Global Lithium Sources—Industrial Use and Future in the Electric Vehicle Industry: a Review
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Solution Mining and Salt Cavern Challenges- SMRI's Role And
Solution Mining Research Institute J. Voigt, L. Van Sambeek, R. Schneider Solution Mining and Salt Cavern Challenges, SMRI’s Role and Research Focus Session: Salt production Keywords: brine cavern, cavern storage, cavern design, cavern research, energy storage, abandonment Abstract Solution Mining Research Institute, Inc., (SMRI) is a world-wide, non-profit, member-driven organization with chief role of providing specialized education, technical reference information, and current issue research to those in the solution mining and storage cavern industries. SMRI has for over 50 years been actively researching subjects of current and future interest to our members and the cavern industry. We are helping train and develop your future industry experts and managers. SMRI technical conferences are held two times each year, one each in North America and Europe, where most SMRI member organizations are based and/or have operations. Each conference has a technical class, includes about 20 technical paper presentations, and provides field trip opportunities to see first-hand various mines, brine/salt production and storage facilities, or historic sites/features to learn how they have been operated and managed. This paper will briefly describe 20 SMRI research projects completed since the 9th World Salt Symposium 2009 in Beijing, list SMRI’s currently active research projects or ongoing programs, and discusses our focus on future cavern research on subjects of value to the industry. SMRI research projects and resulting research reports (“RR”s) are funded entirely by SMRI annual membership dues. Research contractors and host research facilities frequently provide critical access and/or services contributed to the projects at zero or reduced cost. -
Geochemical Alteration of Pyrochlore Group Minerals: Pyrochlore Subgroup
American Mineralogist, Volume 80, pages 732-743, 1995 Geochemical alteration of pyrochlore group minerals: Pyrochlore subgroup GREGORY R. LUMPKIN Advanced Materials Program, Australian Nuclear Science and Technology Organization, Menai 2234, New South Wales, Australia RODNEY C. EWING Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, U.S.A. ABSTRACT Primary alteration of uranpyrochlore from granitic pegmatites is characterized by the substitutions ADYD-+ ACaYO, ANaYF -+ ACaYO, and ANaYOI-I --+ ACaYO. Alteration oc- curred at ""450-650 °C and 2-4 kbar with fluid-phase compositions characterized by relatively low aNa+,high aeaH, and high pH. In contrast, primary alteration of pyrochlore from nepheline syenites and carbonatites follows a different tre:nd represented by the sub- stitutions ANaYF -+ ADYD and ACaYO -+ ADYD. In carbonatites, primary alteration of pyrochlore probably took place during and after replacement of diopside + forsterite + calcite by tremolite + dolomite :t ankerite at ""300-550 °C and 0-2 kbar under conditions of relatively low aHF, low aNa+,low aeaH, low pH, and elevated activities of Fe and Sr. Microscopic observations suggest that some altered pyrochlor1es are transitional between primary and secondary alteration. Alteration paths for these specimens scatter around the trend ANaYF -+ ADYD. Alteration probably occurred at 200-350 °C in the presence of a fluid phase similar in composition to the fluid present during primary alteration but with elevated activities of Ba and REEs. Mineral reactions in the system Na-Ca-Fe-Nb-O-H indicate that replacement of pyrochlore by fersmite and columbite occurred at similar conditions with fluid conpositions having relatively low aNa+,moderate aeaH, and mod- erate to high aFeH.Secondary alteration « 150 °C) is charactlerized by the substitutions ANaYF -+ ADYD,ACaYO -+ ADYD,and ACaXO -+ ADXDtogether with moderate to extreme hydration (10-15 wt% H20 or 2-3 molecules per formula unit). -
Atomic Spectra of Alkali Elements
Atomic Spectra of Alkali Elements S. R. Kulkarni April 10, 2020 Rydberg primarily focused on studying the lines of alkali metals (Lithium, Potassium and Sodium).1 Rydberg organized the various features by their appearance on the pho- tographs:The alkali spectra were more complicated than that of hydrogen. Rydberg recog- nized that were three different types of lines: lines which looked \sharp" (on photographic plates), \principal" (strong lines that showed up in emission and absorption) and those which appeared ‘diffuse”. These series were abbreviated to S, P, D. Later \Fundamental" (F) was added. As noted earlier, Rydberg preferred to work with wavenumbers. Using data from Liveing and Deware he recast Angstrom's formula as follows: N k = k − (1) n 1 (n + µ)2 where kn is the wavenumber of the nth line in a given series. Rydberg kept N fixed to the value measured by Balmer with k1 µ being free parameters. Rydberg found the following formulae for Lithium R ks = ks − ; 2; 3; 4; ::: (2) n 1 (n + S)2 R kp = kp − 1; 2; 3; ::: (3) n 1 (n + P )2 R kd = kd − 2; 3; 4; ::: (4) n 1 (n + D)2 s −1 p −1 where S = 0:5951, P = 0:9596, D = 0:9974, k1 = 28601:6 cm k1 = 43487:7 cm , d −1 k1 = 28598:5 cm and we have switched to the modern notation in which N is replaced by R (the value he found was R = 109721:6 cm−1). Rydberg had confidence in the data that he was able to find a deeper connection between the constants between the series. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Appendix E High-Potential Historic Sites
