Geothermal Handbook: Planning and Financing Power Generation
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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. -
Outcomes of the EU Horizon 2020 DAFNE PROJECT the Omo
POLICY BRIEF October 2020 Outcomes of the EU Horizon 2020 DAFNE PROJECT The Omo-Turkana River Basin Progress towards cooperative frameworks KEY POLICY MESSAGES The OTB has reached a stage of pivotal importance for future development; the time to establish a cooperative framework on water governance is now. Transparency and accountability must be improved in order to facilitate the sharing of data and information, increasing trust and reducing the perception of risk. Benefit-sharing which extends beyond energy could enhance regional integration and improve sustainable development within the basin . THE OMO-TURKANA RIVER BASIN potential for hydropower and irrigation schemes that are, if scientifically and equitably managed, crucial to lift millions within and outside the basin out of extreme poverty; this has led to transboundary cooperation in recent years. This policy brief is derived from research conducted under the €5.5M four-year EU Horizon 2020 and Swiss funded ‘DAFNE’ project which concerns the promotion of integrated and adaptive water resources management, explicitly addressing the WEF Nexus and aiming to promote a sustainable economy in regions where new infrastructure and expanding The Omo-Turkana River Basin (OTB) – for the agriculture has to be balanced with social, purposes of the DAFNE Project – comprises of economic and environmental needs. The project two main water bodies: the Omo River in takes a multi- and interdisciplinary approach to Ethiopia and Lake Turkana which it drains into. the formation of a decision analytical While the Omo River lies entirely within Ethiopian territory, Lake Turkana is shared by framework (DAF) for participatory and both Kenya and Ethiopia, with the majority of integrated planning, to allow the evaluation of Lake Turkana residing within Kenya. -
Historical Volcanism and the State of Stress in the East African Rift System
Historical volcanism and the state of stress in the East African Rift System Article Accepted Version Open Access Wadge, G., Biggs, J., Lloyd, R. and Kendall, J.-M. (2016) Historical volcanism and the state of stress in the East African Rift System. Frontiers in Earth Science, 4. 86. ISSN 2296- 6463 doi: https://doi.org/10.3389/feart.2016.00086 Available at http://centaur.reading.ac.uk/66786/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . To link to this article DOI: http://dx.doi.org/10.3389/feart.2016.00086 Publisher: Frontiers media All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online 1 Historical volcanism and the state of stress in the East African 2 Rift System 3 4 5 G. Wadge1*, J. Biggs2, R. Lloyd2, J-M. Kendall2 6 7 8 1.COMET, Department of Meteorology, University of Reading, Reading, UK 9 2.COMET, School of Earth Sciences, University of Bristol, Bristol, UK 10 11 * [email protected] 12 13 14 Keywords: crustal stress, historical eruptions, East African Rift, oblique motion, 15 eruption dynamics 16 17 18 19 20 21 Abstract 22 23 Crustal extension at the East African Rift System (EARS) should, as a tectonic ideal, 24 involve a stress field in which the direction of minimum horizontal stress is 25 perpendicular to the rift. -
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. -
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. -
Lake Turkana and the Lower Omo the Arid and Semi-Arid Lands Account for 50% of Kenya’S Livestock Production (Snyder, 2006)
Lake Turkana & the Lower Omo: Hydrological Impacts of Major Dam & Irrigation Development REPORT African Studies Centre Sean Avery (BSc., PhD., C.Eng., C. Env.) © Antonella865 | Dreamstime © Antonella865 Consultant’s email: [email protected] Web: www.watres.com LAKE TURKANA & THE LOWER OMO: HYDROLOGICAL IMPACTS OF MAJOR DAM & IRRIGATION DEVELOPMENTS CONTENTS – VOLUME I REPORT Chapter Description Page EXECUTIVE(SUMMARY ..................................................................................................................................1! 1! INTRODUCTION .................................................................................................................................... 12! 1.1! THE(CONTEXT ........................................................................................................................................ 12! 1.2! THE(ASSIGNMENT .................................................................................................................................. 14! 1.3! METHODOLOGY...................................................................................................................................... 15! 2! DEVELOPMENT(PLANNING(IN(THE(OMO(BASIN ......................................................................... 18! 2.1! INTRODUCTION(AND(SUMMARY(OVERVIEW(OF(FINDINGS................................................................... 18! 2.2! OMO?GIBE(BASIN(MASTER(PLAN(STUDY,(DECEMBER(1996..............................................................19! 2.2.1! OMO'GIBE!BASIN!MASTER!PLAN!'!TERMS!OF!REFERENCE...........................................................................19! -
