Long-Term Temperature Evaluation of a Ground-Coupled Heat Pump System Subject to Groundwater Flow
Abstract
:1. Introduction
2. Site Description
2.1. Geological and Hydrogeological Setting
2.2. Ground Heat Exchanger Characteristics
3. Methodology
3.1. Laboratory Measurement of Thermal Conductivity
3.2. In-Situ Heat Injection Test
3.3. Building and Ground Load Evaluation
3.4. GCHP System Simulation
3.4.1. Governing Equations
3.4.2. Model Geometry and Properties
3.4.3. Initial and Boundary Conditions
3.4.4. Model Calibration
4. Results
4.1. Groundwater Flow Conditions
4.2. Subsurface Thermal Conductivity
4.3. In-Situ Heat Injection Test
4.4. GCHP System Simulation
4.4.1. Ground Loads
4.4.2. Model Calibration
4.4.3. System Operation—Twenty-Year Simulations
5. Discussion
6. Conclusions
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
Nomenclature
c | Specific heat capacity [J kg−1 K−1] |
COP | Coefficient of performance [−] |
ε | Volume fraction [−] |
H | Heat source/sink term [W m−3] |
h | Hydraulic head [m] |
K | Hydraulic conductivity tensor [m s−1] |
K | Hydraulic conductivity [m s−1] |
L | Distance [m] |
P | Heating load [W] |
Q | Hydraulic source/sink term [m3 s−1] |
q | Darcy flux tensor [m s−1] |
λ | Thermal conductivity tensor [W m−1 K−1] |
λ | Thermal conductivity [W m−1 K−1] |
ρ | Density [kg m−3] |
ρc | Volumetric heat capacity [J m−3 K−1] |
Ss | Specific storage coefficient [m−1] |
T | Temperature [K] or [°C] |
t | Time [s] |
Thermal hydrodynamic dispersion tensor [W m−2 K−1] | |
u | Heat carrier fluid velocity tensor [m s−1] |
w | Annual recharge [m s−1] |
Subscripts
EOB | Extended Oberbeck-Boussineq approximation |
g | Grout |
gw | Groundwater flow |
il | Inlet pipe |
ol | Outlet pipe |
r | Heat carrier fluid |
s | Subsurface |
Abbreviations
asl | Above sea level |
E | East |
GCHP | Ground-coupled heat pump |
GHE | Ground heat exchanger |
MTPS | Modified transient plane source |
TRT | Thermal response test |
W | West |
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Parameter | Value |
---|---|
Subsurface | |
Specific storage | 10−4 m−1 |
Volumetric heat capacity of water | 4.2 × 106 J m−3 K−1 |
Volumetric heat capacity of subsurface solids | 2.52 × 106 J m−3 K−1 |
Thermal conductivity of water | 0.65 W m−1 K−1 |
GHE | |
Pipe spacing | 0.10 m |
Inlet and outlet pipe diameter | 0.032 m |
Pipe thermal conductivity | 0.39 W m−1 K−1 |
Pipe wall thickness | 0.0038 m |
Heat carrier fluid thermal conductivity | 0.48 W m−1 K−1 |
Heat carrier fluid density | 1033 kg m−3 |
Rock Type | Measurement Method | Number of Samples Analyzed | Average Thermal Conductivity (W m−1 K−1) |
---|---|---|---|
Gabbro | Needle probe | 3 | 1.87 |
Gabbro | MTPS | 2 | 1.82 |
Calcarenite | MTPS | 1 | 3.58 |
Dark shale | MTPS | 3 | 2.42 |
Light shale | MTPS | 3 | 2.85 |
Calibration Parameter | Possible Range | Chosen Value |
---|---|---|
Kx (m s−1) | 10−5–10−3 | 10−4 |
Ky (m s−1) | 10−7–10−3 | 10−4 |
Kz (m s−1) | 10−9–10−3 | 10−6 |
λ borehole filling material (W m−1 K−1) | 1.5–1.9 | 1.75 |
λ host rock solids (W m−1 K−1) | 2.1–2.4 | 2.4 |
Porosity (%) | 3–5 | 3 |
Scenario | Hydraulic Head at Lateral Boundaries (m) | Hydraulic Gradient (m m−1) | Thermal Conductivity of Subsurface Solids (W m−1 K−1) | Thermal Conductivity of Borehole Filling Material (W m−1 K−1) |
---|---|---|---|---|
A | 26–24 | 0.002 | 2.5 | 1.75 |
B | 26–24 | 0.002 | 2.4 | 1.75 |
C | 26–24 | 0.002 | 2.4 | 1.90 |
D | 26–24 | 0.002 | 2.4 | 1.50 |
E | 26–24 | 0.002 | 2.0 | 1.75 |
F | 26–24 | 0.002 | 3.0 | 1.75 |
G | 26–25.7 | 0.0006 | 2.4 | 1.75 |
H | 26–22 | 0.008 | 2.4 | 1.75 |
Scenario | Hydraulic Gradient | Thermal Conductivity of Subsurface Solids | Thermal Conductivity of Borehole Filling Material | GHE Outlet Minimum/Maximum Temperature during Year 20 | |||
---|---|---|---|---|---|---|---|
(%) | (%) | (%) | Heating Mode | Cooling Mode | |||
(°C) | (%) | (°C) | (%) | ||||
A | − | − | − | 6.4 | − | 25.6 | − |
B | 0 | −4 | 0 | 6.4 | 0 | 25.6 | 0 |
C | 0 | −4 | 9 | 6.5 | 2 | 25.4 | −1 |
D | 0 | −4 | −14 | 6.1 | −5 | 26.1 | 2 |
E | 0 | −20 | 0 | 6.1 | −5 | 26.0 | 2 |
F | 0 | 20 | 0 | 6.9 | 8 | 25.1 | −2 |
G | −70 | −4 | 0 | 2.0 | −69 | 31.7 | 24 |
H | 300 | −4 | 0 | 8.3 | 30 | 23.1 | −10 |
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Jaziri, N.; Raymond, J.; Giordano, N.; Molson, J. Long-Term Temperature Evaluation of a Ground-Coupled Heat Pump System Subject to Groundwater Flow. Energies 2020, 13, 96. https://doi.org/10.3390/en13010096
Jaziri N, Raymond J, Giordano N, Molson J. Long-Term Temperature Evaluation of a Ground-Coupled Heat Pump System Subject to Groundwater Flow. Energies. 2020; 13(1):96. https://doi.org/10.3390/en13010096
Chicago/Turabian StyleJaziri, Nehed, Jasmin Raymond, Nicoló Giordano, and John Molson. 2020. "Long-Term Temperature Evaluation of a Ground-Coupled Heat Pump System Subject to Groundwater Flow" Energies 13, no. 1: 96. https://doi.org/10.3390/en13010096
APA StyleJaziri, N., Raymond, J., Giordano, N., & Molson, J. (2020). Long-Term Temperature Evaluation of a Ground-Coupled Heat Pump System Subject to Groundwater Flow. Energies, 13(1), 96. https://doi.org/10.3390/en13010096