Selecting the Optimal Use of the Geothermal Energy Produced with a Deep Borehole Heat Exchanger: Exergy Performance †
Abstract
:1. Introduction
2. Materials and Methods
- Undisturbed/far-field ground temperature: the ground source is, as a precautionary measure, assumed to act as a purely conductive media. The far-field ground temperature profile is assumed to act as a linear function of the depth with a surface value of 25 °C (reference ambient temperature) and a constant temperature gradient over the z-direction, Kg. The values of Kg, and αg are the objectives of the next sensitivity analysis.
- WBHX: the thermal power exchanged between the circulating fluid and the far-field ground temperature is evaluated through a series of equivalent thermal resistances. The axial effects are neglected, however, and the temperature evolution of the fluid along the WHBX ducts is evaluated through the so-called “quasi-3D approach” [36,39]. At a given depth, z, the following differential equation applies:
- District heating: the district heating network is modelled as a water flow to be heated from 60 to 90 °C. The useful flow rate, mDH, and the corresponding thermal power are calculated considering a heat transfer effectiveness of the main DH heat exchanger equal to 0.8. The DH application is only considered if the production temperature of the WBHX must be higher than 100 °C.
- Absorption chiller: the end-user chiller loop works with supply and return temperatures of 7 and 12 °C, respectively. The chiller is assumed to act as an indirect-fired unit, namely the generator is equipped with a heat exchanger that allows the energy transfer between the hot water from the WBHX loop and the refrigerant mixture (e.g., LiBr-H2O). The temperature required at the generator, Tgen, is assumed equal to 100 °C. The heat exchanger within the ABSC generator is assumed to be sufficiently long to ensure a unitary heat transfer effectiveness: in other words, the WBHX fluid leaves the absorption unit with a temperature equal to the one required in the ABSC generator. The performance of the chiller is evaluated through the second law of thermal efficiency method, according to source temperatures and exergy efficiency, ηIIABSC, assumed as constant and equal to 0.3.
- ORC power plant and cooling tower: following the results presented in [36], the considered working fluid is 2-methylpropane (isobutane). Depending on the temperature at the WBHX outlet section, the power of the Hirn cycle is calculated using the following assumption: a condenser temperature equal to 41 °C; a pinch point of the HRSG equal to 5 K; an approach point for all the heat exchangers equal to 10 K; an isentropic and electrical-mechanical efficiency of the turbine equal to 0.85 and 0.95, respectively; and an electrical-mechanical efficiency of the feeding pump equal to 0.6. The power required by the fans in the cooling tower is evaluated according to the model presented in the Appendix of [36]. For each tested configuration, the geometry of the finned surface (i.e., number of rows and number of ducts per row) and the frontal air velocity are optimized to minimize the electricity input, ensuring the required heat exchange at the condenser.
- Thermal diffusivity of the ground: αg = {10−7; 5 × 10−7; 10−6} m2/s
- Thermal conductivity of the ground source: λg = {1; 2; 3} W/(m K)
- Ground temperature gradient: Kg = {30; 60; 90; 120; 150} K/km
- WBHX depth: H = {1, 2, 3, 4, 5} km.
- The WBHX fluid must be in the liquid state. Proper work pressure and flow rate are thus evaluated for each configuration.
- The ground temperature at the well bottom must be higher than 100 °C.
- Configurations resulting in negative exergy efficiency are discarded (e.g., when the auxiliary energy consumption exceeds the power production).
