Geothermal resource distribution and prospects for development and utilization in China

IF 4.2 3区 工程技术 Q2 ENERGY & FUELS
Jinchuan Zhang , Lei Chen , Yuhang Sun , Longfei Xu , Xingxu Zhao , Qianchao Li , Dawei Zhang
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Abstract

China is tectonically composed of a series of plates and orogenic belts and has been influenced by the Pacific and Indian plates since the Late Paleozoic, forming a regular distribution of Mesozoic and Cenozoic granites. As an important source of geothermal energy, granite is the five elements of geothermal enrichment:geothermal sources; geothermal reservoirs; heat transmission; heat caprock; and heat preservation and it is possible to classify the types of geothermal resources in China according to their distribution in combination with neotectonic movements. China's geothermal energy can be divided into hydrothermal and hot dry rock types in basins and orogenic belts, respectively. Geothermal resources can be divided into hydrothermal, rock, magma, and hybrid geothermal types according to the heat carrier type. Basin geothermal resources are dominated by hydrothermal types, while geothermal energy in orogenic belts with granite includes both hydrothermal and hot dry rock types. Geothermal resources in China can be divided into 6 distinct geothermal regions and 13 subregions, of which the Southwest and Southeast China regions and the Qaidam-Qilian and Jiaoliao subregions in North China with Mesozoic and Cenozoic granites are the most favorable areas for high-temperature hydrothermal and hot dry rock sources. China has complex geological conditions, diverse types of geothermal resources, and broad prospects for development and utilization. Having performed extensive shallow hydrothermal geothermal development and utilization and completed various power generation tests, China's geothermal development and utilization is in a critical stage of transition from the direct utilization of shallow hydrothermal resources to high-temperature geothermal or hot dry rock power generation in middle and deep layers. Basic theoretical research, key technology breakthroughs, and policy incentives are the main issues that need to be addressed in the geothermal industry.

中国地热资源分布与开发利用前景
中国在构造上由一系列板块和造山带组成,晚古生代以来受太平洋板块和印度板块的影响,形成了中生代和新生代花岗岩的规则分布。作为地热能的重要来源,花岗岩是地热富集的五要素:地热源、地热储层、热传递、热盖层、热保存,根据其分布情况结合新构造运动可以划分出中国地热资源的类型。中国的地热能可分为热液型和干热岩型,分别位于盆地和造山带。地热资源按热载体类型可分为热液型、岩石型、岩浆型和混合型地热资源。盆地地热资源以热液型为主,而花岗岩造山带的地热能则包括热液型和干热岩型。中国的地热资源可分为 6 个不同的地热区和 13 个亚区,其中中生代和新生代花岗岩的西南和东南地区以及华北的柴达木-祁连和蛟龙亚区是高温热液和干热岩源的最有利地区。中国地质条件复杂,地热资源类型多样,开发利用前景广阔。在广泛开展浅层水热地热开发利用并完成各种发电试验后,我国地热开发利用正处于由浅层水热资源直接利用向中深层高温地热或干热岩发电过渡的关键阶段。基础理论研究、关键技术突破和政策激励是地热产业亟待解决的主要问题。
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来源期刊
Natural Gas Industry B
Natural Gas Industry B Earth and Planetary Sciences-Geology
CiteScore
5.80
自引率
6.10%
发文量
46
审稿时长
79 days
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