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STARS
Case Studies

Improving Closed-Loop Geothermal Predictions with CMG STARS

STARS

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:

  • CMG STARS 
  • COMSOL Multiphysics 
  • GEOSIM (CRIEPI geothermal simulator) 
  • Analytical models

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:

  • Limited hydrothermal reservoirs 
  • Regulatory and environmental restrictions 
  • Large volumes of untapped hot dry rock 

Closed-loop geothermal systems address this by:

  • Circulating fluid in a sealed well system 
  • Extracting heat via conduction and convection

This offers significant advantages:

  • Geographic flexibility: applicable wherever subsurface temperatures are sufficient, regardless of rock permeability or hydrothermal fluid presence
  • Reduced scaling risk: no contact between working fluid and formation water eliminates the mineral precipitation and flow decline issues endemic to open hydrothermal systems
  • Regulatory advantages: lower environmental impact and reduced conflict with hot spring resources and national park regulations
  • Lower induced seismicity risk: no hydraulic fracturing required (unlike Enhanced Geothermal Systems / Hot Dry Rock approaches)

Operational Context

The study evaluated multiple closed-loop configurations to understand how different system architectures respond to subsurface conditions and modeling approaches.

  • CMG STARS → Full reservoir + wellbore + thermal physics 
  • COMSOL → Pipe-flow + conductive heat transfer 
  • GEOSIM → Axisymmetric geothermal model 
  • Analytical → Simplified heat transfer

The study classified closed-loop and related configurations into two primary architectural families, each with multiple sub-variants.

U-Loop Systems

  • Multilateral wells connected at depth 
  • Large heat exchange area

Coaxial Systems

  • Single vertical well with inner/outer flow paths
Family Sub-type Orientation Hydrothermal Field? Description
U-Loop Single-well (U-Loop ) 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.

  • Production temperatures: 
    • ~145-175°C depending on flow rate 
  • Cross-tool variation: 
    • Typically within ±10°C 

2. For configurations where formation-fluid interactions become significant, simulation results showed greater sensitivity to the underlying physical assumptions.

  • STARS: ~130-150°C 
  • COMSOL / GEOSIM: ~100-110°C 
  • Difference: 20-40°C

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

  • CMG STARS provides a more comprehensive representation of subsurface physics, enabling engineers to evaluate closed-loop geothermal systems with greater confidence across a range of configurations.
  • U-loop systems: 
    • Conduction-dominated → tools agree 
  • Coaxial systems: 
    • Convection-sensitive → tools diverge 
  • Ignoring formation convection leads to: 
    • Lower predicted temperatures 
    • Misleading economic conclusions 

Best Practices

  • Select simulation approaches that represent both wellbore and formation-scale heat transfer 
  • Ensure models capture natural convection effects where formation permeability is non-negligible 
  • Use tools capable of predicting realistic production temperatures under long-term operation 
  • Align economic evaluations with physics-based simulation outputs, not simplified assumptions

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.

About This Resource

Reference Publication: https://journal.jogmec.go.jp/content/300399211.pdf

Year: 2023

Software: STARS

Rose Subsurface Assessment is now a part of Computer Modelling Group Ltd.