Ground Source Heat Pump & Geothermal Borehole Calculator

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Size closed-loop vertical geothermal boreholes according to ASHRAE / IGSHPA design methods. Calculate peak thermal loads, net ground extraction and rejection, required total borehole depth, and long-term ground thermal balance.

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Ground Source Heat Pump & Geothermal Borehole Calculator: Free Ground Source Heat Pump & Geothermal Borehole Calculator tool: calculate ground source heat pump (GSHP) vertical geothermal borehole length, ground.

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Building Loads & Heat Pump Performance

Ground Formation & Borehole Specifications

Borehole Sizing & Thermal Exchange

Total Borehole Depth L
488 m
Depth per Borehole
122 m / bore
Ground Heat Extraction (H)
21.3 kW
Ground Heat Rejection (C)
26.6 kW
Governing Design Mode
Cooling Governed
Specific Heat Exchange
54.5 W/m

1. The Thermodynamics of Ground Source Heat Pumps (GSHP)

Ground Source Heat Pumps (geothermal heat pumps) leverage the high thermal inertia of the earth's shallow subsurface as an efficient heat source and sink. While ambient outdoor air temperatures fluctuate wildly from -20°C in winter to +40°C in summer, the undisturbed ground temperature at depths beyond 6 meters remains virtually constant year-round, closely matching the local mean annual air temperature (typically 8°C to 16°C across temperate zones).

2. Fundamental Thermodynamic Heat Balance

The ground heat exchanger does not experience the building's thermal load directly; rather, compressor mechanical work modifies the net thermal flux transferred into or out of the subsurface loop:

A. Heating Mode (Heat Extraction)

W_comp = q_heating / COP_h
q_ground_extract = q_heating - W_comp = q_heating × (1 - 1 / COP_h)

Because electrical power consumed by the compressor generates useful heat delivered to the building interior, the ground needs to supply only a fraction $(1 - 1/COP_h)$ of the total heating load. For a heat pump with $COP_h = 4.0$, exactly 75% of heating comes from the ground and 25% from electricity.

B. Cooling Mode (Heat Rejection)

W_comp = q_cooling / COP_c
q_ground_reject = q_cooling + W_comp = q_cooling × (1 + 1 / COP_c)

In cooling mode, both the building heat and the compressor motor waste heat must be dumped into the borehole loop, making ground rejection substantially larger than building cooling tonnage.

3. ASHRAE Borehole Heat Exchanger Sizing Equation

The total required borehole depth $L$ is calculated using the established ASHRAE cylindrical heat source formulation:

L_h = (q_net_h × (R_b + R_g_short) + q_annual_h × R_g_annual) / (T_g - T_ewt_min)
L_c = (q_net_c × (R_b + R_g_short) + q_annual_c × R_g_annual) / (T_ewt_max - T_g)

Where:

  • $R_b$: Effective borehole thermal resistance ($ ext{m}cdot ext{K/W}$), governed by grout thermal conductivity $k_g$, pipe diameter, and shank spacing.
  • $R_g$: Thermal resistance of the surrounding ground formation based on line-source theory $R_g approx rac{1}{2pi k_s} ln(4alpha t / r_b^2)$.
  • $T_g$: Undisturbed ground temperature (°C).
  • $T_{ewt}$: Entering Water Temperature design bounds (typically $0^circ ext{C}$ minimum in heating with antifreeze, $35^circ ext{C}$ maximum in cooling).

The overall installation depth must equal the maximum of the heating and cooling lengths: $L_{total} = max(L_h, L_c)$.

4. Subsurface Lithology Thermal Properties

Geological Formation Thermal Conductivity $k_s$ Thermal Diffusivity $alpha_s$ Specific Heat Extraction
Granite / Basalt 2.8 – 3.5 W/m·K 1.2 – 1.4 × 10⁻⁶ m²/s 55 – 70 W/m
Limestone / Dolomite 2.3 – 2.8 W/m·K 1.0 – 1.2 × 10⁻⁶ m²/s 45 – 60 W/m
Sandstone 1.9 – 2.4 W/m·K 0.9 – 1.1 × 10⁻⁶ m²/s 40 – 50 W/m
Wet Saturated Clay / Silt 1.4 – 1.8 W/m·K 0.5 – 0.7 × 10⁻⁶ m²/s 30 – 40 W/m
Dry Soil / Uncompacted Sand 0.4 – 0.9 W/m·K 0.2 – 0.4 × 10⁻⁶ m²/s 15 – 25 W/m

5. Long-Term Thermal Ground Imbalance & Auxiliary Hybrid Systems

In commercial office buildings, high internal heat gains from occupants, computers, and solar radiation create a pronounced annual thermal imbalance: annual cooling heat rejected to the ground often exceeds winter heating extraction by a factor of 2:1 to 4:1. Over 20 to 30 years of continuous operation, this thermal accumulation causes the undisturbed ground formation temperature to gradually climb by $0.5^circtext{C}$ to $1.5^circtext{C}$ per decade.

