Geothermal Engineering: Fundamentals & Synergies With
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Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering Prof. Dr. Gioia Falcone Institute of Petroleum Engineering Dept. of Geothermal Engineering & Integrated Energy Systems Geneva, 25th April 2013 Outline • Geothermal within the energy arena • Fundamentals of geothermal energy • Types of geothermal resources • Uses of geothermal energy • Oil & gas expertise for geothermal exploitation • Conclusions Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 2 Fuel Shares of World Total Primary Energy Supply (2010) (IEA 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 3 World Electricity Generation (TWh) from Non-Hydropower Renewables by 2030 Concentrating Solar Power Photovoltaic (ESMAP, 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 4 Cost-Competitiveness of Renewables Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 5 Constant Base Load Production from Geothermal vs. Other Energy Sources (ESMAP, 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 6 2010 World* CO2 Emissions** by Fuel (IEA, 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 7 US CO2 Emissions by Primary Energy Source (ESMAP, 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 8 Outline • Geothermal within the energy arena • Fundamentals of geothermal energy • Types of geothermal resources • Uses of geothermal energy • Oil & gas expertise for geothermal exploitation • Conclusions Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 9 The Earth’s Heat -1 (Gupta & Roy, 2007 ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 10 The Earth’s Heat -2 Total heat flow observed on the Earth’s surface (& T distribution within it) is due to: ● Release of heat due to the cooling of the Earth ● Heat produced by radioactivity (amount of radioactive elements present in rocks releases enough heat to account for ~60% of total heat flow for continental crust) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 11 The Earth’s Heat -3 ● Earth’s cooling process is very slow ● Temperature of mantle has decreased by 300-350°C in 3 billion years, remaining at ~4000°C at its base ● 99% of Earth is hotter than 10000C ● 99% of the 1% is hotter than 1000C (Geothermal Education Office) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 12 Proof of temperature at depth… Direct measurements of T in the Earth’s interior currently limited to a depth of 12.261 km in the Kola super-deep borehole SG-3 (northwest of Russia), with BHT of 180oC. Another reliable measurement of T at great depth is in the 9.101-km deep KTB borehole in Oberpfalz, Germany, with BHT of 265oC. Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 13 Plate Boundaries & Geothermal Spots (Geothermal Education Office ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 14 Plate Tectonics (Geothermal Education Office ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 15 Geothermal Systems Convection & conduction (Dickson & Fanelli, 2004 ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 16 Essential Requirements for a Geothermal System to Exist (1) a large source of heat (2) a reservoir to accumulate heat (3) a barrier to hold the accumulated heat Analogy with petroleum systems (after Gupta & Roy, 2007 ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 17 Outline • Geothermal within the energy arena • Fundamentals of geothermal energy • Types of geothermal resources • Uses of geothermal energy • Oil & gas expertise for geothermal exploitation • Conclusions Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 18 Types of Geothermal Systems . Vapour-dominated . Hot water . Geo-pressured . Magma . Hot Dry rock (HDR) & Enhanced Geothermal Systems (EGS) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 19 Vapour-Dominated Most exploited fields contain water at high P & T>100 oC. When this water is brought to surface, P is reduced and a mixture of saturated steam & water is generated. There are only few geothermal fields producing superheated steam with no associated fluids (dry steam fields). (Gupta & Roy, 2007 ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 20 Hot Water Differ from vapour-dominated fields in that they are characterised by liquid water being the continuous fluid phase. Typically, 60 oC<T<100 oC at depths of 1500 to 3000 m. (Gupta & Roy, 2007 ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 21 Geo-pressured Typically form in a basin in which very rapid filling with sediments takes place, resulting in higher than normal pressure of the hydrothermal water. Often saturated with methane. First identified in the deep sedimentary layers underneath the Gulf of Mexico. Wells flow pressurised to the surface. Water T is 90-200°C. (Gupta & Roy, 2007 ; Texas Renewable Energy Resource Assessment, 2009) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 22 Magma Magma is the ultimate source of all high-temperature geothermal resources. Typically, magma crystallizes to form igneous rocks at temperatures varying from 600 to 1400 oC. Magma has been encountered in situ 3 times during drilling projects—twice in Iceland, and once in Hawaii. However, up to now, the necessary technology has not been developed to recover heat energy from magma. (Gupta & Roy, 2007 ) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 23 Hot Dry Rock (HDR) Hydrothermal resources restricted to countries with favourable geological conditions (i.e. plate boundaries). HDR resources exist where the heat is stored in hot & poorly permeable rocks at shallow depths within the Earth’s crust, without fluid availability to store or transport the heat. HDR is the new frontier of geothermal energy and possibly the area closest to petroleum exploitation Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 24 HDR Concept C 0 Depth, m Depth, Temperature, Temperature, (MIT, 2006) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 25 From HDR to „Deep Geothermal“ • Hot Dry Rock concept first implemented at Fenton Hill in 1977 • Heat stored in deep seated, conductive/radiogenic dominated, tight sediments & hard crystalline basement rocks. • Volcanic, metamorphic, magmatic or sedimentary settings. • Dry / not dry • W-w/o pre-existing fractures or fissures • Also known as: . Hot Fractured Rock . Hot Wet Rock . Enhanced (or Engineered) Geothermal System (EGS) . Deep Heat Mining . Deep Earth Geothermal Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 26 Why Deep? (Breede et al., 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 27 Outline • Geothermal within the energy arena • Fundamentals of geothermal energy • Types of geothermal resources • Uses of geothermal energy • Oil & gas expertise for geothermal exploitation • Conclusions Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 28 Geothermal Energy Uses 1. Direct Use & District Heating Systems 2. Geothermal Heat Pumps 3. Electricity Generation Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 29 Geothermal Energy Use vs. Field T (*) The above are indicative T value only! As technology advances, the T cut-off point changes. (after ESMAP, 2012) Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies with Petroleum Engineering 30 Direct Use & District Heating Geothermal Education Office Prof. Dr. G. Falcone Institute of Petroleum Engineering Geothermal Engineering: Fundamentals & Synergies