A Review on the Separation of Lithium Ion from Leach Liquors of Primary and Secondary Resources by Solvent Extraction with Commercial Extractants
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Improving the Stability of High-Voltage Lithium Cobalt Oxide with a Multifunctional Electrolyte Additive: Interfacial Analyses
nanomaterials Article Improving the Stability of High-Voltage Lithium Cobalt Oxide with a Multifunctional Electrolyte Additive: Interfacial Analyses Xing-Qun Liao 1,2, Feng Li 2, Chang-Ming Zhang 2, Zhou-Lan Yin 1,*, Guo-Cong Liu 3,* and Jin-Gang Yu 1,3,* 1 College of Chemistry and Chemical Engineering, Central South University, Changsha 410083, China; [email protected] 2 Research Institute of Highpower International, Huizhou 516057, China; fl[email protected] (F.L.); [email protected] (C.-M.Z.) 3 School of Chemistry and Materials Engineering, Huizhou University, Huizhou 516007, China * Correspondence: [email protected] (Z.-L.Y.); [email protected] (G.-C.L.); [email protected] (J.-G.Y.); Tel./Fax: +86-731-88879616 (Z.-L.Y.); +86-731-88879616 (J.-G.Y.) Abstract: In recent years, various attempts have been made to meet the increasing demand for high energy density of lithium-ion batteries (LIBs). The increase in voltage can improve the capacity and the voltage platform performance of the electrode materials. However, as the charging voltage increases, the stabilization of the interface between the cathode material and the electrolyte will decrease, causing side reactions on both sides during the charge–discharge cycling, which seriously affects the high-temperature storage and the cycle performance of LIBs. In this study, a sulfate additive, dihydro-1,3,2-dioxathiolo[1,3,2]dioxathiole 2,2,5,5-tetraoxide (DDDT), was used as an effi- cient multifunctional electrolyte additive for high-voltage lithium cobalt oxide (LiCoO2). Nanoscale Citation: Liao, X.-Q.; Li, F.; Zhang, protective layers were formed on the surfaces of both the cathode and the anode electrodes by C.-M.; Yin, Z.-L.; Liu, G.-C.; Yu, J.-G. -
Manufacturing Scalability Implications of Materials Choice in Inorganic Solid-State Batteries Abstract Context & Scale Intro
1 Manufacturing Scalability Implications of Materials Choice in Inorganic 2 Solid-State Batteries 3 Kevin J. Huang1, Gerbrand Ceder2, Elsa A. Olivetti1* 4 5 1Department of Materials Science & Engineering, MIT, Cambridge, MA 02139; 2Department of Materials 6 Science & Engineering, University of California Berkeley, Berkeley, CA 94720, USA 7 Abstract 8 The pursuit of scalable and manufacturable all-solid-state batteries continues to intensify, motivated by the 9 rapidly increasing demand for safe, dense electrical energy storage. In this Perspective, we describe the 10 numerous, often conflicting, implications of materials choices that have been made in the search for 11 effective mitigations to the interfacial instabilities plaguing solid-state batteries. Specifically, we show that 12 the manufacturing scalability of solid-state batteries can be governed by at least three principal 13 consequences of materials selection: (1) the availability, scaling capacity, and price volatility of the chosen 14 materials’ constituents, (2) the manufacturing processes needed to integrate the chosen materials into full 15 cells, and (3) the cell performance that may be practically achieved with the chosen materials and processes. 16 While each of these factors is, in isolation, a pivotal determinant of manufacturing scalability, we show that 17 consideration and optimization of their collective effects and tradeoffs is necessary to more completely 18 chart a scalable pathway to manufacturing. 19 Context & Scale 20 With examples pulled from recent developments in solid-state batteries, we illustrate the consequences of 21 materials choice on materials availability, processing requirements and challenges, and resultant device 22 performance. We demonstrate that while each of these factors is, by itself, essential to understanding 23 manufacturing scalability, joint consideration of all three provides for a more comprehensive understanding 24 of the specific factors that could impede the scale up to production. -
Mica Deposits of the Southeastern Piedmont Part 2
