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Chrom

Cr • Atomic Number 24

Chromium

Chromium is a hard, steel-gray transition metal. The name derives from chroma, the Greek word for color, as chromium compounds appear in many different hues. While it is relatively abundant in the Earth’s crust, it does not occur in pure form in nature. Most ores consist of the mineral chromite.

Trivalent chromium is considered an essential trace element, with dietary needs typically met through a balanced diet. While chromium(III) is beneficial in small doses, hexavalent chromium is toxic, carcinogenic, and mutagenic.

One of the main uses of chromium is in ferrochrome, an iron alloy containing about 60 percent chromium. Chromium alloys are used in the production of oil pipelines, automotive trims, and cutlery, contributing to their shine.

Chromite is also used as a refractory material and as a raw material for producing chromium chemicals.

Major chromium-producing countries include South Africa, India, Kazakhstan, and Turkey.

The largest chromium mine in the world is the Kemi Mine in Finland, operated by Finnish steel producer Outokumpu.

The largest known chromite deposit globally is the Bushveld Complex in South Africa.

In both the EU and the USA, chromium is classified as a critical raw material.

  • History

    Crocoite (red lead ore) was one of the first chromium minerals to be discovered. In Persia and during the Qin Dynasty in China, it was used to produce pigments for bright yellow-orange colors in ceramics. Chromium oxide green has been used for centuries to color glass or enamel. Vincent van Gogh, for example, used "chrome yellow" in his famous Sunflowers series, which includes a total of seven paintings.

    In 1761, German mineralogist Johann Gottlob Lehmann analyzed a red-orange mineral from Siberia, later identified as crocoite. In 1797, French chemist Nicolas-Louis Vauquelin isolated chromium oxide and, by heating it with carbon, obtained chromium metal. Pure chromium was first produced in 1894 by Hans Goldschmidt using the aluminothermic process. The simpler carbon reduction previously used by Vauquelin also produced chromium carbide alongside the metal.

    At the beginning of the 19th century, chromium compounds were used in dyes, paints, and tanning agents.

    In the 1820s, chromium plating (electroplating) was developed to improve the durability and shine of metals. By the end of the 19th century, it was discovered that adding chromium to iron produced stainless steel. Since then, chromium has been an essential component in stainless steel products such as cutlery, machinery, and construction materials.

    During World War II, chromium was considered a strategic material for armor plating, aircraft engines, and weapons. In the post-war era, chrome plating became widespread in automotive parts (bumpers, trim) and household items.

    Due to the presence of toxic hexavalent chromium (Cr⁶⁺) in industrial waste, chromium poses a significant environmental risk.

  • Application

    About 45.000 tons of chromium are mined annually.

    The majority is used in the metallurgical industry. Approximately 70 percent of chromium goes into stainless steel products alone. Other applications in the metal industry include iron alloys (ferrochromium) used in steel production to increase strength and corrosion resistance. Chromium is also a component of superalloys and tool steels for jet engines and gas turbines.

    On chrome-plated faucets, bumpers, and motorcycle parts, the metal provides shine, corrosion resistance, and protection against wear.

    Chromium oxide serves as a pigment for green shades in paints, ceramics, and glass, as well as a refractory material, for example in heat-resistant bricks for furnaces. Chromite is also added to bricks and stones to make them fireproof.

    Although chromium compounds cover the entire color spectrum, only a few of them are used as pigments.

    China is the leading producer of ferrochromium and stainless steel, as well as the largest consumer of chromium.

  • Occurence, Mining and Extraction

    90 percent of the chromium mined worldwide comes from chromite deposits. Other chromium minerals include crocoite, uvarovite, eskolaite, and chromdiopside.

    Global resources amount to over 12 billion tons of chromite, enough to meet demand for centuries. Geographically, 95 percent of the world’s chromium deposits are concentrated in Kazakhstan and Southern Africa.

    The largest chromium producers include South Africa, India, Kazakhstan, and Turkey.

    The largest active chromium mine in the world is the Kemi Mine in Finland, operated by the Finnish steel producer Outokumpu.

    The world’s largest chromite deposit is the Bushveld Complex in South Africa.

  • Substitution

    Chromium is irreplaceable for its most important applications, neither in stainless steel nor in superalloys.

    Chromium-containing scrap can substitute for ferrochrome in some metallurgical applications.

