TY - GEN
T1 - Estimation of fracture surface area based on tracer and temperature histories
AU - Suzuki, Anna
N1 - Funding Information:
The author is pleased to thank Mike Shook for great knowledge about analyzing tracer and temperature data. This work was supported by the JSPS KAKENHI Grant Number 717H049760, whose support are gratefully acknowledged. All data for this paper are properly cited and referred to in the reference list. The source code and the fracture data for Appendix A are properly cited and referred to in the reference list. All experimental data are available from the authors upon request (anna.suzuki@tohoku.ac.jp).
PY - 2017
Y1 - 2017
N2 - In EGS reservoirs, a fracture surface area is one of key uncertainty in development. We propose a method to estimate cumulative fracture surface area for each multiple flow path based on tracer and temperature data with cold water injection. Tracer response is used to obtain the flow properties and determine the pore volume for each flow path. By substituting the pore volumes, analytical solutions of heat transfer equation can consist of measurable and/or controllable properties except fracture surface area for each path. The unknown fracture surface areas are estimated by comparison between the superposition of analytical solutions of heat transfer equations and observed temperature decline. Validation with numerical simulation results suggests that even though the number of flow paths is unknown, use of "virtual flow path" can estimate the pore volumes and fracture surface areas. For the simulation results, temperature history for 28 days (10% of temperature decline) provides reasonable estimation of fracture surface area with error of 15.0%.
AB - In EGS reservoirs, a fracture surface area is one of key uncertainty in development. We propose a method to estimate cumulative fracture surface area for each multiple flow path based on tracer and temperature data with cold water injection. Tracer response is used to obtain the flow properties and determine the pore volume for each flow path. By substituting the pore volumes, analytical solutions of heat transfer equation can consist of measurable and/or controllable properties except fracture surface area for each path. The unknown fracture surface areas are estimated by comparison between the superposition of analytical solutions of heat transfer equations and observed temperature decline. Validation with numerical simulation results suggests that even though the number of flow paths is unknown, use of "virtual flow path" can estimate the pore volumes and fracture surface areas. For the simulation results, temperature history for 28 days (10% of temperature decline) provides reasonable estimation of fracture surface area with error of 15.0%.
KW - Fracture surface area
KW - Optimization
KW - Temperature
KW - Tracer
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M3 - Conference contribution
AN - SCOPUS:85041080980
T3 - Transactions - Geothermal Resources Council
SP - 2865
EP - 2879
BT - Geothermal Energy
PB - Geothermal Resources Council
T2 - Geothermal Resources Council 41st Annual Meeting - Geothermal Energy: Power To Do More, GRC 2017
Y2 - 1 October 2017 through 4 October 2017
ER -