Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size
A new practical method for thermal response test (TRT) is proposed herein to estimate the groundwater velocity and effective thermal conductivity of geological zones. The relaxation time of temperature (RTT) is applied to determine the depths of the zones. The RTT is the moment when the temperature...
Main Authors: | , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2020-06-01
|
Series: | Energies |
Subjects: | |
Online Access: | https://www.mdpi.com/1996-1073/13/13/3297 |
id |
doaj-4045e5ec8da9488db43f01013d2cebbd |
---|---|
record_format |
Article |
spelling |
doaj-4045e5ec8da9488db43f01013d2cebbd2020-11-25T03:31:52ZengMDPI AGEnergies1996-10732020-06-01133297329710.3390/en13133297Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole SizeHobyung Chae0Katsunori Nagano1Yoshitaka Sakata2Takao Katsura3Ahmed A. Serageldin4Takeshi Kondo5Graduate School of Engineering, Hokkaido University, N13-W8, Sapporo 060-8628, JapanGraduate School of Engineering, Hokkaido University, N13-W8, Sapporo 060-8628, JapanGraduate School of Engineering, Hokkaido University, N13-W8, Sapporo 060-8628, JapanGraduate School of Engineering, Hokkaido University, N13-W8, Sapporo 060-8628, JapanGraduate School of Engineering, Hokkaido University, N13-W8, Sapporo 060-8628, JapanNIKKEN SEKKEI Research Institute, 3-737, Kanda Ogawamachi, Chiyoda-ku, Tokyo 101-0052, JapanA new practical method for thermal response test (TRT) is proposed herein to estimate the groundwater velocity and effective thermal conductivity of geological zones. The relaxation time of temperature (RTT) is applied to determine the depths of the zones. The RTT is the moment when the temperature in the borehole recovers to a certain level compared with that when the heating is stopped. The heat exchange rates of the zones are calculated from the vertical temperature profile measured by the optical-fiber distributed temperature sensors located in the supply and return sides of a U-tube. Finally, the temperature increments at the end time of the TRT are calculated according to the groundwater velocities and the effective thermal conductivity using the moving line source theory applied to the calculated heat exchange rates. These results are compared with the average temperature increment data measured from each zone, and the best-fitting value yields the groundwater velocities for each zone. Results show that the groundwater velocities for each zone are 2750, 58, and 0 m/y, whereas the effective thermal conductivities are 2.4, 2.4, and 2.1 W/(m∙K), respectively. The proposed methodology is evaluated by comparing it with the realistic long-term operation data of a ground source heat pump (GSHP) system in Kazuno City, Japan. The temperature error between the calculated results and measured data is 6.4% for two years. Therefore, the proposed methodology is effective for estimating the long-term performance analysis of GSHP systems.https://www.mdpi.com/1996-1073/13/13/3297relaxation time of temperaturethermal response testgroundwater velocitymoving line source theoryoptical fiber distributed temperature sensor |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hobyung Chae Katsunori Nagano Yoshitaka Sakata Takao Katsura Ahmed A. Serageldin Takeshi Kondo |
spellingShingle |
Hobyung Chae Katsunori Nagano Yoshitaka Sakata Takao Katsura Ahmed A. Serageldin Takeshi Kondo Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size Energies relaxation time of temperature thermal response test groundwater velocity moving line source theory optical fiber distributed temperature sensor |
author_facet |
Hobyung Chae Katsunori Nagano Yoshitaka Sakata Takao Katsura Ahmed A. Serageldin Takeshi Kondo |
author_sort |
Hobyung Chae |
title |
Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size |
title_short |
Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size |
title_full |
Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size |
title_fullStr |
Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size |
title_full_unstemmed |
Analysis of Relaxation Time of Temperature in Thermal Response Test for Design of Borehole Size |
title_sort |
analysis of relaxation time of temperature in thermal response test for design of borehole size |
publisher |
MDPI AG |
series |
Energies |
issn |
1996-1073 |
publishDate |
2020-06-01 |
description |
A new practical method for thermal response test (TRT) is proposed herein to estimate the groundwater velocity and effective thermal conductivity of geological zones. The relaxation time of temperature (RTT) is applied to determine the depths of the zones. The RTT is the moment when the temperature in the borehole recovers to a certain level compared with that when the heating is stopped. The heat exchange rates of the zones are calculated from the vertical temperature profile measured by the optical-fiber distributed temperature sensors located in the supply and return sides of a U-tube. Finally, the temperature increments at the end time of the TRT are calculated according to the groundwater velocities and the effective thermal conductivity using the moving line source theory applied to the calculated heat exchange rates. These results are compared with the average temperature increment data measured from each zone, and the best-fitting value yields the groundwater velocities for each zone. Results show that the groundwater velocities for each zone are 2750, 58, and 0 m/y, whereas the effective thermal conductivities are 2.4, 2.4, and 2.1 W/(m∙K), respectively. The proposed methodology is evaluated by comparing it with the realistic long-term operation data of a ground source heat pump (GSHP) system in Kazuno City, Japan. The temperature error between the calculated results and measured data is 6.4% for two years. Therefore, the proposed methodology is effective for estimating the long-term performance analysis of GSHP systems. |
topic |
relaxation time of temperature thermal response test groundwater velocity moving line source theory optical fiber distributed temperature sensor |
url |
https://www.mdpi.com/1996-1073/13/13/3297 |
work_keys_str_mv |
AT hobyungchae analysisofrelaxationtimeoftemperatureinthermalresponsetestfordesignofboreholesize AT katsunorinagano analysisofrelaxationtimeoftemperatureinthermalresponsetestfordesignofboreholesize AT yoshitakasakata analysisofrelaxationtimeoftemperatureinthermalresponsetestfordesignofboreholesize AT takaokatsura analysisofrelaxationtimeoftemperatureinthermalresponsetestfordesignofboreholesize AT ahmedaserageldin analysisofrelaxationtimeoftemperatureinthermalresponsetestfordesignofboreholesize AT takeshikondo analysisofrelaxationtimeoftemperatureinthermalresponsetestfordesignofboreholesize |
_version_ |
1724571212125831168 |