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Closed-loop geothermal systems offer a pathway to unlock heat from non-hydrothermal (“dry”) formations, but their feasibility depends heavily on how heat transfer is modeled.
A comprehensive study conducted by JOGMEC (Japan Oil, Gas and Metals Corporation) evaluated multiple closed-loop configurations using four simulation approaches:
Outcome: CMG STARS predicted production temperatures up to 20-40°C higher than other tools by capturing thermally-driven natural convection in the surrounding formation. This highlighted how modeling assumptions can significantly influence performance predictions across closed-loop geothermal systems.
Significance of Closed Loop Geothermal in Japan
Japan has significant geothermal potential but faces constraints:
Closed-loop geothermal systems address this by:
This offers significant advantages:
Operational Context
The study evaluated multiple closed-loop configurations to understand how different system architectures respond to subsurface conditions and modeling approaches.
The study classified closed-loop and related configurations into two primary architectural families, each with multiple sub-variants.
U-Loop Systems
Coaxial Systems
| Family | Sub-type | Orientation | Hydrothermal Field? | Description |
|---|---|---|---|---|
| U-Loop | Single-well (U-Loop ⓪) | Horizontal | Non-hydrothermal | Pilot scale; one injector, one producer, connected at depth by a single horizontal lateral. Included in simulation for validation only. |
| U-Loop | Multi-well Horizontal (U-Loop ①) | Horizontal laterals | Non-hydrothermal | 12 horizontal lateral wells. Injectors and producers at 3,232 m depth, 75 m well spacing, lateral length ~1,400–1,600 m per leg. |
| U-Loop | Multi-well Deviated (U-Loop ②) | Inclined/ERD laterals | Non-hydrothermal | 12 deviated (30° from vertical at kickoff) lateral wells. Reaches deeper temperature zones than U-Loop ①. |
| Coaxial | Coaxial ① (casing outer) | Vertical | Non-hydrothermal | Uses existing well casing as outer conduit; single insulated inner tube (VIT). No pump pressurization. Limited heat exchange. Included in simulation; excluded from cost analysis. |
| Coaxial | Coaxial ② (double-pipe, non-hydrothermal) | Vertical | Non-hydrothermal | Purpose-built coaxial double-pipe system in formation without natural hot fluid inflow. Working fluid circulated by surface pump. |
| Coaxial | Coaxial ③ (double-pipe, hydrothermal zone) | Vertical | Hydrothermal | Double-pipe in or near a hydrothermal zone; design allows limited hot water inflow at depth (19 t/h or 2 t/h inflow cases studied). Strictly a hybrid, not a pure closed-loop. |
Table 1. Full taxonomy of closed-loop configurations evaluated.
Model Overview
All tools were run with a shared base case representing a hypothetical Japanese geothermal site. Rock properties were defined for two representative lithologies encountered in Japanese geothermal drilling:
| Parameter | Neogene Sedimentary (Rock1) | Quaternary Volcanic (Rock2) | Units |
|---|---|---|---|
| Thermal conductivity | 2.5 | 1.8 | W/(m·K) |
| Density | 2,600 | 2,300 | kg/m³ |
| Specific heat capacity | 900 | 850 | J/(kg·K) |
| Porosity | 0.16 | 0.27 | — |
| Permeability | 1–50 | 30–200 | mD |
| Geothermal gradient (base) | 10.0°C/100m | 10.0°C/100m | — |
| Surface temperature | 15 | 15 | °C |
| Temperature at 3,232 m TVD (base) | ~338 | ~338 | °C |
Table 2. Rock property inputs for base case simulations.
Key Results
1. For configurations where heat transfer is primarily conduction-dominated, all simulation tools showed strong agreement.
2. For configurations where formation-fluid interactions become significant, simulation results showed greater sensitivity to the underlying physical assumptions.
Insight: CMG STARS predicted production temperatures 20-40°C higher than those of other tools by capturing thermally driven natural convection.
3. LCOE (Levelized Cost of Electricity) Analysis
LCOE was calculated over a 30-year project life using standard discounted cash flow methodology, with operating costs, fixed asset taxes, and decommissioning costs included.
| Configuration | LCOE Base Case (¥/kWh) | Well Cost Share (%) | Dominant Cost Driver | Comparison to Conventional Geothermal (¥33.8/kWh avg.) |
|---|---|---|---|---|
| Coaxial ③ (new well) | ~58.3 | ~70% | Well construction vs. low power output | 1.7x conventional |
| Coaxial ③ (existing well + site) | ~43.5 | ~55% | Reduced by well reuse | 1.3x conventional |
| Coaxial ③ (existing well, no site) | ~36.4 | ~40% | Near conventional range | ~1.1x conventional |
| Coaxial ② | ~151.0 | ~80% | Very low power output per well | 4.5x conventional |
| U-Loop ① (Case 2) | ~224.4 | ~90% | High drilling cost for 12 complex wells | 6.6x conventional |
| U-Loop ② (Case 3) | ~158.2 | ~88% | Improved vs. ①; still drilling-dominated | 4.7x conventional |
| U-Loop ② (Case 4 high flow) | ~107.8 | ~85% | Higher flow reduces unit cost | 3.2x conventional |
Table 3. LCOE base case estimates.
Insight: Table 3 indicates that drilling complexity, not thermal performance, is the dominant cost driver for U-loop systems, whereas coaxial systems are more sensitive to thermal modeling accuracy. Accurate temperature prediction, such as that provided by STARS, directly influences these economics.
Key Takeaways
Best Practices
Conclusion
This study demonstrates that:
Simulation methodology plays a critical role in evaluating closed-loop geothermal systems. Approaches that incorporate full subsurface physics, including formation-fluid interactions, can provide a more complete understanding of heat recovery potential and support more informed engineering and investment decisions.
Reference Publication: https://journal.jogmec.go.jp/
Year: 2023
Software: STARS