Geothermal Energy (5 Activities)
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Enhanced Geothermal System (EGS) Fact Sheet
GEOTHERMAL TECHNOLOGIES OFFICE What is an Enhanced Geothermal System (EGS)? A naturally occurring geothermal system, known as a hydrothermal system, is defined by three key elements: heat, fluid, and permeability at depth. An Enhanced Geothermal System (EGS) is a man-made reservoir, created where there is hot rock but insufficient or little natural permeability or fluid saturation. In an EGS, fluid is injected into the subsurface under carefully controlled conditions, Calpine Corporation credit: Photo which cause pre-existing fractures The Geysers field in northern California boasts the largest geothermal complex in the world and the first successful demonstration of EGS technologies in the United States. to re-open, creating permeability. EGS Resource Potential Increased permeability allows fluid to circulate throughout EGS offers the opportunity to access an enormous, domestic, clean energy the now-fractured rock and resource. A 2006 Massachusetts Institute of Technology (MIT) study to transport heat to the predicted that in the United States alone, 100 GWe of cost-competitive 1 surface where electricity capacity could be provided by EGS in the next 50 years. To take advantage of this vast resource, the U.S. Department of Energy’s (DOE) Geothermal can be generated. While Technologies Office (GTO) promotes and invests in industry, academia, and advanced EGS technologies the national laboratories to develop and demonstrate EGS throughout the are young and still under United States. development, EGS has been successfully realized on a pilot scale in Europe and now at two Benefits of Enhanced Geothermal Systems DOE-funded demonstration • EGS has the potential to be an important contributor to the U.S. -
Microgeneration Potential in New Zealand
Prepared for Parliamentary Commissioner for the Environment Microgeneration Potential in New Zealand A Study of Small-scale Energy Generation Potential by East Harbour Management Services ISBN: 1-877274-33-X May 2006 Microgeneration Potential in New Zealand East Harbour Executive summary The study of the New Zealand’s potential for micro electricity generation technologies (defined as local generation for local use) in the period up to 2035 shows that a total of approximately 580GWh per annum is possible within current Government policies. If electricity demand modifiers (solar water heating, passive solar design, and energy efficiency) are included, there is approximately an additional 15,800GWh per annum available. In total, around 16,400GWh of electricity can be either generated on-site, or avoided by adopting microgeneration of energy services. The study has considered every technology that the authors are aware of. However, sifting the technologies reduced the list to those most likely to be adopted to a measurable scale during the period of the study. The definition of micro electricity generation technologies includes • those that generate electricity to meet local on-site energy services, and • those that convert energy resources directly into local energy services, such as the supply of hot water or space heating, without the intermediate need for electricity. The study has considered the potential uptake of each technology within each of the periods to 2010, 2020, and 2035. It also covers residential energy services and those services for small- to medium-sized enterprises (SMEs) that can be obtained by on-site generation of electricity or substitution of electricity. -
Sustainability Guidelines for Geothermal Development
REPORT DECEMBER Sustainability Guidelines for 2013 Geothermal Development Sustainability Guidelines for Geothermal Development WWF Indonesia 2013 Sustainability Guidelines for Geothermal Development ISBN 978-979-1461-35-1 @2013 Published by WWF-Indonesia Supported by British Embassy Jakarta Coordinator Program Indra Sari Wardhani Writer : Robi Royana Technical Editor : Indra Sari Wardhani Technical Contributor : Hadi Alikodra, WWF-Indonesia Budi Wardhana, WWF-Indonesia Nyoman Iswarayoga, WWF-Indonesia Anwar Purwoto, WWF-Indonesia Indra Sari Wardhani, WWF-Indonesia Retno Setiyaningrum, WWF-Indonesia Arif Budiman, WWF-Indonesia Thomas Barano, WWF-Indonesia Zulra Warta, WWF-Indonesia Layout and Design Arief Darmawan WWF Indonesia Graha Simatupang Tower 2 Unit C LetJen TB Simatupang Kav 38 , South Jakarta, 12540 Indonesia Phone: +62-21-782 9461 Fax : +62-21-782 9462 Foreword Energy has become one of the benchmarks of the development of a country and even become a political economic power including Indonesia. Along with the growth of population and economy, it is undeniable that the energy needs of Indonesia also continues to increase rapidly. Most of the source of this energy needs are from non-renewable/ fossil energy such as petroleum, natural gas and coal, and the utilization of it will produce greenhouse gas emissions (GHG) that contribute to global warming and climate change. To improve national energy security in the long term and contribute to global efforts to put a half to climate change, energy conservation and energy diversication through the development of sustainable renewable energy is a necessity. WWF's vision in the energy sector is to encourage the achievement of 100% Renewable Energy in 2050 globally. -
