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Use of Geothermal Resources: Environmental Considerations                   241




                                  N
                                                         0

                                              –60
                                       –20                –80     0
                                                  –40
                                           –40

                                            –20



                                               0     –40      –20
                                                                   0
                                                       –60
                                                        –20
                                   2 km
                                                 Taupo

                                                           0
                                       Lake taupo


            FIGUre 12.8  Contours of the subsidence rates (in mm/yr) in the vicinity of Taupo, New Zealand. The loca-
            tions of wells for geothermal power generation are shown by the partially filled circles. At each of these sites
            there usually are multiple wells. (From Allis, R., Bromley, C., and Currie, S., Geothermics, 38:169–80, 2009.)

            such instances, if permanent radar scatterers can be identified that are independent of the vegetative
            effects. This method is described by Eneva et al. (2009) and they employ it to map the subsidence
            rate in a portion of the Salton Sea area.
              Ground subsidence generally has little impact in geothermal regions, particularly if reinjection
            of the produced mass is employed. However, remote sensing techniques such as satellite interferom-
            etry may provide the means to rapidly assess if subsidence problems are developing and how best
            to mitigate them.

            waTer Use

            As noted in Chapter 9, a significant quantity of water is required to achieve the energy production
            rates necessary to efficiently extract energy from a geothermal fluid. The flow path followed by a
            geothermal fluid at a generating site generally involves the following sequence of stages:

              •   High pressure mixed steam and liquid flow from the wellhead to the separator.
              •   High pressure steam is separated from condensed liquid and piped to the turbine.
              •   Steam  expands  into  the  turbine,  dropping  in  pressure  and  temperature  with  some
                 condensation.
              •   Condensate is separated from steam as steam flows through multiple turbine stages.
              •   Steam exits the turbine through the turbine exhaust and is condensed in the condenser.
              •   Condensed water from the condenser is cooled in the cooling tower.

              Cooling towers spray water into flowing air to result in evaporative cooling. Throughout this
            process about 60–80% of the original steam that enters the turbine ends up evaporating to the atmo-
            sphere. The remaining fluid is collected and reinjected.
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