APPENDIX E HIGH-POTENTIAL HISTORIC SITES National Trails System Act, SEC. 12. [16USC1251] As used in this Act: (1) The term “high-potential historic sites” means those historic sites related to the route, or sites in close proximity thereto, which provide opportunity to interpret the historic significance of the trail during the period of its major use. Criteria for consideration as high-potential sites include historic sig nificance, presence of visible historic remnants, scenic quality, and relative freedom from intrusion.. Mission Ysleta, Mission Trail Indian and Spanish architecture including El Paso, Texas carved ceiling beams called “vigas” and bell NATIONAL REGISTER tower. Era: 17th, 18th, and 19th Century Mission Ysleta was first erected in 1692. San Elizario, Mission Trail Through a series of flooding and fire, the mis El Paso, Texas sion has been rebuilt three times. Named for the NATIONAL REGISTER patron saint of the Tiguas, the mission was first Era: 17th, 18th, and 19th Century known as San Antonio de la Ysleta. The beauti ful silver bell tower was added in the 1880s. San Elizario was built first as a military pre sidio to protect the citizens of the river settle The missions of El Paso have a tremendous ments from Apache attacks in 1789. The struc history spanning three centuries. They are con ture as it stands today has interior pillars, sidered the longest, continuously occupied reli detailed in gilt, and an extraordinary painted tin gious structures within the United States and as ceiling. far as we know, the churches have never missed one day of services. -
Jadar Lithium Mine,Serbia
2021 Jadar Lithium Mine, Serbia A Raw Deal ICT metal mining case study Author Zvezdan Kalmar, CEKOR Editing Emily Gray Design Milan Trivic Cover SN040288, Depositphotos Acknowledgements Association Protect Jadar and Rađevina Center for Ecology and Sustainable Development (Centar za ekologiju i održivi razvoj – CEKOR) is an environmental and development organisation. Apart from monitoring international financial institutions’ activities in Serbia, CEKOR is working on issues in the areas of transport, waste, biodiversity, genetically modified organisms (GMO) and making the city of Subotica sustainable. CEKOR is a member of CEE Bankwatch Network. Coalition for Sustainable Mining, Serbia (Koalicija za održivo rudarstvo u Srbiji – KORS) is an organisation that promotes the application of the strictest social and environmental standards for mining and mineral use in Serbia. CEE Bankwatch Network is the largest network of grassroots, environmental and human rights groups in central and eastern Europe. It monitors public finance institutions that are responsible for hundreds of billions of investments across the globe. Together with local communities and other NGOs Bankwatch works to expose their influence and provide a counterbalance to their unchecked power. About ICT and the mining-related work of CEE Bankwatch Network CEE Bankwatch Network has been monitoring mining projects in Europe and abroad for years. Bankwatch cooperates with the Make ICT Fair consortium, which seeks to reform the information and communication technology (ICT) manufacture and minerals supply chains and to improve the lives of workers and those impacted along different stages of the ICT supply chain. Our long-term cooperation with groups monitoring the impact of mining on people and environment as well as with communities directly affected by mines or smelters strengthens our conviction that the many negative impacts of mining must finally come under the proper scrutiny. -
Presentation Materials
Annual General Meeting 25 November 2016 Creative Resources Leadership Overview § Lepidico is a well funded ASX-listed lithium exploration and development company with an experienced management team § Lepidico’s strategic objective is to become a sustainable lithium producer with a portfolio of assets and pipeline of projects § Lepidico’s exploration initiatives largely focus on hard rock minerals that prior to L-Max® were not traditional sources of lithium § Lepidico is differentiated by having successfully produced lithium carbonate and a suite of by-products from non-traditional hard rock lithium bearing minerals using its patented L-Max® process technology § Lepidico provides exposure to a portfolio of lithium exploration assets through its