3. Results
4. Discussion and Conclusions
Conflicts of Interest
Nomenclature
c | specific heat capacity | [J/kg K] |
specific exergy | [kJ/kg] | |
exergy rate | [W] | |
Kg | temperature gradient | [°C/100 m] |
exergy destruction | [W] | |
IQR interquartile range | ||
k | convective heat transfer | [W/m2 K] |
H | total length of the well | [m] |
mass flow rate | [kg/s] | |
p | pressure | [bar, MPa] |
total thermal power | [W] | |
R | thermal resistance | [mK/W] |
r | radius | [mm] |
T | temperature | [K or °C] |
t | time | [s] |
mechanical/electrical power | [W] | |
z | depth | [m] |
Greek symbols
α | thermal diffusivity | [m2/s] |
η | efficiency | |
λ | thermal conductivity | [W/m K] |
ρ | density | [kg/m3] |
Subscripts, superscripts, acronyms
a | ambient state |
ABSC | absorption chiller |
CP | circulation pump |
CT | cooling tower |
DH | district heating |
DSH+COND | desuperheater + condenser |
dw | downward |
EER | energy efficiency ratio |
EVA | evaporator |
f | fluid |
gen | generator |
HEx | heat-exchanger |
II | second-law |
i | inner |
in | inlet |
o | outer |
ORC | organic Rankine cycle |
out | outlet |
P | pump |
PH | preheater |
ret | return |
s | soil property |
sup | supply |
SH | superheater |
T | turbine |
up | upward |
w | water |
WBHX | WellBore Heat eXchanger |
0 | reference state |
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Parameter | Value |
---|---|
Do/Di Layer 1 | 244.40/226.60 mm |
Do/Di Layer 2 | 226.60/177.8 mm |
Do/Di Layer 3 | 177.8/150.36 mm |
Do/Di Layer 4 | 150.36/88.90 mm |
Do/Di Layer 5 | 88.90/77.92 mm |
Thermal conductivity steel (λ1, λ3, λ5) | 50 W/(mK) |
Thermal conductivity insulation (λ4) | 0.04 W/(mK) |
DH | ABSC | ORC | DH + ABSC | ORC + DH | |
---|---|---|---|---|---|
0.43 | 0.10 | 0.21 | 0.33 | 0.24 | |
329 kW | - | - | 207 | 8 kW | |
- | 184 kW | - | 140 kW | - | |
- | - | 22 kW | - | 22 kW | |
47 kW | 10 kW | 22 kW | 37 kW | 24 kW | |
0.14 | 0.05 | 1 | 0.106 | 0.8 | |
5.4 m3/h | 5.4 m3/h | 5.4 m3/h | 5.4 m3/h | 5.4 m3/h | |
329 kW | 196 kW | 298 kW | 356 | 247 kW | |
73 °C | 100 °C | 80 °C | 68 °C | 90 °C | |
125 °C | 130 °C | 126 °C | 123 °C | 130 °C | |
109 kW | 92 kW | 105 kW | 113 kW | 99 kW | |
45 kW | 48 kW | 44 kW | 45 kW | 45 kW | |
18 kW | 35 kW | 39 kW | 31 kW | 29 kW |
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Alimonti, C.; Conti, P.; Soldo, E. Selecting the Optimal Use of the Geothermal Energy Produced with a Deep Borehole Heat Exchanger: Exergy Performance. Proceedings 2020, 58, 20. https://doi.org/10.3390/WEF-06912
Alimonti C, Conti P, Soldo E. Selecting the Optimal Use of the Geothermal Energy Produced with a Deep Borehole Heat Exchanger: Exergy Performance. Proceedings. 2020; 58(1):20. https://doi.org/10.3390/WEF-06912
Chicago/Turabian StyleAlimonti, Claudio, Paolo Conti, and Elena Soldo. 2020. "Selecting the Optimal Use of the Geothermal Energy Produced with a Deep Borehole Heat Exchanger: Exergy Performance" Proceedings 58, no. 1: 20. https://doi.org/10.3390/WEF-06912
APA StyleAlimonti, C., Conti, P., & Soldo, E. (2020). Selecting the Optimal Use of the Geothermal Energy Produced with a Deep Borehole Heat Exchanger: Exergy Performance. Proceedings, 58(1), 20. https://doi.org/10.3390/WEF-06912