A Comparative Study and Experimental Investigation of Multi-Objective Optimization for Geothermal-Driven Organic Rankine Cycle
Abstract
1. Introduction
- (1)
- This study links working-fluid selection, parametric analysis, and multi-objective optimization within a consistent modelling basis for geothermal-driven ORC assessment.
- (2)
- Explicit feasibility constraints (e.g., pinch-point, superheat/subcooling and operational limits) are incorporated to identify feasible operating/design ranges and to avoid non-physical solutions.
- (3)
- A 20 kW small-scale ORC experiment is used as a feasibility and trend-consistency reference to support physically operable ranges relevant to the modelling assumptions.
- (4)
- A component-level thermo-economic and exergoeconomic perspective is used to interpret trade-offs and to identify dominant contributors affecting Pareto-optimal designs; in particular, the heat-exchanger area requirement under tight pinch constraints is highlighted as a primary cost bottleneck for high-efficiency solutions.
2. System Description
- The system operates under steady-state conditions.
- Changes in kinetic and potential energy are neglected.
- Pressure drops in the evaporator and condenser are considered. Pressure losses along interconnecting pipelines are neglected in this configuration-level study because they are layout-dependent and require plant-specific piping information beyond the present scope. Where needed, their effect can be included as a lumped pressure-drop term applied to the high- and low-pressure sides.
- The geothermal production stream is assumed to be saturated liquid water at the wellhead.
- The pumps and turbine are characterized by their isentropic efficiencies.
3. System Model
3.1. First Law Model
3.2. Second Law Model
3.3. Exergoeconomic Model
3.4. Economic Model
3.5. Heat Exchangers Model
3.6. Multi-Objective Optimization Model
- Maximizing the first law efficiency .
- Maximizing the second law efficiency .
- Maximizing the net power output .
- Minimizing the total product cost .
- Minimizing the total capital investment (TCI).
3.7. Model Validation
4. Fluid Selection
5. Experiment Description
5.1. Experimental Setup
5.2. Experimental Design
6. Result and Discussion
6.1. Parametric Study Discussion
6.2. Multi-Objective Optimization Discussion
7. Conclusions
- R123, R1234ze(E), R1234ze(Z), Isobutane, and R141b are identified as preferred working fluids for geothermal ORC over the investigated temperature range. R141b shows robust performance across a wide range of conditions, whereas Isobutane is more competitive at higher source temperatures (above ~140 °C).
- Within the investigated range, an intermediate evaporator pressure maximizes net power output due to the balance between increased turbine specific work and reduced recoverable heat under finite temperature-approach constraints. Cost-related indicators generally favour higher evaporator pressure until component/heat-transfer constraints become limiting.
- Lower condensation temperatures improve thermodynamic performance by reducing turbine back pressure; however, the preferred region should be selected considering the associated condenser duty and practical cooling conditions.
- The superheat degree has limited influence on the first-law efficiency within the studied range but can reduce net power output and increase heat rejection; therefore, superheating should primarily be set to ensure safe expansion while avoiding excessive thermal margins.
- Subcooling is required to mitigate cavitation risk at the pump inlet; in the present study, a small subcooling margin (around 3 °C) is sufficient for safe operation within the tested envelope.
- Pinch-point temperature differences govern the feasibility of heat recovery and the thermodynamic irreversibility of heat transfer. A balanced selection is recommended, with a small evaporator pinch (≈3 °C) and a moderate condenser pinch (≈5–9 °C) under the investigated conditions. From an economic/exergoeconomic viewpoint, tightening pinch-point constraints drives a rapid increase in the required heat-transfer area, making the evaporator and condenser the primary cost bottleneck for high-efficiency designs and shifting Pareto-optimal solutions against cost-oriented objectives.
- For the high-temperature case (165 °C), the bi-objective and tri-objective optimizations provide operable Pareto trade-offs and representative compromise solutions that balance power, efficiency, and cost.
