Recovery of Copper by Solution Mining Methods David F
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In Situ Leach (ISL) Mining of Uranium
In Situ Leach (ISL) Mining of Uranium (June 2009) l Most uranium mining in the USA and Kazakhstan is now by in situ leach methods, also known as in situ recovery (ISR). l In USA ISL is seen as the most cost effective and environmentally acceptable method of mining, and Australian experience supports this. l Australia's first ISL uranium mine is Beverley, which started operation late in 2000. The proposal for Honeymoon has government approval and it is expected to be operating in 2008. Conventional mining involves removing mineralised rock (ore) from the ground, breaking it up and treating it to remove the minerals being sought. In situ leaching (ISL), also known as solution mining, or in situ recovery (ISR) in North America, involves leaving the ore where it is in the ground, and recovering the minerals from it by dissolving them and pumping the pregnant solution to the surface where the minerals can be recovered. Consequently there is little surface disturbance and no tailings or waste rock generated. However, the orebody needs to be permeable to the liquids used, and located so that they do not contaminate ground water away from the orebody. Uranium ISL uses the native groundwater in the orebody which is fortified with a complexing agent and in most cases an oxidant. It is then pumped through the underground orebody to recover the minerals in it by leaching. Once the pregnant solution is returned to the surface, the uranium is recovered in much the same way as in any other uranium plant (mill). In Australian ISL mines (Beverley and the soon to be opened Honeymoon Mine) the oxidant used is hydrogen peroxide and the complexing agent sulfuric acid. -
Understanding Fluid–Rock Interactions and Lixiviant/Oxidant Behaviour for the In-Situ Recovery of Metals from Deep Ore Bodies
School of Earth and Planetary Science Department of Applied Geology Understanding Fluid–Rock Interactions and Lixiviant/Oxidant Behaviour for the In-situ Recovery of Metals from Deep Ore Bodies Tania Marcela Hidalgo Rosero This thesis is presented for the degree of Doctor of Philosophy of Curtin University February 2020 1 Declaration __________________________________________________________________________ Declaration To the best of my knowledge and belief, I declare that this work of thesis contains no material published by any other person, except where due acknowledgements have been made. This thesis contains no material which has been accepted for the award of any other degree or diploma in any university. Tania Marcela Hidalgo Rosero Date: 28/01/2020 2 Abstract __________________________________________________________________________ Abstract In-situ recovery (ISR) processing has been recognised as a possible alternative to open- pit mining, especially for low-grade resources. In ISR, the fluid–rock interaction between the target ore and the lixiviant results in valuable- (and gangue-) metal dissolution. This interaction is achieved by the injection and recovery of fluid by means of strategically positioned wells. Although the application of ISR has become more common (ISR remains the preferential processing technique for uranium and has been applied in pilot programs for treating oxide zones in copper deposits), its application to hard-rock refractory and low-grade copper-sulfide deposits is still under development. This research is focused on the possible application of ISR to primary copper sulfides usually found as deep ores. Lixiviant/oxidant selection is an important aspect to consider during planning and operation in the ISR of copper-sulfide ores. -
Uranium in Situ Leaching
