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Optimal GSHP–ASHP hybridisation for large-scale tertiary buildings with imbalanced loads Cover

Optimal GSHP–ASHP hybridisation for large-scale tertiary buildings with imbalanced loads

Open Access
|Aug 2026
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Figures & Tables

Table 1

Overview of the ten hybrid GSHP studies reviewed.

REFERENCELOCATIONCLIMATEBUILDINGSYSTEM
Pardo et al. (2010)Valencia (ES)MediterraneanOffice buildingGSHP+ASHP+storage
X. Wang et al. (2010)Harbin (CN)Severe coldDetached houseSolar+GSHP seasonal
You et al. (2014)3 cities (CN)ColdHotelGSHP+AHCa
You et al. (2015)Harbin (CN)Severe coldHotelGSHP+AHCa
Emmi et al. (2017)Vicenza (IT)TemperateDetached housePVT+GSHP+ASHP
Grossi et al. (2018)Bologna (IT)TemperateDetached houseDSHPb dual-source
Zheng et al. (2022)Changsha (CN)Hot summerDormitoryPV+GSHP+ASHP
Li et al. (2024)Handan (CN)ColdResidential complexPVT+GSHP+ASHP
F. Wang et al. (2024)Harbin (CN)Severe coldOffice buildingBIPV/Tc+energy piles
Yue et al. (2025)Qingdao (CN)ColdGymnasiumPVT+GSHP+ASHP+battery

[i] aAHC: aerothermal heat compensator. bDSHP: dual-source heat pump. cBIPV/T: building-integrated PV/thermal.

Table 2

Performance results and ground temperature drift reported across the ten studies. “ΔT soil” refers to the inter-annual ground temperature change (negative = cooling); values after a slash indicate the stabilised value with the hybrid system active. LCC: life-cycle cost; ALCC: annualised life-cycle cost.

REFERENCECOP syst.ΔT soilECON. METRICKEY FINDING
Pardo et al. (2010)3.8N/ABest paybackElec. –60% vs ASHP
X. Wang et al. (2010)6.55+2 K–Solar = 50% of heat
You et al. (2014)2.9–4.7–12.7 K/stableSav. 5–6%COP 4.1→2.0 w/o AHC
You et al. (2015)4.5–15–11.2 K/stableSav. 23.9%Fails yr 7 w/o AHC
Emmi et al. (2017)3.55–3.94–2.5 K (stable)N/APVT+air compet. w/o ground
Grossi et al. (2018)3.1–3.5–4.5 K/stableBHE –30–50%APF opt. depends on BHE
Zheng et al. (2022)4.69–6.3 K/stableALCC –8%COP 3.2→2.9
Li et al. (2024)3.8–6.0–1.4 KASHP cheaperMedium-deep 1,500 m
F. Wang et al. (2024)2.96–3.02+0.7 K (stable)LCC –57–62%Conv. stops yr 11
Yue et al. (2025)6.3–2.9 K/+0.1 KLCC –55%Elec. –71%
Table 3

Economic parameters for LCOE computation.

PARAMETERVALUEUNIT
Drilling cost (equipped borehole)120EUR/m
GSHP cost600EUR/kW
ASHP cost600EUR/kW
Electricity price230EUR/MWh
Weighted average cost of capital (WACC)4%
Analysis horizon10years
Figure 1

System, GSHP and ASHP annual COP as a function of the switching temperature. Dashed curves show the GSHP COP per outdoor air temperature bin (one curve per Tswitch); shaded bands indicate the interquartile range. Grey bars represent the normalised heating demand distribution by temperature bin. Top (a): default GSHP performance map. Bottom (b): steep-gradient GSHP performance map.

Figure 2

Monthly-averaged borefield temperature over 25 years for each switching temperature (Langres, 1,000 kW, default performance map). Lower Tswitch values preserve the ground temperature by limiting geothermal extraction.

Table 4

Optimal hybrid configurations—Montpellier. For each building (rows) and available surface ratio (column groups), the retained configuration minimises LCOE while satisfying Tfluid ∈ [–3°C, 40°C].

