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Mangan

Mn • Atomic Number 25

Manganese

Manganese is a silvery-white, hard, very brittle transition metal. Its physical and chemical properties are similar to those of iron, but it is harder and more brittle. The element is of great biological importance. In plants, manganese plays a role in oxygen production in photosynthetic bacteria, algae, and plants.

Manganese is characterized by a wide variety of oxidation states.

It is a key raw material for the steel industry and is becoming increasingly important in lithium-ion batteries for electric cars.

Manganese occurs naturally mainly as pyrolusite and is mined in large quantities.
The most important producing countries are South Africa, Gabon, and Australia.

The most significant player is South32 from Australia.

  • History

    The name is derived from the Latin term for brownstone, “magnesia nigra,” and thus shares with the element magnesium the geographical reference to the district of Magnesia in the eastern Greek region of Thessaly, where deposits of minerals of both elements have been known since ancient times.

    Manganese dioxide, also known as brownstone, was used as a pigment in prehistoric cave paintings because of its color. Since ancient times, this mineral has also been used as an additive in glass production, as it helps to remove the green tint from natural glass caused by traces of iron ions.

    It was not until 1740 that the Berlin physician and chemist Johann Heinrich Pott was able to show that pyrolusite does not contain iron, as originally assumed, but another, as yet unknown element.

    It was not until a quarter of a century later that the Swedish chemist Johan Gottlieb Gahn succeeded in producing elemental manganese by reducing pyrolusite with carbon.

    In 1839, it was discovered that manganese improves the malleability of iron. In 1856, Robert Forester Mushet showed that the addition of manganese enabled the mass production of steel using the Bessemer process. This led to manganese being used in large quantities for steel production within a short period of time.

    From the mid-18th century onwards, manganese oxide was also used in the production of chlorine.

  • Application

    90 percent of mined manganese goes to the steel industry in the form of ferromanganese as an alloy component. It removes oxygen and sulfur from the steel and at the same time improves hardening. While normal steel contains about one percent manganese, the proportion in manganese steel is around 13 percent. This extremely hard alloy is used in railroad tracks, safes, and bearings, among other things.

  • Occurrence, Mining and Extraction

    Annual production in 2023 was around 20 million tons per year.

    Manganese is found in many deposits around the world. With estimated global reserves of more than 3 billion tons, a shortage of manganese is not expected.

    The most economically important minerals are pyrolusite, manganite, and hausmannite.

    Manganese occurs in large quantities in so-called manganese nodules in the deep sea.

    South Africa is by far the leading mining country for manganese ores. Its market share is around 60 percent. Several mines are located in the very resource-rich Kalahari Basin, where the Australian company South32 operates several mines.

    South32, which was formed in 2015 through a spin-off from BHP Billion, operates Gemco in Australia, one of the most cost-effective manganese mines in the world, and is one of the largest manganese producers in the world.

    Gabon ranks second in manganese production, where Eramet (France) operates the Moanda mine.

  • Substitution

    There is no suitable substitute for manganese.

Manganese, Mn, transition metal, silvery-white metal, brittle metal, steel alloy, battery metal, manganese properties, industrial uses, raw material, natural occurrence, ISE AG metals, iSE AG

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Magnesium

Mg • Atomic Number 12

Magnesium

Magnesium belongs to the alkaline earth metals and is one of the ten most abundant elements in the Earth’s crust. It occurs in numerous minerals and is essential for all cellular life. The human body contains about 24 grams of magnesium, half of which is stored in the bones, a quarter in the muscles, and the rest in the blood and intracellular spaces. In plants, magnesium is found in the cell walls.

Magnesium is chemically inert at room temperature, neither reacting with oxygen nor water, but it is attacked by acids. When burned, magnesium produces an intensely bright white flame and forms magnesium oxide.

Magnesium shares many properties with aluminum but is about one-third lighter and has a significantly lower density.

It is the lightest structural metal and is used in construction, aerospace, and medicine.

In finely divided form, magnesium burns in air with an intense white light.

The largest magnesium producers are China, Russia, Turkey, and Austria.

Key players in China include Magontec Xinguang and Shanxi Yinguang Huasheng Magnesium. Outside China, Dead Sea Magnesium from Israel and VSMPO-AVISMA in Russia are significant.

Magnesium is considered a critical raw material by the EU and South Korea. The USA and Japan classify magnesium as strategic.

  • History

    The first indications of magnesium date back to the 17th century when English farmers encountered bitter-tasting water. It was later found to contain magnesium sulfate, also known as “Epsom salt.”

    Magnesium was first identified in 1755 by Joseph Black in Edinburgh. The first synthesis of metallic magnesium was achieved by Sir Humphry Davy in London in 1808. In 1831, Antoine-Alexandre-Brutus Bussy (École de Pharmacie in Paris) isolated metallic magnesium.

    The name magnesium is derived from Magnesia, a region in Thessaly, Greece, where the mineral magnesia alba was first discovered.

    The first commercial production of magnesium by electrolysis began as early as 1866 at the German Chemical Factory Griesheim-Elektron. The military build-up during World War I significantly increased demand for magnesium for flares, incendiary bombs, and lightweight metal alloys.

    The Dow Chemical Company (USA) became a pioneer in extracting magnesium from seawater (brine).

    During World War II, magnesium production surged dramatically as demand for aircraft, ammunition, and incendiary bombs skyrocketed.

    Pidgeon Process (1941): Canadian scientist Lloyd Pidgeon developed the thermal reduction process (using dolomite and ferrosilicon), which was later adopted by China.

    By the end of the 20th century, China expanded the use of the Pidgeon Process, leveraging inexpensive coal energy. The Chinese province of Shanxi became the center of low-cost magnesium production.

    Today, China dominates global magnesium production, supplying over 85 percent of worldwide demand.

    In 2021, production cuts in China caused prices to surge by 400 percent and sparked numerous diversification initiatives in Western industrial countries.

  • Application

    The global annual consumption of magnesium is about one million tons and is steadily increasing. Magnesium is the easiest structural metal to work with.

    Since pure magnesium has low structural strength, it is mainly used in the form of alloys—typically containing ten percent or less of aluminum, zinc, and manganese—to improve its hardness, tensile strength, as well as casting, welding, and machinability.

    Magnesium alloys have diverse applications. About half of the global magnesium demand comes from the automotive and aerospace industries. With the rise of electromobility, magnesium demand could increase significantly due to its potential for substantial weight savings. Weight reduction is also a key factor in aerospace.

    Additionally, magnesium is a strong reducing agent used in the production of other metals such as titanium, zirconium, and hafnium from their compounds.

    Magnesium is also used in explosives and pyrotechnics.

  • Occurance, Mining and Extraction

    The raw materials for magnesium production are usually the minerals dolomite, magnesite, and carnallite, as well as seawater.

    Most magnesium is produced via the Pidgeon process. In this method, calcined dolomite is heated with fluorspar and ferrosilicon under vacuum to temperatures above 1,000 °C. The resulting gaseous magnesium condenses and is further purified by vacuum distillation.

    The second process is molten salt electrolysis, where magnesium chloride extracted from seawater is heated with the addition of salts (such as sodium chloride). Magnesium collects on the molten salt surface.

    Magnesium is found in minerals like serpentine, chrysotile, and meerschaum. Seawater contains about 0.13 percent magnesium, mainly as dissolved chloride. As carbonate, it occurs in the form of magnesite and dolomite, as well as in many common silicates such as talc, olivine, and most types of asbestos.

    Magnesium is commercially produced by the electrolysis of molten magnesium chloride (MgCl₂), primarily obtained from seawater, and by direct reduction of its compounds with suitable reducing agents.

    China dominates global production with an 85 to 90 percent share. Following China is Russia, where VSMPO-AVISMA produces magnesium from magnesite in the Ural region.

    Austria plays a smaller yet strategically important role for the EU in magnesium supply, being active in magnesium scrap recycling.

    About 30 percent of the global magnesium demand is met through recycling.

  • Substitution

    Aluminum and zinc can replace magnesium in cast and forged products.

    The relatively low weight of magnesium is an advantage over aluminum and zinc in most applications of cast and forged products; however, its higher cost is a disadvantage compared to these substitutes.

    Calcium carbide can be used instead of magnesium for desulfurizing iron and steel. Magnesium is preferred for desulfurization because calcium carbide produces acetylene in the presence of water.

    Aluminum oxide, chromite, and silicon dioxide replace magnesium oxide in some refractory applications.

Magnesium, Mg, alkaline earth metal, light structural metal, magnesium properties, elemental magnesium, magnesium uses, aerospace, construction metal, magnesium production, magnesium alloys, critical raw material, strategic metal, ISE AG metals, ISE AG

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Lithium

Li • Atomic Number 3

Lithium

Lithium is a chemical element belonging to the group of alkali metals. It is the lightest metal with the lowest density under standard conditions.

Lithium is highly reactive and therefore occurs naturally only in compounds. In moist air, elemental lithium reacts upon contact with skin moisture, causing severe burns.

As a trace element, lithium can also be found in mineral water. Small amounts of lithium are present in the human body.

In its metallic form, lithium is a soft, silvery-gray metal with good thermal and electrical conductivity, enabling it to store and transmit energy. This makes the metal highly valuable for battery applications.

The largest lithium-producing country is Australia. The Greenbushes Mine (Albemarle, Tianqi Lithium) in Western Australia is the largest active mine, followed by the Salar de Atacama (SQM) in Chile.

The three largest lithium producers in 2025 are Albemarle, SQM, and Ganfeng Lithium.

  • History

    The Swede Johan August Arfwedson discovered lithium in 1817 while analyzing mineral samples collected by the Brazilian José Bonefácio de Andrada e Silva from the island of Utö in Sweden. In 1818, the German chemist Christian Gottlob Gmelin discovered that lithium salts produce a red flame coloration — lithium is responsible for the red color in fireworks.

    The first industrial lithium production began in 1923 by the German company Metallgesellschaft AG.

    One of the earliest uses of lithium was in medicine. As a pharmaceutical agent, lithium salts are used in psychiatry to treat bipolar affective disorders, mania, depression, and cluster headaches.

    Around 1940, lithium-based lubricants were developed, which continue to be widely used today.

    In the 1950s, lithium was needed for the development of the hydrogen bomb. This led to large-scale lithium mining in the USA, especially at Kings Mountain, North Carolina.

    Later, lithium found industrial applications as an additive in aluminum smelting as well as in glass and ceramics production.

    The most significant application of lithium today is in the battery industry. It is used in lithium-ion batteries, rechargeable batteries found in electric vehicles, energy storage systems, laptops, smartphones, tablets, and other consumer electronics.

    Starting in the 1970s, researchers began using lithium to develop rechargeable batteries. Building on the work of Stanley Whittingham and John Goodenough, Japanese chemical engineer Akira Yoshino achieved a breakthrough in 1983. His research ultimately led to the commercialization of the lithium-ion battery, first utilized by Sony. In 2019, Whittingham, Goodenough, and Yoshino were awarded the Nobel Prize in Chemistry for their battery research.

    From the 2000s onward, this new battery technology triggered a global lithium boom: between 2000 and 2020, lithium production increased sixfold.

  • Application

    Batteries are by far the most important application for lithium. In 2024, around 87 percent of lithium was used in the battery industry. The main drivers of demand for this lightweight metal are the automotive industry and energy storage systems. An electric vehicle battery contains on average six kilograms of lithium, used in the form of lithium carbonate or lithium hydroxide as anode material. Additionally, rechargeable lithium-ion batteries are widely used in laptops, smartphones, and a variety of other electronic devices.

    Lithium is also used as a lubricant and in the glass and ceramics industry. The amounts of lithium used in pharmaceuticals are very small compared to other sectors.

    Lithium is used in small quantities in nuclear energy, where it is needed for the safe operation of cooling systems in pressurized water reactors.

  • Occurence, Mining and Extraction

    Lithium is widely distributed on Earth, but only in very low concentrations. The most relevant lithium-containing minerals are spodumene, petalite, and lepidolite. Other lithium-bearing minerals that are not yet commercially mined for lithium extraction include zinnwaldite and jadarite.

    Significant lithium deposits are also found in salt lakes and geothermal deep waters.

    The largest lithium resources are located in the salt lakes of the South American Lithium Triangle, which includes Argentina, Bolivia, and Chile. Economically relevant lithium concentrations are also present in geothermal waters, such as those in the Upper Rhine Graben.

    In 2024, the global lithium production was 240,000 tons, with consumption estimated at 220,000 tons.

    The most important producing countries are Australia, Chile, China, Zimbabwe, and Argentina. The globally proven and probable resources total 115 million tons, distributed as follows: Argentina and Bolivia each have 23 million tons; Chile 11 million tons; Australia 8.9 million tons; China 6.8 million tons.

    In the USA, one of the largest lithium deposits in the world is located at Thacker Pass in Nevada. Lithium Americas plans to start mining there in 2027. The only active lithium mining in the USA is also in Nevada: Silver Peak, a salt lake deposit operated by Albemarle.

    Lithium is not mined in Europe except in Portugal, where small quantities are extracted as a by-product for the ceramics and glass industries. However, there are larger deposits and numerous mining projects underway, including in northern Portugal itself.

    In Spain, two lithium deposits in the Extremadura region have been known and developed for several years.

    In Serbia’s Jadar Valley, one of Europe’s largest known lithium deposits is located, which the mining company Rio Tinto plans to develop. The mineral jadarite, discovered only in 2004, is not yet commercially mined for lithium.

    At the German-Czech border, probably Europe’s largest lithium deposit is located. Mining on the Czech side is being advanced by the state energy company ČEZ together with the Australian-British firm European Metals. This project has been classified as a strategic project by the European Commission.

    On the German side, the company Zinnwald Lithium is working on mining efforts. Here too, zinnwaldite is the mineral, which has not yet been commercially exploited for lithium.

    In Finland, the company Keliber could begin lithium mining in western Finland as early as 2026. The project, backed by the South African company Sibanye-Stillwater, has received a €150 million loan from the European Investment Bank.

    In addition to hard rock mining, there are projects in Germany and France for lithium extraction from geothermal deep water. The European Commission has granted strategic project status to initiatives by Vulcan Energy Resources in the Upper Rhine Graben and Eramet in the Alsace region.

    The so-called borehole mining is still a young technology that must be adapted individually to each brine due to its different chemical composition. Once developed, however, this extraction method is considered more efficient and environmentally friendly than traditional mining. Market observer Benchmark Minerals expects the growing importance of these lithium deposits in the future.

    In addition to primary mining, lithium recycling will play an increasingly important role in the future. However, current recovery rates are still low because many large lithium-ion batteries have yet to reach the end of their life cycle, and recycling costs in Western industrial countries remain high. China is by far the global leader in recycling lithium and other battery materials, followed by South Korea and Japan.

  • Substitution

    In the near future, lithium in batteries could be replaced by simple salt: The Chinese battery manufacturer CATL already launched the first sodium-ion batteries for electric vehicles in 2021. Competitors such as BYD and Huawei are also following this trend.

    On Earth, sodium is the sixth most abundant element. This means significantly lower procurement costs compared to lithium, as well as better environmental compatibility in production.

  • Sources

    https://lithium.org/a-brief-history-of-lithium/
    https://www.mining-technology.com/marketdata/ten-largest-lithiums-mines/
    https://www.brimco.io/mining/top-lithium-producers/?srsltid=AfmBOoopXf34iihKY38-ayyz6FIFgF68lQkqopDw9VCWh6CgojGKxS7_
    https://cen.acs.org/articles/91/i26/Lithium-Treating-Gout.html
    https://sqmlitio.com/de/nosotros/historia-del-litio/ 
    https://www.gelbe-liste.de/wirkstoffe/Lithium_41883
    https://www.periodensystem-online.de/index.php?el=3&id=history
    https://de.wikipedia.org/wiki/Lithium 
    https://rudolphina.univie.ac.at/lithium 
    https://elements.visualcapitalist.com/the-key-minerals-in-an-ev-battery/
    https://pubs.usgs.gov/periodicals/mcs2025/mcs2025-lithium.pdf
    https://source.benchmarkminerals.com/article/rise-of-dle-will-open-up-new-sources-of-lithium-supply-this-decade 
    https://world--nuclear-org.translate.goog/information-library/current-and-future-generation/lithium?_x_tr_sl=en&_x_tr_tl=de&_x_tr_hl=de&_x_tr_pto=rq
    https://www.catl.com/en/news/6013.html
    www.bbc.com/future/article/20240319-the-most-sustainable-alternatives-to-lithium-batteries
    https://www.eramet.com/en/news/eramet-es-ageli-geothermal-lithium-project-officially-recognized-as-a-strategic-project-by-the-european-union/ 
    https://www.mining-technology.com/news/lithium-americas-fid-thacker/ 
    https://www.albemarle.com/global/de/location/silver-peak-nv-usa

    https://www.researchgate.net/publication/311781588_Lithiumgewinnung_aus_anspruchsvollen_Lagerstatten_Zinnwaldit_und_magnesiumreiche_Salzseen https://www.gtai.de/de/trade/tschechische-republik/branchen/der-grosse-lithiumrausch-1844422

