WETLAND MANAGEMENT PROFILE Great Artesian Basin Spring Wetlands
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Report to Office of Water Science, Department of Science, Information Technology and Innovation, Brisbane
Lake Eyre Basin Springs Assessment Project Hydrogeology, cultural history and biological values of springs in the Barcaldine, Springvale and Flinders River supergroups, Galilee Basin and Tertiary springs of western Queensland 2016 Department of Science, Information Technology and Innovation Prepared by R.J. Fensham, J.L. Silcock, B. Laffineur, H.J. MacDermott Queensland Herbarium Science Delivery Division Department of Science, Information Technology and Innovation PO Box 5078 Brisbane QLD 4001 © The Commonwealth of Australia 2016 The Queensland Government supports and encourages the dissemination and exchange of its information. The copyright in this publication is licensed under a Creative Commons Attribution 3.0 Australia (CC BY) licence Under this licence you are free, without having to seek permission from DSITI or the Commonwealth, to use this publication in accordance with the licence terms. You must keep intact the copyright notice and attribute the source of the publication. For more information on this licence visit http://creativecommons.org/licenses/by/3.0/au/deed.en Disclaimer This document has been prepared with all due diligence and care, based on the best available information at the time of publication. The department holds no responsibility for any errors or omissions within this document. Any decisions made by other parties based on this document are solely the responsibility of those parties. Information contained in this document is from a number of sources and, as such, does not necessarily represent government or departmental policy. If you need to access this document in a language other than English, please call the Translating and Interpreting Service (TIS National) on 131 450 and ask them to telephone Library Services on +61 7 3170 5725 Citation Fensham, R.J., Silcock, J.L., Laffineur, B., MacDermott, H.J. -
Hydrochemical Zoning and Chemical Evolution of the Deep Upper Jurassic Thermal Groundwater Reservoir Using Water Chemical and Environmental Isotope Data
water Article Hydrochemical Zoning and Chemical Evolution of the Deep Upper Jurassic Thermal Groundwater Reservoir Using Water Chemical and Environmental Isotope Data Florian Heine * , Kai Zosseder and Florian Einsiedl * Chair of Hydrogeology, Department of Civil, Geo and Environmental Engineering, Technical University of Munich, Arcisstr. 21, 80333 Munich, Germany; [email protected] * Correspondence: fl[email protected] (F.H.); [email protected] (F.E.); Tel.: +49-(89)-289-25833 (F.E.) Abstract: A comprehensive hydrogeological understanding of the deep Upper Jurassic carbonate aquifer, which represents an important geothermal reservoir in the South German Molasse Basin (SGMB), is crucial for improved and sustainable groundwater resource management. Water chemical data and environmental isotope analyses of δD, δ18O and 87Sr/86Sr were obtained from groundwater of 24 deep Upper Jurassic geothermal wells and coupled with a few analyses of noble gases (3He/4He, 40Ar/36Ar) and noble gas infiltration temperatures. Hierarchical cluster analysis revealed three major water types and allowed a hydrochemical zoning of the SGMB, while exploratory factor analyses identified the hydrogeological processes affecting the water chemical composition of the thermal water. Water types 1 and 2 are of Na-[Ca]-HCO3-Cl type, lowly mineralised and have been recharged 87 86 under meteoric cold climate conditions. Both water types show Sr/ Sr signatures, stable water isotopes values and calculated apparent mean residence times, which suggest minor water-rock Citation: Heine, F.; Zosseder, K.; interaction within a hydraulically active flow system of the Northeastern and Southeastern Central Einsiedl, F. Hydrochemical Zoning Molasse Basin. This thermal groundwater have been most likely subglacially recharged in the south and Chemical Evolution of the Deep of the SGMB in close proximity to the Bavarian Alps with a delineated northwards flow direction. -
Heritage of the Birdsville and Strzelecki Tracks