Mica Deposits of the Southeastern Piedmont Part 2. Amelia District, Virginia GEOLOGICAL SURVEY PROFESSIONAL PAPER 248-B Mica Deposits of the Southeastern Piedmont Part 2. Amelia District, Virginia By RICHARD W. LEMKE, RICHARD H. JAHNS, and WALLACE R.GRIFFITTS GEOLOGICAL SURVEY PROFESSIONAL PAPER 248-B Distribution and structure of pegmatite bodies in the area, their mineralogical characteristics, and the economic possibilities of the mica and other pegmatite minerals UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1952 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 60 cents (paper cover) CONTENTS Page Page Abstract _________________________________________ 103 Description of deposits—Continued Introduction: Field work and acknowledgments._______ 103 Jefferson-Amelia area—Continued Geography of the district____________________________ 104 Jefferson prospects______-_--._-----_------ - 118 Geology of the district-______________________________ 105 McCraw No. 3 (Old Pinchbeck No. 1) mine__. 119 Rock formations,___________________________ 105 McCraw No. 2 (Old Pinchbeck No. 3) mine__ 119 Metamorphic rocks_ ________________________ 105 McCraw No. 1 (Pinchbeck No. 2) mine__---_ 119 Igneous rocks______________________________ 105 Line mine__---___________________________ 120 Structure. _________________________________ 106 Booker mine______________--_-----___----. 120 -
Alteration of Spodumene, Montebrasite and Lithiophilite In
American Mineralogist, Volume 67, pages 97-113, 1982 Alteration of spodumene,montebrasite and lithiophilite in pegmatites of the White PicachoDistrict, Arizona Davrp Lor.rooxrnNo DoNer-uM. Bunr Department of Geology Arizona State University Tempe, Arizona 85281 Abstract The crystallization sequence and metasomatic alteration of spodumene (LiAlSizOe), montebrasite(LiAIPO4(OH,F)), and lithiophilite (Li(Mn,Fe)PO+)are describedfor nine zoned lithium pegmatitesin the White Picacho district, Arizona. The observedcrystalliza- tion trends suggesta progressiveincrease in the activities of lithium species(spodumene follows microcline as the principal alkali aluminosilicate), as well as an increase in the activities of the acidic volatiles phosphorus and fluorine (montebrasite succeedsspodu- mene as the stableprimary lithium phase).Much of the lithiophilite occurs with columbite, apatite, beryl, zircon, and tourmaline in cleavelanditecomplexes that formed in part at the expenseof quartz-spodumenepegmatite. Fracture-controlledpseudomorphic alteration of the primary lithium minerals is widespread and apparently is the result of subsolidus reactionswith residualpegmatitic fluids. Spodumenehas been replacedby eucryptite, albite, and micas. Alteration products of montebrasite include low-fluorine secondary montebrasite,crandallite (tentative), hydroxylapatite, muscovite, brazilianite, augelite (tentative),scorzalite, kulanite, wyllieite, and carbonate-apatite.Secondary phases identi- fied in altered lithiophilite include hureaulite, triploidite, eosphorite, -
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). -
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 -
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 -
SAFETY DATA SHEET Electrolyte Licl 1 Mol/L in Ethanol
SAFETY DATA SHEET according to Regulation (EU) No. 453/2010 Electrolyte LiCl 1 mol/l in ethanol 1. Identification of the substance/mixture and of the company/undertaking 1.1. Product identifier Product code 51350088, 51343183 Synonyms None. 1.2. Relevant identified uses of the substance or mixture and uses advised against Use of the Laboratory chemicals Substance/Preparation 1.3. Details of the supplier of the safety data sheet Company/Undertaking Mettler-Toledo AG Identification ANALYTICAL Sonnenbergstrasse 74 CH-8603 Schwerzenbach Schweiz Tel: +41-44-806-77-11 Fax: +41-44-806-73-50 Email: [email protected] 1.4. Emergency telephone +41-44-251 51 51 (Tox Center) number Revision Date 07.03.2014 Version GHS 1 2. Hazards identification 2.1. Classification of the substance or mixture Electrolyte LiCl 1 mol/l in ethanol (9830) V. GHS 1 / 07.03.2014 Print Date 28.03.2014 Page 1/10 Classification according to Flammable liquids, Cat. 2, H225 Regulation (EC) No. 1272/2008 (GHS/CLP) The product is classified and labelled according to Regulation (EC) No. 1272/2008 (GHS/CLP). Classification according to EU F; R11 Directives 67/548/EEC or 1999/45/EC Additional information For the full text of the phrases mentioned in this Section, see Section 16. 2.2. Label elements F Signal Word Danger Hazard Statements H225: Highly flammable liquid and vapour. Precautionary statements P210b: Keep away from heat, hot surfaces, sparks, open flames and other ignition sources. No smoking. P243: Take precautionary measures against static discharge. P280: Wear protective gloves/ protective clothing/ eye protection/ face protection. -
Separation of Water out of Highly Concentrated Electrolyte Solutions Using Multistage Vacuum Membrane Distillation
