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Table 3 Comparison of measured and modelled specific surface heat flow

From: Influence of depth, temperature, and structure of a crustal heat source on the geothermal reservoirs of Tuscany: numerical modelling and sensitivity study

Location ID Measurement
[mW/m2]
Simulation
[mW/m2]
Difference
[mW/m2]
1 224 265 −41
2 205 297 −92
3 248 247 1
4 111 237 −126
5 250 188 62
6 116 182 −66
7 270 200 70
  1. Locations 1–3 are from boreholes east of the major fault (i.e. Boreholes 1–3), while Locations 4–7 are shallow well measurements from the western part of the study area (see Fig. 9)
  2. Average error (root mean square): 75