Skip to main content

Science – Society – Technology

Table 1 Parametrization of the reference model of the DeepStor site based on average reservoir properties of (former) oil fields in URG, particularly the Leopoldshafen field (Stricker et al. 2020; Banks et al. 2021)

From: Risk of surface movements and reservoir deformation for high-temperature aquifer thermal energy storage (HT-ATES)

Parameter

Value

Reservoir permeability (m2)

2.5 × 10–14b

Permeability of the caprock (m2)

10–18 a

Injection/production flow rate (Ls−1)

2a

Effective porosity of the reservoir (–)

0.15b

Effective porosity of the caprock (–)

0.01a

Thermal conductivity of the reservoir (Wm−1 K−1)

2.5b

Thermal conductivity of the caprock (Wm−1 K−1)

1.5b

Volumetric heat capacity of the reservoir (MJm−3 K−1)

3.15c

Volumetric heat capacity of the caprock (MJm−3 K−1)

3.30c

Injection temperature of the cold well (°C)

70a

Injection temperature of the hot well (°C)

140a

Young’s modulus (reservoir and caprock) (GPa)

10d

Poisson’s ratio (–)

0.3d

Fluid thermal conductivity (Wm−1 K−1)

0.6a

Fluid specific heat capacity (Jkg−1 K−1)

4200a

Fluid density (kgm−3)

1000a

Fluid dynamic viscosity (Pas)

4.18 × 10–4a

Well diameter (m)

0.2159a

  1. The data origin is marked with aour assumptions/simplifications, bdata compilation of Stricker et al. (2020), cScheck (1997) and Magri et al. (2005), dadapted from Marschall and Giger (2014) and Jahn et al. (2016), eCoker and Ludwig (2007). The lithologies under- and overlying the reservoir were not individually parameterized; instead a homogeneous parameterization was used