IAEA-TECDOC-720 Uranium in situ leaching Proceedings Technicala of Committee Meeting held in Vienna, 5-8 October 1992 INTERNATIONAL ATOMIC ENERGY AGENC\ /A Y The IAEA doe t normallsno y maintain stock f reportso thin si s series. However, microfiche copies of these reports can be obtained from IIMIS Clearinghouse International Atomic Energy Agency Wagramerstrasse5 P.O. Box 100 A-1400 Vienna, Austria Orders shoul accompaniee db prepaymeny db f Austriao t n Schillings 100,- in the form of a cheque or in the form of IAEA microfiche service coupons which may be ordered separately from the INIS Clearinghouse. Copies of this IAEA-TECDOC may be obtained from: Nuclear Material Fued san l Cycle Technology Section International Atomic Energy Agency Wagramerstrasse 5 P.O. Box 100 A-1400 Vienna, Austria URANIU SITMN I U LEACHING IAEA, VIENNA, 1993 IAEA-TECDOC-720 ISSN 1011-4289 Printe IAEe th AustriAn y i d b a September 1993 FOREWORD The IAEA's latest published estimates show that nuclear power production worldwide will maintain modest growth well into the next century. These estimates indicate that nuclear energy production will gro averagn wo 1.5y eb % 2.5o t year %pe r worldwide ove nex e decadeso rth tw t s i t I . for this reason that despite the continuing depressed uranium market, the question of uranium supply demand an d remain issun sa e that needaddressee b o st monitoredd dan developmentsw Ne . e du , to the recent entry of the Commonwealth of Independent States and China into the uranium market, increase such a need. -
Supergene Mineralisation of the Boyongan Porphyry Copper-Gold Deposit, Surigao Del Norte, Philippines
Supergene Mineralisation of the Boyongan Porphyry Copper-Gold Deposit, Surigao del Norte, Philippines by Allan Maglaya Ignacio B.Sc. Geology, National Institute of Geological Sciences University of the Philippines Thesis submitted in partial fulfilment of the requirements of the Masters of Economic Geology Degree Centre for Ore Deposit Research, University of Tasmania December, 2005 DECLARATION OF ORIGINALITY This thesis contains no material which has been accepted for a degree of diploma by the University of Tasmania or any other institution, except by way of background information and duly acknowledged in the thesis, and contains no previous material previously pub- lished or written by another person except where due acknowledgement is given. Allan Maglaya Ignacio 01 December 2005 _________________________ STATEMENT OF AUTHORITY OF ACCESS This thesis may not to be made available for loan or copying for 1.5 years following the date this statement was signed. Following that time, the thesis may be available for loan and lim- ited copying in accordance with Copyright Act 1968. Allan Maglaya Ignacio 01 December 2005 _________________________ TABLE OF CONTENTS Page (s) LIST OF FIGURES …………………………………………………….. i - iii LIST OF APPENDICES ………………………………………………… iv ACKNOWLEDGMENTS ………………………………………………. v ABSTRACT ……………………………………………………………... vi - vii 1.0 INTRODUCTION ………………………………………………………. 1 - 8 1.1 Introduction …………………………………………………………. 1 1.2 Aims and Objectives ……………………………………………….. 1 1.3 Methods Employed …………………………………………………. 2 1.4 Location and Accessibility …………………………………………. 3 1.5 Climate ……………………………………………………………... 5 1.6 Previous Work ……………………………………………………… 5 2.0 GEOLOGICAL SETTING ………………………………………………. 9 - 37 2.1 Introduction ………………………………………………………. 9 2.2 Regional Tectonics …………….…………………………………. 9 2.3 Regional and Local Stratigraphy ………………………………... 11 2.3.1 Basement (Cretaceous-Paleogene) ………………………. 11 2.3.2 Bacuag Formation (Oliogocene-Miocene) .…………….. -
Sell-1559, Leaching
CONTACT INFORMATION Mining Records Curator Arizona Geological Survey 416 W. Congress St., Suite 100 Tucson, Arizona 85701 520-770-3500 http://www.azgs.az.gov [email protected] The following file is part of the James Doyle Sell Mining Collection ACCESS STATEMENT These digitized collections are accessible for purposes of education and research. We have indicated what we know about copyright and rights of privacy, publicity, or trademark. Due to the nature of archival collections, we are not always able to identify this information. We are eager to hear from any rights owners, so that we may obtain accurate information. Upon request, we will remove material from public view while we address a rights