Tubular Bioreactor for Hydrogen Sulphide Removal from Geothermal Power Station Cooling Water

Total Page:16

File Type:pdf, Size:1020Kb

Tubular Bioreactor for Hydrogen Sulphide Removal from Geothermal Power Station Cooling Water TUBULAR BIOREACTOR FOR HYDROGEN SULPHIDE REMOVAL FROM GEOTHERMAL POWER STATION COOLING WATER Rob Fullerton – Beca Ltd, New Zealand Taupo – North Island NZ Taupo Wairakei Wairakei Geothermal Power Station • Wairakei – one of earliest geothermal power stations in the world • commissioned 1958 – 1963, installed capacity 192MW • current capacity 157MW Cooling Water System . ~17 m3/s Waikato River water for direct condenser cooling A Station B Station CW in CW out CW = Cooling water Cooling Water System Geothermal steam 0.2m3/s Steam Turbines Cooling water + condensate Direct contact 17m3/s condensers 17.2m3/s Water pumps 157MW power Waikato River Waikato River The Challenge . H2S in the geothermal steam condenses into the cooling water and is discharged back to the river – aquatic impacts 3 . H2S concentration in discharge about 1000mg/m (~1mg/L) . Discharge Permit: H2S discharge to river ─ Prior 2012 : No consented limit - 10,000 kg/week ─ By 20 August 2012: 2,800 kg/week (72% reduction) ─ By 20 August 2016: 630 kg/week (94% reduction) . Requires sulphide reduction to ~50 mg/m3 The Challenge Geothermal steam containing H2S 0.2m3/s Cooling water Steam Turbines + condensate 17.2m3/s Direct contact 1000ppb H2S 17m3/s condensers To be reduced to 50ppb by Cooling water 2012 157MW power Waikato River Waikato River Sulphide Oxidising Bacteria - A Solution? • Need for strategy to control sulphide recognised • Thinking started in 2000 • SOB naturally occurring – esp. in geothermal areas • Biological sulphide oxidation - conversion of H2S to sulphate • SOB biofilm observed on existing outfall structure • Cooling water from power station 30 - 35oC, pH ~6, dissolved CO2 • Could SOB be used to achieve 95% sulphide removal? Initial Pilot Trials – 2000 - 2005 Algae overgrowth Sheets – channels - Pipes The Eureka Moment SOBs seem to grow best in fast moving flow Pilot Testing – Initial pipe trials Sulphide sampling • Biofilm established on inside of pipe – good H2S removal • High velocity prevents excessive biomass build-up • Lack of light prevents algal growth • Pipe bioreactor proved in concept Pilot Testing 2010 100mm dia. x 200m /150mm dia. X 400m SOB Biofilm Beginning section 100m End section 200m 100mm dia. x 200m results 150mm dia. x 400m results Sulphide Removal Model S = substrate concentration 푑푆 휇푚 퐵 푆 µ = maximum specific growth rate = m K = half-saturation constant 푑푡 푌 (퐾푠 + 푆) s B = biomass concentration Y = biomass yield • Sulphide concentration is low B >> S • biofilm quasi-steady state with constant thickness, viz. growth = detachment 푑푆 푆 dS/dt = rate of substrate change = −푣 v = maximum substrate utilisation rate 푑푡 푚 (퐾 + 푆) m 푠 ks = half saturation constant 2 • Calculate removal rate for each pipe segment (gH2S/m /d) • Fit to non-linear least squares Monod model Monod curve fitting 2 3 vm = 13.85 gH2S/m /d Ks = 235mg/m Design Curve Minimum pipe length ~160m +25% safety factor = 200m Pipe bioreactor - process concept 100mm dia. x 200m Outlet Velocity 0.8m/s sulphide Flow = 6.7L/s < 50ppb 100mm Sulphide oxidising bacteria biofilm Power station cooling water forms on pipe Inlet sulphide = 1000ppb inside surface Full scale pipe bioreactor concept plant Flow = 17m3/s ~2000 pipes x 200m in parallel 390km of pipe !! 200 x pipes per layer 10 layers Proposed sulphide treatment system 2012 Geothermal steam + H2S Pipe bioreactor Steam Turbines 17.2m3/s Direct contact 17m3/s condensers 4.2m3/s cooling 13m3/s 1000ppb water 50ppb H2S H2S 157MW power 2,800kg/week 17.2m3/s Waikato River Waikato River Proposed sulphide treatment system 2016 Geothermal steam + H2S 13.2m3/s 1000ppb H2S Pipe bioreactor Steam Turbines Direct contact 13m3/s condensers <80ppb H2S Cooling water 630kg/week 120MW power Waikato River Waikato River Full Scale design Challenges . Design began January 2011 . Never been done before – collaboration between contractor and designer . Physical constraints – high groundwater + hot (60oC) . Power station can’t stop – build off-line . Hydraulics – available head 1.5m – require pumping . Energy efficiency – design low head system . How to install 380km of 100mm dia. HDPE pipe Innovative “over – under” syphon 100m . Bioreactor pipe configuration ― 1890 pipes ― 5 banks of 378 pipes ― 42 pipes x 9 layers ― Magnetic flow meter each bank Bioreactor Layout Site Overview December 2011 Construction of pipe field . PE Pipe Design ─ Extruded on site ─ 100m lengths ─ No joints ─ 2.5mm wall ─ Embedded into weak cement matrix – “soilcrete” ─ 378km in 5 months Construction of pipe field Construction of pipe field Soilcrete embedment made from local pumice sand Construction of pipe field Construction of pipe field Return chamber – end pipe field Pump inlet channel Bioreactor outlet channel Bypass weir Bioreactor Performance Permit Compliance Full scale performance 3 . H2S concentration meeting target of >80% (~50mg/m ) . Power station meeting sulphide mass emission limit of 2,800 kg H2S/week . Optimisation of operating conditions to minimise power consumption . Current performance gives confidence to meet 2016 discharge limit of 630 kg H2S/week The world’s largest tubular bioreactor.
