Pioneer Geothermal Power Station Still Abundant Electricity Supplier

Total Page:16

File Type:pdf, Size:1020Kb

Pioneer Geothermal Power Station Still Abundant Electricity Supplier ELECTRICITY Earth Energy accessible reliable renewable Wairakei Power Station on the banks of the Waikato River. Pioneer Geothermal Power Station Still Abundant Electricity Supplier The world’s first Mike Dunstall, General Manager of Geothermal Resources and KEY BENEFITS: geothermal power Development at Contact Energy, says station to use wet “The construction of Wairakei saw • Renewable energy source New Zealand become the second • Minimal greenhouse steam technology largest producer of geothermal energy, gas emissions and a pioneer in the field.” was commissioned • Generates base load in 1958 at Wairakei, “Since 1960 Wairakei Power Station has electricity which is not been running at 90% or more of its impacted by weather north of Taupō. maximum output and is an important base load station, providing constant electricity to over one hundred KEY FEATURES: thousand homes. Just recently, we have reduced our utilisation of the • Operational for over 60 years oldest Wairakei machines, as our new • 175 MW installed capacity Te Mihi station takes over some of Wairakei’s role” • 1000 GWh of electricity per annum Wairakei’s 25 km2 borefield contains over 150 wells, with a typical depth of 600 m in older wells and as deep as 3000 m in newer wells. Of these, about 65 are in production, extracting hot water and steam from the earth at a rate of 245,000 tons per day, while twenty are injection wells that put about 180,000 tons of water back into the field daily. “WAIRAKEI PAVED THE WAY FOR NEXT GENERATION POWER STATIONS, LIKE TE MIHI. IT HAS PROVEN THAT GEOTHERMAL IN NEW ZEALAND IS ONE OF OUR BEST RENEWABLE AND CLEAN ENERGY RESOURCES AND THE TECHNOLOGY FIRST DEVELOPED AT WAIRAKEI CONTINUES TO INFLUENCE GEOTHERMAL POWER STATION DESIGN AROUND THE WORLD.” Wairakei borefield, where the hot steam is drawn from. “Reinjection reduces effects on the reduced to 1.1 bar. This steam then Since Te Mihi Power Station started Waikato River, where up to 36,000 tons travels through the second low pressure running in 2013, Wairakei has been of separated geothermal water passes part of the turbine before finally reaching reduced in output and is not likely to run daily, and can help manage the life of the the condenser. past 2026 (when its resource consent geothermal field.” Contact Energy is in runs out). Over time, steam utilisation will The binary plant, added in 2004, is the process of bringing river discharges shift to the more modern power plants a modern extension to the Wairakei back to levels that flowed naturally on the Wairakei steam field. Power Station. before the power station was built. Advances in binary technology have Contact Energy is continuing to allowed lower temperature geothermal develop further reinjection to reduce waste water (brine) to be utilised. The river discharges back to levels that design uses a heat exchanger with an flowed naturally before the power isopentane working fluid in the generator. station was built. The isopentane has a very low boiling There are currently 12 electricity point. When heated by previously generators available for service; four unused geothermal water, this working are low pressure, two intermediate fluid easily drives the turbines. The pressure, three mixed pressure, one isopentane is then condensed and intermediate low pressure and two passed back to the heat exchangers to within the binary plant. begin the cycle again. This binary plant The low pressure turbines utilise steam has added another 14 MW of capacity, at 1.1 bar (where the atmospheric using otherwise waste brine to produce pressure is 1 bar), so condensers have electricity. to effectively pull the steam through for Mike says that geothermal is Geothermal steam pipes carry steam to the the turbines to spin. New Zealand’s most reliable, renewable power station. The condensers use cold water from energy source and is comparatively a the Waikato River, which is sprayed into very clean energy. a chamber at the turbine exit. As the “Geothermal is the most reliable source steam condenses it forms a vacuum, of renewable energy, as it is not pulling more steam through. The low influenced by weather. It is also pretty temperature of the water used partly low in environmental impact. There is results in Wairakei’s high efficiency, some carbon dioxide emission from comparable to more modern geothermal Wairakei, but this is many times lower power stations. than fossil fuel plants would emit to Intermediate pressure turbines work on generate the same power. Since 2012 Mike Dunstall a similar principle but use 3.5 bar steam we have also included a bioreactor in General Manager instead and pass their steam on to two the steam condensate system, as part of Geothermal Resources and Development of the low pressure turbines. the changes we are making at Wairakei Contact Energy Ltd. to reduce the impact of steam and hot Wairakei Power Station The mixed pressure turbines are an State Highway 1 water releases to the environment”. intermediate pressure turbine followed Taupō by a low pressure turbine. The steam As the first wet steam geothermal power New Zealand enters the first section at 3.5 bar, it then station and now nearly 60 years old, Phone: +64 (0)7 376 0500 loses some energy as electric power is Wairakei is still running strong. Email: [email protected] generated resulting in its pressure being Website: www.contactenergy.co.nz New Zealand requires reliable, renewable energy sources into the future. Wairakei Research Centre The Government is supporting GNS Science in fostering increased use of 114 Karetoto Road, renewable resources. By 2025, the Government’s Energy Strategy aims Wairakei 3377 for direct use of geothermal energy to account for more than 12 PJ/year. Private Bag 2000, For more information visit our website: Taupo 3352 New Zealand www.gns.cri.nz/earthenergy Phone: +64 7 374 8211 or contact us: Email: [email protected].
