T326 21st Century Rock Flow Properties and Processes: 3D Printing, Digital Rock Physics, and Hydrogeophysics
Wednesday, 25 October 2017
1:30 PM - 5:30 PM
Room 613/614
THERMAL DISPERSION BEHAVIOR UNDER THE INDUCED FLOW FIELD BY THE GWHP SYSTEM
Paper number: T326-15
Program: Technical Sessions
Time: 5:00 PM – 5:15 PM
Authors
-
Dahee JungSeoul National University, Seoul
-
Bo-Hyun LeeSeoul National University, Seoul
-
Kang-Kun LeeSeoul National University, Seoul
Abstract
In addition, pumping and injection in field applications can further increase the magnitude of thermal dispersion. Because the GWHP utilizes a great deal of groundwater as a heat source (or a heat sink), the great perturbation can occur in natural flow system. Under such condition, the influence of the thermal dispersion on the relevant transport processes can be increased.
In this study, lab-scale thermal tracer tests were performed to investigate the thermal dispersion behavior under forced flow field by injection. In the experiments, a resistor and warm water were used as point heat sources with various background flow velocities. The observed thermal breakthrough curves were analyzed by analytical and numerical models. The results suggest that the importance of thermal dispersion can vary with injection rates as well as background flow velocities
Acknowledgements
This work was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIP) (No. 2017R1A2B3002119). This study was also supported by the X-project of the NRF and the Geowater+ project in “Water Resources Management Program” of the MOLIT and the KAIA of Korea. Thermal monitoring was partly supported by the R&D project on Environmental Management of Geologic CO2 Storage from the KETTI (# 201400180003). The BK 21 PLUS project of the Korean government also supported this study.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-301923
© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.