Department for Environment and Heritage Heritage of the Birdsville and Strzelecki Tracks Part of the Far North & Far West Region (Region 13) Historical Research Pty Ltd Adelaide in association with Austral Archaeology Pty Ltd Lyn Leader-Elliott Iris Iwanicki December 2002 Frontispiece Woolshed, Cordillo Downs Station (SHP:009) The Birdsville & Strzelecki Tracks Heritage Survey was financed by the South Australian Government (through the State Heritage Fund) and the Commonwealth of Australia (through the Australian Heritage Commission). It was carried out by heritage consultants Historical Research Pty Ltd, in association with Austral Archaeology Pty Ltd, Lyn Leader-Elliott and Iris Iwanicki between April 2001 and December 2002. The views expressed in this publication are not necessarily those of the South Australian Government or the Commonwealth of Australia and they do not accept responsibility for any advice or information in relation to this material. All recommendations are the opinions of the heritage consultants Historical Research Pty Ltd (or their subconsultants) and may not necessarily be acted upon by the State Heritage Authority or the Australian Heritage Commission. Information presented in this document may be copied for non-commercial purposes including for personal or educational uses. Reproduction for purposes other than those given above requires written permission from the South Australian Government or the Commonwealth of Australia. Requests and enquiries should be addressed to either the Manager, Heritage Branch, Department for Environment and Heritage, GPO Box 1047, Adelaide, SA, 5001, or email [email protected], or the Manager, Copyright Services, Info Access, GPO Box 1920, Canberra, ACT, 2601, or email [email protected]. -
Groundwater Storage Dynamics in the World's
Interactive comment on “Groundwater storage dynamics in the world’s large aquifer systems from GRACE: uncertainty and role of extreme precipitation” by Mohammad Shamsudduha and Richard G. Taylor Marc Bierkens (Referee #1) [email protected] Received and published: 2 January 2020 Reviewer’s comments are italicised, and our responses (R) and revisions (REVISION) are provided in normal fonts. General comments The authors use the results of three different GRACE-based TWS methods and 4 Land surface models to generate an ensemble of groundwater storage anomalies. These are subsequently analyzed by a non-parametric statistical method to separate seasonal signals from non-linear trends and residuals. The main message of the paper is that trends in GWS anomalies (ΔGWS), if existing, are non-linear in the vast majority of main aquifer systems and that rainfall anomalies play an important role in explaining these non-linear trends. I enjoyed reading the paper. I find that it is a well-written with an important message that deserves publication. However, I have a few comments. Moderate comments: 1. I find the lack of reference to estimates based on global hydrological models (GHMS) remarkable. The first spatially distributed global assessment of depletion rates where based on such models and, albeit indirect, should be used in the discussion. They are the basis for the “narratives on global groundwater depletion” that are mentioned in the discussion and the abstract (See https://iopscience.iop.org/article/10.1088/1748- 9326/ab1a5f/meta for an overview of these studies). This is the more remarkable, given that the authors do use Land Surface Models (LSMs) to estimate ΔGWS from GRACE ΔTWS. -
Survey Guidelines for Australia's Threatened Fish
Survey guidelines for Australia’s threatened fish Guidelines for detecting fish listed as threatened under the Environment Protection and Biodiversity Conservation Act 1999 Authorship and acknowledgments This report updates and expands on a report prepared in May 2004 by Australian Museum ichthyologist John Pogonoski and approved by AMBS Senior Project Manager Jayne Tipping. The current (2011) report includes updates to the 2004 report and additional information regarding recently listed species, current knowledge of all the listed species and current survey techniques. This additional information was prepared by Australian Museum ichthyologists Dr Doug Hoese and Sally Reader. Technical assistance was provided by AMBS ecologists Mark Semeniuk and Lisa McCaffrey. AMBS Senior Project Manager Glenn Muir co- ordinated the project team and reviewed the final report. These guidelines could not