Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects

Abstract A fully coupled thermal‐hydraulic‐mechanical (THM) model was developed to investigate the underlying response mechanisms during heat extraction in fractured geothermal reservoirs. The random fracture network in the stimulated zone was reproduced based on the fractal theory. The coupled mode...

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Main Authors: Songcai Han, Yuanfang Cheng, Qi Gao, Chuanliang Yan, Zhongying Han, Jincheng Zhang
Format: Article
Language:English
Published: Wiley 2019-10-01
Series:Energy Science & Engineering
Subjects:
Online Access:https://doi.org/10.1002/ese3.386
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spelling doaj-539d3eaf8dd04a569be1b98354c06eff2020-11-25T02:08:49ZengWileyEnergy Science & Engineering2050-05052019-10-01751705172610.1002/ese3.386Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effectsSongcai Han0Yuanfang Cheng1Qi Gao2Chuanliang Yan3Zhongying Han4Jincheng Zhang5School of Petroleum Engineering China University of Petroleum (East China) Qingdao ChinaSchool of Petroleum Engineering China University of Petroleum (East China) Qingdao ChinaSchool of Petroleum Engineering China University of Petroleum (East China) Qingdao ChinaSchool of Petroleum Engineering China University of Petroleum (East China) Qingdao ChinaSchool of Petroleum Engineering China University of Petroleum (East China) Qingdao ChinaResearch Institute of Petroleum Engineering, Sinopec Beijing ChinaAbstract A fully coupled thermal‐hydraulic‐mechanical (THM) model was developed to investigate the underlying response mechanisms during heat extraction in fractured geothermal reservoirs. The random fracture network in the stimulated zone was reproduced based on the fractal theory. The coupled model accounts for the dominant physical phenomena including (a) fluid flow, heat transport, and solid deformation in porous media and fractures; (b) local thermal nonequilibrium (LTNE) between rock matrix and flowing fluid; and (c) temperature‐dependent fluid thermodynamic properties and stress‐dependent pore and fracture permeability. The proposed model was validated by several analytic solutions. Sequentially, the evolution of pore pressure, equivalent temperature, effective stress, and reservoir permeability was analyzed. The sensitivity of the heat extraction performance to fracture network morphology was discussed. Results show that interconnected large‐scale fractures dominate mass and heat transport. Widely distributed small‐scale fractures contribute to the cooling of the heat rock mass along many flow paths in parallel. The change in effective stress associated with fully coupled thermo‐poroelastic effects may induce fracture shear dilation and pore expansion, resulting in an enhancement of the overall reservoir permeability. There is a significant temperature difference between the solid phase and the fluid phase in fractures, but not in porous media. It is more reasonable to use the LTNE theory to analyze the heat extraction of fractured geothermal reservoirs. The fracture network morphology has a profound effect on heat extraction efficiency and injectivity. Undeveloped fracture networks will result in a higher injection pressure, earlier thermal breakthrough, and shorter lifetime, but higher heat extraction ratio. Properly increasing the fracture density can delay the thermal breakthrough time, prolong the service life, and improve the injectivity. Fully connected fracture networks may result in thermal short‐circuiting and earlier thermal breakthrough. Generating a complex and scattered fracture network but without preferential channels is conducive to extracting more heat from geothermal reservoirs.https://doi.org/10.1002/ese3.386fracture network morphologyfractured geothermal reservoirsheat extraction performancethermo‐poroelastic responsesTHM coupling
collection DOAJ
language English
format Article
sources DOAJ
author Songcai Han
Yuanfang Cheng
Qi Gao
Chuanliang Yan
Zhongying Han
Jincheng Zhang
spellingShingle Songcai Han
Yuanfang Cheng
Qi Gao
Chuanliang Yan
Zhongying Han
Jincheng Zhang
Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
Energy Science & Engineering
fracture network morphology
fractured geothermal reservoirs
heat extraction performance
thermo‐poroelastic responses
THM coupling
author_facet Songcai Han
Yuanfang Cheng
Qi Gao
Chuanliang Yan
Zhongying Han
Jincheng Zhang
author_sort Songcai Han
title Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
title_short Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
title_full Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
title_fullStr Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
title_full_unstemmed Investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
title_sort investigation on heat extraction characteristics in randomly fractured geothermal reservoirs considering thermo‐poroelastic effects
publisher Wiley
series Energy Science & Engineering
issn 2050-0505
publishDate 2019-10-01
description Abstract A fully coupled thermal‐hydraulic‐mechanical (THM) model was developed to investigate the underlying response mechanisms during heat extraction in fractured geothermal reservoirs. The random fracture network in the stimulated zone was reproduced based on the fractal theory. The coupled model accounts for the dominant physical phenomena including (a) fluid flow, heat transport, and solid deformation in porous media and fractures; (b) local thermal nonequilibrium (LTNE) between rock matrix and flowing fluid; and (c) temperature‐dependent fluid thermodynamic properties and stress‐dependent pore and fracture permeability. The proposed model was validated by several analytic solutions. Sequentially, the evolution of pore pressure, equivalent temperature, effective stress, and reservoir permeability was analyzed. The sensitivity of the heat extraction performance to fracture network morphology was discussed. Results show that interconnected large‐scale fractures dominate mass and heat transport. Widely distributed small‐scale fractures contribute to the cooling of the heat rock mass along many flow paths in parallel. The change in effective stress associated with fully coupled thermo‐poroelastic effects may induce fracture shear dilation and pore expansion, resulting in an enhancement of the overall reservoir permeability. There is a significant temperature difference between the solid phase and the fluid phase in fractures, but not in porous media. It is more reasonable to use the LTNE theory to analyze the heat extraction of fractured geothermal reservoirs. The fracture network morphology has a profound effect on heat extraction efficiency and injectivity. Undeveloped fracture networks will result in a higher injection pressure, earlier thermal breakthrough, and shorter lifetime, but higher heat extraction ratio. Properly increasing the fracture density can delay the thermal breakthrough time, prolong the service life, and improve the injectivity. Fully connected fracture networks may result in thermal short‐circuiting and earlier thermal breakthrough. Generating a complex and scattered fracture network but without preferential channels is conducive to extracting more heat from geothermal reservoirs.
topic fracture network morphology
fractured geothermal reservoirs
heat extraction performance
thermo‐poroelastic responses
THM coupling
url https://doi.org/10.1002/ese3.386
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