Eintrag weiter verarbeiten
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy
Gespeichert in:
| Zeitschriftentitel: | Journal of Geophysical Research: Solid Earth |
|---|---|
| Personen und Körperschaften: | , , , , , , , |
| In: | Journal of Geophysical Research: Solid Earth, 112, 2007, B12 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
American Geophysical Union (AGU)
|
| Schlagwörter: |
| author_facet |
Chiodini, G. Baldini, A. Barberi, F. Carapezza, M. L. Cardellini, C. Frondini, F. Granieri, D. Ranaldi, M. Chiodini, G. Baldini, A. Barberi, F. Carapezza, M. L. Cardellini, C. Frondini, F. Granieri, D. Ranaldi, M. |
|---|---|
| author |
Chiodini, G. Baldini, A. Barberi, F. Carapezza, M. L. Cardellini, C. Frondini, F. Granieri, D. Ranaldi, M. |
| spellingShingle |
Chiodini, G. Baldini, A. Barberi, F. Carapezza, M. L. Cardellini, C. Frondini, F. Granieri, D. Ranaldi, M. Journal of Geophysical Research: Solid Earth Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics |
| author_sort |
chiodini, g. |
| spelling |
Chiodini, G. Baldini, A. Barberi, F. Carapezza, M. L. Cardellini, C. Frondini, F. Granieri, D. Ranaldi, M. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/2006jb004896 <jats:p>In order to test the potentiality of soil CO<jats:sub>2</jats:sub> diffuse degassing measurements for the study of underground mass and heat transfer in geothermal systems detailed surveys were performed at Latera caldera, which is an excellent test site, because of the abundant available subsurface data. Over 2500 measurements of soil CO<jats:sub>2</jats:sub> flux revealed that endogenous CO<jats:sub>2</jats:sub> at Latera caldera concentrates on a NE‐SW band coinciding with a structural high of fractured Mesozoic limestones hosting a water‐dominated high‐enthalpy geothermal reservoir. The total hydrothermal CO<jats:sub>2</jats:sub> degassing from the structural high has been evaluated at 350 t d<jats:sup>−1</jats:sup> from an area of 3.1 km<jats:sup>2</jats:sup>. It has been estimated that such a CO<jats:sub>2</jats:sub> release would imply a geothermal liquid flux of 263 kg s<jats:sup>−1</jats:sup>, with a heat release of 239 MW. The chemical and isotopic composition of the gas indicates a provenance from the geothermal reservoir and that CO<jats:sub>2</jats:sub> is partly originated by thermal metamorphic decarbonation in the hottest deepest parts of the system and partly has a likely mantle origin. The ratios of CO<jats:sub>2</jats:sub>, H<jats:sub>2</jats:sub>, CH<jats:sub>4</jats:sub>, and CO to Ar were used to estimate the T‐P conditions of the reservoir. Results cluster at T ∼ 200–300°C and P<jats:sub>CO2</jats:sub> ∼ 100–200 bars, close to the actual well measurements. Finally, the approach proved to be an excellent tool to investigate the presence of an active geothermal reservoir at depth and that the H<jats:sub>2</jats:sub>‐CO<jats:sub>2</jats:sub>‐CH<jats:sub>4</jats:sub>‐CO‐Ar gas composition is a useful T‐P geochemical indicator for such CO<jats:sub>2</jats:sub> rich geothermal systems.</jats:p> Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy Journal of Geophysical Research: Solid Earth |
| doi_str_mv |
10.1029/2006jb004896 |
| facet_avail |
Online Free |
| finc_class_facet |
Geographie Chemie und Pharmazie Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft Biologie Allgemeine Naturwissenschaft Physik Technik Geologie und Paläontologie |
| format |
ElectronicArticle |
| fullrecord |
blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDA2amIwMDQ4OTY |
| id |
ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDA2amIwMDQ4OTY |
| institution |
DE-Gla1 DE-Zi4 DE-15 DE-Pl11 DE-Rs1 DE-105 DE-14 DE-Ch1 DE-L229 DE-D275 DE-Bn3 DE-Brt1 DE-Zwi2 DE-D161 |
| imprint |
American Geophysical Union (AGU), 2007 |
| imprint_str_mv |
American Geophysical Union (AGU), 2007 |
| issn |
0148-0227 |