have been produced without the assistance of a number of experts. Individuals who have shared their knowledge and experience for the purpose of preparing this report are indicated in Appendix A. Disclaimer The views and opinions contained in this document are not necessarily those of the Australian Government. The contents of this document have been compiled using a range of source materials and while reasonable care has been taken in its compilation, the Australian Government does not accept responsibility for the accuracy or completeness of the contents of this document and shall not be liable for any loss or damage that may be occasioned directly or indirectly through the use of or reliance on the contents of the document. © Commonwealth of Australia 2011 This work is copyright. You may download, display, print and reproduce this material in unaltered form only (retaining this notice) for your personal, non-commercial use or use within your organisation. -
Groundwater and Global Change: Trends, Opportunities and Challenges
SIDE PUBLICATIONS SERIES :01 Groundwater and Global Change: Trends, Opportunities and Challenges Jac van der Gun UNITED NATIONS WORLD WATER ASSESSMENT PROGRAMME Published in 2012 by the United Nations Educational, Scientific and Cultural Organization 7, Place de Fontenoy, 75352 Paris 07 SP, France © UNESCO 2012 All rights reserved ISBN 978-92-3-001049-2 The designations employed and the presentation of material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The ideas and opinions expressed in this publication are those of the authors; they are not necessarily those of UNESCO and do not commit the Organization. Photographs: Cover: © africa924 / Shutterstock © Rolffimages / Dreamstime © Frontpage / Shutterstock.com p.i: © holgs / iStockphoto p.ii: © Andrew Zarivny p.2: © Aivolie / Shutterstock p.4: © Jorg Hackemann / Shutterstock p.17: © Jac van der Gun p.31: © Aivolie / Shutterstock p.33: © Hilde Vanstraelen Original concept (cover and layout design) of series: MH Design / Maro Haas Layout: Pica Publishing LTD, London–Paris / Roberto Rossi Printed by: UNESCO Printed in France Groundwater and global change: Trends, opportunities and challenges Author: Jac van der Gun Contributors: Luiz Amore (National Water Agency, Brazil), Greg Christelis (Ministry of Agriculture, Water and Forestry, Nambia), Todd Jarvis (Oregon State University, USA), Neno Kukuric (UNESCO-IGRAC) Júlio Thadeu Kettelhut (Ministry of the Environment, Brazil), Alexandros Makarigakis (UNESCO, Ethiopia), Abdullah Abdulkader Noaman (Sana’a University, Yemen), Cheryl van Kempen (UNESCO-IGRAC), Frank van Weert (UNESCO-IGRAC). -
Environment Management Manual
Procedure Document No. 2617 Document Title Environment Management Manual Area HSE Issue Date 23 August 2017 Major Process Environment Sub Process Management Review Authoriser Jacqui McGill – Asset President Version Number 16 Olympic Dam 1 INTRODUCTION ............................................................................................................................ 3 1.1 Glossary and defined terms ................................................................................................. 3 1.2 Purpose and scope .............................................................................................................. 3 1.3 How to use the EPMP .......................................................................................................... 4 2 REGULATORY FRAMEWORK ..................................................................................................... 5 2.1 Key legal requirements ........................................................................................................ 5 2.2 Compliance with routine reporting obligations ..................................................................... 6 2.3 Amendments to the EPMP ................................................................................................... 6 2.4 Environmental outcomes and criteria .................................................................................. 7 2.5 Enforcement process (Indenture and Mining Code) ............................................................ 7 2.6 ALARA and best practicable -
Carmichael Coal Mine Project Great Artesian Basin Springs Research