issue. CONSTRAINTS STATEMENT The Arizona Geological Survey does not claim to control all rights for all materials in its collection. These rights include, but are not limited to: copyright, privacy rights, and cultural protection rights. The User hereby assumes all responsibility for obtaining any rights to use the material in excess of “fair use.” The Survey makes no intellectual property claims to the products created by individual authors in the manuscript collections, except when the author deeded those rights to the Survey or when those authors were employed by the State of Arizona and created intellectual products as a function of their official duties. The Survey does maintain property rights to the physical and digital representations of the works. QUALITY STATEMENT The Arizona Geological Survey is not responsible for the accuracy of the records, information, or opinions that may be contained in the files. The Survey collects, catalogs, and archives data on mineral properties regardless of its views of the veracity or accuracy of those data. -
Characterization & Modification of Copper and Iron Oxide Nanoparticles for Application As Absorber Material in Silicon Base
Characterization & Modification of Copper and Iron Oxide Nanoparticles for Application as Absorber Material in Silicon based Thin Film Solar Cells Maurice René Nuys Member of the Helmholtz Association Member of the Energie & Umwelt / Energie & Umwelt / Energy & Environment Energy & Environment Band/ Volume 291 Band/ Volume 291 ISBN 978-3-95806-096-8 ISBN 978-3-95806-096-8 Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment Band / Volume 291 Forschungszentrum Jülich GmbH Institute of Energy and Climate Research Photovoltaics (IEK-5) Characterization & Modification of Copper and Iron Oxide Nanoparticles for Application as Absorber Material in Silicon based Thin Film Solar Cells Maurice René Nuys Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment Band / Volume 291 ISSN 1866-1793 ISBN 978-3-95806-096-8 Bibliographic information published by the Deutsche Nationalbibliothek. The Deutsche Nationalbibliothek lists this publication in the Deutsche Nationalbibliografie; detailed bibliographic data are available in the Internet at http://dnb.d-nb.de. Publisher and Forschungszentrum Jülich GmbH Distributor: Zentralbibliothek 52425 Jülich Tel: +49 2461 61-5368 Fax: +49 2461 61-6103 Email: [email protected] www.fz-juelich.de/zb Cover Design: Grafische Medien, Forschungszentrum Jülich GmbH Printer: Grafische Medien, Forschungszentrum Jülich GmbH Copyright: Forschungszentrum Jülich 2015 Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment, Band / Volume 291 D 82 (Diss. RWTH Aachen University, 2015) ISSN 1866-1793 ISBN 978-3-95806-096-8 The complete volume is freely available on the Internet on the Jülicher Open Access Server (JuSER) at www.fz-juelich.de/zb/openaccess. Neither this book nor any part of it may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, microfilming, and recording, or by any information storage and retrieval system, without permission in writing from the publisher. -
(Hypogene) Sulphate Minerals in Ore Deposits2
ECONOMIC GEOLOGY WITH WHICH IS INCORPORATED THE AMERICAN GEOLOGIST VOL. XIV DECEMBER, I9I 9 No. 8 PRIMARY (HYPOGENE) SULPHATE MINERALS IN ORE DEPOSITS2 B. S. BUTLER. CONTENTS. PAOE. Introduction ......................................................... Sulphate Minerals .................................................... Character of Ore Solutions as Indicated by Volcanic Emanations ....... 590 Conditions of Format'ion of Sulphur Trioxide ......................... 593 Formation of Sulphuric Acid in Nature ............................... 594 Formation of Primary Sulphate Minerals ............................. 596 Summary ............................................................ 6o8 Acknowledgment .................................. -................... 609 INTRODUCTION. In studyingore depositsthe writer has severaltimes been con.