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Calcium

Ca • Atomic Number 20

Calcium

Calcium is an alkaline earth metal. After iron and aluminum, it is the third most abundant metal and the fifth most abundant element in the Earth's crust. Calcium occurs naturally only in compounds, mostly in the form of calcite. These include limestone, calcite, marble, chalk, and shell limestone. Entire mountain ranges, such as the Northern Limestone Alps in Austria, can consist of calcium ores. Gypsum is another form of large natural calcium deposits.

Calcium is essential for plants and animals. It is an important component of bones, teeth, shells, mussels, and plant cell walls. Calcium also plays a crucial role in signal transmission within the nervous system. The human body consists of about two percent calcium.

The most important industrial application of calcium is in the construction industry, mainly as gypsum and as an additive in mortar. Other uses are found in the steel and metal industry, paper manufacturing, water treatment, chemical industry, and as a fertilizer.

The largest producers of gypsum, limestone, and lime are China and the USA. Since the deposits are widely distributed across the globe, there is virtually no scarcity of this raw material.

  • History

    Limestone has been used for tens of thousands of years. Crushed limestone was already used as a pigment (white chalk) in prehistoric cave paintings. Lime mortar was used in constructions as early as 10.000 BC in Mesopotamia and in ancient Egypt. The outer walls of the Great Pyramid of Giza (around 2600 BC) were made of Tura limestone. The ancient Romans used lime concrete in the construction of the Pantheon.

    The name “Calcium” is derived from the Latin word calx. The Romans used this term to denote lime, limestone, chalk, and mortar made from lime.

    The silvery, relatively soft and light metal was first isolated in 1808 by Sir Humphry Davy, after he distilled mercury from an amalgam produced by the electrolysis of a mixture of lime and mercury oxide.

  • Application

    The most commonly used calcium compound across various industries is calcium carbonate, also known as limestone, which is inexpensive and versatile.

    It is the main component of the most important building materials: cement, mortar, and concrete. Calcium carbonate is used in the paper industry as a filler or coating to achieve smoothness and brightness. In agriculture, limestone is used to improve acidic soils.

    Calcium oxide, also known as quicklime, is produced by heating the raw material calcium carbonate. Calcium oxide is used in steel production, water treatment, and chemical manufacturing.

    Calcium hydroxide (slaked lime) is used in wastewater treatment, leather tanning, and mortar production.

    Calcium sulfate (gypsum or plaster) is another application in the building materials industry. Calcium chloride is used in road de-icing agents, food preservatives, concrete accelerators, and drying agents.

    Pure calcium metal is used as an alloying element for aluminum, copper, lead, magnesium, and other base metals, as a deoxidizer for certain high-temperature alloys, and as a getter in vacuum tubes.

    The production volumes of calcium metal are relatively low compared to other metals, ranging from 10.000 to 20.000 tons annually.

  • Occurence, Mining and Extraction

    Calcium is a very abundant element in the Earth’s crust and occurs in numerous minerals, many of which are economically significant.

    The most common sources of calcium are carbonate minerals such as calcite, found in limestone, marble, and chalk. Calcium is also present in sulfate minerals like gypsum and anhydrite, in phosphate minerals such as apatite, and in silicate minerals including wollastonite, plagioclase feldspar, and grossular.

    The main producing countries of calcium metal are China, Russia, France, and the USA.

  • Substitution

    Limestone (calcium carbonate) is a substitute for lime (calcium oxide) in many applications, such as agriculture, flux production, and sulfur removal. Limestone contains fewer reactive substances, reacts more slowly, and may have additional disadvantages compared to lime depending on the application. However, limestone is significantly cheaper than lime.

    Calcined gypsum is an alternative material for industrial plasters and mortars.

    Cement, cement kiln dust, fly ash, and lime kiln dust are potential substitutes for some construction applications of lime.

    Magnesium hydroxide is a substitute for lime in pH regulation, and magnesium oxide is a substitute for dolomitic lime as a flux in steel production.

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Cadmium

Cd • Atomic Number 48

Cadmium

Cadmium is a silvery, shiny, soft, and malleable metal. Physically, cadmium is similar to zinc but denser and softer.

A cadmium bar can be bent and produces a crackling sound, known as “tin cry,” which is also observed with a few other metals. With an abundance of about 0.2 grams per ton in the Earth’s crust, cadmium is a rare element.

It is often found in association with zinc ores as greenockite (cadmium sulfide) or as cadmium carbonate. Elemental cadmium is even rarer. However, deposits exist in eastern Siberia, Kazakhstan, and the U.S. state of Nevada. Today, cadmium is primarily obtained as a byproduct of zinc production.

