Shallow geothermal energy system in fractured basalt: A case study from Kollafjørður, Faroe Islands, NE-Atlantic Ocean
• A shallow (≈200 m) geothermal energy system, located in the Faroe Islands in the Northeast Atlantic, is examined. • The likely meteoric water flowing in the wells is approximately 27°C, with the capacity of heating >150 privet houses. • The abnormally high water temperatures in these artesian w...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Eidesgaard, Ó.R. [verfasserIn] |
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E-Artikel |
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Englisch |
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2019 |
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19 |
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Enthalten in: Brain regions that retain the spatial layout of tactile stimuli during working memory – A - Schmidt, Timo Torsten ELSEVIER, 2018, an international journal of geothermal research and its applications, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:82 ; year:2019 ; pages:296-314 ; extent:19 |
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10.1016/j.geothermics.2019.07.005 |
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| 520 | |a • A shallow (≈200 m) geothermal energy system, located in the Faroe Islands in the Northeast Atlantic, is examined. • The likely meteoric water flowing in the wells is approximately 27°C, with the capacity of heating >150 privet houses. • The abnormally high water temperatures in these artesian wells can be explained by a topography-driven vertical convection. • The water flows into the wells from the north-northwest through fractures and flow tops and bases in the basalt. • Of six influx zones, three are water carrying fractures that stike N-S and dip E. | ||
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10.1016/j.geothermics.2019.07.005 doi GBV00000000000780.pica (DE-627)ELV047727632 (ELSEVIER)S0375-6505(18)30361-4 DE-627 ger DE-627 rakwb eng 610 VZ LING DE-30 fid 44.64 bkl 44.90 bkl Eidesgaard, Ó.R. verfasserin aut Shallow geothermal energy system in fractured basalt: A case study from Kollafjørður, Faroe Islands, NE-Atlantic Ocean 2019 19 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • A shallow (≈200 m) geothermal energy system, located in the Faroe Islands in the Northeast Atlantic, is examined. • The likely meteoric water flowing in the wells is approximately 27°C, with the capacity of heating >150 privet houses. • The abnormally high water temperatures in these artesian wells can be explained by a topography-driven vertical convection. • The water flows into the wells from the north-northwest through fractures and flow tops and bases in the basalt. • Of six influx zones, three are water carrying fractures that stike N-S and dip E. Shallow-geothermal energy Elsevier Faroe Islands Elsevier Fractured basalt Elsevier Optical televiewer Elsevier Wireline logs Elsevier Plateau basalt Elsevier Schovsbo, N.H. oth Boldreel, L.O. oth Ólavsdóttir, J. oth Enthalten in Elsevier Science Schmidt, Timo Torsten ELSEVIER Brain regions that retain the spatial layout of tactile stimuli during working memory – A 2018 an international journal of geothermal research and its applications Amsterdam [u.a.] (DE-627)ELV000984256 volume:82 year:2019 pages:296-314 extent:19 https://doi.org/10.1016/j.geothermics.2019.07.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OLC-PHA 44.64 Radiologie VZ 44.90 Neurologie VZ AR 82 2019 296-314 19 |
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Shallow geothermal energy system in fractured basalt: A case study from Kollafjørður, Faroe Islands, NE-Atlantic Ocean |
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• A shallow (≈200 m) geothermal energy system, located in the Faroe Islands in the Northeast Atlantic, is examined. • The likely meteoric water flowing in the wells is approximately 27°C, with the capacity of heating >150 privet houses. • The abnormally high water temperatures in these artesian wells can be explained by a topography-driven vertical convection. • The water flows into the wells from the north-northwest through fractures and flow tops and bases in the basalt. • Of six influx zones, three are water carrying fractures that stike N-S and dip E. |
| abstractGer |
• A shallow (≈200 m) geothermal energy system, located in the Faroe Islands in the Northeast Atlantic, is examined. • The likely meteoric water flowing in the wells is approximately 27°C, with the capacity of heating >150 privet houses. • The abnormally high water temperatures in these artesian wells can be explained by a topography-driven vertical convection. • The water flows into the wells from the north-northwest through fractures and flow tops and bases in the basalt. • Of six influx zones, three are water carrying fractures that stike N-S and dip E. |
| abstract_unstemmed |
• A shallow (≈200 m) geothermal energy system, located in the Faroe Islands in the Northeast Atlantic, is examined. • The likely meteoric water flowing in the wells is approximately 27°C, with the capacity of heating >150 privet houses. • The abnormally high water temperatures in these artesian wells can be explained by a topography-driven vertical convection. • The water flows into the wells from the north-northwest through fractures and flow tops and bases in the basalt. • Of six influx zones, three are water carrying fractures that stike N-S and dip E. |
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| title_short |
Shallow geothermal energy system in fractured basalt: A case study from Kollafjørður, Faroe Islands, NE-Atlantic Ocean |
| url |
https://doi.org/10.1016/j.geothermics.2019.07.005 |
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| author2 |
Schovsbo, N.H. Boldreel, L.O. Ólavsdóttir, J. |
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Schovsbo, N.H. Boldreel, L.O. Ólavsdóttir, J. |
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| doi_str |
10.1016/j.geothermics.2019.07.005 |
| up_date |
2024-07-06T16:56:38.240Z |
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