Recommended publications
  • 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]
  • 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]
  • Waikato River & Hydro Lakes
    Waikato River & Hydro Lakes Image Josh Willison E A S T E R N R1 E G I O N Waikato River Fishery The Waikato River flows out of Lake Taupō, through the central north island and Waikato regions before joining the sea south of Auckland at Port Waikato on the west coast. It is the longest river in NZ at about 425 km in length. A considerable length of the Waikato River flows within the Eastern Fish & Game region, and that portion also contains 5 hydro lakes. The Eastern region starts below Huka Falls near Taupō and ends just below Lake Maraetai. The river and its hydro lakes offer a huge amount of angling opportunity and many parts seldom see an angler. There are opportunities for trolling, fly and spin fishing, and bait fishing is also permitted on the Waikato River and its lakes. In summer when water temperatures rise excellent fishing can be had at the mouths of tributary streams where fish tend to congregate seeking cooler water conditions. As well as holding rainbow and brown trout the river and hydro lakes also contain other fish species in various areas including pest fish such as Rudd and carp and in some places catfish. If any of these species are caught anglers should kill them and dispose of them carefully and never transfer them to other waters. As the river and its lakes are used for hydro-power generation the water levels can fluctuate dramatically and without warning and due to this care is needed when on and around the river.
    [Show full text]
  • Te Mihi Power Station Contact Energy | Investor Day | 6 November 2018 6 November 20181 Disclaimer
    2018 Investor day Te Mihi Power Station Contact Energy | Investor day | 6 November 2018 6 November 20181 Disclaimer This presentation may contain projections or forward-looking statements regarding a variety of items. Such forward-looking statements are based upon current expectations and involve risks and uncertainties. Actual results may differ materially from those stated in any forward-looking statement based on a number of important factors and risks. Although management may indicate and believe that the assumptions underlying the forward-looking statements are reasonable, any of the assumptions could prove inaccurate or incorrect and, therefore, there can be no assurance that the results contemplated in the forward-looking statements will be realised. EBITDAF, underlying profit, free cash flow and operating free cash flow are non-GAAP (generally accepted accounting practice) measures. Information regarding the usefulness, calculation and reconciliation of these measures is provided in the supporting material. Furthermore, while all reasonable care has been taken in compiling this presentation, Contact accepts no responsibility for any errors or omissions. This presentation does not constitute investment advice. Contact Energy | Investor day | 6 November 2018 2 Agenda 1 Wholesale James Kilty 2 Geothermal advantage Mike Dunstall 3 Geothermal options James Kilty 4 Closing remarks and Q&A Dennis Barnes Contact Energy | Investor day | 6 November 2018 3 Wholesale – James Kilty Contact Energy | Investor day| 6 November 2018 Wholesale James Kilty – Chief Generation and Development Officer 1 Environment and strategy 2 Organising for success 3 Wholesale market outlook Contact Energy | Investor day | 6 November 2018 5 About Contact * - All figures as at June 30 2018 Contact Energy | Investor day | 6 November 2018 6 Sustainability is business as usual Sustainability is about integrating diverse interests into our strategy to ensure long term People value creation.
