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Title: Thermal drawdown-induced flow channeling in a single fracture in EGS

Journal Article · · Geothermics

Here, the evolution of flow pattern along a single fracture and its effects on heat production is a fundamental problem in the assessments of engineered geothermal systems (EGS). The channelized flow pattern associated with ubiquitous heterogeneity in fracture aperture distribution causes non-uniform temperature decrease in the rock body, which makes the flow increasingly concentrated into some preferential paths through the action of thermal stress. This mechanism may cause rapid heat production deterioration of EGS reservoirs. In this study, we investigated the effects of aperture heterogeneity on flow pattern evolution in a single fracture in a low-permeability crystalline formation. We developed a numerical model on the platform of GEOS to simulate the coupled thermo-hydro-mechanical processes in a penny-shaped fracture accessed via an injection well and a production well. We find that aperture heterogeneity generally exacerbates flow channeling and reservoir performance generally decreases with longer correlation length of aperture field. The expected production life is highly variable (5 years to beyond 30 years) when the aperture correlation length is longer than 1/5 of the well distance, whereas a heterogeneous fracture behaves similar to a homogeneous one when the correlation length is much shorter than the well distance. Besides, the mean production life decreases with greater aperture standard deviation only when the correlation length is relatively long. Although flow channeling is inevitable, initial aperture fields and well locations that enable tortuous preferential paths tend to deliver long heat production lives.

Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office; National Science Foundation (NSF)
Grant/Contract Number:
AC52-07NA27344; CBET-1133849
OSTI ID:
1294696
Alternate ID(s):
OSTI ID: 1367999
Report Number(s):
LLNL-JRNL-670552; S0375650516000067; PII: S0375650516000067
Journal Information:
Geothermics, Journal Name: Geothermics Vol. 61 Journal Issue: C; ISSN 0375-6505
Publisher:
ElsevierCopyright Statement
Country of Publication:
United Kingdom
Language:
English
Citation Metrics:
Cited by: 103 works
Citation information provided by
Web of Science

Cited By (9)

An analytical thermohydraulic model for discretely fractured geothermal reservoirs: ANALYTICAL THERMOHYDRAULIC MODEL journal September 2016
Experiments and Simulations of Fully Hydro-Mechanically Coupled Response of Rough Fractures Exposed to High-Pressure Fluid Injection journal February 2018
Three-dimensional flow characterization in a joint with plumose pattern journal August 2018
Inferring Geothermal Reservoir Processes at the Raft River Geothermal Field, Idaho, USA, Through Modeling InSAR-Measured Surface Deformation journal May 2018
Thermal Attenuation and Lag Time in Fractured Rock: Theory and Field Measurements From Joint Heat and Solute Tracer Tests journal December 2018
Spatial Mapping of Fracture Aperture Changes With Shear Displacement Using X‐ray Computerized Tomography journal July 2019
Field Comparison of DNA‐Labeled Nanoparticle and Solute Tracer Transport in a Fractured Crystalline Rock journal August 2019
Solute tracer test quantification of the effects of hot water injection into hydraulically stimulated crystalline rock journal June 2020
Dipole and Convergent Single-Well Thermal Tracer Tests for Characterizing the Effect of Flow Configuration on Thermal Recovery journal October 2019

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