Alcolapia Grahami ERSS
Lake Magadi Tilapia (Alcolapia grahami) Ecological Risk Screening Summary U.S. Fish & Wildlife Service, March 2015 Revised, August 2017, October 2017 Web Version, 8/21/2018 1 Native Range and Status in the United States Native Range From Bayona and Akinyi (2006): “The natural range of this species is restricted to a single location: Lake Magadi [Kenya].” Status in the United States No records of Alcolapia grahami in the wild or in trade in the United States were found. The Florida Fish and Wildlife Conservation Commission has listed the tilapia Alcolapia grahami as a prohibited species. Prohibited nonnative species (FFWCC 2018), “are considered to be dangerous to the ecology and/or the health and welfare of the people of Florida. These species are not allowed to be personally possessed or used for commercial activities.” Means of Introductions in the United States No records of Alcolapia grahami in the United States were found. 1 Remarks From Bayona and Akinyi (2006): “Vulnerable D2 ver 3.1” Various sources use Alcolapia grahami (Eschmeyer et al. 2017) or Oreochromis grahami (ITIS 2017) as the accepted name for this species. Information searches were conducted under both names to ensure completeness of the data gathered. 2 Biology and Ecology Taxonomic Hierarchy and Taxonomic Standing According to Eschmeyer et al. (2017), Alcolapia grahami (Boulenger 1912) is the current valid name for this species. It was originally described as Tilapia grahami; it has also been known as Oreoghromis grahami, and as a synonym, but valid subspecies, of -
Lake Turkana National Parks - 2017 Conservation Outlook Assessment (Archived)
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Lake Turkana National Parks - 2017 Conservation Outlook Assessment (archived) IUCN Conservation Outlook Assessment 2017 (archived) Finalised on 26 October 2017 Please note: this is an archived Conservation Outlook Assessment for Lake Turkana National Parks. To access the most up-to-date Conservation Outlook Assessment for this site, please visit https://www.worldheritageoutlook.iucn.org. Lake Turkana National Parks عقوملا تامولعم Country: Kenya Inscribed in: 1997 Criteria: (viii) (x) The most saline of Africa's large lakes, Turkana is an outstanding laboratory for the study of plant and animal communities. The three National Parks serve as a stopover for migrant waterfowl and are major breeding grounds for the Nile crocodile, hippopotamus and a variety of venomous snakes. The Koobi Fora deposits, rich in mammalian, molluscan and other fossil remains, have contributed more to the understanding of paleo-environments than any other site on the continent. © UNESCO صخلملا 2017 Conservation Outlook Critical Lake Turkana’s unique qualities as a large lake in a desert environment are under threat as the demands for water for development escalate and the financial capital to build major dams becomes available. Historically, the lake’s level has been subject to natural fluctuations in response to the vicissitudes of climate, with the inflow of water broadly matching the amount lost through evaporation (as the lake basin has no outflow). The lake’s major source of water, Ethiopia’s Omo River is being developed with a series of major hydropower dams and irrigated agricultural schemes, in particular sugar and other crop plantations. -
Geothermal Power Development in New Zealand - Lessons for Japan