    [Show full text]
  • Paleohydrology and Sedimentology of a Post–1.8 Ka Breakout Flood from Intracaldera Lake Taupo, North Island, New Zealand
    Paleohydrology and sedimentology of a post–1.8 ka breakout flood from intracaldera Lake Taupo, North Island, New Zealand V. Manville* Geology Department, University of Otago, P.O. Box 56, Dunedin, New Zealand, and Wairakei Research Centre, Institute of Geological and Nuclear Sciences, Private Bag 2000, Taupo, New Zealand J. D. L. White Geology Department, University of Otago, P.O. Box 56, Dunedin, New Zealand B. F. Houghton Wairakei Research Centre, Institute of Geological and Nuclear Sciences, C. J. N. Wilson } Private Bag 2000, Taupo, New Zealand ABSTRACT INTRODUCTION The Taupo Volcanic Zone, in the central North Island of New Zealand, includes a high concen- Sudden releases of impounded water from Failures of natural or artificial dams have tration of calderas and composite cones, and lakes in volcanic regions constitute a major caused many of the largest known floods, and abundant volcanic lakes vulnerable to breakout and frequently repeated hazard. An outburst constitute a significant threat to life and property floods (Healy, 1975). We present evidence for the flood from Taupo caldera, New Zealand, (Costa, 1988; Costa and Schuster, 1988). Out- catastrophic release of ~20 km3 of water from the released ~20 km3 of water, within decades burst events have occurred in a variety of envi- Taupo caldera following blockage of the caldera- following an ignimbrite-emplacing eruption, ronments and settings, including the enormous lake outlet during the Taupo 1.8 ka eruption ca. 1.8 ka. Paleohydrologic reconstruction of Pleistocene outbursts from glacial and pluvial (Wilson and Walker, 1985). We reconstruct the the Taupo flood provides estimates of peak dis- lakes in North America (e.g., Baker, 1973; Baker paleohydraulic parameters associated with this charge at the outlet in the range 17 000–35 000 and Bunker, 1985; Lord and Kehew, 1987) and flood using dimensionless and physical models m3/s.
    [Show full text]
  • Notice Concerning Copyright Restrictions
    NOTICE CONCERNING COPYRIGHT RESTRICTIONS This document may contain copyrighted materials. These materials have been made available for use in research, teaching, and private study, but may not be used for any commercial purpose. Users may not otherwise copy, reproduce, retransmit, distribute, publish, commercially exploit or otherwise transfer any material. The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Under certain conditions specified in the law, libraries and archives are authorized to furnish a photocopy or other reproduction. One of these specific conditions is that the photocopy or reproduction is not to be "used for any purpose other than private study, scholarship, or research." If a user makes a request for, or later uses, a photocopy or reproduction for purposes in excess of "fair use," that user may be liable for copyright infringement. This institution reserves the right to refuse to accept a copying order if, in its judgment, fulfillment of the order would involve violation of copyright law. A GIA, pe Agenda item II.A.2 (b) GEOTHERMAL POWER DEVELOPMENT AT WAIRAKEI, NEW ZEALAND H. Christopher H. Armstead * New Zealand's goethermal power scheme at an earlier project, now abandoned, to install a Wairakei has been generating power since November chemical distillation plant at Wairakei, taking steam 1958. The load carried is 65 MW or more, and outputs at 50 lb/sq in. gauge and exhausting at * lb/sq in. up to 101 million kWh per week have been generated, gauge. This plant, which was to have been combined equivalent to about 12 per cent of the total energy with topping sets on the upstream side and condens- production in North Island.
    [Show full text]
  • The Taupo-Rotorua Hot-Plate
    111 Proc. 14th New Zealand Geothermal Workshop 1992 THE TAUPO-ROTORUA HOT-PLATE Alex McNabb Department of Mathematics Massey University, Palmerston North ABSTRACT - A qualitative model of the hydrothermal systems in the Taupo Volcanic Zone originating from a common hot-plate is presented and tested for viability against data from the Wairakei Geothermal Field and various available geophysical and chemical measurements. The concept of a deep dense stably-stratified hot brine layer forming the hot plate is presented as an inevitable consequence of the phase properties of the system at high pressures and temperatures. 1. INTRODUCTION 3. CONVECTION SYSTEM The centralNorth Island volcanic zone contains about fifteen The concept of a down-flow of cold ground-water over the geothermal fields lying in a thirty kilometre wide and one whole of the Taupo Volcanic Zone (TVZ) onto a hot plate hundred kilometre long strip stretching from Turangi to where it is heated and convected to the surface in a number of Kawerau. Detailed studies at Wairakei, Broadlands and plumes and discharged as geothermal activity is consistent Kawerau reveal these structures to be buoyant plumes of hot with the following data and analysis. The magmatic water chloride water rising in cold ground-water. They have a content of hydrothermal waters was estimated by Wilson cross-sectional area of 15 to 20 squarekilometres, a spacing (Ellis Wilson, 1960) to be at most 10 per cent, so that between plumes of about 15 kilometres, a plume most of the water discharged is of meteoric origin and enters temperature beneath a superficial boiling zone of about the system at the surface.
