Geothermal Power Development in New Zealand - Lessons for Japan
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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. -
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. -
Ages on Weathered Plio-Pleistocene Tephra Sequences, Western North Island, New Zealand
riwtioll: Lowe. D. ~.; TiP.I>CU. J. M.: Kamp. P. J. J.; Liddell, I. J.; Briggs, R. M.: Horrocks, 1. L. 2001. Ages 011 weathered Pho-~Je.stocene tephra sequences, western North Island. New Zealand. Ill: Juviglle. E.T.: Raina!. J·P. (Eds). '"Tephras: Chronology, Archaeology', CDERAD editeur, GoudeL us Dossiers de f'ArcMo-Logis I: 45-60. Ages on weathered Plio-Pleistocene tephra sequences, western North Island, New Zealand Ages de sequences de tephras Plio-Pleistocenes alteres, fie du Nord-Ouest, Nouvelle lelande David J. Lowe·, J, Mark Tippett!, Peter J. J, Kamp·, Ivan J. LiddeD·, Roger M. Briggs· & Joanna L. Horrocks· Abstract: using the zircon fISsion-track method, we have obtainedfive ages 011 members oftwo strongly-...-eathered. silicic, Pliocene·Pleislocelle tephra seql/ences, Ihe KOIIIUQ and Hamilton Ashformalions, in weslern North !sland, New Zealand. These are Ihe jirst numerical ages 10 be oblained directly on these deposils. Ofthe Kauroa Ash sequence, member KI (basal unit) was dated at 2,24 ± 0.19 Ma, confirming a previous age ofc. 1.25 Ma obtained (via tephrochronology)from KlAr ages on associatedbasalt lava. Members K1 and X3 gave indistinguishable ages between 1,68.±0,/1 and 1.43 ± 0./7 Ma. Member K11, a correlQlilV! ojOparau Tephra andprobably also Ongatiti Ignimbrite. was dated at 1.18:i: 0.11 Ma, consistent with an age of 1.23 ± 0.02 Ma obtained by various methodr on Ongaiiti Ignimbrite. Palaeomagnetic measurements indicated that members XI3 to XIJ (top unit, Waiterimu Ash) are aged between c. 1.2 Ma and O. 78 Mo. Possible sources of/he Kauroa Ash Formation include younger \!Oleanic centres in the sOllthern Coromandel Volcanic Zone orolder volcanic cenlres in the Taupo Volcanic Zone, or both. -
BEFORE Palmerston North City Council in the MATTER of The
BEFORE Palmerston North City Council IN THE MATTER of the Resource Management Act 1991 AND IN THE MATTER of Proposed Plan Change 15B to the Palmerston North City Plan. STATEMENT OF EVIDENCE OF ERIC PYLE 3rd December 2015 Groundfloor 114 The Terrace PO Box 553 Wellington 6140 Ph: 64 4 499 5025 Fax: 64 4 473 6754 www.windenergy.org.nz Evidence of Eric Pyle Before Palmerston North City Council November 2015 Introduction 1. My name is Eric Pyle. I am employed by the New Zealand Wind Energy Association (‘NZWEA’ or ‘Association’) as its Chief Executive and have the authority of the Association to provide this evidence on its behalf. 2. My position involves overall responsibility for all of NZWEA’s activities promoting, encouraging and enabling the uptake of wind energy in New Zealand both within the wind industry and to a wide range of stakeholders including Government, regulators and the public. I have held this position since July 2011. 3. I have a background spanning 20 years in environmental management and energy. My role exposes me to the full range of wind energy-related activities across New Zealand. 4. Most recently I was employed by the Ministry of Research Science and Technology and had responsibility for environmental, energy, natural hazards and social research. This role required me to take a broad overview of the environmental management and energy systems in both New Zealand and globally and understand both the immediate and long term issues facing New Zealand and where research and development could add value. 5. Prior to working for the Ministry of Research, Science and Technology I was employed by the Royal Forest and Bird Protection Society as its Conservation Manager. -
Geothermal Project Reports List.Xlsx