Geothermal Power Development in New Zealand - Lessons for Japan - Research Report Emi Mizuno, Ph.D. Senior Researcher Japan Renewable Energy Foundation February 2013 Geothermal Power Development in New Zealand – Lessons for Japan 2-18-3 Higashi-shimbashi Minato-ku, Tokyo, Japan, 105-0021 Phone: +81-3-6895-1020, FAX: +81-3-6895-1021 http://jref.or.jp An opinion shown in this report is an opinion of the person in charge and is not necessarily agreeing with the opinion of the Japan Renewable Energy Foundation. Copyright ©2013 Japan Renewable Energy Foundation.All rights reserved. The copyright of this report belongs to the Japan Renewable Energy Foundation. An unauthorized duplication, reproduction, and diversion are prohibited in any purpose regardless of electronic or mechanical method. 1 Copyright ©2013 Japan Renewable Energy Foundation.All rights reserved. Geothermal Power Development in New Zealand – Lessons for Japan Table of Contents Acknowledgements 4 Executive Summary 5 1. Introduction 8 2. Geothermal Resources and Geothermal Power Development in New Zealand 9 1) Geothermal Resources in New Zealand 9 2) Geothermal Power Generation in New Zealand 11 3) Section Summary 12 3. Policy and Institutional Framework for Geothermal Development in New Zealand 13 1) National Framework for Geothermal Power Development 13 2) Regional Framework and Process 15 3) New National Resource Consent Framework and Process for Proposals of National Significance 18 4) Section Summary 21 4. Environmental Problems and Policy Approaches 22 1) Historical Environmental Issues in the Taupo Volcanic Zone 22 2) Policy Changes, Current Environmental and Management Issues, and Policy Approaches 23 3) Section Summary 32 5. -
093-070513 EGEC Kapp and Kreuter Hybrid
Proceedings European Geothermal Congress 2007 Unterhaching, Germany, 30 May-1 June 2007 The Concept of Hybrid Power Plants in Geothermal Applications Bernd Kapp and Horst Kreuter Baischstraße 7, D-76133 Karlsruhe [email protected] and [email protected] Keywords: hybrid concept, geothermal, biogas, power about 115°C or more depending on the arrangement of the plant heat exchanger in the cycle and the value of the geothermal energy. In addition to the higher heat input in the rankine ABSTRACT cycle the temperature increase of the fluid leads to a higher In many regions of Germany, the temperature of efficiency in the cycle. Both, ORC and Kalina Cycle, show a strong transient of the efficiency in the temperature range geothermal brine that can be tapped in natural reservoirs between 100°C and 120°C. generally is below 120°C. The production of electricity is economically not feasible in most of these areas, because Different thermodynamic calculations with the software with low temperatures the degree of efficiency and thus the Thermoflow were performed to investigate the influence of amount of produced power is too small. With the new the hybrid concept compared to the common stand-alone hybrid concept, it is now possible to feed in energy from a solution of a geothermal power plant (figure 2). A second renewable energy source into the geothermal power comparison between the different cycles (Kalina and ORC cycle while raising the temperature at the same time. using isobutane) is shown in figure 3. 1. INTRODUCTION Electricity generation out of a geothermal energy source depends on the local geological situation. -
View (State Party of Kenya, 2020)
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org Kenya Lake System in the Great Rift Valley - 2020 Conservation Outlook Assessment Kenya Lake System in the Great Rift Valley 2020 Conservation Outlook Assessment SITE INFORMATION Country: Kenya Inscribed in: 2011 Criteria: (vii) (ix) (x) The Kenya Lake System in the Great Rift Valley , a natural property of outstanding beauty, comprises three inter-linked relatively shallow lakes (Lake Bogoria, Lake Nakuru and Lake Elementaita) in the Rift Valley Province of Kenya and covers a total area of 32,034 hectares. The property is home to 13 globally threatened bird species and some of the highest bird diversities in the world. It is the single most important foraging site for the lesser flamingo anywhere, and a major nesting and breeding ground for great white pelicans. The property features sizeable mammal populations, including black rhino, Rothschild's giraffe, greater kudu, lion, cheetah and wild dogs and is valuable for the study of ecological processes of major importance. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 01 Dec 2020 SIGNIFICANT CONCERN The three lakes which make up the Kenya Lake System World Heritage site are subject to pronounced and unpredictable fluctuations in rainfall, water levels and alkalinity – factors which determine the movements of flamingoes and other birds between these lakes, and others beyond. Waterbird counts over the past 20 years suggest that bird populations are stable, but their distribution has changed, with uncertainties over the future of the lakes as the catchment areas come under progressively more intensive land use, with the loss of wetlands through livestock grazing, with increasingly large volumes of water abstracted upstream for agriculture, whilst floods are becoming more severe, with the associated sediments carried into and accumulating within the lakes.