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Group 4 element

physical science Maturity 11-13 Next article →

Group 4 is the second group of transition metals found in the periodic table. This family is often called the titanium group or the titanium family. It consists of four specific elements: titanium (Ti), zirconium (Zr), hafnium (Hf), and rutherfordium (Rf). These elements are all hard, silvery metals. While the first three occur naturally in the Earth's crust, rutherfordium is a synthetic element. This means it does not exist in nature and must be produced by scientists in a laboratory.

The chemical behavior of these metals is defined by their electron configurations. Most of their chemistry is dominated by a group oxidation state of +4. This refers to the charge an atom carries when it reacts. Zirconium and hafnium are very similar because of a phenomenon called the lanthanide contraction. This effect happens because the addition of 4f elements shrinks the expected increase in atomic radius. Consequently, zirconium and hafnium have nearly identical properties. Titanium is somewhat different because it is smaller. It can also exist in a +3 oxidation state, which is a less stable charge.

HeavyMineralsBeachSand
HeavyMineralsBeachSand

Although these metals are chemically reactive, they appear very stable in their bulk form. This is due to the formation of a dense oxide layer on their surface. When the metal is exposed to air, it creates a thin skin of oxide. This layer protects the metal from corrosion and attacks from many acids and alkalis. Even if the layer is removed, it will reform itself. However, they are not invincible. If the metal is finely divided into small particles, it can become pyrophoric. This means it can react directly and rapidly with oxygen, hydrogen, or even nitrogen.

HeavyMineralsBeachSand
HeavyMineralsBeachSand

History shows that discovering these elements required great persistence. Zircon was used as a gemstone since ancient times, but its composition remained a mystery for a long time. In 1789, German chemist Martin Heinrich Klaproth analyzed the mineral jargoon and found a new oxide. He could not isolate the element itself. In 1791, William Gregor identified titanium in illenite sand in Cornwall, Great Britain. He found a metal oxide that he could not identify. Klaproth later rediscovered this oxide in 1795 in the village of Boinik, Hungary. He named the element after the Titans of Greek mythology.

HeavyMineralsBeachSand
HeavyMineralsBeachSand

Finding hafnium was much more difficult than finding the other members. In 1914, Henry Moseley used X-ray spectroscopy to show how atomic numbers determine an element's place in the table. His work suggested that element 72 was missing. After some scientific controversy regarding previous claims, Dirk Coster and Georg von Hevesy searched zirconium ores. They successfully discovered hafnium in 1923 in Copenhagen, Denmark. They named it after Hafnia, the Latin name for the city. The delay in finding it was caused by its rarity and its extreme similarity to zirconium.

HeavyMineralsBeachSand
HeavyMineralsBeachSand

Researchers also had to struggle to identify rutherfordium. In 1964, a team at the Joint Institute for Nuclear Research claimed to have produced it. However, more conclusive evidence came in 1969 from the University of California, Berkeley. They synthesized element 104 by bombarding a californium-249 target with carbon-12 ions. This led to a naming dispute between the Dubna group and the Berkeley group. Eventually, an international working party decided to use the name rutherfordium in 1997. This name honors the scientist Ernest Rutherford.

HeavyMineralsBeachSand
HeavyMineralsBeachSand

Producing these metals requires specialized industrial processes. One common method is the Kroll process used to create workable metals. In this process, oxides are reacted with coal and chlorine to create chlorides. These chlorides are then reacted with magnesium to yield the pure metal. Another method is the chemical transport reaction developed by van Arkel and de Boer. This involves passing hafnium tetraiodide vapor over a heated tungsten filament. At high temperatures, the metal is released and forms a solid coating on the filament.

HeavyMineralsBeachSand
HeavyMineralsBeachSand

The abundance of these metals varies greatly across the Earth's crust. Titanium is quite common, ranking as the seventh most abundant metal. It has an abundance of 6320 ppm. Zirconium is much rarer, with an abundance of 162 ppm. Hafnium is even scarcer, appearing at only 3 ppm. These metals are often found in heavy mineral sands in beach environments. These deposits, known as placer deposits, form when erosion materials concentrate due to their specific gravity.

HeavyMineralsBeachSand
HeavyMineralsBeachSand
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