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Assessment of submarine geothermal resources and development of tools to quantify their energy potentials for environmentally sustainable development

机译:评估海底地热资源和开发量化其能量潜力以实现环境可持续发展的工具

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Submarine geothermal reservoirs contain huge amounts of energy, not been used so far but recently considered for exploitation. Their energy potentials are much larger than those of onshore geothermal resources and can cover significant parts of the global future energy demands in an environmentally sustainable way. There are two types: (ⅰ) deep resources along oceanic spreading centers, where uprising magma heats fluids circulating through fissured rocks, which emerge at vents at temperatures up to 460 ℃, mixing with seawater (depth: 1000-4000 m below sea level), and (ⅱ) coastal shallow resources where geothermal fluids emerge at fractures (depth: 1 -50 m). The total length of deep systems is ~65,000 km and there are sites where pressure and temperature are high enough that they are at supercritical conditions. The first part of this paper assesses global information on submarine geothermal resources, concluding that - using mature technology from onshore geothermal and offshore hydrocarbon exploitation - submarine geothermal resources can be an economical affordable option for energy supplies at small-large scale. In the second part a - generally valid - robust, mathematical approach is developed to quantify these resources and its applicability is demonstrated using two examples. In Baja California (Mexico), the coastal submarine geothermal potential per cubic kilometer of rock of Punta Banda, Wagner Depression and Gulf of California resulted 245, 350 and 528 MW_T/km~3, respectively. Transforming only 1 % of this energy into electricity the capacity of the Gulf of California alone is ~26,000 MW_e. The submarine geothermal system of Santorini Caldera (Greece) yielded 869 MW_e (reservoir 100 km~3).
机译:海底地热库蕴藏着巨大的能量,目前尚未使用,但最近被考虑用于开采。它们的能源潜力远大于陆上地热资源,并且可以以环境可持续的方式满足全球未来能源需求的重要部分。有两种类型:(ⅰ)沿海洋扩散中心的深层资源,起义岩浆加热通过裂隙岩石循环的流体,这些流体在温度高达460℃的通风口处出现,并与海水混合(深度:低于海平面1000-4000 m)以及(ⅱ)裂缝中出现地热流体的沿海浅层资源(深度:1 -50 m)。深层系统的总长度约为6.5万公里,有些地方的压力和温度都很高,以至于它们处于超临界状态。本文的第一部分评估了有关海底地热资源的全球信息,得出的结论是,利用陆上地热和近海油气开采的成熟技术,海底地热资源可以成为小规模能源供应的经济实惠选择。在第二部分中,开发了一种(通常有效的)健壮的数学方法来量化这些资源,并使用两个示例演示了其适用性。在墨西哥下加利福尼亚州,蓬塔班达,瓦格纳凹陷和加利福尼亚湾每立方公里岩石的沿海海底地热潜力分别为245、350和528 MW_T / km〜3。仅将这种能源的1%转换为电能,仅加利福尼亚湾的容量就约为2.6万兆瓦。圣托里尼火山口(希腊)的海底地热系统产生869 MW_e(储层100 km〜3)。

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