An Assessment of Geothermal Direct Heat Use in New Zealand
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Waikato Sports Facility Plan Reference Document 2 June 2014
Waikato Sports Facility Plan Reference Document JUNE 2014 INTERNAL DRAFT Information Document Reference Waikato Sports Facility Plan Authors Craig Jones, Gordon Cessford Sign off Version Internal Draft 4 Date 4th June 2014 Disclaimer: Information, data and general assumptions used in the compilation of this report have been obtained from sources believed to be reliable. Visitor Solutions Ltd has used this information in good faith and makes no warranties or representations, express or implied, concerning the accuracy or completeness of this information. Interested parties should perform their own investigations, analysis and projections on all issues prior to acting in any way with regard to this project. Waikato Sports Facility Plan Reference Document 2 June 2014 Waikato Sports Facility Plan Reference Document 3 June 2014 CONTENTS 1.0 Introduction 5 2.0 Our challenges 8 3.0 Our Choices for Maintaining the network 9 4.0 Key Principles 10 5.0 Decision Criteria, Facility Evaluation & Funding 12 6.0 Indoor Court Facilities 16 7.0 Aquatic Facilities 28 8.0 Hockey – Artifical Turfs 38 9.0 Tennis Court Facilities 44 10.0 Netball – Outdoor Courts 55 11.0 Playing Fields 64 12.0 Athletics Tracks 83 13.0 Equestrian Facilities 90 14.0 Bike Facilities 97 15.0 Squash Court Facilities 104 16.0 Gymsport facilities 113 17.0 Rowing Facilities 120 18.0 Club Room Facilities 127 19.0 Bowling Green Facilities 145 20.0 Golf Club Facilities 155 21.0 Recommendations & Priority Actions 165 Appendix 1 - School Facility Survey 166 Waikato Sports Facility Plan Reference Document 4 June 2014 1.0 INTRODUCTION Plan Purpose The purpose of the Waikato Facility Plan is to provide a high level strategic framework for regional sports facilities planning. -
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. -
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 ......................................................................................................................... -
FT1 Australian-Pacific Plate Boundary Tectonics
Geosciences 2016 Annual Conference of the Geoscience Society of New Zealand, Wanaka Field Trip 1 25-28 November 2016 Tectonics of the Pacific‐Australian Plate Boundary Leader: Virginia Toy University of Otago Bibliographic reference: Toy, V.G., Norris, R.J., Cooper, A.F., Sibson, R.H., Little, T., Sutherland, R., Langridge, R., Berryman, K. (2016). Tectonics of the Pacific Australian Plate Boundary. In: Smillie, R. (compiler). Fieldtrip Guides, Geosciences 2016 Conference, Wanaka, New Zealand.Geoscience Society of New Zealand Miscellaneous Publication 145B, 86p. ISBN 978-1-877480-53-9 ISSN (print) : 2230-4487 ISSN (online) : 2230-4495 1 Frontispiece: Near-surface displacement on the Alpine Fault has been localised in an ~1cm thick gouge zone exposed in the bed of Hare Mare Creek. Photo by D.J. Prior. 2 INTRODUCTION This guide contains background geological information about sites that we hope to visit on this field trip. It is based primarily on the one that has been used for University of Otago Geology Department West Coast Field Trips for the last 30 years, partially updated to reflect recently published research. Copies of relevant recent publications will also be made available. Flexibility with respect to weather, driving times, and participant interest may mean that we do not see all of these sites. Stops are denoted by letters, and their locations indicated on Figure 1. List of stops and milestones Stop Date Time start Time stop Location letter Aim of stop Notes 25‐Nov 800 930 N Door Geol Dept, Dunedin Food delivery VT, AV, Nathaniel Chandrakumar go to 930 1015 N Door Geology, Dunedin Hansens in Kai Valley to collect van 1015 1100 New World, Dunedin Shoping for last food supplies 1115 1130 N Door Pick up Gilbert van Reenen Drive to Chch airport to collect other 1130 1700 Dud‐Chch participants Stop at a shop so people can buy 1700 1900 Chch‐Flockhill Drive Chch Airport ‐ Flockhill Lodge beer/wine/snacks Flockhill Lodge: SH 73, Arthur's Pass Overnight accommodation; cook meal 7875. -
2016 Pilot Waikato River Report Card: Methods and Technical Summary
