Article

Recovery of lithium from Uyuni salar brine

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Abstract

A hydrometallurgical process was developed to recover lithium from a brine collected from Salar de Uyuni, Bolivia, which contains saturated levels of Na, Cl and sulphate, low Li (0.7–0.9 g/L Li) and high Mg (15–18 g/L Mg). Unlike other commercial salar brines currently being processed, the high levels of magnesium and sulphate in Uyuni brine would create difficulties during processing if conventional techniques were used. A two-stage precipitation was therefore first adopted in the process using lime to remove Mg and sulphate as Mg(OH)2 and gypsum (CaSO4.2H2O). Boron (at 0.8 g/L in the raw brine), a valuable metal yet deleterious impurity in lithium products, could also be mostly recovered from the brine by adsorption at a pH lower than pH11.3 in this first stage. The residual Mg and Ca (including that added from lime) which were subsequently precipitated as Ca–Mg oxalate could be roasted to make dolime (CaO ∙ MgO) for re-use in the first stage of precipitation. Evaporation of the treated brine up to 30 folds would produce 20 g/L Li liquors. The salt produced during evaporation was a mixture of NaCl and KCl, containing acceptable levels of sulphate, Mg, Ca, etc. The final precipitation of lithium at 80–90 °C produced a high purity (99.55%) and well crystalline lithium carbonate.

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... To effectively utilize and recover liquid lithium resources, it is crucial to develop efficient extraction methods. The main methods for extracting lithium from liquid lithium resources include precipitation [4], solvent extraction [5,6], membrane separation [7], electrochemical methods [8,9], and adsorption [10]. Among them, the adsorption technique has attracted significant research attention for its straightforward operation and economic efficiency. ...
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... At this stage, various salts precipitate as water is removed. Ion salts that do not precipitate spontaneously, such as boron, calcium, magnesium, and sulfates, must be removed through chemical treatment [32,33]. ...
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... Many of the salt-lake brines that have high potential for resource recovery using solar evaporation have high concentrations of divalent cations. For example, in lithium containing brines the concentration of magnesium can be as high as 3 wt % and the concentration of calcium can be as high as 2.4 wt %. 39,40 Table S1 summarizes the ion concentrations of selected lithium containing brines throughout the world. In commercialized processes, such as the chemical precipitation method currently used for lithium mining, reducing the concentration of the divalent cations is the costliest step as they can prevent high lithium recoveries from some brines. ...
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... Under specified conditions, the extraction of boron reach a rate of 99.07%, and water is employed as a stripping agent to recover the solvent. The effluent stream then proceeds to the first precipitation stage (Pr 1) to remove Mg 2+ and other ions such as Fe 2+ and Ni 2+ (Chagnes and Swiatowska, 2015;Karidakis et al., 2005;An et al., 2012). Lithium recovery processes face difficulties with handling large quantities of magnesium as it needs to be recovered as a by-product to enhance the economic efficiency of the process while minimizing the loss of lithium. ...
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... Due to the similar chemical compositions, the recovery of lithium from the waste liquid of rock salt brine can refer to salt lake brine methods that contain precipitation (Wang et al. 2017;han et al 2018), adsorption (Li et al. 2020), solar pond , solvent extraction (Song et al. 2020), membrane (Chung et al. 2008) and electrodialysis methods (Xiong et al. 2021). The precipitation method is a traditional method that uses carbonate (An et al. 2012), aluminate (Zhong et al. 2021), and phosphate (he et al. 2017) to precipitate lithium. In this study, the amorphous Al(Oh) 3 produced by AlCl 3 · 6h 2 O and NaOh was used to precipitate Li + in the waste liquid from rock salt brine with the formation of LiCl · 2Al(Oh) 3 · xh 2 O salt (Kotsupalo et al. 2013;Paranthaman et al. 2017). ...