In the chemical industry, cadmium is an unavoidable byproduct of zinc, lead, and copper extraction.

The metal and many of its compounds are toxic and carcinogenic. Due to its high toxicity, the use of cadmium is declining. Since 2011, it has been banned in jewelry, soldering alloys, and PVC within the European Union.

Cadmium metal and compounds are mainly used in nickel-cadmium batteries, but also in alloys, coatings, and pigments. It is increasingly used in cadmium telluride thin-film solar modules (CdTe).

China, South Korea, Canada, and Japan are global leaders in cadmium refining.

Cadmium is not classified as a globally prioritized critical raw material, but in some sectors—military, aerospace, and niche electronics—it is considered strategically important.

  • History

    Cadmium was discovered around the year 1820. The chemists Carl Wilhelm Gottlob Kastner, Friedrich Strohmeyer, and the physician Johann Roloff independently came across the element at roughly the same time.

    For a long time, cadmium sulfides and selenides were used as pigments, ranging in color from yellow to reddish-brown. Cadmium yellow, for instance, was detected in Claude Monet’s painting "Bordighera."

    Starting in 1925, Bayer AG began industrial production of cadmium yellow. Until 1980, cadmium yellow was the official color of the German Federal Post Office. Even today, the yellow mailboxes in Germany still bear this color.

    Early reports from the 19th century already pointed to the harmful health effects of the metal. Nevertheless, cadmium iodide was used at the time to treat swollen joints and frostbite.

  • Application

    The majority of cadmium produced is used in rechargeable nickel-cadmium batteries (NiCd batteries). These batteries provide essential emergency power functions to ensure the safety of passengers in the event of a power outage in subways, high-speed trains, and aircraft.

    In consumer products, the use of NiCd batteries has been banned in the EU since 2017.

    Larger quantities of cadmium are also used for corrosion-resistant coatings (cadmium plating) on steel, aerospace components, and fasteners. However, their use is restricted in the EU due to associated health risks.

    Another economically valuable compound is cadmium sulfide (CdS), a bright yellow pigment known as cadmium yellow. It is used in high-quality paints and artist pigments due to its color stability.

    Cadmium telluride (CdTe) is used in thin-film photovoltaic cells, the second most common solar technology after silicon. The market leader in this field is the U.S. company First Solar.

  • Occurence, Mining and Extraction

    Approximately 24,000 tonnes of refined cadmium are produced globally each year.

    Sphalerite is the most economically important zinc ore mineral and also contains small amounts of cadmium. Cadmium is primarily obtained from zinc ores and concentrates.

    The leading production countries are China, South Korea, Canada, and Japan.

    Korea Zinc is considered the most important cadmium producer. Other major players include Nyrstar (Trafigura), Teck Resources (Canada), Hindustan Zinc (India), Glencore (Switzerland), and Boliden (Sweden). In China, the Zhuzhou Smelter Group is regarded as the leading cadmium producer.

    In the EU, the recycling rate for cadmium is estimated at around 30 percent.

  • Substitution

    Batteries with other chemical compositions, particularly lithium-ion batteries, can replace NiCd batteries in many applications.

    Where the surface properties of a coating are not critical (e.g. for fasteners in aircraft), coatings such as zinc-nickelcan replace cadmium in many coating applications.

    Cerium sulfide is used as a substitute for cadmium pigments, primarily in plastics. Barium stabilizers can replace barium-cadmium stabilizers in flexible polyvinyl chloride (PVC) applications.

    Thin-film technologies based on copper indium gallium diselenide and perovskite materials continue to be researched, but are not yet commercially viable.

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Bismuth

Bi • Atomic Number 83

Bismuth

Bismuth is hard, brittle, coarse-crystalline, and shiny with a reddish sheen. It occurs in the Earth's crust about as frequently as silver. It is characterized by diamagnetism and its density anomaly: when solidifying, bismuth expands by about 3,3 percent. After mercury, it has the lowest thermal conductivity among metals, and its electrical conductivity is very poor. Among heavy metals, it has the lowest toxicity. However, bismuth powder can pose an explosion risk under certain conditions.

Bismuth is mainly used in pharmaceuticals, cosmetics, alloys, and the chemical industry and is employed in a number of niche applications.

Important producing countries are China, Laos, Vietnam, and Japan.

The largest active bismuth mine is the Shizhuyuan Polymetallic Mine in the Chinese province of Hunan, operated by Hunan Nonferrous Metals.