Supplementary Materials
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
Nomenclature
| Roman symbols | Greek symbols | ||
| A | Heat transfer area | convective heat-transfer coefficient | |
| Bo | Bond number | thickness | |
| cost rate | first-law efficiency | ||
| specific exergy cost | second-law efficiency | ||
| specific heat capacity | pump isentropic efficiency | ||
| CRF | capital recovery factor | turbine/expander isentropic efficiency | |
| specific heat capacity | dynamic viscosity | ||
| equivalent diameter | kinematic viscosity | ||
| exergy rate | density | ||
| riction factor in pressure-drop correlation | surface tension | ||
| gravitational acceleration | pressure drop | ||
| Grashof number | |||
| specific enthalpy | Subscripts and abbreviations | ||
| interest rate | 0 | ambient | |
| thermal conductivity | 1–10 | state points | |
| characteristic length/heat-transfer length | c | cold loop | |
| mass flow rate | h | hot loop | |
| Nusselt number | w | water | |
| pressure | wf | working fluid | |
| purchased equipment cost | ev | evaporator | |
| Prandtl number | cn | condenser | |
| heat-transfer rate | hex | heat exchanger | |
| Reynolds number | orc | ORC loop | |
| specific entropy | p | pump | |
| temperature | turbine/ | ||
| total capital investment | ph | physical | |
| velocity | s | isentropic process | |
| power | l | liquid | |
| plate width | pp | pinch-point; pay back period | |
| X | annual plant operation hours | ||
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| Study | Focus/Method | Output |
|---|---|---|
| Habka et al. (2014) [22] | Geothermal ORC–CHP; configuration comparison | CHP configuration insights |
| Eerdeweghe et al. (2018) [23] | Low-T geothermal ORC–CHP; optimization | CHP plant choice |
| Wang et al. (2022) [21] | Geothermal ORC; multi-objective + fluid selection | Ranked/selected solutions |
| This work | Constraint-aware workflow; screening, sensitivity, mult-objective Pareto | Operable Pareto sets; feasible operating ranges |
| Performance Parameter | Unit | Present Work | [15] |
|---|---|---|---|
| kg/s | 3.53 | 3.61 | |
| kW | 175.40 | 180.91 | |
| kW | 12.67 | 13.07 | |
| kJ/s | 1457.9 | 1456.85 | |
| % | 11.16 | 11.52 | |
| % | 35.87 | 35.05 |
| Parameter | Value |
|---|---|
| Environment temperature | 15 °C |
| Environment pressure | 101.325 kPa |
| Cooling water temperature | 15 °C |
| Geothermal water flow rate | 100 kg/s |
| Pumps isentropic efficiency | 95% |
| Turbine isentropic efficiency | 89% |
| Interest rate | 5% |
| Plant economic life | 20 years |
| Annual operating hours | 8000 h |
| Parameters | Value |
|---|---|
| Geothermal water Temperature (°C) | 70, 100, 140, 180 |
| Geothermal water Mass flow rate (kg/s) | 100 |
| Condensation Temperature (°C) | 40 |
| Superheat (°C) | 10 |
| Subcooling (°C) | 3 for , 10 for |
| Working Fluid | ) |
|---|---|
| R141b | 70~180 °C |
| R123 | 70~140 °C |
| R1234ze(E) | 100~140 °C |
| R1234ze(Z) | 180 °C |
| Isobutane | 180 °C |
| Temperature (°C) | Flow Rate (L/s) | Mineralization (g/L) | Heat Storage Rock Layer |
|---|---|---|---|
| 97 | 113.5 | 0.3~0.9 | Granite |
| Measured Parameters | Instrument | Model | Manufacturer | Measuring Range | Accuracy |
|---|---|---|---|---|---|