wholly owned properties, JV’s and IP licence agreements in Asia, Australia, Canada, Europe and South America § At 30 September 2016 Lepidico had A$3.0M in cash and no debt 2 New sources of lithium § Micas and phosphates have been largely overlooked as a source of lithium as no commercially viable process was available to extract the lithium and process through to lithium chemicals prior to L-Max® § Lithium bearing micas Lepidolite and Zinnwaldite contain up to 5% Li2O and like spodumene, are hosted in pegmatites § Lepidolite and Zinnwaldite often occur with tin and tantalum bearing minerals as well as with spodumene § Lithium phosphates such as Amblygonite contain up to 10% Li2O Lepidolite (light purple) Zinnwaldite (dArk grey) Ambygonite/MontebrAsite K(Li,Al,Rb)3(Al,Si)4O10(F,OH)2 KLiFeAl(AlSi3)O10(OH,F)2 -
Session 1 Sources and Availability of Materials for Lithium Batteries
Session 1: Sources and Availability of Materials for Lithium Batteries Session 1 Sources and Availability of Materials for Lithium Batteries Adrian Griffin Managing Director, Lithium Australia NL ABSTRACT Lithium, as a feedstock for the battery industry, originates from two primary sources: hard-rock (generally spodumene and petalite), and brines. Brine processing results in the direct production of lithium chemicals, whereas the output from hard-rock production is tradeable mineral concentrates that require downstream processing prior to delivery, as refined chemicals, into the battery market. The processors of the concentrates, the 'converters', are the major constraint in a supply chain blessed with abundant mineral feed. The battery industry must overcome the constraints imposed by the converters, and this can be achieved through the application of the Sileach™ process, which produces lithium chemicals from concentrates direct, without the need for roasting. The cathode chemistries of the most efficient lithium batteries have a common thread – a high dependence on cobalt. Battery manufacturers consume around 40% of the current production of cobalt, a by-product of the nickel and copper industries. This means cobalt is at a tipping point – production will not keep up with demand. In the short term, the solution lies in developing alternative cathode compositions, while in the longer term recycling may be the answer. Lithium Australia NL is researching the application of its Sileach™ process to waste batteries to achieve a high-grade, low-cost source of battery materials and, in so doing, ease the supply constraints on cathode metals. To ensure that the battery industry is sustainable, better utilisation of mineral resources, more efficient processing technology, an active battery reprocessing capacity and less reliance on cobalt as a cathode material are all necessary. -
Helium Adsorption on Lithium Substrates
JLowTempPhys DOI 10.1007/s10909-007-9516-5 Helium Adsorption on Lithium Substrates E. Van Cleve · P. Taborek · J.E. Rutledge Received: 25 July 2007 / Accepted: 13 September 2007 © Springer Science+Business Media 2007 Abstract We have developed a cryogenic pulsed laser deposition (PLD) system to deposit lithium films onto a quartz crystal microbalance (QCM) at 4 K. Adsorption isotherms of 4He on lithium were measured in the temperature range between 1.42 K and 2.5 K. The isotherms are qualitatively different from isotherms on strong sub- strates such as gold and weak substrates such as cesium. There is no evidence of the formation of solid-like layers of helium, and the helium coverage is approximately linear in the pressure over a wide range. By measuring the low coverage slope of the isotherms, the binding energy of helium to lithium was found to be approxi- mately −13.6 K. For lithium substrates less than approximately 100 layers thick, the chemical potential at which the superfluid transition was observed was surprisingly sensitive to the details of lithium deposition. Keywords Helium films · Pulsed laser deposition · Superfluidity · Alkali metal 1 Introduction When helium is adsorbed onto a strong heterogenous substrate such as gold, the first 2 or 3 statistical layers are solid-like. The nature of these layers is not yet clear, but the layers are amorphous and do not participate significantly in superflow at high coverages. Superfluidity on strong substrates requires a minimum critical coverage to saturate the solid-like layers, and the superfluid phase which forms at higher cover- ages flows over these layers and does not interact directly with the strong, short range This work was supported by NSF grant DMR 0509685. -
Mixing-Induced Precipitation in Brine Mining: Reactive Transport Modeling / ALEJANDRO GARCÍA-GIL (1), MAR GARCÍA-ALCARAZ (2), ENRIC VAZQUEZ (2), CARLOS AYORA (2*)
