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首页> 外文期刊>Geothermics >Shallow geothermal energy system in fractured basalt: A case study from Kollafjørður, Faroe Islands, NE-Atlantic Ocean
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Shallow geothermal energy system in fractured basalt: A case study from Kollafjørður, Faroe Islands, NE-Atlantic Ocean

机译:玄武岩断裂中的浅层地热能系统:以北大西洋东北部法罗群岛的科拉夫约拉德尔为例

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摘要

A shallow (approximate to 200 m) geothermal energy system is examined in the Faroe Islands, a 60-million-year-old volcanic archipelago in the Northeast Atlantic. The geothermal water has a heating capacity of approximately 150 individual households and consists of meteoric water approximately 3 years old. Water temperatures as high as 27 degrees C in artesian wells are explained by a topography-driven vertical convection. The water flows into the boreholes from the north-northwest through fractures and flow tops and bases in the basalt exposed in surrounding high terrains. Of six influx zones, three are water carrying fractures that strike N-S and dip E.
机译:在法罗群岛上研究了一个浅层(约200 m)的地热能系统,该法罗群岛位于东北大西洋,具有6000万年的历史。地热水的供热能力约为150个家庭,由大约3年的流水组成。地形驱动的垂直对流解释了自流井中水温高达27摄氏度。水通过裂缝从西北向西北流入钻孔,并流向周围高地的玄武岩中的顶部和底部。在六个涌水区中,三个是带水裂缝,撞击南北向和北倾E。

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