Geothermal Energy 4

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Geothermal Energy 4 ( geothermal-energy-4 )

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Geothermal Energy Chapter 4 has a large influence on the installed cost (Lund and Boyd, 2009). The LCOH reported in Table 4.8 assumed 25 to 30% as the load factor and 20 years as the operational lifetime. It is worth taking into account that actual LCOH are influenced by electricity market prices, as operation of GHPs requires auxiliary power input. In the USA, recent trends in lower natural gas prices have resulted in poor GHP project economics com- pared to alternative options for heat supply, and drilling costs continue to be the largest barrier to GHP deployment. Industrial applications are more difficult to quantify, as they vary widely depending upon the energy requirements and the product to be pro- duced. These plants normally require higher temperatures and often compete with power plant use; however, they do have a high load factor of 0.40 to 0.70, which improves the economics. Industrial applications vary from large food, timber and mineral drying plants (USA and New Zealand) to pulp and paper plants (New Zealand). 4.8 Potentialdeployment19 Geothermal energy can contribute to near- and long-term carbon emis- sions reductions. In 2008, the worldwide geothermal-electric generation was 67.2 TWhe (Sections 4.4.1 and 4.7.3) and the heat generation from geothermal direct uses was 121.7 TWhth (Section 4.4.3). These amounts of energy are equivalent to 0.24 EJ/yr and 0.44 EJ/yr, respectively, for a total of 0.68 EJ/yr (direct equivalent method). The IEA (2010) reports only 0.41 EJ/yr (direct equivalent method) as the total primary energy supply from geothermal resources in 2008 (see Chapter 1); the reason for this dif- ference is unclear. Regardless, geothermal resources provided only about 0.1% of the worldwide primary energy supply in 2008. By 2050, however, geothermal could meet roughly 3% of global electricity demand and 5% of the global demand for heating and cooling, as shown in Section 4.8.2. This section starts by presenting near-term (2015) global and regional deployments expected for geothermal energy (electricity and heat) based on current geothermal-electric projects under construction or planned, observed historic growth rates, as well as the forecast generation of electricity and heat. Subsequently, this section presents the middle- and long-term (2020, 2030, 2050) global and regional deployments, compared to the IPCC AR4 estimate, displays results from scenarios reviewed in Chapter 10 of this report, and discusses their feasibility in terms of technical potential, regional conditions, supply chain aspects, technological-eco- nomic conditions, integration-transmission issues, and environmental and social concerns. Finally, the section presents a short conclusion regarding potential deployment. 19 Complementary perspectives on potential deployment based on a comprehensive assessment of numerous model-based scenarios of the energy system are presented in Chapter 10 and Sections 10.2 and 10.3 of this report. 4.8.1 Near-term forecasts Reliable sources for near-term geothermal power deployment forecasts are the country updates recently presented at the World Geothermal Congress 2010. This congress is held every five years, and experts on geothermal development in several countries are asked to prepare and present a paper on the national status and perspectives. According to projections included in those papers, which are based on the capacity of geothermal-electric projects stated as under construction or planned, the geothermal-electric installed capacity in the world is expected to reach 18.5 GWe by 2015 (Bertani, 2010). This represents an annual average growth of 11.5% between 2010 and 2015, based on the present conditions and expecta- tions of geothermal markets. This annual growth rate is larger than the historic rates observed between 1970 and 2010 (7%, Table 4.4), and reflects increased activity in several countries, as mentioned in Section 4.4. Assuming the countries’ projections of geothermal-electric deployment are fulfilled in the next five years, which is uncertain, the regional deployments by 2015 are shown in Table 4.9. Note that each region has its own growth rate but the average global rate is 11.5%. Practically all the new power plants expected to be on line by 2015 will be conventional (flash and binary) utilizing hydrothermal resources, with a small contribution from EGS projects. The worldwide development of EGS is forecasted to be slow in the near term and then accelerate, as expected technological improve- ments lower risks and costs (see Section 4.6). The country updates did not include projections for geothermal direct uses (heat applications, including GHP). Projecting the historic annual growth rate in the period 1975 to 2010 (Table 4.4) for the following five years results in a global projection of 85.2 GWth of geothermal direct uses by 2015. The expected deployments and thermal genera- tion by region are also presented in Table 4.9. By 2015, total electric generation could reach 121.6 TWh/yr (0.44 EJ/yr) while direct gen- eration of heat, including GHP, could attain 224 TWhth/yr (0.8 EJ/yr). On a regional basis, the forecast deployment for harnessing identi- fied and hidden hydrothermal resources varies significantly in the near term. In Europe, Africa and Central Asia, large deployment is expected in both electric and direct uses of geothermal, while in India and the Middle East, only a growing deployment in direct uses is projected with no electric uses projected over this time frame. The existing installed capacity in North America (USA and Mexico) of 4 GWe, mostly from mature developments, is expected to increase almost 60% by 2015, mainly in the USA (from 3,094 to 5,400 MWe, according to Lund et al. (2010b) and Bertani (2010). In Central America, the future geothermal-electric deployment has been esti- mated at 4 GWe (Lippmann, 2002), of which 12% has been harnessed so far (~0.5 GWe ). South American countries, particularly along the 428

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