HEAT and TEMPERATURE Heat Is a Type of ENERGY. When Absorbed
HEAT AND TEMPERATURE Heat is a type of ENERGY. When absorbed by a substance, heat causes inter-particle bonds to weaken and break which leads to a change of state (solid to liquid for example). Heat causing a phase change is NOT sufficient to cause an increase in temperature. Heat also causes an increase of kinetic energy (motion, friction) of the particles in a substance. This WILL cause an increase in TEMPERATURE. Temperature is NOT energy, only a measure of KINETIC ENERGY The reason why there is no change in temperature at a phase change is because the substance is using the heat only to change the way the particles interact (“stick together”). There is no increase in the particle motion and hence no rise in temperature. THERMAL ENERGY is one type of INTERNAL ENERGY possessed by an object. It is the KINETIC ENERGY component of the object’s internal energy. When thermal energy is transferred from a hot to a cold body, the term HEAT is used to describe the transferred energy. The hot body will decrease in temperature and hence in thermal energy. The cold body will increase in temperature and hence in thermal energy. Temperature Scales: The K scale is the absolute temperature scale. The lowest K temperature, 0 K, is absolute zero, the temperature at which an object possesses no thermal energy. The Celsius scale is based upon the melting point and boiling point of water at 1 atm pressure (0, 100o C) K = oC + 273.13 UNITS OF HEAT ENERGY The unit of heat energy we will use in this lesson is called the JOULE (J). -
Geothermal Energy
Geothermal energy Adele Manzella CNR - Institute of Geosciences and Earth Resources Via Moruzzi 1 – 56124 PISA, Italy [email protected] Geothermal Energy Pros Cons Research What is How is used frontiers Status and perspectives What is the source of geothermal energy? What part is used? What is Geothermal Energy IGG – Institute of Geosciences and Earth Resources National Research Council of Italy WHAT is Geothermal energy Geothermal Energy The basis of geothermal energy is the From Greek gêo (earth) e immense heat content of the earth’s thermòs (heat) interior: the Earth is slowly cooling down. Since billions of years the heat in the Earth Crust is constantly supplied by Heat inside the Earth the decay of natural radioactive isotopes or the cooling of hot, shallow magmatic ~ 30 °C/km bodies. > 1000 °C > 3000 °C The resource is vast and ubiquitous and > 5000 °C has a corresponding large potential for utilization. WHAT is Geothermal energy Temperature in the ground has a daily (few cm) and seasonal (few meters) fluctuations, becoming essentially constant and equal to the average air temperature at about 18-20 m depth. Below this depth, it essentially increases with depth (geothermal gradient). Shallow geothermal: exploits the underground constant T= average air T The resource is vast and ubiquitous and has a corresponding large potential for Deep geothermal: exploits the utilization. underground heat at T>> air T WHAT is Geothermal energy The temperature increase with depth, as well as volcanoes, geysers, hot springs etc., are in a sense the visible or tangible expression of the heat in the interior of the Earth, but this heat also engenders other phenomena that are less discernable by man, but of such magnitude that the Earth has been compared to an immense "thermal engine”. -
Geothermal Power and Interconnection: the Economics of Getting to Market David Hurlbut
Geothermal Power and Interconnection: The Economics of Getting to Market David Hurlbut NREL is a national laboratory of the U.S. Department of Energy, Office of Energy Efficiency & Renewable Energy, operated by the Alliance for Sustainable Energy, LLC. Technical Report NREL/TP-6A20-54192 April 2012 Contract No. DE-AC36-08GO28308 Geothermal Power and Interconnection: The Economics of Getting to Market David Hurlbut Prepared under Task No. WE11.0815 NREL is a national laboratory of the U.S. Department of Energy, Office of Energy Efficiency & Renewable Energy, operated by the Alliance for Sustainable Energy, LLC. National Renewable Energy Laboratory Technical Report 15013 Denver West Parkway NREL/TP-6A20-54192 Golden, Colorado 80401 April 2012 303-275-3000 • www.nrel.gov Contract No. DE-AC36-08GO28308 NOTICE This report was prepared as an account of work sponsored by an agency of the United States government. Neither the United States government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States government or any agency thereof. Available electronically at http://www.osti.gov/bridge Available for a processing fee to U.S. -
Abandoned Mines Can Be Used As Geothermal Energy Source