Recommended publications
  • Strong Iwi Involvement in River Clean-Up Projects
    DECEMBER 2018 A newsletter from the Strong iwi involvement in MESSAGE FROM river clean-up projects THE CE It has been a busy end of year for THE WAIKATO RIVER AUTHORITY HAS ANNOUNCED $6 MILLION FOR RIVER the WRA. We completed our 8th CLEAN-UP PROJECTS IN ITS JUST COMPLETED FUNDING ROUND, WITH MORE funding round and it was great to THAN A THIRD OF THESE PROJECTS BEING IWI LED. see projects successfully lifted from the Restoration Strategy Overall, a total of 38 projects have been The largest project to be funded this year that Environment Minister funded in 2018. is a continuation of the Waipā Catchment Parker launched earlier this year. Authority Co-chairs Hon John Luxton and Plan implementation which will involve Our advocacy for the Vision & Roger Pikia, say a feature of the funding working with approximately 70 farmers Strategy has been pursued across round has been a close alignment with the and landowners within identified priority a number of fora. We held our Restoration Strategy for the Waikato and catchments. The $1.6 million of funding AGM on the back of publishing Waipā rivers and the strong participation will work towards reducing sediment our 2017/18 Annual Report. We of River Iwi. levels going into the Waipā River and its have also received positive media tributaries. Sediment from the Waipā “In recent years there has been a clear coverage across several articles River is a major factor in reducing the trend for successful projects to reflect in as many weeks. One of these water quality in the lower Waikato River.
    [Show full text]
  • Waikato River Adare Flood Hazard Report
    The Adare Limited Company Limited Waikato River Adare Flood Hazard Report 17 May 2018 Prepared by Awa Environmental Limited for The Adare Company Limited The Adare Limited Company Limited Waikato River Adare Flood Hazard Report Project No. J000098 Document title Waikato River Adare Flood Hazard Report Document number 03 Version number 03 Date 17 May 2018 Project manager Craig Martell Author TonyTrueman Awa Environmental Limited 115 Tory Street, Te Aro, Wellington 6011, Phone:+64 04 455 0990 www.awa.kiwi Document History Version Date Description Author Reviewed 1 02/11/2017 Review TonyTrueman Craig Martell 2 29/03/2018 Preliminary Issue Tony Trueman Tony Trueman 3 17/05/2018 Review Tony Trueman Tony Trueman COPYRIGHT: The concepts and information contained in this document are the property of Awa Environmental Ltd. Use or copying of this document in whole or in part without the written permission of constitutes an infringement of copyright. iii The Adare Limited Company Limited Waikato River Adare Flood Hazard Report Contents Contents ................................................................................................................................................. iv 1 Introduction .................................................................................................................................... 1 2 1% AEP River Flooding Assessment ................................................................................................ 2 2.1 1% AEP Flood Hazard Extent ..................................................................................................