As ground temperature rises, summer cooling COP degrades and peak entering water temperatures ($EWT$) can exceed heat pump operational limits. To prevent runaway thermal drift, geothermal engineers design Hybrid Ground Source Heat Pump (HGSHP) systems:

  • Cooling-Dominated Climates: A supplemental fluid cooler, evaporative cooling tower, or night-sky radiation panel is integrated to reject excess peak summer heat to the atmosphere, allowing the borehole field to be sized for the lower heating load (reducing drilling CapEx by up to $40%$).
  • Heating-Dominated Climates: Solar thermal collectors or photovoltaic-thermal (PVT) hybrid panels recharge the borehole field during summer and shoulder months, injecting low-grade solar heat into the ground to maintain undisturbed thermal equilibrium.

6. Step-by-Step Worked Commercial Borehole Sizing Example

Consider an educational campus building with the following heating and cooling design specifications:

  • Peak heating load: $q_h = 75text{ kW}$, heat pump $COP_h = 4.0$
  • Peak cooling load: $q_c = 110text{ kW}$, heat pump $COP_c = 5.0$
  • Local undisturbed bedrock temperature: $T_g = 12.0^circtext{C}$
  • Lithology: Saturated limestone formation ($k_s = 2.4text{ W/m}cdottext{K}$)
  • Thermally enhanced bentonite grout ($k_g = 1.6text{ W/m}cdottext{K}$)
  • Design EWT limits: $T_{ewt,min} = 1.0^circtext{C}$ in winter; $T_{ewt,max} = 32.0^circtext{C}$ in summer

Step 1: Calculate Net Ground Heat Extraction and Rejection:

Heating Extraction: q_ground_h = 75 × (1 - 1 / 4.0) = 75 × 0.75 = 56.25 kW
Cooling Rejection: q_ground_c = 110 × (1 + 1 / 5.0) = 110 × 1.20 = 132.0 kW

Step 2: Determine Specific Heat Transfer Capacity per Meter:
For limestone with thermally enhanced grout, typical specific exchange rates under design $Delta T$ are:

ΔT_heat = 12.0 - 1.0 = 11.0 K ==> q_spec_h ≈ 48.0 W/m
ΔT_cool = 32.0 - 12.0 = 20.0 K ==> q_spec_c ≈ 62.0 W/m

Step 3: Calculate Required Borehole Field Lengths:

L_heating = (56,250 W) / (48.0 W/m) = 1,172 meters
L_cooling = (132,000 W) / (62.0 W/m) = 2,129 meters

Cooling governs the installation design: total borehole depth required is $L_{total} = 2,129text{ meters}$.

Step 4: Layout Borehole Array Configuration:
Selecting 16 boreholes arranged in a $4 times 4$ grid:

Depth per borehole = 2,129 m / 16 bores = 133.1 meters / borehole (approx. 436 feet)

Spacing between boreholes is set to $6.0text{ meters}$ to mitigate inter-borehole thermal interference over multi-year cycles.

7. Environmental Protection & Antifreeze Selection

Because closed-loop borehole heat exchangers penetrate shallow potable aquifers, environmental regulations (such as EPA Underground Injection Control and VDI 4640) impose rigorous material standards:

  • Circulation Fluid Safety: In cold climates where loop temperatures drop below $0^circtext{C}$, non-toxic USP-grade Propylene Glycol (typically $20%$ to $25%$ by volume with corrosion inhibitors) or bio-ethanol is mandatory. Toxic ethylene glycol is strictly prohibited to safeguard groundwater.
  • Pressure Testing & Grouting Integrity: Loop piping must be fabricated from high-density polyethylene (HDPE 100 or PE 4710) rated to SDR 11. Full-depth bottom-to-top pressure tremie grouting seals the borehole annulus, preventing surface contaminants from migrating into deep groundwater aquifers.

Frequently Asked Questions

A GSHP harnesses the relatively stable year-round temperature of the earth (typically 10-16 deg C). In winter, it extracts heat from the ground to heat the building. In summer, it reverses operation, extracting heat from the building and rejecting it into the cooler earth.

In cooling mode, the ground heat exchanger must absorb both the heat removed from the building and the compressor electrical work: q_rejected = q_cooling * (1 + 1 / COP_c). In heating mode, compressor power contributes to heating, reducing ground extraction: q_extracted = q_heating * (1 - 1 / COP_h).

Commercial vertical boreholes typically range between 80 and 180 meters (250 to 600 feet) in depth, spaced 5 to 7 meters apart to prevent long-term thermal overlap.

In cooling-dominated or heating-dominated climates with unequal annual thermal loads, more heat is rejected into or extracted from the ground over decades than can naturally dissipate, causing the undisturbed ground temperature to drift and degrading heat pump COP over time.