2016 Pilot Waikato River Report Card: Methods and Technical Summary Prepared for Waikato River Authority March 2016 2016 Pilot Waikato River Report Card: Methods and Technical Summary Prepared by: Bruce Williamson (Diffuse Sources) John Quinn (NIWA) Erica Williams (NIWA) Cheri van Schravendijk-Goodman (WRRT) For any information regarding this report please contact: National Institute of Water & Atmospheric Research Ltd PO Box 11115 Hamilton 3251 Phone +64 7 856 7026 NIWA CLIENT REPORT No: HAM2016-011 Report date: March 2016 NIWA Project: WRA14203 Quality Assurance Statement Reviewed by: Dr Bob Wilcock Formatting checked by: Alison Bartley Approved for release by: Bryce Cooper Photo: Waikato River at Wellington Street Beach, Hamilton. [John Quinn, NIWA] 2016 Pilot Waikato River Report Card: Methods and Technical Summary Contents Summary ............................................................................................................................ 9 Reflections from the Project Team ..................................................................................... 12 1 Introduction ............................................................................................................ 18 1.1 Report Cards ........................................................................................................... 18 1.2 2015 Pilot Waikato River Report Cards .................................................................. 20 1.3 Purpose of this Technical Summary ....................................................................... -
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. -
Cumulative Impacts Assessment Along the Waikato
http://waikato.researchgateway.ac.nz/ Research Commons at the University of Waikato Copyright Statement: The digital copy of this thesis is protected by the Copyright Act 1994 (New Zealand). The thesis may be consulted by you, provided you comply with the provisions of the Act and the following conditions of use: Any use you make of these documents or images must be for research or private study purposes only, and you may not make them available to any other person. Authors control the copyright of their thesis. You will recognise the author’s right to be identified as the author of the thesis, and due acknowledgement will be made to the author where appropriate. You will obtain the author’s permission before publishing any material from the thesis. Responses of wild freshwater fish to anthropogenic stressors in the Waikato River of New Zealand A thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy at The University of Waikato by David W. West Department of Biological Sciences The University of Waikato Hamilton, New Zealand 2007 Abstract To assess anthropogenic impacts of point-source and diffuse discharges on fish populations of the Waikato River, compare responses to different discharges and identify potential sentinel fish species, we sampled wild populations of brown bullhead catfish (Ameiurus nebulosus, (LeSueur, 1819)), shortfin eel (Anguilla australis Richardson, 1848), and common bully (Gobiomorphus cotidianus McDowall, 1975) in the Waikato River. Sites upstream and downstream of: geothermal; bleached kraft mill effluent (BKME); sewage and thermal point-source discharges were sampled. At each site, the population parameters, relative abundance, age structure and individual indices such as: condition factor; and organ (gonad, liver, and spleen) somatic weight ratios; and number and size of follicles per female were assessed. -
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. -
Age and Growth of Wild-Caught Grass Carp in the Waikato River Catchment
Age and growth of wild-caught grass carp in the Waikato River catchment Cindy Baker and Joshua Smith DOC RESEARCH & DEVELOPMENT SERIES 238 Published by Science & Technical Publishing Department of Conservation PO Box 10–420 Wellington, New Zealand DOC Research & Development Series is a published record of scientific research carried out, or advice given, by Department of Conservation staff or external contractors funded by DOC. It comprises reports and short communications that are peer-reviewed. Individual contributions to the series are first released on the departmental website in pdf form. Hardcopy is printed, bound, and distributed at regular intervals. Titles are also listed in our catalogue on the website, refer www.doc.govt.nz under Publications, then Science and Research. © Copyright April 2006, New Zealand Department of Conservation ISSN 1176–8886 ISBN 0–478–14077–0 This is a client report commissioned by Waikato Conservancy and funded from the Science Advice Fund. It was prepared for publication by Science & Technical Publishing; editing and layout by Ian Mackenzie. Publication was approved by the Chief Scientist (Research, Development & Improvement Division), Department of Conservation, Wellington, New Zealand. In the interest of forest conservation, we support paperless electronic publishing. When printing, recycled paper is used wherever possible. CONTENTS Abstract 5 1. Introduction 6 2. Methods 6 3. Results 7 4. Discussion 9 5. Conclusions 10 6. Acknowledgements 10 7. References 11 Age and growth of wild-caught grass carp in the Waikato River catchment Cindy Baker and Joshua Smith National Institute of Water & Atmospheric Research Ltd, PO Box 11-115, Hamilton, New Zealand ABSTRACT Two relatively small grass carp (Ctenopharyngodon idellus) were captured in the lower Waikato River basin, New Zealand: one from Lake Whangape (1.65 kg, 435 mm fork length (FL)), and one from Pungarehu Canal, below the floodgates to Lake Waikare (3.1 kg, 570 mm FL). -
