A novel flow-resistor network model for characterizing enhanced geothermal system heat reservoir

被引:1
作者
Guo, Jian [1 ,2 ]
Cao, Wenjiong [1 ,2 ]
Wang, Yiwei [1 ,2 ]
Jiang, Fangming [1 ,2 ]
机构
[1] Chinese Acad Sci, Guangzhou Inst Energy Convers, Lab Adv Energy Syst, Key Lab Renewable Energy, Guangzhou 510640, Guangdong, Peoples R China
[2] Chinese Acad Sci, Guangzhou Inst Energy Convers, Guangdong Key Lab New & Renewable Energy Res & De, Guangzhou 510640, Guangdong, Peoples R China
基金
中国国家自然科学基金;
关键词
enhanced geothermal systems; flow-resistor network model; fracture characteristics; heat reservoir; SOULTZ-SOUS-FORETS; HOT DRY ROCK; NUMERICAL-SIMULATION; EGS; FRANCE; EXTRACTION; GRANITE; SITE;
D O I
10.1007/s11708-018-0555-1
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The fracture characteristics of a heat reservoir are of critical importance to enhanced geothermal systems, which can be investigated by theoretical modeling. This paper presents the development of a novel flow-resistor network model to describe the hydraulic processes in heat reservoirs. The fractures in the reservoir are simplified by using flow resistors and the typically complicated fracture network of the heat reservoir is converted into a flow-resistor network with a reasonably simple pattern. For heat reservoirs with various fracture configurations, the corresponding flow-resistor networks are identical in terms of framework though the networks may have different section numbers and the flow resistors may have different values. In this paper, numerous cases of different section numbers and resistor values are calculated and the results indicate that the total number of flow resistances between the injection and production wells is primarily determined by the number of fractures in the reservoir. It is also observed that a linear dependence of the total flow resistance on the number of fractures and the relation is obtained by the best fit of the calculation results. Besides, it performs a case study dealing with the Soultz enhanced geothermal system (EGS). In addition, the fracture numbers underneath specific well systems are derived. The results provide insight on the tortuosity of the flow path between different wells.
引用
收藏
页码:99 / 106
页数:8
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