| issn_str_mv |
0148-0227 |
| language |
English |
| mega_collection |
American Geophysical Union (AGU) (CrossRef) |
| match_str |
chiodini2007carbondioxidedegassingatlateracalderaitalyevidenceofgeothermalreservoirandevaluationofitspotentialenergy |
| publishDateSort |
2007 |
| publisher |
American Geophysical Union (AGU) |
| recordtype |
ai |
| record_format |
ai |
| series |
Journal of Geophysical Research: Solid Earth |
| source_id |
49 |
| title |
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_unstemmed |
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_full |
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_fullStr |
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_full_unstemmed |
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_short |
Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_sort |
carbon dioxide degassing at latera caldera (italy): evidence of geothermal reservoir and evaluation of its potential energy |
| topic |
Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics |
| url |
http://dx.doi.org/10.1029/2006jb004896 |
| publishDate |
2007 |
| physical |
|
| description |
<jats:p>In order to test the potentiality of soil CO<jats:sub>2</jats:sub> diffuse degassing measurements for the study of underground mass and heat transfer in geothermal systems detailed surveys were performed at Latera caldera, which is an excellent test site, because of the abundant available subsurface data. Over 2500 measurements of soil CO<jats:sub>2</jats:sub> flux revealed that endogenous CO<jats:sub>2</jats:sub> at Latera caldera concentrates on a NE‐SW band coinciding with a structural high of fractured Mesozoic limestones hosting a water‐dominated high‐enthalpy geothermal reservoir. The total hydrothermal CO<jats:sub>2</jats:sub> degassing from the structural high has been evaluated at 350 t d<jats:sup>−1</jats:sup> from an area of 3.1 km<jats:sup>2</jats:sup>. It has been estimated that such a CO<jats:sub>2</jats:sub> release would imply a geothermal liquid flux of 263 kg s<jats:sup>−1</jats:sup>, with a heat release of 239 MW. The chemical and isotopic composition of the gas indicates a provenance from the geothermal reservoir and that CO<jats:sub>2</jats:sub> is partly originated by thermal metamorphic decarbonation in the hottest deepest parts of the system and partly has a likely mantle origin. The ratios of CO<jats:sub>2</jats:sub>, H<jats:sub>2</jats:sub>, CH<jats:sub>4</jats:sub>, and CO to Ar were used to estimate the T‐P conditions of the reservoir. Results cluster at T ∼ 200–300°C and P<jats:sub>CO2</jats:sub> ∼ 100–200 bars, close to the actual well measurements. Finally, the approach proved to be an excellent tool to investigate the presence of an active geothermal reservoir at depth and that the H<jats:sub>2</jats:sub>‐CO<jats:sub>2</jats:sub>‐CH<jats:sub>4</jats:sub>‐CO‐Ar gas composition is a useful T‐P geochemical indicator for such CO<jats:sub>2</jats:sub> rich geothermal systems.</jats:p> |
| container_issue |
B12 |
| container_start_page |
0 |
| container_title |
Journal of Geophysical Research: Solid Earth |
| container_volume |
112 |
| format_de105 |
Article, E-Article |
| format_de14 |
Article, E-Article |
| format_de15 |
Article, E-Article |
| format_de520 |
Article, E-Article |
| format_de540 |
Article, E-Article |
| format_dech1 |
Article, E-Article |
| format_ded117 |
Article, E-Article |
| format_degla1 |
E-Article |
| format_del152 |
Buch |
| format_del189 |
Article, E-Article |
| format_dezi4 |
Article |
| format_dezwi2 |
Article, E-Article |
| format_finc |
Article, E-Article |
| format_nrw |
Article, E-Article |
| _version_ |
1792346969262260226 |
| geogr_code |
not assigned |
| last_indexed |
2024-03-01T17:47:26.144Z |
| geogr_code_person |
not assigned |
| openURL |
