<<

Geothermal Applications GthlCliGeothermal Cooling

Dr. Horst Kreuter, CEO

Renewable Energy Training Programm, 10 July 2012, ESMAP – IFC, Washington DC, USA Outline

1 Cooling Demand: Worldwide, Energy, Costs 2 Principles of Cooling Technology 3 District Cooling 4 Geology and Geothermal for Cooling Purposes 5 Geoth erm al Coolin g an d Di stri ct Coolin g 6 Geothermal Cooling – Example from Qatar 7 Conclusion

Page ƒ 2 Cooling Demand USA 2010

ƒ Residential cooling energy consumption: 315 billion kWh ƒ Commercial cooling energy consumption: 164 billion kWh ƒ Together 12 % of total U.S. electricity consumption ƒ 9.2 Cent / kWh

164 bil kWh 316 bil kWh

Other Electricity Usage

Electricity Use for 3265 bil kWh Residential Cooling

Electricity Use for Commercial Cooling

U. S. Elect ri cit y C onsumpti on 2010

Page ƒ 3 Cooling Demand USA Projection

ƒ EIA projection to 2035 Residential Cooling Demand

Page ƒ 4 Cooling Demand USA Projection

ƒ EIA projection to 2035 Commercial Cooling Demand

Page ƒ 5 Cooling Demand Europe Projection

ƒ Increasing electricity demand in Europe for cooling

modified after Aebischer et al. (2007) Page ƒ 6 Existing Cooling Technologies

ƒ Air-cooled ƒ Water-cooled chillers ƒ Evaporative-cooled chillers ƒ Dry fluid coolers

ƒ Cost extensive CliCooling energy ƒ CO2 emissions mostly produced ƒ Negative environmental by fossil fuels itimpact

Page ƒ 7 Principles of Cooling Technology

ƒ Functional principle based on the evaporation cycle of a binary system: • Evaporation of cooling agent • bound in vaporous high pressure to a sorption agent or soltlvent • Sorption agent is replenished to evaporation process after thermal expulsion • Transfer of cooling energy to end consumer via pipeline network

ƒ Absorption : evaporation cycle NH3/water or water/Li-Br ƒ Adsorption chiller: evaporaton cycle solid agent, e.g. Si-gel/water

Page ƒ 8 Scheme of cooling processes

Page ƒ 9 Physical cooling effect of refrigerant evaporation

Compression Chiller Type Energy Source Coolinggg Agent Type Compression Mechanical Electric power Halons, clorinated Compression CHC, clor free hdhydrocar bons Adsorption Thermal Heat energy Li-Br/water or absorption loop t=85°C – 150°C ammonia/water as absorption agent Absorption Thermal Heat energy Water with solid as adsorption of t=55°C – 95°C adsorppgtion agent water steam (e.g.silica-gel)

Page ƒ 10 Absorption chiller – Advantages

ƒ NH3/water → Tin -60 °C

ƒ Water/Li-Br → Tin +5 °C ƒ Noise reduced ƒ Cost-effective ƒ Reliable in power supply ƒ Energy efficient ƒ Can easily be operated bthlby geothermal energy

Source: www.de.wikipedia.org Page ƒ 11 Absorption chiller – Operating mode

ƒ Driven by hot water with broad temperature range ƒ Zero ozone depletion potential ƒ No halons, no oil changes ƒ Low power consumption ƒ Noice-reduced ƒ Stable cooling supply Source: modified after www.de.wikipedia.org ƒ Easy in maintenance ƒ Fluct uati ons are avoid ed b y use of geoth erma l energy ƒ Use with small localized chillers.

Page ƒ 12 Absorption cooling – Cooling circuit

Modified after http://www.eurocooling.com/public_html/articleseagroup.htm

Page ƒ 13 Geology and Geothermal for Cooling Purposes

Using ground water circulating along natural fault and fracture systems

Page ƒ 14 Principles of Geothermal Production

ƒ Water-bearing sediments with high porosity and permeability, e. g. karstic voids, fractured and jointed carbonates ƒ Water temperatures between 70°C to 120°C required ƒ Desired production rates between 50 l/s and 75 l/s ƒ Two-well system: injection and production well

Page ƒ 15 Geothermal Cooling Cycle

Page ƒ 16 Principles of district cooling

ƒ Cooling production in a central unit driven by primary energy ƒ Distribution to consumer via network of insulated pipelines ƒ Cooling storage system: cooling stored as or ice

PiPrimary energy source Dist ri ct cooli ng Consumer

fuel/oil industrial

natural residential gas commerical

RES: geothermal sports facilities

Page ƒ 17 Principles of District Cooling

ƒ Local resources can be combined to different cooling sources. Cold water may be extracted from • Oceans • Lakes • Rivers • Ground water ƒ Use of surplus heat • Conversion of surplus heat into cooling • Recycling in district networks ƒ High-efficiency chillers necessary ƒ District Coolinggj fulfills the objectives of the EU ener gyyygy policy: sustainability, competitiveness and supply security.