Great Artesian Bain Springs Research Plan Carmichael Coal Mine Project Great Artesian Basin Springs Research Plan Version 6c, 10 September 2019 1 | P a g e Great Artesian Bain Springs Research Plan Document Control & Version Control Document Title: Great Artesian Basin Springs Research Plan Document No: CCMP-000000-PLN-HY-000100 Document Type: Plan First Issue Date: 26 July 2018 Rev Issue Date Description of Revisions Made Author Code 1 26/6/18 Submission to the Adani Commonwealth Government Jacobs 2 6/12/18 Updates based on feedback from Adani the Commonwealth Government CDM Smith 3 22/3/19 Updates based on feedback from Adani the Commonwealth Government CDM Smith 4 27/6/19 Updates based on feedback from Adani the Commonwealth Government CDM Smith 5 7/8/19 Updates based on feedback from Adani the Commonwealth Government 6 22/8/19 Updates based on feedback from Adani the Commonwealth Government 6a 28/8/19 Minor correction Adani 6b 6/9/19 Minor correction Adani 6c 10/9/19 Minor correction Adani 2 | P a g e Great Artesian Bain Springs Research Plan Contents 1 Introduction .................................................................................................................................... 7 1.1 Project Description .................................................................................................................. 7 1.2 EBPC Act Approval 2010/5736, Condition 25 ......................................................................... 9 1.3 Document structure ........................................................................................................... -
Supplement of Earth Syst
Supplement of Earth Syst. Dynam., 11, 755–774, 2020 https://doi.org/10.5194/esd-11-755-2020-supplement © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of Groundwater storage dynamics in the world’s large aquifer systems from GRACE: uncertainty and role of extreme precipitation Mohammad Shamsudduha and Richard G. Taylor Correspondence to: Mohammad Shamsudduha ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. Supplementary Table S1. Characteristics of the world’s 37 large aquifer systems according to the WHYMAP database including aquifer area, total number of population, proportion of groundwater (GW)-fed irrigation, mean aridity index, mean annual rainfall, variability in rainfall and total terrestrial water mass (ΔTWS), and correlation coefficients between monthly ΔTWS and precipitation with reported lags. ) 2 2) Correlation between between Correlation precipitation TWS and (lag in month) GW irrigation (%) (%) GW irrigation on based zones Climate Aridity indices Mean (2002-16) annual precipitation (mm) Rainfall variability (%) (cm TWS variance WHYMAP aquifer number name Aquifer Continent (million)Population area (km Aquifer Nubian Sandstone Hyper- 1 Africa 86.01 2,176,068 1.6 30 12.1 1.5 0.16 (13) Aquifer System arid Northwestern 2 Sahara Aquifer Africa 5.93 1,007,536 4.4 Arid 69 17.3 1.9 0.19 (8) System Murzuk-Djado Hyper- 3 Africa 0.35 483,817 2.3 8 36.6 1.3 0.20 (-8) Basin arid Taoudeni- Hyper- 4 Africa 0.35 -
Australia's Desert Fish Have Flourished for Millennia in a Changeable Environment TEXT by ROBERT LEHANE and BARRY SKIPSEY
Australia's desert fish have flourished for millennia in a changeable environment TEXT BY ROBERT LEHANE AND BARRY SKIPSEY Afloat in the Red Centre, pioneering freshwater fish researcher Hamar Midgley, assisted by his wife Mary at the oars, plies his science on one of the Finke River's permanent waterholes - refuges during dry times I for Australia's remarkable desert fish. About 10 species are found widely throughout Central Australia. The Midgleys found five at this NT waterhole, with bony bream, foreground, the most common. APRIL - JUNE 1996 105 • CHORUS OF BIRDS had shat- are literally the gene pools of Aus- tered the icy calm of the tralia's desert fish. Like the outback's A. winter sunriseI tanhrd woken other ephemeral watercourses, the peered Finke has only a few permanent holes, flap of my swag as a warming yellow but it's in them that fish survive dry gjow rose over the Finke River water- times, dodging predators and endur- hole. With each passing minute, the ing scorching summer days and bit- red dunes bordering the opposite bank terly cold winter nights. Then, like ripened to a richer hue. desert flowers, these remnant popula- Alerted by splashing, I shifted my tions explode into life when rains gaze back to the waterhole, where I come, multiplying and dispersing with saw — to my astonishment — a pair of long-awaited floodwaters to repopu- pelicans. I'd never seen these grand late the rivers and ephemeral lakes. birds so deep in Central Australia — To learn about these tenacious ani- I was only 110 kilometres south of mals, Fa joined an expedition led by Alice Springs. -