macla nº 20. julio ‘15 revista de la sociedad española de mineralogía 59 Mixing-Induced Precipitation in Brine Mining: Reactive Transport Modeling / ALEJANDRO GARCÍA-GIL (1), MAR GARCÍA-ALCARAZ (2), ENRIC VAZQUEZ (2), CARLOS AYORA (2*) (1) Departamento de Geología. Universidad Zaragoza, Pedro Cerbuna, 12. 50009 Zaragoza (2) Grupo Hidrología Subterránea, UPC-CSIC, Instituto de Diagnóstico Ambiental y Estudios del Agua, Jordi Girona 18, 08034 Barcelona INTRODUCTION planes (probably stratification planes). It is 12 to 15 m thick and has high Continental brines have become the hydraulic conductivities. (II) A less leading raw material for lithium permeable body of 2 to 8 m thick acting production worldwide. Lithium-bearing as an aquitard which consist of halite brines are found in salt aquifers (mainly that may have gypsum levels. (III) Unit B halite) in the nucleus of salars (salt is a semi-confined aquifermade up of flats). Because of extremely high halite, 8 to 11 m thick and highly evaporation rates, the primary discharge conductive. (IV) A lowpermeability body occurs by evaporation keeping the water is at the bottom of the mined system. table below the surface. Two different brines are identified in Brines are exploited through pumping aquifers “A” and “B” with a transition wells or ditches excavated in halite brine in the aquitard separating those aquifers and evaporation of the brine in aquifers. Brine extraction is carried out solar ponds to further concentration. In via brine pumping fields, i.e. horizontal fig 2. Gypsum precipitates around in a well. this type of mining, such as that in drains (1 km length) connected with REACTIVE TRANSPORT MODELING Atacama (Chile), a fast and drastic loss vertical extraction well (Fig. -
Federal LCA Commons Elementary Flow List: Background, Approach, Description and Recommendations for Use
EPA/600/R-19/092 | September 2019 | www.epa.gov/research The Federal LCA Commons Elementary Flow List: Background, Approach, Description and Recommendations for Use 0 Federal LCA Commons Elementary Flow List: Background, Approach, Description and Recommendations for Use by Ashley Edelen, Troy Hottle, Sarah Cashman Eastern Research Group Wesley Ingwersen U.S. EPA/National Risk Management Research Laboratory/ Land and Materials Management Division ii Notice/Disclaimer Although the U.S. Environmental Protection Agency, through its Office of Research and Development, funded and conducted the research described herein under an approved Quality Assurance Project Plan (Quality Assurance Identification Number G-LMMD-0031522-QP-1-0), with the support of Eastern Research Group, Inc. through EPA Contract Number EP-C-16-015, it does not necessarily reflect the views of the Agency, and no official endorsement should be inferred. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. iii Foreword The U.S. Environmental Protection Agency (U.S. EPA) is charged by Congress with protecting the Nation's land, air, and water resources. Under a mandate of national environmental laws, the Agency strives to formulate and implement actions leading to a compatible balance between human activities and the ability of natural systems to support and nurture life. To meet this mandate, U.S. EPA's research program is providing data and technical support for solving environmental problems today and building a science knowledge base necessary to manage our ecological resources wisely, understand how pollutants affect our health, and prevent or reduce environmental risks in the future. -
(WANA) WATER REGIME by MOHAMMAD ABU HAWAS
MINING BRINE AND WATER: DESALINATION IN THE CONTEXT OF THE WEST ASIA – NORTH AFRICA (WANA) WATER REGIME By MOHAMMAD ABU HAWASH Submitted to Central European University School of Public Policy In partial fulfilment for the degree of Master of Public Administration Supervisor: Thilo Bodenstein Budapest, Hungary / Vienna, Austria 2021 CEU eTD Collection Table of Contents Statement of Authorship ............................................................................................................................ 3 Abstract ........................................................................................................................................................ 4 Acknowledgements ..................................................................................................................................... 5 List of Figures .............................................................................................................................................. 6 List of Tables ............................................................................................................................................... 6 List of Illustrations ...................................................................................................................................... 7 List of Abbreviations .................................................................................................................................. 8 Introduction ..............................................................................................................................................