17 February 2011 Abandoned mines can be used as geothermal energy source Scientists have reviewed the potential for worldwide development of geothermal energy systems in old, unused mines. The technology is proven in many sites and could therefore help increase the share of renewable energy sources in the energy mix, offering sustainability and job creation, which may make mining operations more appealing to investors, communities and policymakers. The mineral industry is energy intensive and is therefore focusing on developing energy efficiency and cleaner production technologies. It is also expensive to open, operate and close mines, but few are ever considered as being useful once they have been closed. They are often located on marginal, unproductive land in remote, harsh environments and nearby communities may only live in the area as a direct result of the mine. Being often highly dependent on the mine and on imports of (fossil) fuel, such communities are highly unsustainable. The researchers argue that mines could be used post-closure for energy generation (heating and cooling) using the natural heat contained in the mine water. Geothermal energy systems could be implemented to extract this heat using heat pumps, from both closed and potentially working mines. This would offer local employment and energy resilience to the surrounding communities. Other uses of the energy may include melting snow on icy roads (instead of using salt) or supplying heat for fish farms and greenhouses. Several other technologies can extract energy from abandoned mines, including compressed air storage or the direct use of warm mine water to regulate the temperature of microalgae raceway ponds, allowing a longer growing season for cultivation; key products that can be obtained from the microalgae include nutraceuticals and biofuels. -
Geothermal Energy?
Renewable Geothermal Geothermal Basics What Is Geothermal Energy? The word geothermal comes from the Greek words geo (earth) and therme (heat). So, geothermal energy is heat from within the Earth. We can recover this heat as steam or hot water and use it to heat buildings or generate electricity. Geothermal energy is a renewable energy source because the heat is continuously produced inside the Earth. Geothermal Energy Is Generated Deep Inside the Earth Geothermal energy is generated in the Earth's core. Temperatures hotter than the sun's surface are continuously produced inside the Earth by the slow decay of radioactive particles, a process that happens in all rocks. The Earth has a number of different layers: The core itself has two layers: a solid iron core and an outer core made of very hot melted rock, called magma. The mantle surrounds the core and is about 1,800 miles thick. It is made up of magma and Source: Adapted from a rock. National Energy Education The crust is the outermost layer of the Earth, the Development Project land that forms the continents and ocean floors. It graphic (Public Domain) can be 3 to 5 miles thick under the oceans and 15 to 35 miles thick on the continents. The Earth's crust is broken into pieces called plates. Magma comes close to the Earth's surface near the edges of these plates. This is where volcanoes occur. The lava that erupts from volcanoes is partly magma. Deep underground, the rocks and water absorb the heat from this magma. The temperature of the rocks and water gets hotter and hotter as you go deeper underground. -
And Geothermal Power in Iceland a Study Trip
2007:10 TECHNICAL REPORT Hydro- and geothermal power in Iceland A study trip Ltu and Vattenfall visit Landsvirkjun May 1-5, 2007 Isabel Jantzer Luleå University of Technology Department of Civil, Mining and Environmental Engineering Division of Mining and Geotechnical Engineering 2007:10|: 102-1536|: - -- 07⁄10 -- Hydro- and geothermal power in Iceland A study trip Ltu and Vattenfall visit Landsvirkjun May 1 – 5, 2007 Iceland is currently constructing the largest hydropower dam in Europe, Kárahnjúkar. There are not many possibilities to visit such construction sites, as the opportunity to expand hydropower is often restricted because of environmental or regional regulations limitations. However, the study trip, which was primarily designed for the visitors from Vattenfall, gave a broad insight in the countries geology, energy resources and production, as well as industrial development in general. This report gives an overview of the trip, summarizes information and presents pictures and images. I want to thank Vattenfall as organization, as well as a large number of individuals at Vattenfall, for giving me the opportunity for participation. Further, I want to express my sincere gratitude to the Swedish Hydropower Center, i.e. Svensk Vattenkraft Centrum SVC, Luleå University of Technology, and individuals at Elforsk for providing me the possibility to take part in this excursion. It has been of great value for me as a young person with deep interest in dam design and construction and provided me with invaluable insights. Luleå, May 2007 Isabel Jantzer Agenda During three days we had the possibility to travel over the country: After the first day in Reykjavik, we flew to Egilstadir in the north eastern part of the country, from where we drove to the Kárahnjúkar dam site and visited the Alcoa aluminium smelter at Reydarfjördur Fjardaál afterwards. -
