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Overview of Geothermal Resource Utilization and Potential in East African Rift System

机译:东非裂口系统地热资源利用与潜力概述

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The Great East African Rift System (EARS) is one of themajor tectonic structures of the earth that extends for about 6500 km from the Middle East (Dead Sea-Jordan Valley) in the North to Mozambique in the south. This system consists of three main arms: the Red Sea Rift; the Gulf of Aden Rift; and the East African Rift which develops through Eritrea, Ethiopia, Kenya, Tanzania, Zambia, Malawi and northern Mozambique floored by a thinned continental crust. The EARS is composed of two rift trends; the eastern and western branches. The western branch develops from Uganda throughout Lake Tanganyika, where it joins the Eastern branch, following the border between Rwanda and Zaire. The western branch is, however, much less active in terms of volcanism although both branches are seismically and tectonically active today. The East African Rift is one of the most important zones of the world where the heat energy of the interior of the Earth escapes to the surface in the form of volcanic eruptions, earthquakes and the upward transport of heat by hot springs and natural vapor emanations (fumaroles). As a consequence, the EARS appears to possess a remarkable geothermal potential. The eastern branch, that forms the Ethiopian and Kenyan rifts, possesses, by far, the most extensive geothermal resource base in Africa and one of the most extensive in the world. Countries such as Djibouti, Uganda, Eritrea and other countries in southeastern Africa have lesser but still important resource bases. Using today's technologies, Eastern Africa has the potential to generate about 2,500-6,500 MW of energy from geothermal power. East African Countries using, or having carried out research on, geothermal resources include: Djibouti, Eritrea, Ethiopia, Kenya, Tanzania, Uganda, and Zambia. Among these, Kenya is the leading country in using geothermal energy for electricity production followed by Ethiopia. Kenya is generating a total of about 130 MWe of electricity using geothermal energy resources. In Ethiopia, a geothermal pilot power plant with a total installed capacity of 7.2 MWe was built but is not operating due to technical problems. Countries such as Djibouti, Eritrea, Tanzania and Uganda are at exploration stage. Other countries such as Rwanda, Malawi and the Malagasy Republic have, to date, not gone beyond the resource potential inventory work.
机译:伟大的东非裂谷系统(耳朵)是地球的构造构造之一,距离北部的中东(死海 - 乔丹谷)延伸约6500公里,南部莫桑比克。该系统由三个主要武器组成:红海裂缝; aden裂谷的海湾;通过厄立特里亚,埃塞俄比亚,肯尼亚,坦桑尼亚,赞比亚,马拉维和莫桑比克北部的东非裂缝,由薄薄的大陆地壳铺板。耳朵由两个裂缝趋势组成;东部和西部分支机构。西部分公司从乌干达湖都在唐安尼卡湖,在卢旺达和扎伊尔之间的边界之后加入东部分公司。然而,西部分公司就火山而言,虽然两个分支机构今天都在地震和根本上活跃起来。东非裂谷是世界上最重要的地区之一,地球内部的热能以火山喷发,地震的形式逃到表面,热弹簧和天然蒸气散发( Fumaroles)。因此,耳朵似乎具有显着的地热潜力。到目前为止,建立埃塞俄比亚和肯尼亚裂谷的东部分公司,拥有非洲最广泛的地热资源基地,也是世界上最广泛的地热资源基础。 Djibouti,乌干达,厄立特里亚等国家等国家都有较小但仍然重要的资源基础。利用当今的技术,东部非洲有可能从地热力产生约2,500-6,500兆瓦的能量。东非国家使用或进行了研究,地热资源包括:吉布提,厄立特里亚,埃塞俄比亚,肯尼亚,坦桑尼亚,乌干达和赞比亚。其中,肯尼亚是利用地热能源用于电力生产之后的领先国家。肯尼亚使用地热能资源共产生约130米的电力。在埃塞俄比亚,建造了一款具有总装机容量7.2 MWE的地热试验机电厂,但由于技术问题而不是运营。吉布提,厄立特里亚,坦桑尼亚和乌干达等国家都在探索阶段。迄今为止,卢旺达,马拉维和马拉维共和国等国家没有超越资源潜在库存工作。

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