ƒ Principles: http://www.youtube.com/watch?v=smirXWp6KTg

Page ƒ 18 Geothermal District Cooling

ƒ Geothermal meets the temperature requirements of absorption and adsorption technology → cooling efficiency ƒ Evaporation cycle can be driven by thermal water extracted fom deep geothermal energy reservoirs ƒ Heat is transferred on that is coupled with an evaporating cooling unit. ƒ Centralized cooling station supplies district buildings ƒ No fossil fuels will be consumed

ƒ No CO2 emissions from combustion processes → geothermal source

Page ƒ 19 Geothermal Europe

ƒ 212 geothermal district heating installations operating in Europe 2011 ƒ Almost 1 .7 GWth installed capacity

Page ƒ 20 Geothermal District Cooling

Page ƒ 21 Geothermal District Cooling - Motivation

Primary energy source: Primary energy source: Geothermal energy + oil and natural gas efficient technology

District Cooling

cut of CO2 No high CO2 Dependency emissions dependency emissions on oil and on oil/gas gas exports exports X Page ƒ 22 Geothermal Cooling – Example from Qatar

CO2 emissions per capita (2007) among the Middle East countries

Data source: Worldbank (2010)

Page ƒ 23 Geological Setting

ƒ Qatar part of stable Arabian interior platform ƒ Dominated by ~ 10 km thick sedimentary sequences deposited since Paleocene (Alsharan and Nairn,,) 1994) ƒ Predominantly carbonates, evaporites, A bitumen-rich black shales A ‘ ƒ Structure dominated by NNE-SSW trending Qatar South Fars Arch ƒ Thorough oil and gas exploration on- and offshore ƒ MiMain pro duc tion hor izons w ithin Jurassic and Cretaceous sediments

modified after Alsharan and Nairn (1997)

Page ƒ 24 Geological cross-section

ƒ GthlGeothermal gradi ditbtent between 30°C/km to 40°C/km ƒ Aquifers in Jurassic and/or Cretaceous sediments expected ƒ High salinity concentrations expected ƒ Good production rates expected

Page ƒ 25 modified after Alsharan and Nairn (1997) Qatar host of 2022 FIFA World Cup

Chance to take Strengthen Qatar‘s responsibility for climate position in the and environmental discussion on protection sustainable games

Chance to a fundamental change in Qatar‘s energy policy: Switching from fossil fuel to RES. Page ƒ 26 Qatar and Geothermal District Cooling ƒ 63% of Qatar’s domestic energy production is used for domestic district

cooling, totally driven by fossil fuels → high CO2 footprint to residentials ƒ Rising cooling demand requires sustainable source of energy production for Qatar ƒ Operating geothermal energy necessarily requires detailed hydrogeological and geological feasibility studies ƒ Qatar offers a prospective country for installing geothermal energy ƒ Suitable temperature regime is expected in the subsurface

ƒ GfGeothermal saves fossil reserves, improves CO 2 footprint ƒ RES strengthens Qatar’s position in the discussion on climate change among the GCC

Page ƒ 27 Conclusion

ƒ District cooling with natural sources offers environmental saving alternative and preserves fossil resources ƒ Geothermal district cooling uses the geothermal source and transfers heat to a high-efficient chiller ƒ Adequate chilling technology: ad-/absorption chillers

ƒ Less CO2 emissions ƒ Less investments ƒ Less oppgerating costs

Page ƒ 28 Contact

GeoThermal Engineering GmbH Baischstraße 7 76133 Karlsruhe Germany

Phone: +49 721 570 446 80 Fax: +49 721 570 446 89 Email: [email protected] Web: www.geo -tdet.de

Page ƒ 29 Thank you for your attenti on! Dr. Horst Kreuter, CEO

Renewable Energy Training Programm, 10 July 2012, ESMAP – IFC, Washington DC, USA