A Comprehensive Review of Thermal Energy Storage
sustainability Review A Comprehensive Review of Thermal Energy Storage Ioan Sarbu * ID and Calin Sebarchievici Department of Building Services Engineering, Polytechnic University of Timisoara, Piata Victoriei, No. 2A, 300006 Timisoara, Romania; [email protected] * Correspondence: [email protected]; Tel.: +40-256-403-991; Fax: +40-256-403-987 Received: 7 December 2017; Accepted: 10 January 2018; Published: 14 January 2018 Abstract: Thermal energy storage (TES) is a technology that stocks thermal energy by heating or cooling a storage medium so that the stored energy can be used at a later time for heating and cooling applications and power generation. TES systems are used particularly in buildings and in industrial processes. This paper is focused on TES technologies that provide a way of valorizing solar heat and reducing the energy demand of buildings. The principles of several energy storage methods and calculation of storage capacities are described. Sensible heat storage technologies, including water tank, underground, and packed-bed storage methods, are briefly reviewed. Additionally, latent-heat storage systems associated with phase-change materials for use in solar heating/cooling of buildings, solar water heating, heat-pump systems, and concentrating solar power plants as well as thermo-chemical storage are discussed. Finally, cool thermal energy storage is also briefly reviewed and outstanding information on the performance and costs of TES systems are included. Keywords: storage system; phase-change materials; chemical storage; cold storage; performance 1. Introduction Recent projections predict that the primary energy consumption will rise by 48% in 2040 [1]. On the other hand, the depletion of fossil resources in addition to their negative impact on the environment has accelerated the shift toward sustainable energy sources. -
IB Questionbank
Topic 3 Past Paper [94 marks] This question is about thermal energy transfer. A hot piece of iron is placed into a container of cold water. After a time the iron and water reach thermal equilibrium. The heat capacity of the container is negligible. specific heat capacity. [2 marks] 1a. Define Markscheme the energy required to change the temperature (of a substance) by 1K/°C/unit degree; of mass 1 kg / per unit mass; [5 marks] 1b. The following data are available. Mass of water = 0.35 kg Mass of iron = 0.58 kg Specific heat capacity of water = 4200 J kg–1K–1 Initial temperature of water = 20°C Final temperature of water = 44°C Initial temperature of iron = 180°C (i) Determine the specific heat capacity of iron. (ii) Explain why the value calculated in (b)(i) is likely to be different from the accepted value. Markscheme (i) use of mcΔT; 0.58×c×[180-44]=0.35×4200×[44-20]; c=447Jkg-1K-1≈450Jkg-1K-1; (ii) energy would be given off to surroundings/environment / energy would be absorbed by container / energy would be given off through vaporization of water; hence final temperature would be less; hence measured value of (specific) heat capacity (of iron) would be higher; This question is in two parts. Part 1 is about ideal gases and specific heat capacity. Part 2 is about simple harmonic motion and waves. Part 1 Ideal gases and specific heat capacity State assumptions of the kinetic model of an ideal gas. [2 marks] 2a. two Markscheme point molecules / negligible volume; no forces between molecules except during contact; motion/distribution is random; elastic collisions / no energy lost; obey Newton’s laws of motion; collision in zero time; gravity is ignored; [4 marks] 2b. -
Thermal Energy: Using Water to Heat a School
Thermal Energy: Using Water to Heat a School Investigation Notebook NYC Edition © 2018 by The Regents of the University of California. All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage or retrieval system, without permission in writing from the publisher. Teachers purchasing this Investigation Notebook as part of a kit may reproduce the book herein in sufficient quantities for classroom use only and not for resale. These materials are based upon work partially supported by the National Science Foundation under grant numbers DRL-1119584, DRL-1417939, ESI-0242733, ESI-0628272, ESI-0822119. The Federal Government has certain rights in this material. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation. These materials are based upon work partially supported by the Institute of Education Sciences, U.S. Department of Education, through Grant R305A130610 to The Regents of the University of California. The opinions expressed are those of the authors and do not represent views of the Institute or the U.S. Department of Education. Developed by the Learning Design Group at the University of California, Berkeley’s Lawrence Hall of Science. Amplify. 55 Washington Street, Suite 800 Brooklyn, NY 11201 1-800-823-1969 www.amplify.com Thermal Energy: Using Water to Heat a School