    [Show full text]
  • OHAAKI = a POINTER to the FUTURE Johnw
    Pmc. 1Ith New Zealand Geothermal Workshop 1989 OHAAKI = A POINTER TO THE FUTURE JohnW. Malcolmson Eiectricorp Production, Eiectridty Corporation of New Zealand Ltd ABSTRACT But the Minister's statement to Parliament in 1947 This paper briefly outlines the history of the really marks the beginning of the geothermal power development of the Ohaaki geothermal field and story. Conventional steam plant was virtually discusses some of the more recent legislative and damned for anything but standby purposes on the environmental issues that would now have to be grounds of high capital cost, long delivery and taken into account if a similar power station were cost and availability of fuel. Imported oil, even built today. These legislative and environmental then, was considered prohibitively expensive, and issues will make it more difficult to build future New Zealand Coal was seen as a very limited geothermal power stations in New Zealand. There resource. But the statement contains these are also a number of design concepts that may be significant words: approached differently If the project were comnenced today. These are briefly outlined and "There is one possibility which must not be discussed. overlooked and that i s the use of natural steam for power generation. It is proposed to investigate this matter without delay..." INTRODUCTION From that time on geothermal development was a reality. The DSIR began on the trail which made Electricorp will never build another Ohaaki! New Zealand the world leader in the investigation and application of geothermal power. By 1950 During this address I will cover the reasons why investigation had concentrated along a three and a Electricorp will never build another Ohaaki.
    [Show full text]
  • Habitat Characteristics of Geothermally Influenced Waters in the Waikato
    HABITAT CHARACTERISTICS OF GEOTHERMALLY INFLUENCED WATERS IN THE WAIKATO MARK I. STEVENS1, ASHLEY D. CODY2 AND IAN D. HOGG1 1Centre for Biodiversity and Ecology Research Department of Biological Sciences School of Science and Technology The University of Waikato Private Bag 3105 Hamilton, New Zealand Telephone 64-7-838 4139 Facsimile 64-7-838 4324 Email: [email protected] 2Geothermal and Geological Consultant 10 McDowell Street, Rotorua Email: [email protected] CBER Consultancy Report Number 25 Prepared for Environment Waikato, Hamilton June 2003 TABLE OF CONTENTS REPORT CONTEXT AND OVERVIEW .......................................................... 5 GEOTHERMAL SITES ....................................................................................... 8 1. ATIAMURI ................................................................................................... 8 1.1 Whangapoa Springs ............................................................................... 8 1.2 Matapan Road Springs ........................................................................ 13 1.3 Ohakuri Road Springs ......................................................................... 13 2. HOROHORO SPRINGS ............................................................................. 14 2.1 Horohoro Springs ................................................................................ 14 3. MOKAI ........................................................................................................ 18 3.1 Mulberry Road, Waipapa Stream ...................................................
    [Show full text]
  • 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.
    [Show full text]
  • Geology of the Wairakei-Tauhara Geothermal System, New Zealand
    Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Geology of the Wairakei-Tauhara Geothermal System, New Zealand Greg Bignall, Sarah Milicich, Ernesto Ramirez, Michael Rosenberg, Geoff Kilgour, Andrew Rae Private Bag 2000, Taupo, Wairakei Research Centre, GNS Science, New Zealand [email protected] Keywords: Geology, stratigraphy, structure, Wairakei- Defining the nature and extent of the formations Tauhara geothermal system, Taupo Volcanic Zone encountered by drilling is key to understanding the hydrology of the system. Knowledge of the strata and ABSTRACT structures at Wairakei-Tauhara has evolved during the 50 years of resource development, with more than 45 In the last 4 years to mid 2009, more than 45 geothermal production and injection wells drilled at Wairakei and wells (i.e., production, shallow (<600 m deep) steam, Tauhara in 2005-2009. Since 2005, well drilling to >1500 injection and exploration) have been drilled by Contact m depth (below -1000 mRSL) has provided new insights Energy Ltd. in the Wairakei and Tauhara Geothermal into the deep stratigraphy of Te Mihi area (western Fields. New information on the stratigraphy below ~1500 m Wairakei), and eastern/northeastern parts of Tauhara. The drilled depth at Wairakei (including the deepest well new insights include a series of previously unknown deep WK247, drilled to 2759 mCHF VD; -2246 mRSL), and volcanic formations; intersection of the greywacke previously unexplored parts of the Tauhara Geothermal basement at -1484 mRSL in the NE part of the Tauhara Field, has prompted a revision of their geology and Geothermal Field (TH17); at Wairakei the basement is now stratigraphic nomenclature.
    [Show full text]