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Preliminary Assessment of Offshore Geothermal Resource Potential of Portugal - The Case of Azorean Deep-Sea Hydrothermal Vents

机译:葡萄牙海上地热资源潜力的初步评价 - 氮料深海水热通风口的案例

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Hydrothermal vents are submarine hot springs and geysers that originate in volcanically active areas often at mid-ocean ridges, where the planet tectonic plates are spreading apart and magma wells up to or close to the surface of the seafloor. Hydrothermal circulation at the deep ocean ridges is an essential complex process regulating mass and energy transfer from the interior of the Earth through the oceanic lithosphere, to the hydrosphere and the atmosphere. Hydrothermal venting has long been recognised to provide significant fluxes of both heat and chemicals to the deep ocean. Hydrothermal fluids are generally with high heat flows and dissolved minerals, making them an excellent target for exploitation of hydrothermal energy and mineral resources. The energy extraction from the hydrothermal vents could provide a carbon-free and sustainable source of energy for the future generations. A substantial number of hydrothermal fields are located in the vicinity of the Azorean archipelago (Portugal) comprising high-temperature fluids under supercritical conditions. The hydrothermal vents of the Azores are a chain of vents that are fragments of the Mid-Atlantic Ridge. These geological structures, developed from masses of basalt, are of a geomorphological interest, in addition to being a rich ecosystem of diverse subaquatic plant and animal life. Although challenges and barriers exist in exploring mid-ocean ridge hydrothermal vents, these resources remain to be one of the most potential and stable sources of renewable energy. The study at hand presents a preliminary assessment of geothermal resource potential of the Azorean hydrothermal vents using a modified version of the volumetric stored-heat assessment method developed by the United States Geological Society (USGS) (1979) and the energy balance method presented by G.Hiriart (2010). The further part of the study aims at using the obtained data to assess the technological and economic potential of energy extraction from the hydrothermal vents.
机译:水热通风口是潜艇的温泉和闲暇距离往往在中海山脊的火山活跃区域,行星构造板块散布在海底的表面或靠近海底表面的岩石井。深海山脊的水热循环是一种基本复杂的过程调节质量和从地球内部通过海洋岩石圈的能量转移到水圈和气氛。已经认识到水热通风,以为深海提供热量和化学品的显着助水。水热流体通常具有高热流和溶解的矿物质,使其成为利用水热能和矿产资源的优异目标。来自水热通风口的能量提取可以为后代提供无碳和可持续的能源来源。大量的水热场位于氮素群岛(葡萄牙)附近,包括在超临界条件下的高温流体。亚速尔群体的水热通风口是一系列通风口,是大西洋中脊的碎片。除了成为富裕的眶下植物和动物生命的生态系统之外,这些地质结构是一种从玄武岩中发育的。虽然探索中海岭水热通风口中存在挑战和障碍,但这些资源仍然是可再生能源最潜力和稳定的来源之一。手头的研究用来使用由美国地质学会(USGS)(1979)(1979)(1979)(1979)(1979)开发的体积储存 - 热评估方法的改良版本和G的能量平衡方法)初步评估氮料热量通风口的地热资源潜力。 .Hriart(2010)。该研究的其他部分旨在使用所获得的数据来评估来自水热通风口的能量提取的技术和经济潜力。

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