- fronted with the problemof accountingfor the formation of sulphateminerals that are apparentlyprimary. These minerals occur at placeswhere no evidencecan be found of their forma- tion by surface oxidation. Either they were formed directly 'by igneousemanations or, if they were formed by surfaceagencies, those agenciesmust have effectedthe depositionof other asso- ciatedminerals that would ordinarily •beregarded as of hypogene origin. An attemptwill be madeto analyzethis problemby start- ing with the belief, 'basedon deductionsfrom field observations, that the sulphatesin certaindeposits have •een formed directlyby x Published by permission of the Director, United State Geological Survey. 58x 5.82 B. S. BUTLER. -
Changes in Bornite (Cu5fes4) After Heating in Air: Mössbauer Effect
Vol. 134 (2018) ACTA PHYSICA POLONICA A No. 5 Proceedings of the All-Polish Seminar on Mössbauer Spectroscopy, Goniądz, Poland, June 17–20, 2018 Changes in Bornite (Cu5FeS4) after Heating in Air: Mössbauer Effect Study M. Kądziołka-Gaweła;∗ and Z. Adamczykb aInstitute of Physics, University of Silesia in Katowice, 75 Pułku Piechoty 1a, 41-500 Chorzów, Poland bInstitute of Applied Geology, Silesian University of Technology, Akademicka 2, 44-100 Gliwice, Poland The phase transitions and structural behaviour in natural bornite sample were investigated after heat treatment in air in a temperature range of (180÷500) ◦C using high-resolution Faraday, X-ray diffraction and 57Fe Mössbauer spectroscopy studies. X-ray diffraction and the Mössbauer spectroscopy results show that polymorph phases can exist only at high temperatures, and at a temperature of 220 ◦C a process of decomposition of bornite structure starts. Hematite is a main Fe-bearing phase and Cu is located mainly in cooper oxides present in the sample after annealing at 500 ◦C. DOI: 10.12693/APhysPolA.134.1044 PACS/topics: 76.80.+y, 91.60.–x, 88.10.jn 1. Introduction 2. Experimental procedure Bornite (Cu5FeS4), also known as peacock ore, is a The natural sample of bornite was chosen for detailed widespread natural mineral that is composed of non- analyses. The bornite sample was taken from the Per- toxic and earth-abundant elements. Natural bornite mian copper-silver deposit from the Fore-Sudetic Mon- (L-bornite) crystallizes in the orthorhombic structure ocline and was collected in a Lubin mine located about with space group P bca. -
THE Possibly Hypogene KARSTIC IRON ORE DEPOSIT of WARDA
COBISS: 1.01 The PossiblY HYpogene Karstic Iron Ore Deposit of Warda near Ajloun (Northern Jordan), its MineralogY, GeochemistrY and Historic Mine Hipogeni kraški izvor železovih sedimentov V Wardi pri Ajlounu (Severna Jordanija): mineralogija, geokemija in zgodovinski rudnik Ahmad AL-Malabeh1, Stephan Kempe2, Horst-Volker Henschel3 Heiko Hofmann4 & Heinz Jürgen Tobschall5 Abstract UDC 553.3(569.5) Izvleček UDK 553.3(569.5) Ahmad Al-Malabeh, Stephan Kempe, Horst-Volker Henschel, Ahmad Al-Malabeh, Stephan Kempe, Horst-Volker Henschel, Heiko Hofmann & Heinz Jürgen Tobschall: The possibly hypo- Heiko Hofmann & Heinz Jürgen Tobschall: Hipogeni kraški gene karstic iron ore deposit of Warda near Ajloun (Northern izvor železovih sedimentov v Wardi pri Ajlounu (Severna Jor- Jordan), its mineralogy, geochemistry and historic mine danija): mineralogija, geokemija in zgodovinski rudnik In this study the iron ore deposit of the historic Warda mine V študiji obravnavamo železovo rudišče Warda (okrožje (District of Ajloun, Northern Jordan) and its speleological im- Ajloun v Severni Jordaniji) in njegov speleološki pomen. portance is discussed. The number of known dissolutional caves Število kraških jam v Jordaniji je majhno, kljub dejstvu, da je in Jordan is very low, in spite of the fact, that large sections of kamninska podlaga velikega dela dežele kredni apnenec. Edina the country are underlain by Cretaceous limestone. The only znana velika jama je hipogeni blodnjak (maze cave) Al-Daher, large cave yet discovered is Al-Daher Cave, a hypogene maze (Kempe et al. 2006). Rudo v Wardi je v času križarskih vojn ko- cave (Kempe et al. 2006). The Warda Iron Deposit was mined pal eden od Saladinovih častnikov. -
