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Table 1 Proposed assessment criteria for suitability categorization of shallow geothermal development by vertical closed-loop GSHP in fracture developed regions (depth < 200 m)

From: Investigation and evaluation methods of shallow geothermal energy considering the influences of fracture water flow

Categorization

Thermophysical properties of energy storage rock mass

Aquifer properties

Energy flow in fracture water

Note

Overall heat capacity, Cr, kJ/(kg ℃)

Overall heat conductivity, λr, W/m K

Thickness, H, m

Volumetric water flow rate, qmax, 10L/s

Water flow velocity, um/s

Departure from rock temperature, ΔT

Optimum

 > 1 (DZ/T 225-2009 2009)

> 1.5 (DZ/T 225-2009 2009)

> 30 (DB37/T 4308-2021 2021; DZ/T 225-2009 2009)

 > 10 (very abundant)

 > 1000 (Jiang et al. 2018)

 > 10(Cheng et al. 2018)

Meeting all 6 requirements

Suitable

0.5–1 (DZ/T 225-2009 2009)

0.9–1.5 (DZ/T 225-2009 2009)

10–30 (DB37/T 4308-2021 2021; DZ/T 225-2009 2009)

1–10 (abundant)

400–1000 (Jiang et al. 2018)

5–10 (Cheng et al. 2018)

Except optimum and unsuitable indexes

Unsuitable

 < 0.5 kJ (DZ/T 225-2009 2009)

 < 0.9 (DZ/T 225-2009 2009)

 < 10 (DB37/T 4308-2021 2021; DZ/T 225-2009 2009)

0.1–1 (unabundant)

 < 400 (Jiang et al. 2018)

 < 5 (Cheng et al. 2018)

Meeting at least 4 requirements