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... Lime softening is also used in industry to reduce Mg 2 + concentrations through the addition of limewater, Ca(OH) 2 or simply CaO, to raise the pH and precipitate Mg 2 + as Mg(OH) 2 . [50,51] Based on the K sp of Mg(OH) 2 (1.5×10 À 11 ), we reasoned that increasing the sample pH from 7.4 to 11 ([OH À ] = 10 À 3 M) would promote Mg(OH) 2 precipitation to yield a final Mg 2 + concentration in solution of~15 μM. As demonstrated in Supporting Information, Figure S7, there is little decrease in the fluorescence signal in the presence of 5 mM level of Mg 2 + in comparison with that of non-target metal ions. ...
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... It involves the calcium hydroxide and sodium oxalate usage in a two-step precipitation method. This eliminates magnesium, along with other impurities such as boron and sulfur [133]. According to a proposed double-drop technique, deionized water was combined with AlCl 3 ·6H 2 O and introduced into the brine. ...
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... During the lithium concentration process, one of the main impurities is magnesium, which, in excess, in the most concentrated ponds, generates the precipitation of lithium carnallite, and therefore, lithium yield losses. On the other hand, magnesium presents drawbacks in subsequent purification stages, which makes it necessary to remove it to ensure a high-purity lithium carbonate or lithium hydroxide product [37]. ...
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Citation: Torres, D.; Pérez, K.; Galleguillos Madrid, F.M.; Leiva, W.H.; Gálvez, E.; Salinas-Rodríguez, E.; Gallegos, S.; Jamett, I.; Castillo, J.; Saldana, M.; et al. Salar de Atacama Lithium and Potassium Productive Process. Metals 2024, 14, 1095. Abstract: The average lithium content in the Earth's crust is estimated at about 0.007%. Despite this, lithium is considered abundant and widely distributed, with significant extraction from various sources. Notably, the brines in the Salar de Atacama are highlighted for their high lithium concen-tration~1800 mg/L. Lithium is currently recovered from these brines through a solar evaporation process. The brine is transferred through a series of ponds, increasing the lithium concentration from 0.2% to 6% over 18 months, while decanting other minerals like potassium, magnesium, and boron. This method is the most efficient and cost-effective globally due to the Salar de Atacama's high lithium concentration of approximately 1800 ppm and the region's intense solar radiation, which facilitates evaporation at no economic cost. This manuscript describes in detail the lithium and potassium extraction processes used in the Salar de Atacama.
... CaO is the most commonly used precipitant, which tends to be combined in a two-stage precipitation process with Na 2 C 2 O 4 , Na 2 CO 3 , NaOH, or evaporation. An et al. (2012) reported the extraction of high-purity lithium carbonate from Uyuni Salar with a Li concentration of 0.7-0.9 g/L and a high Mg concentration of 15-18 g/L on a two-stage precipitation process. ...
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... Similar observations were noted in [42], where it was shown that at concentration ratios up to 20, lithium losses are negligible, but above this value, they can reach up to 60%, depending on the final lithium concentration in the brine. Other authors [43], investigating the evaporation of real brines under natural sunlight, demonstrated minimal lithium losses (<0.004%), although the concentration ratio was rather low, i.e., around 5. ...