CONFIG.SURFACE 100%SURFACE 70%SURFACE 50%
nnrefdTSWCOPLCOEnnrefdTSWCOPLCOEnnrefdTSWCOPLCOE
%m°C%ref%m°C%ref%m°C%ref
500 kW, 0% HL7012.283.8092.37010.283.7992.3808.083.8099.9
500 kW, 20% HL8011.2114.7493.5809.3104.5895.6907.4114.7799.9
1000 kW, 0% HL8011.2114.4790.87010.083.8190.8807.983.8197.8
1000 kW, 20% HL8011.2114.7693.0809.3104.5995.1807.984.13100.8
2000 kW, 0% HL7012.083.8291.17010.083.8291.1807.983.8298.3
2000 kW, 20% HL8011.2104.6095.4809.484.14101.1807.984.15101.1

[i] n/nref: borehole count vs. reference; d: borehole spacing; Tsw: switching temperature; COP: global system COP (heating + cooling); LCOE: relative to reference geothermal installation (100% = same cost). HL: cooling-to-heating load ratio.

Table 5

Optimal hybrid configurations—Langres. Same conventions as Table 4.

CONFIG.SURFACE 100%SURFACE 70%SURFACE 50%
nnrefdTSWCOPLCOEnnrefdTSWCOPLCOEnnrefdTSWCOPLCOE
%m°C%ref%m°C%ref%m°C%ref
500 kW, 0% HL7011.963.4685.27010.043.1389.2807.943.1396.3
500 kW, 20% HL7011.963.8588.27010.043.5192.8807.963.8794.3
1000 kW, 0% HL7012.063.4685.77010.043.1489.5807.943.1496.8
1000 kW, 20% HL7012.063.8688.87010.043.5493.2807.943.55100.1
2000 kW, 0% HL7012.073.6483.57010.043.1788.6807.943.1796.4
2000 kW, 20% HL7012.073.9285.07010.063.7786.6807.963.7794.1
Figure 3

Effect of GSHP rated extraction intensity on 10-year average energy yield and geothermal coverage (Montpellier, 1,000 kW, 60% cooling ratio, 20 boreholes at 200 m).

Figure 4

Annual performance degradation of the base-load hybrid system (Langres, 1,000 kW, heating only, 20 boreholes at 200 m). Top: energy yield (bars) and geothermal heat share (line). Bottom: mean borefield temperature.

Table 6

Base-load hybrid system performance (10-year average, 1,000 kW, 20 boreholes at 200 m). The ref row gives the GSHP-only reference for direct comparison. HL: cooling-to-heating load ratio; d: borehole spacing; yield: energy delivered per metre of borehole per year; fh, fc: geothermal heating and cooling coverage.

CONFIGURATIONd(m)YIELD kWh/m/yrCOP syst.fh(%)fc (%)LCOE EUR/MWh
Montpellier (GSHP 80 W/m = 320 kW)
0% HL, ref10424.84100–352
0% HL, hybrid121493.6554–208
0% HL, hybrid81203.5144–210
20% HL, ref10614.93100100281
20% HL, hybrid122073.946171180
20% HL, hybrid81883.865471181
60% HL, ref10925.02100100233
60% hybrid122894.207058147
60% HL, hybrid82864.196860147
Langres (GSHP 200 kW)
0% HL, ref10374.11100–364
0% HL, hybrid121282.8132–176
0% HL, hybrid8932.7223–178
20% HL, ref10584.32100100279
20% HL, hybrid122193.214261151
20% HL, hybrid81953.153661152
Language: English
Page range: 53 - 53
Submitted on: Mar 19, 2026
Accepted on: May 8, 2026
Published on: Aug 31, 2026
Published by: European Council for an Energy Efficient Economy (eceee)
In partnership with: Paradigm Publishing Services

© 2026 Hugo Marchand, Chloé Duchayne, published by European Council for an Energy Efficient Economy (eceee)
This work is licensed under the Creative Commons Attribution 4.0 License.