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1.3 Conceptual Models of Geothermal Reservoirs  31

                                                                                    Geodynamic
                                                                                     context

                                   Low permeability,                   Shallow
                                  shallow formations  Near surface systems, heat
                                                       pumps           aquifers
                             100 °C                                            1 km 2 km 3 km

                                     Low permeability,  Heat, electricity?  Hydrothermal
                                                                                      °C/100 m
                                     deep formations              reservoirs
                           Temperature  300 °C  Hot dry  Heat, electricity, hydrogen  3 km 6 km 9 km
                                                     Enhanced
                                                                                      5
                                                    geothermal
                                                     systems
                                        rocks
                                                                                 °C/100 m  °C/100 m


                                                       Supercritical reservoirs
                                                                                 10      2.5
                                                        Electricity, hydrogen
                             500 °C                                            5 km 10 km15 km
                                            100 kg s −1    200 kg s −1  300 kg s −1  Depth and gradients
                                                        Water/vapor

                         Figure 1.17  Sketch section showing the variety of reservoirs
                         that can be used for heat extraction and the different uses
                         of the geothermal energy.

                         of the following four independent parameters: heat, fluid flow, permeability, and
                         appropriate orientation of the stress field in relation to the permeability network.
                         Among these parameters, only fluid flow and permeability can be enhanced
                         by engineering. These parameters are summarized in one sketch section that
                         illustrates the variety of reservoirs that can be used for heat extraction and the
                         various uses of the geothermal energy (Figure 1.17).
                           Following chapters will analyze the different processes of stimulation that
                         can be applied for achieving such improvement. Lessons learned from the
                         Soultz EGS experiment, the sustainable development of the Larderello field
                         in Italy, and the Icelandic geothermal power network, among other case his-
                         tories, show that the concept of geothermal reservoir must not be too re-
                         stricted. Experiences of stimulation can be realized by extending active geothermal
                         fields and the development of binary plants makes possible the exploitation
                                                                              ◦
                         of geothermal reservoirs with minimum temperatures of 85–100 Cfor power
                         generation.
                           A reservoir is also defined by its economic viability. Many other parameters such
                         as the price of the steel involved in drilling, cost of drilling depending on the
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