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In recent years, the demand for lithium, essential to the high-tech and battery sectors, has increased rapidly. The majority of lithium carbonate is now sourced from continental brines in Latin America, owing to the lower production costs and reduced environmental impact. In Europe, often overlooked but promising lithium resources could include highly mineralized underground waters. Therefore, this study investigates the enrichment of these low-grade solutions (<100 mg/L Li) through evaporation followed by solvent extraction (SX) processes under specific conditions. The effectiveness and the technical feasibility of lithium extraction were evaluated using binary synthetic, multicomponent semi-synthetic, and real brine samples. The popular tributyl phosphate/methyl isobutyl ketone (TBP/MIBK) system, supplemented with FeCl3 and AlCl3 as co-extractants, was employed as the organic phase. Evaporation resulted in significant lithium losses (up to 80%), reduced to ~10% by washing the crystallisate obtained during evaporation with ethanol. The results from SX tests revealed differences between the synthetic and real brines. While the synthetic brines exhibited satisfactory lithium extraction yields (91%), the real brines showed a significantly lower extraction efficiency (~32%), rendering the tested system ineffective. Solid phase precipitation during the SX trials was observed for both the synthetic and real brines, which were concentrated before the SX stage, highlighting the challenges in lithium-recovery processes. However, semi-synthetic brine trials yielded promising results, with a satisfactory extraction efficiency (76%), and the absence of physical problems (emulsion, long disengagement, etc.). This reveals the importance of the chemical composition of brines and emphasizes the need for varied procedural approaches in lithium-recovery processes.
... Moreover, a high lithium loading leads to rapid saturation of the adsorbent and increases the cost of adsorbent regeneration [33]. The recovery of lithium as Li 2 CO 3 by chemical precipitation from Uyuni salar brine wastewater from the aluminum anode industry was reported by Álvarez-Ayuso et al. [34]. Wei et al., in 2005, applied the selective precipitation to produce purified Li 2 CO 3 from dilute Li-rich brine to increase the practical value of Li-rich brine that is obtained using the conventional treatment method. ...
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As a key ingredient of batteries for electric vehicles (EVs), lithium plays a significant role in climate change mitigation, but lithium has considerable impacts on water and society across its life cycle. Upstream extraction methods—including open‐pit mining, brine evaporation, and novel direct lithium extraction (DLE)—and downstream processes present different impacts on both the quantity and quality of water resources, leading to water depletion and contamination. Regarding upstream extraction, it is critical for a comprehensive assessment of lithium's life cycle to include cumulative impacts related not only to freshwater, but also mineralized or saline groundwater, also known as brine. Legal frameworks have obscured social and ecological impacts by treating brine as a mineral rather than water in regulation of lithium extraction through brine evaporation. Analysis of cumulative impacts across the lifespan of lithium reveals not only water impacts in conventional open‐pit mining and brine evaporation, but also significant freshwater needs for DLE technologies, as well as burdens on fenceline communities related to wastewater in processing, chemical contaminants in battery manufacturing, water use for cooling in energy storage, and water quality hazards in recycling. Water analysis in lithium life cycle assessments (LCAs) tends to exclude brine and lack hydrosocial context on the environmental justice implications of water use by life cycle stage. New research directions might benefit from taking a more community‐engaged and cradle‐to‐cradle approach to lithium LCAs, including regionalized impact analysis of freshwater use in DLE, as well as wastewater pollution, cooling water, and recycling hazards from downstream processes. This article is categorized under: Human Water > Human Water Human Water > Water Governance Human Water > Water as Imagined and Represented Science of Water > Water and Environmental Change
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Forward osmosis (FO) using deep eutectic solvents (DESs) as the draw solution (DS) was used in liquid mining of lithium from a synthesized brine, which was used as the feed...
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Processing of petalite concentrate from the Bikita deposits in Zimbabwe for production of high-purity Li2CO3 has been studied. XRF and ICP-OES analysis showed that the concentrate consists of oxides of Li, Si, and Al as major components, with an average Li2O content of 4.10%. XRD examination confirmed that the sample is a petalite. Processing of the petalite involves roasting the pre-heated concentrate with concentrated H2SO4 followed by water leaching of the resulting Li2SO4, solution purification and precipitation of Li2CO3. The effects of roasting temperature, stirring speed, solid to liquid ratio, leaching temperature and time on the lithium dissolution are reported. The dissolution rates are significantly influenced by roasting temperature and stirring speed. Water-washed lithium carbonate with a purity of 99.21% (metal basis) was produced. Synthesised and commercial Li2CO3 samples were characterised and compared using X-ray diffraction (XRD) and thermogravimetric analysis (TGA).