Bismuth is a critical raw material for the EU, Japan, and South Korea, while the USA classifies the element as strategic.

  • History

    Bismuth has been known since very early times because it occurs both in native form and in compounds. However, it was long not clearly recognized as a distinct metal and was often confused with lead, antimony, and tin.

    It is suspected that long before its official discovery, bismuth was used in mines as a pigment for silver-colored writings and miniature paintings. For this purpose, bismuth was smelted from bismite or bismuth ochre. In the 14th century, it was discovered in elemental form in the Saxon Ore Mountains.

    By the mid-15th century, bismuth gained importance as an alloying component for printing types. Adding bismuth both lowers the melting point and makes the printing types harder and more resistant to wear.

    Bismuth was recognized as a distinct element after the mid-18th century by the chemists Claude François Geoffroy and Johann Heinrich Pott.

  • Application

    The largest application areas for bismuth are found in the metal industry, pharmaceuticals (especially as Pepto-Bismol), cosmetics, and the chemical industry. Due to its antiseptic properties, it is used in burn ointments. In eyeshadows, lipsticks, and nail polishes, it provides a pearlescent shimmer.

    Metallic bismuth is mainly used in alloys, to which it imparts special properties such as a low melting point and expansion upon solidification. Bismuth is therefore a useful component of type metal alloys, which produce clean castings. It is also an important component in low-melting alloys. These so-called fusible alloys are used in fire detectors and sprinkler systems.

    A bismuth-manganese alloy has proven effective as a permanent magnet.

    In solders, ammunition, fishing weights, and radiation shielding, bismuth is increasingly used as a lead substitute due to its non-toxicity.

    Another emerging market could result from the development of new classes of semiconductors, thermoelectric materials, and topological insulators. Furthermore, bismuth could be relevant for the advancement of quantum computers.

  • Occurence

    Around 18.000 tons of bismuth are produced globally each year, with most of it coming from China, which holds about an 80 percent market share. Other mining and production countries include Laos, South Korea, Vietnam, and Japan.

    Native bismuth is rare in nature. The most common bismuth-containing ores are bismuthinite (bismuth glance), bismite (bismuth ochre), and wismutite.

    Bismuth deposits are often associated with lead, zinc, tin, and silver ores. It is found, for example, in tungsten ores in South Korea, lead ores in Mexico, copper ores in Bolivia, and both lead and copper ores in Japan.

    Since the beginning of the 21st century, China has taken a leading role worldwide in both the mining and refining of bismuth.

    Commercial bismuth is mostly obtained as a by-product during the smelting and refining of lead, tin, copper, silver, and gold ores.

    The largest active mine producing bismuth is the Shizhuyuan Polymetallic Mine in the Chinese province of Hunan, operated by Hunan Nonferrous Metals. Bismuth is mainly obtained as a by-product during tungsten processing.

    Other significant producers include Zhuzhou Keneng New Material, Hunan Jinwang Bismuth Industrial, Yunnan Tin Group (YTC) in China; Met-Mex Peñoles in Mexico; Masan High-Tech Materials in Vietnam; 5N Plus in Canada; Belmont Metals in the USA; Comibol in Bolivia; and Korea Zinc in South Korea.

  • Substitution

    In fusible alloys, bismuth can be replaced by the much more expensive indium or gallium. Cheaper tin-lead alloys are also an option, but their toxicity must be taken into account.

    In radiation shielding, it can be substituted by tungsten, lead, or depleted uranium.
    Instead of Pepto-Bismol, aluminum/magnesium hydroxide (antacids) or proton pump inhibitors (PPIs) can be used in pharmaceuticals.

    In cosmetic products, the pearlescent effect can be achieved using mica-based pigments instead of bismuth oxychloride.

    In fishing weights, bismuth can be replaced with steel, tin, or the more expensive tungsten.

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Beryllium

Cer • Ce • Atomic Number 58

Beryllium

Beryllium is a very hard and brittle lightweight metal. It is three times lighter than aluminum and six times stronger than steel. The element is also characterized by its natural resistance to corrosion, excellent electrical conductivity, and high heat capacity.

Due to these properties, beryllium is of great interest to the aerospace and defense industries. Despite its unique characteristics, beryllium is rarely used overall because of its high cost and toxicity.

In 2024, an estimated 360 tons of beryllium were mined worldwide. By far the most important producer is the USA, which also holds 60 percent of the world’s known reserves. Leading beryllium producers include Materion. Other mining countries are China, Mozambique, and Nigeria.