url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Carbon+dioxide+degassing+at+Latera+caldera+%28Italy%29%3A+Evidence+of+geothermal+reservoir+and+evaluation+of+its+potential+energy&rft.date=2007-12-01&genre=article&issn=0148-0227&volume=112&issue=B12&jtitle=Journal+of+Geophysical+Research%3A+Solid+Earth&atitle=Carbon+dioxide+degassing+at+Latera+caldera+%28Italy%29%3A+Evidence+of+geothermal+reservoir+and+evaluation+of+its+potential+energy&aulast=Ranaldi&aufirst=M.&rft_id=info%3Adoi%2F10.1029%2F2006jb004896&rft.language%5B0%5D=eng |
| SOLR | |
| _version_ | 1792346969262260226 |
| author | Chiodini, G., Baldini, A., Barberi, F., Carapezza, M. L., Cardellini, C., Frondini, F., Granieri, D., Ranaldi, M. |
| author_facet | Chiodini, G., Baldini, A., Barberi, F., Carapezza, M. L., Cardellini, C., Frondini, F., Granieri, D., Ranaldi, M., Chiodini, G., Baldini, A., Barberi, F., Carapezza, M. L., Cardellini, C., Frondini, F., Granieri, D., Ranaldi, M. |
| author_sort | chiodini, g. |
| container_issue | B12 |
| container_start_page | 0 |
| container_title | Journal of Geophysical Research: Solid Earth |
| container_volume | 112 |
| description | <jats:p>In order to test the potentiality of soil CO<jats:sub>2</jats:sub> diffuse degassing measurements for the study of underground mass and heat transfer in geothermal systems detailed surveys were performed at Latera caldera, which is an excellent test site, because of the abundant available subsurface data. Over 2500 measurements of soil CO<jats:sub>2</jats:sub> flux revealed that endogenous CO<jats:sub>2</jats:sub> at Latera caldera concentrates on a NE‐SW band coinciding with a structural high of fractured Mesozoic limestones hosting a water‐dominated high‐enthalpy geothermal reservoir. The total hydrothermal CO<jats:sub>2</jats:sub> degassing from the structural high has been evaluated at 350 t d<jats:sup>−1</jats:sup> from an area of 3.1 km<jats:sup>2</jats:sup>. It has been estimated that such a CO<jats:sub>2</jats:sub> release would imply a geothermal liquid flux of 263 kg s<jats:sup>−1</jats:sup>, with a heat release of 239 MW. The chemical and isotopic composition of the gas indicates a provenance from the geothermal reservoir and that CO<jats:sub>2</jats:sub> is partly originated by thermal metamorphic decarbonation in the hottest deepest parts of the system and partly has a likely mantle origin. The ratios of CO<jats:sub>2</jats:sub>, H<jats:sub>2</jats:sub>, CH<jats:sub>4</jats:sub>, and CO to Ar were used to estimate the T‐P conditions of the reservoir. Results cluster at T ∼ 200–300°C and P<jats:sub>CO2</jats:sub> ∼ 100–200 bars, close to the actual well measurements. Finally, the approach proved to be an excellent tool to investigate the presence of an active geothermal reservoir at depth and that the H<jats:sub>2</jats:sub>‐CO<jats:sub>2</jats:sub>‐CH<jats:sub>4</jats:sub>‐CO‐Ar gas composition is a useful T‐P geochemical indicator for such CO<jats:sub>2</jats:sub> rich geothermal systems.</jats:p> |
| doi_str_mv | 10.1029/2006jb004896 |
| facet_avail | Online, Free |
| finc_class_facet | Geographie, Chemie und Pharmazie, Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft, Biologie, Allgemeine Naturwissenschaft, Physik, Technik, Geologie und Paläontologie |
| format | ElectronicArticle |
| format_de105 | Article, E-Article |
| format_de14 | Article, E-Article |
| format_de15 | Article, E-Article |
| format_de520 | Article, E-Article |
| format_de540 | Article, E-Article |
| format_dech1 | Article, E-Article |
| format_ded117 | Article, E-Article |
| format_degla1 | E-Article |
| format_del152 | Buch |
| format_del189 | Article, E-Article |
| format_dezi4 | Article |
| format_dezwi2 | Article, E-Article |
| format_finc | Article, E-Article |
| format_nrw | Article, E-Article |
| geogr_code | not assigned |
| geogr_code_person | not assigned |
| id | ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDA2amIwMDQ4OTY |