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The granites of South-West England are a potential source of lithium which is generally found within the mica mineral, zinnwaldite. It is mainly found in the central and western end of the St. Austell granite. When kaolin extraction occurs in these areas a mica-rich waste product is produced which is currently disposed of in tailings storage facilities. In this study a tailings sample containing 0.84% Li2O was upgraded by a combination of froth flotation, using dodecylamine as the collector, and wet high intensity magnetic separation (WHIMS) to 2.07% Li2O. The concentrate was then roasted with various additives, including limestone, gypsum and sodium sulphate, over a range of temperatures. The resulting products were then pulverised before being leached with water at 85°C. Analysis of these products by XRD revealed that the water-soluble sulphates, KLiSO4 and Li2KNa(SO4)2, were produced under specific conditions. A maximum lithium extraction of approximately 84% was obtained using gypsum at 1050°C. Sodium sulphate produced a superior lithium extraction of up to 97% at 850°C. In all cases iron extraction was very low.Preliminary tests on the leach solution obtained by using sodium sulphate as an additive have shown that a Li2CO3 product with a purity of >90% could be produced by precipitation with sodium carbonate although more work is required to reach the industrial target of >99%.
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The demand for lithium is expected to increase by almost 60% from 102,000t to 162,000t, with batteries accounting for more than 40,000t of the growth. Lithium ion batteries offer exceptional power-to-weight ratios suitable for small applications such as laptops and digital cameras. Several elements are combined with lithium to make a safe cathode for automotive applications such as Vanadium with Li3V2(PO4)3 providing the highest voltage and specific energy. Vanadium is most commonly used as a steel hardener and strengthener, and is added to construction and other steels at a level of from one to four per cent. Lithium can be obtained from evaporated brines, hard rock minerals and clays. The least expensive source of lithium carbonate is brine recovered from salars in the Andes of South America, where high winds and solar energy evaporate brines to economic levels.
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A zinnwaldite concentrate with 1.40% Li processed in this study was prepared from zinnwaldite wastes (0.21% Li) using dry magnetic and grain size separations. Zinnwaldite wastes originated from dressing Sn-W ores, which were mined in the past in the Czech Republic in Cínovec area. The extraction process of lithium, so-called gypsum method consisted of sintering the concentrate with CaSO4 and Ca(OH)2, subsequent leaching of the sinters obtained in H2O, solution purification and precipitation of Li2CO3. It was observed that almost 96% lithium extraction was achieved if sinters prepared at 950°C were leached at 90°C, liquid-to-solid ratio = 10: 1, reaction time of 10 min. The weight ratio of the concentrate to CaSO4 to Ca(OH)2 was 6 : 4.2 : 2. Lithium carbonate product containing almost 99% Li2CO3 was separated from the condensed leach liquor, from which calcium was removed by carbonate precipitation.
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There are several saline waters which contain large amount of Mg2+, such as sea water, natural brine, ore leaching, process stream, geothermal brine, bittern, etc. Typically, magnesium chloride aqueous is rejected during the potash process and disposal of this can comprise significant environmental issues. Thus the aimed extraction of this salt can avail environmentally and economically. In this study, main facets of the recovery process for pilot plant probe were studied in a laboratory scale. The magnesium chloride was extracted from concentrate with help of the chemical precipitation and evaporation-crystallization processes. For more extraction efficiency carnalit water washing and added recycle stream methods were investigated, separately. The recovery yield and magnesium chloride purity was obtained 75% and 98%, respectively.
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The precipitation of magnesium hydroxide from aqueous solutions by reaction with calcium hydroxide has been studied in agarose gel by electron microscopy and diffraction. The first stage, which dominates at very low Mg2+ concentrations, is the formation of thin single crystals of magnesium hydroxide, some 500 nm or less in diameter. At higher concentrations, these are overgrown to produce larger particles, thicker towards the outside, and generally consisting of several crystallites, with a common c-axis, but imperfectly aligned in the ab plane. The implications for growth mechanisms, and for the production of magnesium hydroxide from seawater, are discussed.