Geothermal Project Reports List.xlsx Geothermal Project Reports List Call Number Title Author 1979.01 Corrosion testing in geothermal systems ABDURRAHMAN, M. 1979.03 Evaluation of the North Davao geothermal prospect, Mindanao, Southern Philippines AREVALO, E. 1979.04 Geothermal pilot plant studies in Broadlands BASYARI, A. 1979.05 Two-phase geothermal fluid transmission application to El Tatio Geothermal Field, Chile BENABARRE, J. 1979.06 Geochemistry of hydrothermal alteration of the Ohaki Rhyolite, Broadlands Geothermal Field, New Zealand BOGIE, I. 1979.07 Gravity anomalies over the Ngawha Geothermal Field, Northland, New Zealand CORDON, U. 1979.08 Economic analysis of geothermal plant DANU, H. 1979.09 Preliminary study of the binary cycle with reference to its application to the geothermal resources in India RAO, D.H. 1979.10 Mapping and chemical survey of surface distance features, Ngawha Geothermal Field, Northland, New TESFAGIORGIS, P. Zealand 1979.12 Geothermal well design - prediction of flow and heat transfer KANGUA, J.F. 1979.15 Non-electrical uses of geothermal energy - downhole heat exchanger design LEE, K. 1979.16 Mapping of vents associated with Putahi Rhyolite, Northland, N.Z. LETELIER, M. 1979.17 Setting of the geothermal fields of Tibet and a discussion of associated heat source problems LIAO, Z. 1979.19 The potential of the Manito geothermal system, South-Eastern Luzon, Philippines OBUSAN, R. 1979.20 A literature survey of geopressured systems PENG, D-J. 1979.21 Build-up test analysis of Ngawha and Kamojang wells PRATOMO, H. 1979.22 Thermodynamics of geothermal plant - optimisation studies TARIGAN, G. 1979.23 More efficient use of geothermal heat at Broadlands Lucerne Company's drying plant VAN DE WYDEVEN, F. -
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. -
The Centre for Building Performance Research and the School Of
LINZEY | Making a Place: Mangakino 1946-62 | AHA: Architectural History Aotearoa (2008) vol 5:65-71 Making a Place: Mangakino 1946-62 Kate Linzey, Interior Design, Weltec, Wellington ABSTRACT: In between Whakamaru (1949-56) and Maraetai (1946-53) dams, on the Waikato River, sits Mangakino. Planned and built from c1948 to 1951, by the Town Planning section of the Ministry of Works, the civic centre was to provide housing and services for the work force on the Maraetai scheme. The architectural design of these dams has previously been discussed as the work of émigré architect, Fredrick Neumann/Newman (Leach), and the town, as that of Ernst Plischke (Lloyd-Jenkins, Sarnitz). In 1949 the plan for Mangakino was published, alongside the plan for Upper Hutt, in the February-March edition of the Design Review. As two "rapidly growing towns," Upper Hutt and Mangakino are briefly reviewed in the context of two essays ("Who wants community centres?" and "Community Centres" by HCD Somerset), an outline of the curriculum of the new School of Architecture and Town Planning, run by the Architectural Centre, and notification of the 1948 Town Planning Amendment Act. As published in the Design Review, the plan of Mangakino includes a church in the south west, with the sporting facilities to the north and Rangatira Drive flanking a shopping strip on the east. The church sits in a field of grass, isolated and apparently serene. In the drawing published in the monograph Ernst Plischke, however, this building has been cropped off. Focusing on the case of Mangakino, this essay will review the discourse of town planning for secular and religious communities in the late 1940s. -
Mathematical Modelling of Wairakei Geothermal Field
ANZIAM J. 50(2009), 426–434 doi:10.1017/S1446181109000212 MATHEMATICAL MODELLING OF WAIRAKEI GEOTHERMAL FIELD MALCOLM A. GRANT1 (Received 1 November, 2008; revised 22 April, 2009) Abstract Mathematical modelling of Wairakei geothermal field is reviewed, both lumped- parameter and distributed-parameter models. In both cases it is found that reliable predictions require five to ten years of history for calibration. With such calibration distributed-parameter models are now used for field management. A prudent model of Wairakei, constructed without such historical data, would underestimate field capacity and provide only general projections of the type of changes in surface activity and subsidence. 2000 Mathematics subject classification: primary 86A99. Keywords and phrases: geothermal, reservoir modelling, Wairakei, review. 