Study of Corrosion Potential Measurements As a Means to Monitor the Storage and Stabilisation Processes of Archaeological Copper Artefacts
Proceedings of Metal 2004 National Museum of Australia Canberra ACT 4-8 October 2004 ABN 70 592 297 967 Study of corrosion potential measurements as a means to monitor the storage and stabilisation processes of archaeological copper artefacts K. Leyssensa, A. Adriaensa, E. Pantosb and C. Degrignyc a Ghent University, Department of Analytical Chemistry, Krijgslaan 281 – S12, B-9000 Ghent, Belgium b CCLRC, Synchrotron Radiation Department, Daresbury Laboratory, Warrington, UK WA4 4AD c Malta Centre for Restoration, East Wing, Royal Naval Hospital, Bighi, Kalkara, Malta __________________________________________________________________________________________ Abstract Archaeological copper artefacts recovered from wet saline environments are often stored in tap water and stabilized in sodium sesquicarbonate solutions. Modification of the natural patina and development of active corrosion can occur during these processes. This implies that monitoring of storage/stabilisation processes is necessary. The focus of the study consists of examining how corrosion potential (Ecorr) measurements can contribute in providing information on the effectiveness of storage and stabilisation treatments. This paper reports on the Ecorr versus time plots of artificially prepared copper coupons (covered or not with corrosion layers) immersed in tap water and a sodium sesquicarbonate solution. Synchrotron radiation XRD was performed in parallel to understand the reactions that take place during the immersion processes. Keywords: corrosion potential measurements, XRD, copper, saline environments, storage, stabilisation, sodium sesquicarbonate, tap water 1. Introduction Archaeological copper artefacts recovered from wet saline environments should not be exposed directly to the atmosphere, especially when they contain aggressive chloride species, as the metal will then corrode at an accelerated rate in the oxygen-rich air (Scott 2002, p125). -
Metals from Ores: an Introduction
CRIMSONpublishers http://www.crimsonpublishers.com Mini Review Aspects Min Miner Sci ISSN 2578-0255 Metals from Ores: An Introduction Fathi Habashi* Department of Mining, Laval University, Canada *Corresponding author: Fathi Habashi, Department of Mining, Metallurgical and Materials Engineering, Laval University, Quebec City, Canada Submission: October 09, 2017; Published: December 11, 2017 Introduction of metallic lustre. Of these about 300 are used industrially in the chemical industry, in building materials, in fertilizers, as fuels, etc., chemical composition, constant physical properties, and a A mineral is a naturally occurring substance having a definite characteristic crystalline form. Ores are a mixture of minerals: they are processed to yield an industrial mineral or treated chemically and are known as the industrial minerals Figure 3. to yield a single or several metals. Ores that are generally processed for only a single metal are those of iron, aluminium, chromium, tin, mercury, manganese, tungsten, and some ores of copper. Gold ores may yield only gold, but silver is a common associate. Nickel ores are always associated with cobalt, while lead and zinc always occur together in ores. All other ores are complex yielding a number of metals. before being treated by chemical methods to recover the metals. Ores undergo a beneficiation process by physical methods and grinding then separation of the individual mineral by physical Figure 2: Metals and metalloids obtained from ores. Beneficiation processes involve liberation of minerals by crushing methods (gravity, magnetic, etc.) or physicochemical methods pyrometallurgical, and electrochemical methods. Metals and (flotation) Figure 1. Chemical methods involve hydrometallurgical, metalloids obtained from ores are shown in Figure 2. -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee,