Spodumene | |
---|---|
General | |
Category | Inosilicate |
Formula (repeating unit) | lithium aluminium silicate, LiAl(SiO3)2 |
IMA symbol | Spd [1] |
Strunz classification | 9.DA.30 |
Dana classification | 65.1.4.1 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/c |
Unit cell | a = 9.46 Å, b = 8.39 Å c = 5.22 Å β = 110.17°; Z = 4 |
Identification | |
Color | Highly variable: white, colorless, gray, pink, lilac, violet, yellow and green, may be bicolored; emerald green – hiddenite; lilac – kunzite; yellow – triphane |
Crystal habit | prismatic, generally flattened and elongated, striated parallel to {100}, commonly massive |
Twinning | Common on {100} |
Cleavage | Perfect prismatic, two directions {110} ∧ {110} at 87° |
Fracture | Uneven to subconchoidal |
Tenacity | Brittle |
Mohs scale hardness | 6.5–7 |
Luster | Vitreous, pearly on cleavage |
Streak | white |
Specific gravity | 3.03–3.23 |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.648–1.661 nβ = 1.655–1.670 nγ = 1.662–1.679 |
Birefringence | δ = 0.014–0.018 |
Pleochroism | Strong in kunzite: α-purple, γ-colorless; hiddenite: α-green, γ-colorless |
2V angle | 54° to 69° |
Fusibility | 3.5 |
Solubility | insoluble |
Other characteristics | Tenebrescence, chatoyancy |
References | [2] [3] [4] [5] |
Spodumene is a pyroxene mineral consisting of lithium aluminium inosilicate, Li Al(Si O 3)2, and is a commercially important source of lithium. It occurs as colorless to yellowish, purplish, or lilac kunzite (see below), yellowish-green or emerald-green hiddenite, prismatic crystals, often of great size. Single crystals of 14.3 m (47 ft) in size are reported from the Black Hills of South Dakota, United States. [6] [7]
The naturally-occurring low-temperature form α-spodumene is in the monoclinic system, and the high-temperature β-spodumene crystallizes in the tetragonal system. α-spodumene converts to β-spodumene at temperatures above 900 °C. [5] Crystals are typically heavily striated parallel to the principal axis. Crystal faces are often etched and pitted with triangular markings.[ not verified in body ]
Spodumene was first described in 1800 for an occurrence in the type locality in Utö, Södermanland, Sweden. It was discovered by Brazilian naturalist Jose Bonifacio de Andrada e Silva. The name is derived from the Greek spodumenos (σποδούμενος), meaning "burnt to ashes", owing to the opaque ash-grey appearance of material refined for use in industry. [2]
Spodumene occurs in lithium-rich granite pegmatites and aplites. Associated minerals include: quartz, albite, petalite, eucryptite, lepidolite and beryl. [3]
Transparent material has long been used as a gemstone with varieties kunzite and hiddenite noted for their strong pleochroism. Source localities include Democratic Republic of Congo, Afghanistan, Australia, Brazil, Madagascar (see mining), Pakistan, Québec in Canada, and North Carolina and California in the U.S.
Since 2018, the Democratic Republic of Congo (DRC) has been known to have the largest lithium spodumene hard rock deposit in the world, with mining operations occurring in the central DRC territory of Manono, Tanganyika Province. [8] As of 2021, the Australian company AVZ Minerals [9] is developing the Manono Lithium and Tin project and has a resource size of 400 million tonnes of high grade low impurities at 1.65% lithium oxide (Li 2 O) [10] spodumene hard-rock based on studies and drilling of Roche Dure, one of several pegmatites in the deposit.
Spodumene is an important source of lithium, for use in ceramics, mobile phones and batteries (including for automotive applications), medicine, Pyroceram and as a fluxing agent. As of 2019, around half of lithium is extracted from mineral ores, which mainly consist of spodumene. Lithium is recovered from spodumene by dissolution in acid, or extraction with other reagents, after roasting to convert it to the more reactive β-spodumene. The advantage of spodumene as a lithium source compared to brine sources is the higher lithium concentration, but at a higher extraction cost. [11]
In 2016, the price was forecast to be $500–600/ton for years to come. [12] However, price spiked above $800 in January 2018, and production increased more than consumption, reducing the price to $400 in September 2020. [13] [14]
World production of lithium via spodumene was around 80,000 metric tonnes per annum in 2018, primarily from the Greenbushes pegmatite of Western Australia and from some Chinese and Chilean sources. The Talison Minerals mine in Greenbushes, Western Australia (involving Tianqi Lithium, Albemarle Corporation and Global Advanced Metals), is reported to be the world's second largest and to have the highest grade of ore at 2.4% Li2O (2012 figures). [15]
In 2020, Australia expanded spodumene mining to become the leading lithium producing country in the world. [16]
An important economic concentrate of spodumene, known as spodumene concentrate 6 or SC6, is a high-purity lithium ore with approximately 6 percent lithium content being produced as a raw material for the subsequent production of lithium-ion batteries for electric vehicles. [17] [18]
Extraction of lithium from spodumene, often spodumene concentrate 6 (SC6), is challenging due to the tight binding of lithium in the crystal structure.
Traditional lithium refining in the 2010s involves acid leaching of lithium-containing ores, precipitation of impurities, concentration of the lithium solution, and then conversion to lithium carbonate or lithium hydroxide. These refining methods result in significant quantities of caustic waste effluent and tailings, which are usually either highly acidic or alkali. [11]
Another processing method relies on pyrometallurgical processing of SC6—roasting at high temperatures exceeding 800 °C (1,470 °F) to convert the spodumene from the tightly-bound alpha structure to a more open beta structure from which the lithium is more easily extracted—then cooling and reacting with various reagents in a sequence of hydrometallurgical processing steps. Some offer the use of non-caustic reagents and result in reduced waste streams, potentially allowing the use of a closed-loop refining process. [19]
Suitable extraction reagents include alkali metal sulfates, such as sodium sulfate; sodium carbonate; chlorine; or hydrofluoric acid. [20] A common form of more highly refined lithium is lithium hydroxide, commonly used as an input in the battery industry to manufacture lithium-ion (Li-ion) battery cathode material.
This section needs additional citations for verification .(November 2022) |
Hiddenite is a pale, emerald-green gem variety first reported from Alexander County, North Carolina, U.S. [21] It was named in honor of William Earl Hidden (16 February 1853 – 12 June 1918), mining engineer, mineral collector, and mineral dealer. [22] [ additional citation(s) needed ]
This emerald-green variety of spodumene is colored by chromium, just as for emeralds. Some green spodumene is colored with substances other than chromium; such stones tend to have a lighter color; they are not true hiddenite.
Kunzite is a purple-colored gemstone, a variety of spodumene, with the color coming from minor to trace amounts of manganese. Exposure to sunlight can fade its color. [22]
Kunzite was discovered in 1902, and was named after George Frederick Kunz, Tiffany & Co's chief jeweler at the time, and a noted mineralogist. [22] It has been found in Brazil, the U.S., Canada, CIS, Mexico, Sweden, Western Australia, Afghanistan and Pakistan. [22] [23]
Triphane is the name used for yellowish varieties of spodumene. [24]
Amblygonite is a fluorophosphate mineral, (Li,Na)AlPO4(F,OH), composed of lithium, sodium, aluminium, phosphate, fluoride and hydroxide. The mineral occurs in pegmatite deposits and is easily mistaken for albite and other feldspars. Its density, cleavage and flame test for lithium are diagnostic. Amblygonite forms a series with montebrasite, the low fluorine endmember. Geologic occurrence is in granite pegmatites, high-temperature tin veins, and greisens. Amblygonite occurs with spodumene, apatite, lepidolite, tourmaline, and other lithium-bearing minerals in pegmatite veins. It contains about 10% lithium, and has been utilized as a source of lithium. The chief commercial sources have historically been the deposits of California and France.
Beryl ( BERR-əl) is a mineral composed of beryllium aluminium silicate with the chemical formula Be3Al2Si6O18. Well-known varieties of beryl include emerald and aquamarine. Naturally occurring hexagonal crystals of beryl can be up to several meters in size, but terminated crystals are relatively rare. Pure beryl is colorless, but it is frequently tinted by impurities; possible colors are green, blue, yellow, pink, and red (the rarest). It is an ore source of beryllium.
Lithium is a chemical element; it has symbol Li and atomic number 3. It is a soft, silvery-white alkali metal. Under standard conditions, it is the least dense metal and the least dense solid element. Like all alkali metals, lithium is highly reactive and flammable, and must be stored in vacuum, inert atmosphere, or inert liquid such as purified kerosene or mineral oil. It exhibits a metallic luster. It corrodes quickly in air to a dull silvery gray, then black tarnish. It does not occur freely in nature, but occurs mainly as pegmatitic minerals, which were once the main source of lithium. Due to its solubility as an ion, it is present in ocean water and is commonly obtained from brines. Lithium metal is isolated electrolytically from a mixture of lithium chloride and potassium chloride.