    [Show full text]
  • Waikato District Council
    WAIKATO DISTRICT COUNCIL Report and Decisions of the Waikato District Plan Hearings Panel REPORT 2 Ohinewai Rezoning 24 May 2021 Commissioners Dr Phil Mitchell (Chair) Mr Paul Cooney (Deputy Chair) Mr Dynes Fulton Mr Weo Maag Page | 1 Decision Report 2: Ohinewai Rezoning Report and Decisions of the Waikato District Plan Hearings Panel Page | 2 Decision Report 2: Ohinewai Rezoning Report and Decisions of the Waikato District Plan Hearings Panel TABLE OF CONTENTS 1 Introduction ................................................................................................................................... 5 2 The APL submission ...................................................................................................................... 9 3 Statutory and planning framework ............................................................................................ 15 4 Site suitability and physical characteristics ............................................................................... 18 5 Three Waters Infrastructure ...................................................................................................... 20 6 Natural hazards ........................................................................................................................... 24 7 Transport and traffic ................................................................................................................... 26 8 Economic effects .........................................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • A Study of Some Effects of the Wairakei Geothermal Power Station Upon the Waikato River
    TANE 21, 1975 A STUDY OF SOME EFFECTS OF THE WAIRAKEI GEOTHERMAL POWER STATION UPON THE WAIKATO RIVER by G.J. Cox*, Sally M. Naylor f, and D.E. Thomson ft SUMMARY The effects of heated discharges from the Wairakei Geothermal Power Scheme upon the Waikato River have been investigated. Water temperature, oxygen content and mercury concentration were measured at a number of points above and below the station and aquatic life was studied (the data on the flora has yet to be fully analysed and can thus only be described briefly here). Marked local effects on both the aquatic life and paramaters of water quality were observed. However, although further investigation is warranted, particularly of the discharge rates of heavy metals such as mercury, the scheme does not appear to contribute significantly to the pollution of the Waikato River. INTRODUCTION A number of reports dealing with various aspects of the Wairakei Geothermal Power Station and its effects on the Waikato River have been published since the station became operative in the late 1950's. This work has recently been summarised by Axtmann1 who included a number of New Zealand Electricity Department reports in his references. However certain topics such as thermal mixing and the effects of the outputs from both station and bore fields on the aquatic life, have been virtually ignored. It was chiefly to provide some information on these that the present study was initiated. The study was confined to a single week in the mid-winter (11 to 16 August) of 1974. The power station-bore complex has two outlets into the Waikato River, the more obvious one being the discharge of cooling water used to condense the stream which is used to drive the powerhouse turbines.
    [Show full text]
  • Meremere Roading Cases Tudy
    1 Reference: Harmsworth, G.R. 2005: Roading Case Study: Transit New Zealand and Ngati Naho, Meremere œ Springhill Road. Contract to Opus International Consultants New Zealand Ltd. 6 pp. FRST programme: Roading enhanced by M,ori values and Knowledge (OPSX0301) http://www.transportco2.org.nz/ FRST programme: Roading enhanced by Mori values and knowledge Case study: Transit New Zealand and Ngati Naho, Meremere œ Springhill Road Garth Harmsworth, Landcare Research [email protected] Background Construction on a 100-m section of the Waikato Expressway (major 4-lane highway), between Mercer and Longswamp, was temporarily stopped in 2002 while a solution was sought between the parties, Transit New Zealand (Transit) and the local hap> Ng,ti Naho, regarding a significant cultural "taniwha" (a M,ori mythological creature) and wetland site. The issue was widely publicised nationally and internationally in 2002 when it came to the attention of the media. The small wetland and culturally significant site (~30 m by 20 m) was located between the existing road and the Waikato River, adjacent to the planned Expressway. Transit NZ had also identified the vicinity as having —higher environmental value than adjacent land“ (Transit New Zealand 2002b) and there was a spring feeding a small remnant of kahikatea trees ( Podocarpus dacrydiodes ) œ a fact never presented by the media. —While a lot of the area we are working on is in swamp, this section over about 30 metres appears to be a spring which may be significant for a large stand of kahikatea trees, which need to be protected“ (Transit New Zealand 2002b), —The discussions to date with Ngati Naho had focussed on how the Expressway could be constructed past this section in a manner which preserved the nature of the site“ (Transit New Zealand 2002b).
    [Show full text]
  • 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.