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Precipitation of magnesium hydroxide is the first step in the production of various magnesium compounds from seawater. Although the process is well known, kinetic data for the precipitation reaction using slaked lime and dolomite is not available in the literature. In this study, the global kinetics of precipitation of magnesium hydroxide from seawater were investigated by monitoring the total calcium and magnesium composition of species smaller than 2 μm. The effects of temperature and dolomite particle size were also investigated.
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In this study, Li2CO3 was extracted from a zinnwaldite concentrate with 1.21% Li and 0.84% Rb prepared from zinnwaldite wastes (0.21% Li, 0.20% Rb). These wastes originated from dressing of Sn–W ores, which were mined in the Czech Republic in the past. Processing of the zinnwaldite concentrate consisted of roasting the concentrate with CaCO3 followed by water leaching of the resulting calcines. This method made it possible to extract about 90% of Li as well as Rb. Lithium carbonate products were separated from leach liquor using two different procedures. The first one comprised conversion of the original alkaline leach liquor to carbonated solution by CO2 bubbling, solution purification and Li2CO3 crystallization during water evaporation. The second procedure consisted of lithium solvent extraction from the original leach liquor using LIX 54 and TOPO as an extraction agent followed by stripping with diluted H2SO4, solution purification and lithium carbonate precipitation with K2CO3. Water-washed lithium carbonate salts were produced in both procedures and contained almost 99.5% Li2CO3 with the first method providing higher yield. Mother liquors after Li2CO3 crystallization and/or inorganic phases after lithium solvent extraction are suitable intermediates for production of rubidium compounds, such as Rb2CO3, Rb2SO4 or RbOH.
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Magnesium hydroxide is a valuable chemical produced almost in pure form from seawater and its bitterns through precipitation process. Product size distribution of magnesium hydroxide affects the ease of downstream processes of filtration and drying. Therefore, gaining insight into kinetic information in order to improve the size distribution of product particles is essential. In this work, a mechanistic model has been developed for precipitation of magnesium hydroxide from sea bittern. The parameters of model equations based on the population balance concept have been determined using the experimental data of precipitation from a pure synthetic solution containing 3% Mg2+ and a sea bittern from salt production unit of a local petrochemical complex. The model suggests a higher nucleation rate coefficient and a lower growth rate coefficient for precipitation from the sea bittern compared to that from pure synthetic solution. The nucleation increase and growth decrease which were attributed to the effects of impurities in the bittern, would decrease the settling velocity of the product particles and therefore make the filtration process in industrial use more difficult. However, a larger coefficient of agglomeration rate was predicted by the model for precipitation from the bittern favor to product settling.
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Endothermically decomposing mineral fillers, such as aluminium or magnesium hydroxide, magnesium carbonate, or mixed magnesium/calcium carbonates and hydroxides, such as naturally occurring mixtures of huntite and hydromagnesite are in heavy demand as sustainable, environmentally benign fire retardants. They are more difficult to deploy than the halogenated flame retardants they are replacing, as their modes of action are more complex, and are not equally effective in different polymers. In addition to their presence (at levels up to 70%), reducing the flammable content of the material, they have three quantifiable fire retardant effects: heat absorption through endothermic decomposition; increased heat capacity of the polymer residue; increased heat capacity of the gas phase through the presence of water or carbon dioxide. These three contributions have been quantified for eight of the most common fire retardant mineral fillers, and the effects on standard fire tests such as the LOI, UL 94 and cone calorimeter discussed. By quantifying these estimable contributions, more subtle effects, which they might otherwise mask, may be identified.