Separation of water out of highly concentrated electrolyte solutions using multistage vacuum membrane distillation Bin Jiang Master of Science Thesis KTH School of Industrial Engineering and Management Energy Technology EGI-2013-082MSC EKV967 Division of Heat and Power SE-100 44 STOCKHOLM Master of Science Thesis EGI-2013-082MSC EKV967 Separation of water out of highly concentrated electrolyte solutions using multistage vacuum membrane distillation Bin Jiang Approved Examiner Supervisor 26.09.2013 Andrew Martin Daniel Minilu Woldemariam Commissioner Contact person Abstract Absorption dehumidification requires regeneration system to regenerate diluted desiccant solutions, which are still highly concentrated. A novel multi-stage vacuum membrane distillation system was applied for separating water out of the highly concentrated solution. The performance of this novel membrane distillation system with high concentration solution is studied, as well as the effect of solution concentration, heating temperature and feed flow rate on concentration increase, permeate flux and specific energy consumption was studied. Feed solutions are LiCl solution (22-30 wt%) and CH3COOK solution (50-60 wt%).Other experimental parameters studied were: heating temperature, 70-80 °C, feed flow rate, 1.2-2.0 l/min. Response surface method is applied for model building, in order to provide a better understanding of the interactions between different parameters. Compared with pure water, high concentration solution has lower vapor pressure, which leads to lower permeate flux. The highest concentration the system can reach is 36.5 wt% for LiCl solution and over 70 wt% for CH3COOK solution, when the heating temperature is 80 °C. Lower concentration and higher heating temperature will result in larger increase in concentration, higher permeate flux and also lower specific energy consumption. -
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. -
Lithium Data Sheet
98 LITHIUM (Data in metric tons of lithium content unless otherwise noted) Domestic Production and Use: The only lithium production in the United States was from a brine operation in Nevada. Two companies produced a wide range of downstream lithium compounds in the United States from domestic or imported lithium carbonate, lithium chloride, and lithium hydroxide. Domestic production data were withheld to avoid disclosing company proprietary data. Although lithium markets vary by location, global end-use markets are estimated as follows: batteries, 65%; ceramics and glass, 18%; lubricating greases, 5%; polymer production, 3%; continuous casting mold flux powders, 3%; air treatment, 1%; and other uses, 5%. Lithium consumption for batteries has increased significantly in recent years because rechargeable lithium batteries are used extensively in the growing market for portable electronic devices and increasingly are used in electric tools, electric vehicles, and grid storage applications. Lithium minerals were used directly as ore concentrates in ceramics and glass applications. Salient Statistics—United States: 2015 2016 2017 2018 2019e Production W W W W W Imports for consumption 2,750 3,140 3,330 3,420 2,500 Exports 1,790 1,520 1,960 1,660 1,700 Consumption, estimated1 2,000 3,000 3,000 3,000 2,000 Price, annual average, battery-grade lithium carbonate, dollars per metric ton2 6,500 8,650 15,000 17,000 13,000 Employment, mine and mill, number 70 70 70 70 70 Net import reliance3 as a percentage of estimated consumption >25 >50 >50 >50 >25 Recycling: One domestic company has recycled lithium metal and lithium-ion batteries since 1992 at its facility in British Columbia, Canada. -
A Study of Lithium Precursors on Nanoparticle Quality
Electronic Supplementary Material (ESI) for Nanoscale. This journal is © The Royal Society of Chemistry 2021 Electronic Supplementary Information Elucidating the role of precursors in synthesizing single crystalline lithium niobate nanomaterials: A study of lithium precursors on nanoparticle quality Rana Faryad Ali, Byron D. Gates* Department of Chemistry and 4D LABS, Simon Fraser University, 8888 University Drive Burnaby, BC, V5A 1S6, Canada * E-mail: [email protected] This work was supported in part by the Natural Sciences and Engineering Research Council of Canada (NSERC; Grant No. RGPIN-2020-06522), and through the Collaborative Health Research Projects (CHRP) Partnership Program supported in part by the Canadian Institutes of Health Research (Grant No. 134742) and the Natural Science Engineering Research Council of Canada (Grant No. CHRP 462260), the Canada Research Chairs Program (B.D. Gates, Grant No. 950-215846), CMC Microsystems (MNT Grant No. 6345), and a Graduate Fellowship (Rana Faryad Ali) from Simon Fraser University. This work made use of 4D LABS (www.4dlabs.com) and the Center for Soft Materials shared facilities supported by the Canada Foundation for Innovation (CFI), British Columbia Knowledge Development Fund (BCKDF), Western Economic Diversification Canada, and Simon Fraser University. S1 Experimental Materials and supplies All chemicals were of analytical grade and were used as received without further purification. Niobium ethoxide [Nb(OC2H5)5, >90%] was obtained from Gelest Inc., and benzyl alcohol (C7H7OH, 99%) and triethylamine [N(C2H5)3, 99.0%] were purchased from Acros Organics and Anachemia, respectively. Lithium chloride (LiCl, ~99.0%) was obtained from BDH Chemicals, and lithium bromide (LiBr, ≥99.0%), lithium fluoride (LiF, ~99.9%), and lithium iodide (LiI, 99.0%) were purchased from Sigma Aldrich.