    [Show full text]
  • TOI MOANA BAY of PLENTY GROWTH STUDY: OPPORTUNITIES REPORT May 2015 P R E FA C E
    MINISTERS’ FOREWORD As Ministers for Economic Development, Primary Industries and Māori Development, we believe strongly that building successful and more resilient regions is key to building a prosperous nation. Recognising and capitalising on the opportunities and strengths of different regions is vital to enable each region to provide employment and a good standard of living for its people and to maximise each region’s contribution to the economic and social wellbeing of New Zealand. The Regional Economic Activity Reports and Enterprise and regional economic (REAR) have allowed us to understand development agencies to bring investment and compare regional performance at a and ultimately employment into the high level. Through the REAR’s, we know regions. that the current economic and social The Bay of Plenty Regional Growth Study performance of regions varies significantly. is the second study in this programme and The Regional Growth Studies programme follows the Northland Regional Growth provides an independent view of specific Study which was released in February regions chosen because their potential is 2015. It provides a view that has been not yet fully realised. Within each of these developed through evidence and with input regions there are excellent success stories from key businesses and economic players and some pockets of high deprivation. This in the region. It provides the region and deprivation can only be fully addressed central government with a shared view through wealth creation and higher levels of the potential of the region and its local of employment. communities. The Regional Growth Studies explore The Bay of Plenty region (that includes opportunities to achieve growth in the Taupo district for the purposes of this investment, incomes and employment by study) is blessed with enviable natural sector.
    [Show full text]
  • Historic Overview - Pokeno & District
    WDC District Plan Review – Built Heritage Assessment Historic Overview - Pokeno & District Pokeno The fertile valley floor in the vicinity of Pokeno has most likely been occupied by Maori since the earliest days of their settlement of Aotearoa. Pokeno is geographically close to the Tamaki isthmus, the lower Waikato River and the Hauraki Plains, all areas densely occupied by Maori in pre-European times. Traditionally, iwi of Waikato have claimed ownership of the area. Prior to and following 1840, that iwi was Ngati Tamaoho, including the hapu of Te Akitai and Te Uri-a-Tapa. The town’s name derives from the Maori village of Pokino located north of the present town centre, which ceased to exist on the eve of General Cameron’s invasion of the Waikato in July 1863. In the early 1820s the area was repeatedly swept by Nga Puhi war parties under Hongi Hika, the first of several forces to move through the area during the inter-tribal wars of the 1820s and 1830s. It is likely that the hapu of Pokeno joined Ngati Tamaoho war parties that travelled north to attack Nga Puhi and other tribes.1 In 1822 Hongi Hika and a force of around 3000 warriors, many armed with muskets, made an epic journey south from the Bay of Islands into the Waikato. The journey involved the portage of large war waka across the Tamaki isthmus and between the Waiuku River and the headwaters of the Awaroa and hence into the Waikato River west of Pokeno. It is likely warriors from the Pokeno area were among Waikato people who felled large trees across the Awaroa River to slow Hika’s progress.
    [Show full text]
  • News Release
    December 27, 2017 NEWS RELEASE www.jogmec.go.jp Japan Oil Gas and Metals National Corporation Division in Charge: Planning and Finance Division TEL:+81-3-6758-8001 FAX:+81-3-6758-8087 PR in Charge: Public Relations Division TEL:+81-3-6758-8106 FAX:+81-3-6758-8008 Report of “JAPAN-NEW ZEALAND GEOTHERMAL WORKSHOP” Japan Oil, Gas and Metals National Corporation (JOGMEC), GNS Science International Limited (GNS Science) and New Zealand Trade and Enterprise (NZTE) held the “JAPAN - NEW ZEALAND GEOTHERMAL WORKSHOP” in Rotorua, New Zealand, on the 20th and 21st of November 2017. This was the second time for JOGMEC and GNS Science to host the event, and more than 100 people joined from New Zealand and Japan. The workshop covered the fields of geothermal development, hot springs and geysers, and the environment, for each of the countries; and 14 speakers ranging from geothermal developers, local governments, research institutes, and representatives from Maori and local community groups presented their achievements and experience of sustainable geothermal development. JOGMEC and GNS Science also organized a field trip, which included visiting geothermal power plants, showing direct and cascade usage of geothermal, and geysers. This workshop was based on the MOU signed the 16th of July 2015, between JOGMEC and GNS Science. The MOU contained cooperative bilateral relations in order to facilitate technical cooperation in the field of evaluation and mitigation of environmental impacts, the development of survey methodologies, improving methods for management, the sustainability of geothermal reservoirs, and promotion of public acceptance of geothermal developments. New Zealand has more than 6 decades of history of geothermal power generation, and plenty of geothermal resources, with double the geothermal power plant capacity of Japan - even though Japan has 50 years’ experience of geothermal power generation.
    [Show full text]