Lithium, Li, alkaline earth metal, light metal, low density metal, battery metal, lithium properties, reactive metal, lithium uses, lithium in batteries, lithium extraction, lithium production, strategic metal, ISE AG metals, ISE AG

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Indium

In • Atomic Number 49

Indium

Indium is a rare, silvery-white, and soft heavy metal. It is softer than lead and can be easily deformed. Like tin, the pure metal emits a high-pitched “scream” when bent.

Its abundance in the Earth's crust is comparable to that of silver.

It has the unusual property of adhering to and wetting clean glass and other surfaces in its molten state. This makes indium valuable for creating hermetic seals between glass, metals, quartz, ceramics, and marble.

The metal is frequently used in the manufacture of semiconductor devices. However, its most important application is in touchscreens, flat-panel displays (LCDs and OLEDs), and solar modules.

The element occurs in trace amounts in many minerals, especially those containing zinc and lead, from which it is extracted as a byproduct.

The main producing countries are China, South Korea, and Japan.

Key companies include Zhuzhou Smelter Group in China and Korea Zinc in South Korea.

  • History

    Indium was discovered in 1863 by the German chemists Ferdinand Reich and Hieronymus Theodor Richter during the analysis of zinc ore samples. The presence of a prominent indigo-blue spectral line inspired the name.

    A larger quantity of indium was first exhibited at the 1867 World’s Fair in Paris.

    After an initial application starting in 1933 as an alloy component in dental gold, the extensive use of indium began with World War II. The United States used it as a coating in heavily stressed aircraft bearings.

    After World War II, indium was primarily employed in the electronics industry, as solder material, and in low-melting alloys. Its use in control rods for nuclear reactors also became important with the increasing adoption of nuclear energy. This led to a first significant rise in the price of indium by 1980.

    Starting in 1987, two new indium compounds were developed: the semiconductor indium phosphide and indium tin oxide, which is conductive and transparent in thin layers. Indium tin oxide became particularly important with the development of liquid crystal displays. Due to high demand, since 1992 the majority of indium has been further processed into indium tin oxide.

  • Application

    Indium is mainly used as indium tin oxide (ITO), a transparent, conductive coating essential for touchscreens, flat-panel displays (LCDs and OLEDs), and solar modules. About three-quarters of the demand for indium comes from touchscreens, LCD and OLED monitors, and foldable displays.

    Ten to fifteen percent is used in the manufacture of solar cells (thin-film solar cells, perovskite solar cells).

    Indium also plays a role in nuclear reactors.

  • Occurence, Mining and Extraction

    The worldwide indium production amounts to approximately 1.000 tons annually.

    Indium is a byproduct of zinc mining (about 1 ton of indium per 1.000 tons of zinc). Ninety percent of global production is extracted from the zinc ore sphalerite.

    China, Canada, and Peru have zinc deposits with significant indium content, with China dominating the global indium production market with a share of over 50 percent. The largest indium company is Zhuzhou Smelter Group.

    About 30 percent of indium now comes from recycling.

  • Substitution

    Antimony tin oxide coatings have been developed as an alternative to ITO coatings in LCDs.

    Carbon nanotube coatings have been developed as an alternative to ITO coatings in flexible displays, solar cells, and touchscreens.

    Poly(3,4-ethylenedioxythiophene) (PEDOT) has also been developed as a replacement for ITO in flexible displays and organic light-emitting diodes (OLEDs). Copper or silver nanowires have been investigated as substitutes for ITO in touchscreens.

    Graphene has been developed as a replacement for ITO electrodes in solar cells and has also been studied as a substitute for ITO in flexible touchscreens.

    Hafnium can replace indium in control rod alloys for nuclear reactors.

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