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Precipitation of magnesium hydroxide from hard coal mine brine, which contained 2.84 kg/m[sup 3] Mg[sup 2+] and 68.06 kg/m[sup 3] Cl[sup [minus]], by means of sodium hydroxide was tested. In order to increase the sedimentation and filtration rates of the acquired Mg(OH)[sub 2] a so-called forming (of the precipitate) was applied which consisted in introduction of NaOH to a solution containing Mg[sup 2+] ions without stirring. The mixture was then left to stand for some time (called time of forming) and then stirred in order to get quantitative reaction. Within the time of forming, [tau] = 0--24 h, the sedimentation rate increased about 5 times and the filtration rate increased about 60 times. Humidity of the filter cake was also reduced. The microscopic observation showed an increase of particles, and X-ray structural analysis showed an increase in degree of order of Mg(OH)[sub 2] crystal structure when the time of forming increased.
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The chemical precipitation of magnesium from sulphate solution, resulting from heap leaching of nickeliferous laterites with sulphuric acid, was studied. Magnesium was removed as hydroxide using calcium hydroxide (Ca(OH)2) and the precipitate produced was a mixture of magnesium hydroxide (Mg(OH)2) and gypsum (CaSO4·2H2O). The variables studied were the temperature and the stoichiometric quantity of Ca(OH)2. The responses measured were magnesium removal and the specific surface of the precipitate. Design of the experiments and statistical analysis of the data were used in order to determine the main effects and interactions of the factors. Scanning electron microscopy (SEM) was also used to investigate the effect of precipitation conditions on the morphological characteristics of the Mg(OH)2–CaSO4·2H2O mixture. Kinetic analysis with the aid of Nielsen theory allowed the determination of the Mg(OH)2 formation mechanism. The use of a magnesium hydroxide–gypsum mixture as a filler material was also examined. The suitability of the precipitate was evaluated by measuring a set of properties that can characterize a material as a filler and by measuring mechanical properties of polymers filled with the precipitate at various addition levels. The magnesium hydroxide–gypsum precipitate proved to be promising for this application, as it was found to have similar properties with other commercial products.
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Among other applications, magnesium hydroxide is commonly used as a flame-retardant filler in composite materials, as well as a precursor for magnesium oxide refractory ceramic. The microstructure of the powder is of prime importance in both technical applications. The influence of synthesis parameters on the morphological characteristics of magnesium hydroxide nanoparticles precipitated in dilute aqueous medium was studied. Several parameters were envisaged such as chemical nature of the base precipitant, type of counter-ion, temperature and hydrothermal treatment. Special attention was given to the obtaining of platelet-shaped, nanometric and de-agglomerated powders. The powders were characterized in terms of particle size distribution, crystal habits, morphology and ability to be re-dispersed in water. X-ray diffraction (XRD), scanning electron microscopy (SEM), transmission electron microscopy (TEM), nitrogen adsorption and laser diffusion analyses were used for this purpose.
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The cumulative availability curve shows the quantities of a mineral commodity that can be recovered under current conditions from existing resources at various prices. The future availability of a mineral commodity depends on the shape of its cumulative availability curve (determined by geologic considerations, such as the nature and incidence of the available mineral deposits), the speed at which society moves up the curve (determined by future demand and the extent to which this demand is satisfied by recycling), and shifts in the curve (determined by cost-reducing technological change and other factors). While the shape of the curve for any given mineral commodity may or may not be known, it is knowable since the geologic processes responsible for the curve's shape took place many years ago. In contrast, the factors governing how fast society moves up the curve and how the curve shifts over time are not only unknown but also unknowable. Using lithium as an example, this article shows that knowledge about the shape of the cumulative availability curve can by itself provide useful insights for some mineral commodities regarding the potential future threat of shortages due to depletion. Despite the inherent uncertainties surrounding the future growth in lithium demand as well as the uncertainties regarding the future cost-reducing effects of new production technologies, the shape of the lithium cumulative availability curve indicates that depletion is not likely to pose a serious problem over the rest of this century and well beyond.