Malacologia, 1989, 31(1): 1-140 an Endemic Radiation Of
MALACOLOGIA, 1989, 31(1): 1-140 AN ENDEMIC RADIATION OF HYDROBIID SNAILS FROM ARTESIAN SPRINGS IN NORTHERN SOUTH AUSTRALIA: THEIR TAXONOMY, PHYSIOLOGY, DISTRIBUTION AND ANATOMY By W.F. Ponder, R. Hershler*, and B. Jenkins, The Australian Museum, Sydney South, NSW, 2000, Australia CONTENTS INTRODUCTION Absence of fauna The mound springs—a brief description Conservation Geomorphology and water chemistry ACKNOWLEDGMENTS Spring groups and complexes REFERENCES Climate APPENDIX 1 MATERIALS AND METHODS List of stations Taxonomy List of springs not sampled Taxonomic rationale Stations at which no hydrobiids were Materials collected Methods Locality maps Characters APPENDIX 2 Anatomy Tables of measurements Physiology Materials Methods ABSTRACT RESULTS Taxonomy Artesian springs between Marree and Fonscochlea Oodnadatta contain an endemic fauna of Fonscochlea (Wolfgangia) hydrobiid snails that have undergone an Trochidrobia adaptive radiation in which habitat parti- Anatomy tioning and size displacement are clearly Anatomical description of evident. Ten new species in two new en- Fonscochlea accepta demic genera, Fonscochlea and Trochidro- Anatomical description of bia, are described. Three of the species of Trochidrobia punicea Fonscochlea are divided into a total of six Physiology geographic forms, which are not formally named. Two geographic forms are restricted DISCUSSION to single springs, the remainder being found Evolution and relationships of fauna in several springs, spring groups, or com- Geological history plexes of springs. Fonscochlea is divided in Relationships of mound-spring inver- to two subgenera, Fonscochlea s.s. contain- tebrates ing five species and Wolfgangia with a single Evolution of species within mound species. springs Both genera are represented in most Dispersal springs, with up to five taxa present in single springs in the Freeling Springs Group and in Environmentally-induced variation some of the other springs in the northern part Ecology and behaviour of the spring system. -
Hydrogeological Overview of Springs in the Great Artesian Basin
Hydrogeological Overview of Springs in the Great Artesian Basin M. A. (Rien) Habermehl1 Abstract The Great Artesian Basin (GAB) is a regional groundwater system consisting of aquifers and confining beds within the sedimentary Eromanga, Surat and Carpentaria Basins. They under- lie arid to semi-arid regions across 1.7 million km2, or one-fifth of the Australian continent. Artesian springs of the GAB are naturally occurring outlets of groundwater from the confined aquifers. Springs predominantly occur near the eastern recharge margins and the south-western and western discharge margins of the GAB. These zones of natural groundwater discharge represent areas of permanent water, with widely recognised cultural, spiritual and subsistence importance to Indigenous people for tens of thousands of years. The unique hydrogeological environments – discharge, hydrochemistry and substrate – support a range of endemic flora and fauna protected under the EPBC Act (1999). Springs have formed in many areas across the GAB; however, the largest concentrations occur near the south-western margins of the basin. Supporting these flowing artesian springs is a multi-layered aquifer system, comprising Jurassic- to Cretaceous-age sandstones and siltstone, and confining beds of mudstones. Hydrogeological, hydrochemical and isotope hydrology studies show that most artesian springs and flowing water bores in the GAB derive their water from the main Jurassic–Lower Cretaceous Cadna-owie Formation – Hooray Sandstone aquifer and its equivalents. Focusing on springs in South Australia, this paper provides a summary of the hydrogeology of the GAB, including zones of recharge and regional groundwater flow directions, with a major focus on summarising under- standing of the occurrence and formation of springs.