| Temperature | K type Thermocouple | WRT-191 | Wuxi Hualwei Instrument Co., Ltd., Wuxi, China | −40~350 °C | ±0.5% |
| Pressure | Diffused silicon pressure transmitter | 3051TG | Rosemount Inc. (Emerson), Chanhassen, MN, USA | 0~1.5 MPa | ±0.2% |
| Flow | Vortex flowmeter | HL-LUGB | Jiangsu Hualiu Instrument Co., Ltd., Huai’an (Jinhu County), China | 0.3~3 kg/s | ±0.5% |
| Variable | Range | Number of Levels |
|---|---|---|
| A (ORC loop flow) | 0.3~1.2 kg/s | 5 (0.3,0.53,0.75,0.97,1.2) |
| B (Heat loop flow) | 7~20 t/h | 5 (7,10.25,13.5,16.75,20) |
| C (Cold loop flow) | 12~38 t/h | 5 (12,18.5,25,31.5,38) |
| D (Heat loop temperature) | 80~110 °C | 5 (80,87.5,95,102.5,110) |
| E (Cold loop temperature) | 20~40 °C | 5 (20,25,30,35,40) |
| F (Connected load) | 21~30 kW | 4 (21,24,27,30) |
| Variable | Range |
|---|---|
| Evaporator pressure | 0.4~2.2 MPa |
| Condensation temperature | 30~90 °C |
| Superheat degree | 0~50 °C |
| Subcooling degree | 3~10 °C |
| Evaporator pinch-point temperature difference | 3~10 °C |
| Condenser pinch-point temperature difference | 3~10 °C |
| Tuning Parameters | Value |
|---|---|
| Population Size | 50 for bi-objective 100 for tri-objective |
| Stop Generation | 300 |
| Mutation Probability | 0.01 |
| Crossover Probability | 0.8 |
| Obj. Set | 100 °C (Figure 10) | 165 °C (Figure 11) | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
(MPa) | (°C) | (°C) | (°C) | (°C) | (°C) | (MPa) | (°C) | (°C) | (°C) | (°C) | (°C) | |
| (a) | 0.4493 | 30.00 | 0.47 | 3.60 | 3.10 | 9.74 | 1.2456 | 30.04 | 7.29 | 4.66 | 3.09 | 6.84 |
| (b) | 0.4385 | 30.00 | 0.01 | 4.09 | 3.00 | 3.00 | 1.1003 | 30.00 | 1.09 | 5.30 | 3.00 | 4.07 |
| (c) | 0.4708 | 30.00 | 0.24 | 3.92 | 3.22 | 9.99 | 1.3760 | 31.58 | 6.53 | 4.09 | 4.23 | 9.59 |
| (d) | 0.4400 | 30.00 | 3.65 | 3.60 | 3.00 | 3.99 | 1.0570 | 30.00 | 0.35 | 5.81 | 3.12 | 3.52 |
| (e) | 0.4987 | 30.00 | 8.97 | 3.13 | 10.00 | 10.00 | 1.5100 | 30.00 | 16.85 | 3.44 | 10.00 | 5.29 |
| (f) | 0.5080 | 30.00 | 0.02 | 4.20 | 3.08 | 9.93 | 1.3500 | 30.00 | 0.06 | 7.39 | 3.57 | 9.75 |
| (g) | 0.3870 | 30.00 | 0.79 | 4.50 | 9.91 | 10.00 | 1.4030 | 30.12 | 6.41 | 4.06 | 4.00 | 10.00 |
| (h) | 0.4420 | 30.00 | 0.58 | 4.09 | 3.00 | 4.98 | 1.2270 | 30.03 | 2.35 | 4.92 | 3.01 | 3.17 |
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Xie, K.; He, H.; Li, Y. A Comparative Study and Experimental Investigation of Multi-Objective Optimization for Geothermal-Driven Organic Rankine Cycle. Modelling 2026, 7, 44. https://doi.org/10.3390/modelling7020044
Xie K, He H, Li Y. A Comparative Study and Experimental Investigation of Multi-Objective Optimization for Geothermal-Driven Organic Rankine Cycle. Modelling. 2026; 7(2):44. https://doi.org/10.3390/modelling7020044
Chicago/Turabian StyleXie, Kaiyi, Haotian He, and Yuzheng Li. 2026. "A Comparative Study and Experimental Investigation of Multi-Objective Optimization for Geothermal-Driven Organic Rankine Cycle" Modelling 7, no. 2: 44. https://doi.org/10.3390/modelling7020044
APA StyleXie, K., He, H., & Li, Y. (2026). A Comparative Study and Experimental Investigation of Multi-Objective Optimization for Geothermal-Driven Organic Rankine Cycle. Modelling, 7(2), 44. https://doi.org/10.3390/modelling7020044

