Heat Flow Correction for the High-Permeability Formation: A Case Study for Xiong'an New Area
文献类型：期刊论文
| 作者 | Wang, Zhuting1; Gao, Peng3; Jiang, Guangzheng2; Wang, Yibo2; Hu, Shengbiao2 |
| 刊名 | LITHOSPHERE
 |
| 出版日期 | 2021 |
| 卷号 | 2021期号:1页码:15 |
| ISSN号 | 1941-8264 |
| DOI | 10.2113/2021/9171191 |
| 英文摘要 | The Xiong'an New Area is located at the western Bohai Bay Basin, 150 km south of Beijing, China. The area has tremendous high heat flow value within the sedimentary layer, and the average value can reach 90 mWmiddotm-2 within the Niutuozhen Uplift. However, combining the basal heat flow at the top of the metamorphic layer with the heat flow value which was contributed by the radiogenic heat production from the overlying formation, the surface heat flow value was only 65.1 mW.m(-2) in this area. Thus, the heat flow value within the sedimentary layer was greatly influenced by other factors. In this study, based on the continuous temperature measurements data from 4 boreholes, thermos-physical parameters (conductivity, radioactive heat production, density, and heat capacity) from 90 rock sample measurements, and the regional stratigraphic development, a two-dimensional thermal-hydraulic modelling was carried out to study the influence of the heat refraction and groundwater convection on the heat flow value. According to calculation results, the heat flow disturbance caused by heat refraction was 10 mW.m(-2), and the disturbance value was 20 mW.m(-2) for the groundwater convection. Furthermore, when the high-permeability layer thickness was a certain value, with the increasing high-permeability layer buried depth, the influence of the groundwater convection on the temperature field which was used for the heat flow calculation became weak. While when the high-permeability layer buried depth was set up, the influence of the groundwater convection on the above temperature field became stronger with the increasing high-permeability layer thickness. |
| WOS关键词 | BOHAI BAY BASIN ; THERMAL-CONDUCTIVITY ; CHINA ; LITHOSPHERE ; GENERATION ; EVOLUTION ; REGIME ; ROCKS |
| 资助项目 | Fundamental Research Funds for the Central Universities[2021-11032] ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine[2021210075] ; National Key R&D Program of China[2018YFC0604302] ; Key R&D Program of Shandong Province[2019GSF109053] |
| WOS研究方向 | Geochemistry & Geophysics ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000718195900002 |
| 出版者 | GEOSCIENCEWORLD |
| 资助机构 | Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; National Key R&D Program of China ; National Key R&D Program of China ; Key R&D Program of Shandong Province ; Key R&D Program of Shandong Province ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; National Key R&D Program of China ; National Key R&D Program of China ; Key R&D Program of Shandong Province ; Key R&D Program of Shandong Province ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; National Key R&D Program of China ; National Key R&D Program of China ; Key R&D Program of Shandong Province ; Key R&D Program of Shandong Province ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; Research on Heat Disaster and Utilization Technology of Geothermal Resources in Deep Mine ; National Key R&D Program of China ; National Key R&D Program of China ; Key R&D Program of Shandong Province ; Key R&D Program of Shandong Province |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/103852]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 通讯作者 | Gao, Peng |
| 作者单位 | 1.China Univ Min & Technol, Sch Mines, Xuzhou 221116, Jiangsu, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.China Geol Survey, Oil & Gas Survey, Beijing 100083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Zhuting,Gao, Peng,Jiang, Guangzheng,et al. Heat Flow Correction for the High-Permeability Formation: A Case Study for Xiong'an New Area[J]. LITHOSPHERE,2021,2021(1):15. |
| APA | Wang, Zhuting,Gao, Peng,Jiang, Guangzheng,Wang, Yibo,&Hu, Shengbiao.(2021).Heat Flow Correction for the High-Permeability Formation: A Case Study for Xiong'an New Area.LITHOSPHERE,2021(1),15. |
| MLA | Wang, Zhuting,et al."Heat Flow Correction for the High-Permeability Formation: A Case Study for Xiong'an New Area".LITHOSPHERE 2021.1(2021):15. |
入库方式： OAI收割
来源：地质与地球物理研究所
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