In the EU, USA, China, Japan, South Korea, and Russia, beryllium is considered a critical or strategic raw material.

These metals are very commonly used in industry and are therefore traded as futures contracts on the LME (London Metal Exchange).

  • History

    The element beryllium was discovered in 1798 by the French chemist Louis-Nicolas Vauquelin in the minerals beryl and emerald. In the 1920s, copper-beryllium alloys were first used in German telephone switchboard relays.

    The first commercially successful process for producing pure beryllium was developed in 1932, initially used in medical X-ray windows.

    Beryllium oxide ceramics were employed in insulating circuits of radio tubes.

    In the 1940s, the element found its place in the defense industry: in high-precision gyroscopic navigation and targeting instruments for the navy and air force, and in nuclear weapons as a neutron moderator.

    After World War II, demand for beryllium increased for use in telecommunications technologies, the automotive industry, and aerospace. A heat shield made of beryllium was onboard the Mercury space capsule during the first manned space flight in 1961.

    In the 1990s, new beryllium materials such as aluminum-beryllium metal matrix composites were developed. The applications of beryllium increasingly shifted from defense, aerospace, and aviation toward automotive electronics, IT, and energy production.

    Nickel-beryllium alloys in crash sensors improve the functionality of life-saving airbags.

  • Application

    Worldwide consumption of beryllium remains low. In 2024, an estimated 360 tons were produced. Of this, 21 percent is used in defense, aerospace, and aviation, 20 percent in industrial components, and 15 percent in the automotive industry. In the EU, beryllium is classified as a critical raw material.

    The majority of globally produced beryllium (about 80 percent) is used in copper alloys. The reliability of copper-beryllium alloys enables high-performance, electrically conductive connections for critical systems such as aircraft and medical electronics, airbag and anti-lock braking systems in vehicles, as well as fire suppression systems. In mobile phones and electronic devices, beryllium extends the device lifespan.

    As a pure metal, beryllium is used in medical X-ray windows and in highly precise navigation and targeting systems for the military.

    Beryllium ceramics are employed in photovoltaic cells, significantly increasing their efficiency.

    Beryllium also plays a role in nuclear research and power generation, serving both as a neutron moderator in nuclear power plants and as a neutron source. The experimental fusion reactor ITER in southern France is lined with beryllium plates that act as a protective layer. Beryllium is also essential for nuclear weapons production. Therefore, the United States enforces strict export controls on beryllium.

    Beryllium-containing alloys, in their solid form as found in end products, pose no special health risks. However, certain processing methods generate dust particles that, if inhaled, can cause serious lung diseases.

  • Occurence, Mining and Extraction

    There are about 30 known minerals containing beryllium. For economic mining, beryl and bertrandite are relevant. Beryl contains between three and five percent beryllium but is harder than bertrandite, which complicates refining. Therefore, most beryllium mines today exploit bertrandite deposits despite their lower beryllium content (0,3–1,5 percent).

    More than half of the world’s beryllium production comes from the USA. The largest deposit is located in the state of Utah and is operated by Materion. The proven and probable bertrandite reserves in Utah total approximately 19,000 tons of beryllium.

    Worldwide known beryllium reserves are estimated at over 100,000 tons, with 60 percent located in the USA. The largest deposits in the USA are found at Spor Mountain in Utah, McCullough Butte in Nevada, Black Hills in South Dakota, Sierra Blanca in Texas, Seward Peninsula in Alaska, and Gold Hill in Utah.

    Beryllium production in the USA includes mining, ore processing, manufacturing, distribution, and recycling of beryllium-containing products. Japan does not mine beryllium ores but imports them for its refineries. In Kazakhstan, beryllium is refined from large stockpiles dating back to the Soviet era.

    China has significantly increased its beryllium production in recent years, more than tripling it between 2015 and 2021. Given its strategic importance for defense and the military, China established a "Strategic Alliance for Technological Innovation in the Chinese Beryllium Industry" in 2020.

  • Substitution

    Since beryllium is expensive compared to other materials, it is used in applications where its properties are critical. In some cases, certain metal matrix or organic composites, high-strength aluminum alloys, pyrolytic graphite, silicon carbide, steel, or titanium can replace beryllium metal or beryllium composites.

    Copper alloys with nickel and silicon, tin, titanium, or other alloying elements, or phosphor bronze alloys (copper-tin-phosphorus) can substitute for beryllium-copper alloys, although this may result in significant performance reductions.

    Aluminum nitride or boron nitride can replace beryllium oxide.

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