华北赋煤区地热资源富集模式及开发利用方向

Heat accumulation model and utilization direction of geothermal resources in coalbearing areas of North China

  • 摘要: 【目的】 中国是煤炭大国,在煤炭行业迫切需要转型的形势下,研究赋煤区的地热资源成因与分布规律十分必要。华北赋煤区地热资源储量占全国的74.7%,是中国地热资源最富集的区域之一。区内分布有渤海湾盆地、鄂尔多斯盆地、沁水盆地和南华北盆地等主要含煤盆地,其岩石圈热状态自东向西逐步降低。地热储包括新生界砂岩孔隙型和寒武-奥陶系碳酸盐岩岩溶-裂隙型两大类型。碳酸盐岩岩溶-裂隙热储温度高、水量大、易于回灌,是煤田区地热勘查与开发利用的优先选择。【方法】 针对煤田区地热地质的特点,开展地热系统动力学分析,优选华北赋煤区的地热勘查与开发区域。【结果和结论】 提出煤田区有以下4种聚热模式:(1)煤层与碳酸盐岩地层储盖组合传导聚热;(2)基岩面起伏变化传导聚热;(3)断裂带地下水活动对流聚热;(4)碳酸盐岩基岩面风化壳岩溶以及侵入体接触面岩溶对流聚热。并结合实例进行数值模拟分析。在此基础上,指出华北赋煤区地热勘查与开发优先方向是深部碳酸盐岩储层中的地热资源。地热能作为非碳基能源之一,以其储量大、清洁、输出连续的特点,在未来社会对电力、燃料和热力三大能源需求中的热力供应方面尤其可以做出重要贡献,而中国地热与煤炭资源在空间分布上的重叠,使地热开发利用成为煤炭行业转型的有效途径之一。

     

    Abstract: Objective China is a coal-rich country. In the urgent need for energy transition of the coal industry, it is necessary to study the genesis and occurrence of geothermal resources in the coal-bearing areas. The geothermal reserves in the North China coal-bearing areas account for 74.7% of the whole country, which is of the region with the most abundant geothermal resources in China. There are major coal-bearing basins in North China, including: Bohai Bay Basin, Ordos Basin, Qinshui Basin and South North China Basin, etc. The thermal strength gradually decreases from east to west. There are two types of geothermal reservoirs, i.e. Cenozoic sandstone pore type and Cambrian-Ordovician carbonate karst-fractured type. The carbonate karst-fractured geothermal reservoir has higher temperature, larger water yield and is easy to reinject, which will be the priority exploration targets of geothermal resources development in coal-bearing areas. Methods Taking the coal-bearing area in North China as an example, an analysis of the dynamics of the geothermal systems in the region is carried out to address the special geological conditions of the coal-bearing areas. Results and Conclusions Several heat accumulation models are proposed for the coal-bearing area: (1) The combination of coal seams and carbonate rock reservoirs with a conductive heat accumulation mechanism. (2) The later variation of the bedrock elevation with a conductive heat accumulation mechanism. (3) Groundwater circulation in the fault zones with a convective heat accumulation mechanism. (4) Groundwater circulation in the weathered karst zones in the uplifted carbonate bedrock surface with a conductive and convective "dualtrack" heat accumulation mechanism. Numerical models are built for a few case examples to verify these mechanisms. On this basis, it is pointed out that the priority for future exploration and development of the geothermal resources in the deep carbonate reservoir with a sandstone or a loose sediment cover. Geothermal energy is a non-carbon-based energy source that is expected to make significant contributions to the heat supply among the electricity, fuel, and heat demand due to its advantages such as large in quantity, clean, stable and continuous in supply. The overlap in the spatial distribution of geothermal and coal resources in North China makes geothermal development and utilization an effective way for the transition of the coal energy industry into a cleaner one and the realization of carbon neutrality.

     

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