Page 42 - Geothermal Energy Renewable Energy and The Environment
P. 42

Sources of Geothermal Heat: Earth as a Heat Engine                           25


                 –30         –15       0        15       30         45           Heat flow
                                                                                      2
                                                                                 (mW/m )
                              Iceland                                               > 150
                       IS
                                                                                    80 – 150
                                                                                    50 – 80
                                                                                    30 – 50
                                                         FI
                                                                                    < 30
                        60
                                          NO                        RU
                                                SE
                                                         EE
                                                          LV
                                Soultz-sous-  DK
                                  forets                 LT
                       IE
                             GB                             BY
                                     NL
                                    BE              PL
                                          DE
                                       LU
                                                CZ                UA
                                                    SK
              45                                                MD
                                FR    CH       AT   HU
                                               SI          RO
                                                 HR
                                          IT
                                                   BA
                                                       YU
                                                            BG
                                                        MK
               PT      ES                             AL
                                                        GR            TR
                                          Larderello
                                                             Aydin
                                                                  Denizli

            FIGUre 2.8  (See color insert following page 17.0..) Heat flow map of Europe. (Modified from the European
            Community Nr. 17811.)

              The map of heat flow in Europe (Figure 2.8) presents the same range of heat flow values as seen
            within the United States. However, Europe’s geological history over the last 50 million years is
            complex, making it difficult to interpret heat flow in terms of plate tectonics processes. The stand-
            out exception to this is, of course, Iceland, which is a hotspot that sits directly atop the Mid-Atlantic
            spreading system. Noted in Figure 2.8 are some of the current sites where geothermal power is
            being generated or actively pursued. Note that they occur in close proximity to areas with high
            surface heat flow.
              It is important to point out that geothermal resources are more widespread than that which is
            useful for power production. As we will discuss in Chapters 10 and 11, so-called direct use applica-
            tions, in which warm geothermal waters are used for heating and a variety of other applications, and
            the deployment of ground source heat pumps can also be important ways in which to utilize geo-
            thermal energy. In that same analysis undertaken by the International Energy Agency mentioned
            previously (IEA 2006) it was estimated that more than 72 countries employed geothermal energy
            for such applications. The thermal energy utilized was equivalent to more than 273 TJ/yr, which
            is equivalent to 75,940 GWh/yr (Lund, Freeston, and Boyd 2005). Using geothermal energy for
            such applications displaces electrical demand and improves energy efficiency. Although not always
            included in discussions of geothermal energy, such applications can have a very significant impact
            on global energy use and the sources employed for energy generation.
   37   38   39   40   41   42   43   44   45   46   47