costa, Crater, Crater floor, Dangerous conditions, Degassing, Different time slices, Diffuse emission, Dioxide, Dispersion, Dispersion figure, Dispersion model, Earth degassing, February, Flow behavior, Flow rates, Flux measurements, Folch, Forest canopy, Fossa crater, Friction velocity, Frondini, Further details, Geochemistry, Geochemistry geophysics geosystems, Geophys, Geophysics, Geosystems, Granieri, Hankin, Hazard assessment, Health hazard, High order scheme, Horseshoe lake, Input data, Instantaneous releases, Istituto nazionale, Lake nyos, Layer model, Major hazard risk assessment, Mammoth mountain, Manziana, Mater, Meteorological, Meteorological conditions, Meteorological data, Meteorological station, Model applications, National institute, Natural sources, Nighttime duration, Open path, Order scheme, Plume, Regional aquifers, Rogie, Shallow layer model, Shallow layer simulation, Simulation, Southern italy, Temporal evolution, Terrain elevation, Time evolution, Time span, Transport model, Vadose zone, Volcanic unrest, Volcanol, Water column, Water pool, Water pools, White dots, Wind conditions, Wind direction, Wind speed.
Abstract
Several nonvolcanic sources in central Italy emit a large amount of carbon dioxide (CO2). Under stable atmospheric conditions and/or in the presence of topographic depressions, the concentration of CO2, which has a molecular mass greater than that of air, can reach high values that are lethal to humans or animals. Several episodes of this phenomenon were recorded in central Italy and elsewhere. In order to validate a model for the dispersion of a heavy gas and to assess the consequent hazard, we applied and tested the code TWODEE‐2, an improved version of the established TWODEE model, which is based on a shallow‐layer approach that uses depth‐averaged variables to describe the flow behavior of dense gas over complex topography. We present results for a vented CO2 release at Caldara di Manziana in central Italy. We find that the model gives reliable results when the input quantity can be properly defined. Moreover, we show that the model can be a useful tool for gas hazard assessment by evaluating where and when lethal concentrations for humans and animals are reached.
Url:
DOI: 10.1029/2007GC001762
Affiliations:
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Le document en format XML
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<term>Carbon dioxide</term>
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<term>Complex topography</term>
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<term>Computational domain</term>
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<term>Dangerous conditions</term>
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<term>Instantaneous releases</term>
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<term>Time span</term>
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<term>Volcanic unrest</term>
<term>Volcanol</term>
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<term>Calm ambient</term>
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<term>Computational domain</term>
<term>Computational geophysics</term>
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<term>Continuous releases</term>
<term>Costa</term>
<term>Crater</term>
<term>Crater floor</term>
<term>Dangerous conditions</term>
<term>Degassing</term>
<term>Different time slices</term>
<term>Diffuse emission</term>
<term>Dioxide</term>
<term>Dispersion</term>
<term>Dispersion figure</term>
<term>Dispersion model</term>
<term>Earth degassing</term>
<term>February</term>
<term>Flow behavior</term>
<term>Flow rates</term>
<term>Flux measurements</term>
<term>Folch</term>
<term>Forest canopy</term>
<term>Fossa crater</term>
<term>Friction velocity</term>
<term>Frondini</term>
<term>Further details</term>
<term>Geochemistry</term>
<term>Geochemistry geophysics geosystems</term>
<term>Geophys</term>
<term>Geophysics</term>
<term>Geosystems</term>
<term>Granieri</term>
<term>Hankin</term>
<term>Hazard assessment</term>
<term>Health hazard</term>
<term>High order scheme</term>
<term>Horseshoe lake</term>
<term>Input data</term>
<term>Instantaneous releases</term>
<term>Istituto nazionale</term>
<term>Lake nyos</term>
<term>Layer model</term>
<term>Major hazard risk assessment</term>
<term>Mammoth mountain</term>
<term>Manziana</term>
<term>Mater</term>
<term>Meteorological</term>
<term>Meteorological conditions</term>
<term>Meteorological data</term>
<term>Meteorological station</term>
<term>Model applications</term>
<term>National institute</term>
<term>Natural sources</term>
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<term>Open path</term>
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<term>Terrain elevation</term>
<term>Time evolution</term>
<term>Time span</term>
<term>Transport model</term>
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<term>Volcanic unrest</term>
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<term>Wind conditions</term>
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<term>Wind speed</term>
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<front><div type="abstract">Several nonvolcanic sources in central Italy emit a large amount of carbon dioxide (CO2). Under stable atmospheric conditions and/or in the presence of topographic depressions, the concentration of CO2, which has a molecular mass greater than that of air, can reach high values that are lethal to humans or animals. Several episodes of this phenomenon were recorded in central Italy and elsewhere. In order to validate a model for the dispersion of a heavy gas and to assess the consequent hazard, we applied and tested the code TWODEE‐2, an improved version of the established TWODEE model, which is based on a shallow‐layer approach that uses depth‐averaged variables to describe the flow behavior of dense gas over complex topography. We present results for a vented CO2 release at Caldara di Manziana in central Italy. We find that the model gives reliable results when the input quantity can be properly defined. Moreover, we show that the model can be a useful tool for gas hazard assessment by evaluating where and when lethal concentrations for humans and animals are reached.</div>
</front>
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<affiliations><list><country><li>Italie</li>
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<name sortKey="Cardellini, C" sort="Cardellini, C" uniqKey="Cardellini C" first="C." last="Cardellini">C. Cardellini</name>
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<name sortKey="Folch, A" sort="Folch, A" uniqKey="Folch A" first="A." last="Folch">A. Folch</name>
<name sortKey="Granieri, D" sort="Granieri, D" uniqKey="Granieri D" first="D." last="Granieri">D. Granieri</name>
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<country name="Royaume-Uni"><noRegion><name sortKey="Hankin, R K S" sort="Hankin, R K S" uniqKey="Hankin R" first="R. K. S." last="Hankin">R. K. S. Hankin</name>
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