Lithium carbonate is an inorganic compound, the lithium salt of carbonic acid with the formula Li
2CO
3. This white salt is widely used in processing metal oxides. It is on the World Health Organization's List of Essential Medicines for its efficacy in the treatment of mood disorders such as bipolar disorder.
Topaz is a silicate mineral made of aluminum and fluorine with the chemical formula Al2SiO4(F, OH)2. It is used as a gemstone in jewelry and other adornments. Common topaz in its natural state is colorless, though trace element impurities can make it pale blue or golden brown to yellow-orange. Topaz is often treated with heat or radiation to make it a deep blue, reddish-orange, pale green, pink, or purple.
A pegmatite is an igneous rock showing a very coarse texture, with large interlocking crystals usually greater in size than 1 cm (0.4 in) and sometimes greater than 1 meter (3 ft). Most pegmatites are composed of quartz, feldspar, and mica, having a similar silicic composition to granite. However, rarer intermediate composition and mafic pegmatites are known.
Pleochroism is an optical phenomenon in which a substance has different colors when observed at different angles, especially with polarized light.
Hiddenite is a pale-to-emerald green variety of spodumene that is sometimes used as a gemstone.
Elbaite, a sodium, lithium, aluminium boro-silicate, with the chemical composition Na(Li1.5Al1.5)Al6Si6O18(BO3)3(OH)4, is a mineral species belonging to the six-member ring cyclosilicate tourmaline group.
Mining in Afghanistan was controlled by the Ministry of Mines and Petroleum, prior to the August 15th takeover by the Taliban. It is headquartered in Kabul with regional offices in other parts of the country. Afghanistan has over 1,400 mineral fields, containing barite, chromite, coal, copper, gold, iron ore, lead, natural gas, petroleum, precious and semi-precious stones, salt, sulfur, lithium, talc, and zinc, among many other minerals. Gemstones include high-quality emeralds, lapis lazuli, red garnet and ruby. According to a joint study by The Pentagon and the United States Geological Survey, Afghanistan has an estimated US$1 trillion of untapped minerals.
Manono is a town and territory in Tanganyika Province, Democratic Republic of the Congo.
Hiddenite, North Carolina, United States, is a centre for the mining of gemstones. Three larger mines found there are Adams Mine, NAEM and the Emerald Hollow Mine. They are collectively known as the Hiddenite Gem Mines.
Greenbushes mine is an open-pit lithium mining operation located south of the town of Greenbushes, Western Australia. It is the world's largest hard-rock lithium mine, producing approximately 1.95 million tonnes of lithium spodumene annually. The mine is 250 kilometres south of Perth and 90 kilometres southeast of the port of Bunbury.
The Manono-Kitolo mine is a former tin and coltan mine, which also contains one of the largest lithium reserves globally, in the Democratic Republic of the Congo. The mine is located in southern Democratic Republic of the Congo in Tanganyika Province. The Manono-Kitolo mine has reserves amounting to 120 million tonnes of lithium ore grading 0.6% lithium thus resulting 0.72 million tonnes of lithium.
Tianqi Lithium Corp is a Chinese mining and manufacturing company based in Sichuan.
Australia has one of the biggest lithium reserves and is the biggest producer of lithium by weight, with most of its production coming from mines in Western Australia. Most Australian lithium is produced from hard-rock spodumene, in contrast to other major producers like Argentina, Chile and China, which produce it mainly from salt lakes.
The Harding Pegmatite Mine is a former adit mine that extracted lithium, tantalum, and beryllium from a Precambrian pegmatite sill. It ceased operations in 1958 and its owner, Arthur Montgomery, donated it to the University of New Mexico, which runs the site as an outdoor geology laboratory with mineral collecting permitted on a small scale.
Aquamarine is a pale-blue to light-green variety of the beryl family, with its name relating to water and sea. The color of aquamarine can be changed by heat, with a goal to enhance its physical appearance. It is the birth stone of March.
The Finnis Lithium Project is a lithium mine situated near Darwin in the Northern Territory, Australia. It is being developed by Core Lithium.
The Sandawana Mines are a mining complex in Mberengwa District, Midlands Province of Zimbabwe, primarily known for its emeralds. The mines are sixty-five kilometers south of the town of Mberengwa.