Numerical investigation of fluid flow and heat transfer in a doublet enhanced geothermal system with CO2 as the working fluid (CO2-EGS)

被引:127
作者
Luo, Feng [1 ]
Xu, Rui-Na [1 ]
Jiang, Pei-Xue [1 ]
机构
[1] Tsinghua Univ, Dept Thermal Engn, Lab Thermal Sci & Power Engn Minist Educ, Beijing Key Lab CO2 Utilizat & Reduct Technol, Beijing 100084, Peoples R China
基金
国家高技术研究发展计划(863计划); 对外科技合作项目(国际科技项目); 中国国家自然科学基金;
关键词
Enhanced geothermal system; CO2; Induced fracture; Injection/production well perforation placement; Numerical simulation; SUPERCRITICAL PRESSURES; GERMAN BASIN; CONVECTION; EGS; SIMULATION; STORAGE; ENERGY; WELL;
D O I
10.1016/j.energy.2013.10.048
中图分类号
O414.1 [热力学];
学科分类号
摘要
Enhanced geothermal system with CO2 instead of water as the working fluid (CO2-EGS) has attracted much interest due to the additional benefit of CO2 geological storage during the power generation process. This paper describes numerical analyses of a doublet CO2-EGS system, focusing on the influence of the CO2 injection rate, the permeability of induced fractures near the wellbores, the injection/production well perforation placement, the working fluid, and the heat transfer between the wellbores and the surrounding reservoir. The larger permeability in the induced fractures around the wellbores allows the fluid to more easily flow through the reservoir up to a critical fracture permeability, with further increases of the fracture permeability further reducing the pressure loss a little but the cost is not worth the added benefit. Induced fractures around the wellbores result in little difference among different wellbores perforation locations in the reservoir. Increased CO2 injection rates reduce the heat transfer between the wellbores and the surrounding reservoir so that this heat transfer can be neglected at large mass flow rates. With CO2 as the working fluid, the CO2 temperature decreases significantly going up the production well. This paper presents some important implications for CO2-EGS system for further numerical studies as well as for practical projects. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:307 / 322
页数:16
相关论文
共 39 条
[1]  
[Anonymous], 2006, US GUID
[2]   Electricity generation using a carbon-dioxide thermosiphon [J].
Atrens, Aleks D. ;
Gurgenci, Hal ;
Rudolph, Victor .
GEOTHERMICS, 2010, 39 (02) :161-169
[3]   CO2 Thermosiphon for Competitive Geothermal Power Generation [J].
Atrens, Aleks D. ;
Gurgenci, Hal ;
Rudolph, Victor .
ENERGY & FUELS, 2009, 23 (1-2) :553-557
[4]   Modeling the coupling between free and forced convection in a vertical permeable slot:: Implications for the heat production of an Enhanced Geothermal System [J].
Bataille, Arnaud ;
Genthon, Pierre ;
Rabinowicz, Michel ;
Fritz, Bertrand .
GEOTHERMICS, 2006, 35 (5-6) :654-682
[5]  
Batchelor A.S, 2006, FUTURE GEOTHERMAL EN
[6]   3D numerical modeling of hydrothermal processes during the lifetime of a deep geothermal reservoir [J].
Bloecher, M. G. ;
Zimmermann, G. ;
Moeck, I. ;
Brandt, W. ;
Hassanzadegan, A. ;
Magri, F. .
GEOFLUIDS, 2010, 10 (03) :406-421
[7]  
Brown D., 2000, P 25 WORKSHOP GEOTHE, P233
[8]  
Burns KL., 2000, P WORLD GEOTH C 2000, P99
[9]   Numerical simulation of a supercritical CO2 geothermosiphon [J].
Fard, M. Haghshenas ;
Hooman, K. ;
Chua, H. T. .
INTERNATIONAL COMMUNICATIONS IN HEAT AND MASS TRANSFER, 2010, 37 (10) :1447-1451
[10]   Analysis of borehole temperature data in the Northeast German Basin:: continuous logs versus bottom-hole temperatures [J].
Förster, A .
PETROLEUM GEOSCIENCE, 2001, 7 (03) :241-254