Figure 1
![Schematic of the UCG process (linked vertical wells method), with water entering from the surrounding rocks [6].](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/6473793b4e662f30ba53f835/j_sgem-2021-0004_fig_001.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20251105%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20251105T123905Z&X-Amz-Expires=3600&X-Amz-Signature=433c806066c50b18329a5949fd105086612e085fd4ec5f64af8b979f288ed04e&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
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Material parameter values of individual geological layers_
| Layer | Roof min [m] | Roof max [m] | f [−] | N [Pa] | A [Pa] | α [−] | ρs [Mg/m3] | K [m/s] | cv [J/kg/K] | λ [W/m/K] |
|---|---|---|---|---|---|---|---|---|---|---|
| Sandstone | 4.7 | 10.9 | 0.15 | 2.31E+09 | 3.46E+09 | 1.16E-05 | 2.6 | 5.00E-07 | 1100 | 3.1 |
| Clayey pebble | 25.2 | 32.7 | 0.28 | 3.90E+06 | 2.40E+07 | 6.00E-06 | 2.53 | 3.00E-06 | 639 | 2.5 |
| Clay | 50 | 50 | 0.31 | 1.32E+07 | 6.91E+07 | 5.80E-06 | 2.38 | 3.00E-08 | 566 | 2.1 |
| Coal* | 53 | 53 | 0.2 | 5.80E+08 | 8.70E+08 | 5.00E-06 | 1.21 | 5.00E-09 | 1250 | 0.5 |
| Clay | 57.2 | 69.8 | 0.4 | 1.28E+06 | 9.42E+06 | 5.90E-06 | 2.62 | 6.00E-08 | 481 | 2.9 |
| Clayey sand | 80.5 | 95 | 0.32 | 1.30E+06 | 9.00E+06 | 6.00E-06 | 2.49 | 1.20E-06 | 889 | 3.5 |
| Clay | 125.9 | 149.9 | 0.37 | 2.50E+06 | 1.85E+07 | 6.10E-06 | 2.71 | 7.00E-08 | 514 | 1.4 |
| Silty clay | 166.1 | 184 | 0.28 | 3.30E+06 | 1.50E+07 | 6.00E-06 | 2.66 | 5.00E-08 | 612 | 1.9 |
Thermal parameters of individual pore fluids and medium_
| Thermal expansion coefficient 1) [1/K] | Initial heat transfer coefficient [W/m/K] | specific heat [J/kg/K] | |
|---|---|---|---|
| Water | 69·10−6 | 0.6 | 4150 |
| Water vapour | 1/T | 16.2·10−3 | 1970 |
| Medium | - | λ = (1 − f) λs + fλf | cν = (ρ1 cνs + ρ2 cνf) / ρ |