1. Introduction Wairakei geothermal field is located in the North Island of New Zealand, in the Taupo Volcanic Zone. In the late 1940s there was one geothermal field developed for electrical generation in the world, Laraderello in Italy. This example, and a looming electricity shortage, led to the decision to develop Wairakei for power generation. The first drilling showed a field markedly different from Larderello, as it was full of hot water rather than the expected steam. The subsequent development had a large element of exploration, and there was a significant scientific effort to understand the physical nature of the field. The power station was built by 1958, but research continued thereafter, and to the present day. Part of this effort was mathematical modelling. As pressures drew down with exploitation, it was discovered that the drawdown at depth was extremely uniform across the entire field, so that a single pressure history described this drawdown. -
Where Is Taupo? It Is Situated at the North-Eastern Part of Lake Taupo, at the Outlet Where It Flows Into the Waikato River
Taupo in New Zealand Taupo is located on the shores of New Zealand’s largest lake – Lake Taupo Taupo is a riverside town unhurried by the bustle of everyday life; where the day begins with the serene gurgling of a large freshwater lake, and nights end with bonfires. It is an urban paradise where worries float away in the waters of the clear blue Lake Taupo, the town’s patron lake. Things to Do in Taupo With a variety of water bound activities like jet boating, water skiing, kayaking, whitewater rafting, and world-class fishing, the adventurist will never get bored in this town. Set sail to history in ancient Maori rock carvings at Mine Bay, which can only be seen from the water. Or, lie in wait as you cast the bait for some of the finest trout at Turangi, the largest natural trout fishery in the world. Even if you are more of a land mammal, this resort town has plenty to offer you. Take a walk down the Craters of the Moon, which takes you down a mythical world of colorful soils, steam vents, and explosive bubbling craters. This also tells you the story of Lake Taupo’s fiery birth in the geysers and boiling mud pools. As you walk north of Lake Taupo, be awed by the magnificent Huka Falls, and watch 220,000 liters of water thundering off a cliff every second. This is New Zealand’s most popular tourist attraction. Explore the Tongariro National Park filled with 80,000 hectares of hot springs, emerald lakes and alpine meadows. -
Notes on the Early History of Wairakei
Proceedings 20th Geothermal Workshop 1998 NOTES ON THE EARLY HISTORY OF WAIRAKEI R.S. 11Fiesta Grove, Raumati Beach, New Zealand SUMMARY These notes outline the major circumstancesand events influencing the decision to investigate the resources of New Zealand, together with problems faced in the early days of the development of They cover the period fiom 1918when the first suggestion for the investigationof the resource appeareduntil early 1953when Wairakei's development began in earnest. 1. INTRODUCTION would be more economical than the further use of water." 1924) 1.1. Early Interest in the Resource Eighty years ago, on 2 February, 1918, the Coincidentally, in 1925, a 250 generator was Masterton Chamber of Commerce requested the operating at the Geysers. However, no further Minister of Public Works to enquire into the development was being carried out because of the utilization of thermal energy for industrial and competition hydro and natural gas. other purposes, pointing out that the Italians were 1980). In other words, although now generating electrical energy fiom thermal districts the intensively developed geothermal field and were using it for lighting, and in the world, the Geyser's early development was munitions manufacture with great success. inhibited for much the same reasons as was New 1918). However, another four decades passed Zealand's. before New Zealand could say with some truth that it was using electricity fiom thermal The literature from this period is district "with great success". sparse, but one publication of significance is Geological Survey Bulletin 37. (Grange, 1937). Among a number of similar suggestions which This is the first detailed description of the geology appeared over the next two decades, perhaps the of the Zone and made an most unusual New Zealand's High important contribution to the subsequent Commissioner in London.