| imprint | American Geophysical Union (AGU), 2007 |
| imprint_str_mv | American Geophysical Union (AGU), 2007 |
| institution | DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161 |
| issn | 0148-0227 |
| issn_str_mv | 0148-0227 |
| language | English |
| last_indexed | 2024-03-01T17:47:26.144Z |
| match_str | chiodini2007carbondioxidedegassingatlateracalderaitalyevidenceofgeothermalreservoirandevaluationofitspotentialenergy |
| mega_collection | American Geophysical Union (AGU) (CrossRef) |
| physical | |
| publishDate | 2007 |
| publishDateSort | 2007 |
| publisher | American Geophysical Union (AGU) |
| record_format | ai |
| recordtype | ai |
| series | Journal of Geophysical Research: Solid Earth |
| source_id | 49 |
| spelling | Chiodini, G. Baldini, A. Barberi, F. Carapezza, M. L. Cardellini, C. Frondini, F. Granieri, D. Ranaldi, M. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/2006jb004896 <jats:p>In order to test the potentiality of soil CO<jats:sub>2</jats:sub> diffuse degassing measurements for the study of underground mass and heat transfer in geothermal systems detailed surveys were performed at Latera caldera, which is an excellent test site, because of the abundant available subsurface data. Over 2500 measurements of soil CO<jats:sub>2</jats:sub> flux revealed that endogenous CO<jats:sub>2</jats:sub> at Latera caldera concentrates on a NE‐SW band coinciding with a structural high of fractured Mesozoic limestones hosting a water‐dominated high‐enthalpy geothermal reservoir. The total hydrothermal CO<jats:sub>2</jats:sub> degassing from the structural high has been evaluated at 350 t d<jats:sup>−1</jats:sup> from an area of 3.1 km<jats:sup>2</jats:sup>. It has been estimated that such a CO<jats:sub>2</jats:sub> release would imply a geothermal liquid flux of 263 kg s<jats:sup>−1</jats:sup>, with a heat release of 239 MW. The chemical and isotopic composition of the gas indicates a provenance from the geothermal reservoir and that CO<jats:sub>2</jats:sub> is partly originated by thermal metamorphic decarbonation in the hottest deepest parts of the system and partly has a likely mantle origin. The ratios of CO<jats:sub>2</jats:sub>, H<jats:sub>2</jats:sub>, CH<jats:sub>4</jats:sub>, and CO to Ar were used to estimate the T‐P conditions of the reservoir. Results cluster at T ∼ 200–300°C and P<jats:sub>CO2</jats:sub> ∼ 100–200 bars, close to the actual well measurements. Finally, the approach proved to be an excellent tool to investigate the presence of an active geothermal reservoir at depth and that the H<jats:sub>2</jats:sub>‐CO<jats:sub>2</jats:sub>‐CH<jats:sub>4</jats:sub>‐CO‐Ar gas composition is a useful T‐P geochemical indicator for such CO<jats:sub>2</jats:sub> rich geothermal systems.</jats:p> Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy Journal of Geophysical Research: Solid Earth |
| spellingShingle | Chiodini, G., Baldini, A., Barberi, F., Carapezza, M. L., Cardellini, C., Frondini, F., Granieri, D., Ranaldi, M., Journal of Geophysical Research: Solid Earth, Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy, Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics |
| title | Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_full | Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_fullStr | Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_full_unstemmed | Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_short | Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| title_sort | carbon dioxide degassing at latera caldera (italy): evidence of geothermal reservoir and evaluation of its potential energy |
| title_unstemmed | Carbon dioxide degassing at Latera caldera (Italy): Evidence of geothermal reservoir and evaluation of its potential energy |
| topic | Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics |
| url | http://dx.doi.org/10.1029/2006jb004896 |