The First Crossing of the Southern Alps of New Zealand Author(S): Edward A
The First Crossing of the Southern Alps of New Zealand Author(s): Edward A. Fitz Gerald Source: The Geographical Journal, Vol. 7, No. 5 (May, 1896), pp. 483-499 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1773992 Accessed: 24-06-2016 18:50 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 137.99.31.134 on Fri, 24 Jun 2016 18:50:23 UTC All use subject to http://about.jstor.org/terms THE FIRST CROSSING OF THE SOUTHERN ALPS OF NEW ZEALAND. 483 :fixed by observation; 200 miles further west the dead reckoning agreed within half a mile of the longitude obtained by an occultation observed by Mr. Littledale, and compiled by Mr. Coles; and at Shushal, near the Ladak frontier, where the survey terminated, there was, after a traverse of 1700 miles, only a difference of 1J mile between Mr. Littledale's position and that given by the Trignometrical Survey of India. We not only have to thank Mr. -
PART ONE This Management Plan
F I S H AND GAME NEW ZEALAND WEST COAST REGION SPORTS FISH AND GAME MANAGEMENT PLAN To manage, maintain and enhance the sports fish and game resource in the recreational interests of anglers and hunters AIRPORT DRIVE PO BOX 179 HOKITIKA 1 2 FOREWORD FROM THE CHAIRMAN I am pleased to present the Sportsfish and Game Management Plan for the West Coast Fish and Game Council. This plan has been prepared in line with the statutory responsibilities of Fish and Game West Coast following extensive consultation with a wide range of stakeholders. It identifies issues and establishes goals, objectives, and implementation methods for all output classes. While it provides an excellent snapshot-in-time of Fish and Game West Coast it should be noted that, as well as ongoing issues, there are likely to be further challenges in the future which will have the potential to impact on angler/hunter opportunities and satisfaction. To this extent, this plan must be seen as a document designed to be capable of addressing changing requirements by way of the annual workplan and in response to ongoing input from anglers and hunters, as well as other users of fish and game habitat. The West Coast Fish and Game Council welcomes such input. Andy Harris Chairman 3 SPORTS FISH AND GAME MANAGEMENT PLAN To manage, maintain and enhance the sports fish and game resource in the recreational interests of anglers and hunters CONTENTS Foreword from the chairman ................................................. 3 Contents .................................................................................... 4 Executive summary .................................................................. 5 PART ONE This management plan ............................................................ 6 Introduction .............................................................................. 8 PART TWO Goals and objectives ............................................................ -
THE IMPORTANCE of INFREQUENT EARTHQUAKES ALONG the ALPINE FAULT by Andrew Wells
LANDSCAPE DISTURBANCE HISTORY IN WESTLAND, NEW ZEALAND: THE IMPORTANCE OF INFREQUENT EARTHQUAKES ALONG THE ALPINE FAULT A thesis submitted in partial fulfilment of the requirements for the Degree of Doctor of Philosophy at Lincoln University by Andrew Wells Lincoln University 1998 ii ABSTRACT Abstract of a thesis submitted in partial fulfilment of the requirements for the Degree of Doctor of Philosophy LANDSCAPE DISTURBANCE HISTORY IN WESTLAND, NEW ZEALAND: THE IMPORTANCE OF INFREQUENT EARTHQUAKES ALONG THE ALPINE FAULT by Andrew Wells This thesis investigates landscape disturbance history in Westland since 1350 AD. Specifically, I test the hypothesis that large-magnitude regional episodes of natural disturbance have periodically devastated portions of the landscape and forest, and that these were caused by infrequent earthquakes along the Alpine Fault. Forest stand history reconstruction was used to determine the timing and extent of erosion and sedimentation events that initiated new forest cohorts in a 1412 ha study area in the Karangarua River catchment, south Westland. Over 85 % of the study area was disturbed sufficiently by erosion/sedimentation since 1350 AD to initiate new forest cohorts. During this time four episodes of catchment-wide disturbance impacted the study area, and these took place about 1825 AD ± 5 years (Ruera episode), 1715 AD ± 5 years (Sparkling episode), 1615 AD ± 5 years (McTaggart episode), and 1445 AD ± 15 years (Junction episode). The three most recent episodes disturbed 10 %, 35-40 % and 32-50 % respectively of the study area. The Junction episode disturbed at least 6 % of the study area, but elimination of evidence by more recent disturbances prevented an upper limit being defined.