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Soil diffuse degassing and thermal energy fluxes from the southern Lakki plain, Nisyros (Greece)

Identifieur interne : 000228 ( Main/Merge ); précédent : 000227; suivant : 000229

Soil diffuse degassing and thermal energy fluxes from the southern Lakki plain, Nisyros (Greece)

Auteurs : Tatjana Brombach [Suisse] ; Johannes C. Hunziker [Suisse] ; Giovanni Chiodini [Italie] ; Carlo Cardellini [Italie] ; Luigi Marini [Italie]

Source :

RBID : Pascal:01-0176542

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English descriptors

Abstract

Two diffuse soil CO2 flux surveys from the southern Lakki plain show that CO2 is mainly released from the hydrothermal explosion craters. The correspondence between high CO2 fluxes and elevated soil temperatures suggests that a flux of hot hydrothermal fluids ascends towards the surface. Steam mostly condenses near the surface and the heat given off is conductively transferred to the atmosphere through the soil, accompanied by a large CO2 flux. It was calculated, that 68 t d-1 of hydrothermal CO2 are released through the total surveyed area of ∼1.3 km2. Admitting that a steam flux of 2200 t d-1 accompanies this CO2 flux, the thermal energy released through steam condensation amounts to 58 MW.

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Pascal:01-0176542

Le document en format XML

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<name sortKey="Brombach, Tatjana" sort="Brombach, Tatjana" uniqKey="Brombach T" first="Tatjana" last="Brombach">Tatjana Brombach</name>
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<country>Suisse</country>
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<title xml:lang="en" level="a">Soil diffuse degassing and thermal energy fluxes from the southern Lakki plain, Nisyros (Greece)</title>
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<name sortKey="Brombach, Tatjana" sort="Brombach, Tatjana" uniqKey="Brombach T" first="Tatjana" last="Brombach">Tatjana Brombach</name>
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<s1>Institut de Minéralogie et Pétrographie, Université de Lausanne</s1>
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<country>Suisse</country>
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<orgName type="university">Université de Lausanne</orgName>
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<name sortKey="Hunziker, Johannes C" sort="Hunziker, Johannes C" uniqKey="Hunziker J" first="Johannes C." last="Hunziker">Johannes C. Hunziker</name>
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<s1>Institut de Minéralogie et Pétrographie, Université de Lausanne</s1>
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<country>Suisse</country>
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<region nuts="3" type="region">Canton de Vaud</region>
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<orgName type="university">Université de Lausanne</orgName>
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<name sortKey="Chiodini, Giovanni" sort="Chiodini, Giovanni" uniqKey="Chiodini G" first="Giovanni" last="Chiodini">Giovanni Chiodini</name>
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<name sortKey="Cardellini, Carlo" sort="Cardellini, Carlo" uniqKey="Cardellini C" first="Carlo" last="Cardellini">Carlo Cardellini</name>
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<s2>Napoli</s2>
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<country>Italie</country>
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<name sortKey="Marini, Luigi" sort="Marini, Luigi" uniqKey="Marini L" first="Luigi" last="Marini">Luigi Marini</name>
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<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Greek Aegean Islands</term>
<term>carbon dioxide</term>
<term>condensation</term>
<term>craters</term>
<term>degassing</term>
<term>diffusion</term>
<term>explosions</term>
<term>fluid phase</term>
<term>flux</term>
<term>geothermal energy</term>
<term>hydrothermal activity</term>
<term>soil gases</term>
<term>temperature</term>
<term>water vapor</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Dégazage</term>
<term>Diffusion</term>
<term>Gaz sol</term>
<term>Energie géothermique</term>
<term>Flux</term>
<term>Dioxyde carbone</term>
<term>Cratère</term>
<term>Explosion</term>
<term>Activité hydrothermale</term>
<term>Température</term>
<term>Phase fluide</term>
<term>Vapeur eau</term>
<term>Condensation</term>
<term>Iles Egée Grèce</term>
<term>Ile Nisyros</term>
<term>Plaine Lakki</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr">
<term>Condensation</term>
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<front>
<div type="abstract" xml:lang="en">Two diffuse soil CO
<sub>2</sub>
flux surveys from the southern Lakki plain show that CO
<sub>2</sub>
is mainly released from the hydrothermal explosion craters. The correspondence between high CO
<sub>2</sub>
fluxes and elevated soil temperatures suggests that a flux of hot hydrothermal fluids ascends towards the surface. Steam mostly condenses near the surface and the heat given off is conductively transferred to the atmosphere through the soil, accompanied by a large CO
<sub>2</sub>
flux. It was calculated, that 68 t d
<sup>-1</sup>
of hydrothermal CO
<sub>2</sub>
are released through the total surveyed area of ∼1.3 km
<sup>2</sup>
. Admitting that a steam flux of 2200 t d
<sup>-1</sup>
accompanies this CO
<sub>2</sub>
flux, the thermal energy released through steam condensation amounts to 58 MW.</div>
</front>
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<li>Suisse</li>
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<name sortKey="Brombach, Tatjana" sort="Brombach, Tatjana" uniqKey="Brombach T" first="Tatjana" last="Brombach">Tatjana Brombach</name>
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<name sortKey="Hunziker, Johannes C" sort="Hunziker, Johannes C" uniqKey="Hunziker J" first="Johannes C." last="Hunziker">Johannes C. Hunziker</name>
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<name sortKey="Chiodini, Giovanni" sort="Chiodini, Giovanni" uniqKey="Chiodini G" first="Giovanni" last="Chiodini">Giovanni Chiodini</name>
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<name sortKey="Cardellini, Carlo" sort="Cardellini, Carlo" uniqKey="Cardellini C" first="Carlo" last="Cardellini">Carlo Cardellini</name>
<name sortKey="Marini, Luigi" sort="Marini, Luigi" uniqKey="Marini L" first="Luigi" last="Marini">Luigi Marini</name>
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