Transition metal
Rhodium is a chemical element; it has symbol Rh and atomic number 45. It is a very rare, dark silvery-white, hard, corrosion-resistant transition metal. It is a noble metal and a member of the platinum group. It has only one naturally occurring isotope, which is 103Rh. Naturally occurring rhodium is usually found as a free metal or as an alloy with similar metals and rarely as a chemical compound in minerals such as bowieite and rhodplumsite. It is one of the rarest and most valuable precious metals. Rhodium is a group 9 element (cobalt group). It is used for the enhancement of jewelry.
Rhodium is found in platinum or nickel ores with the other members of the platinum group metals. It was discovered in 1803 by William Hyde Wollaston in one such ore, and named for the rose color of one of its chlorine compounds.
The element's major use (consuming about 80% of world rhodium production) is as one of the catalysts in the three-way catalytic converters in automobiles. Because rhodium metal is inert against corrosion and most aggressive chemicals, and because of its rarity, rhodium is usually alloyed with platinum or palladium and applied in high-temperature and corrosion-resistant coatings. White gold is often plated with a thin rhodium layer to improve its appearance, while sterling silver is often rhodium-plated to resist tarnishing.
Rhodium detectors are used in nuclear reactors to measure the neutron flux level. …
Rhodium (from Greek: ῥόδον rhodon, meaning 'rose') was discovered in 1803 by William Hyde Wollaston, soon after he discovered palladium. He used crude platinum ore presumably obtained from South America. His procedure started by dissolving the ore in aqua regia, precipitating the platinum as ammonium chloroplatinate by adding ammonium chloride (NH4Cl). Adding zinc precipitated a mixture of copper, lead, palladium, and rhodium. Dilute nitric acid dissolved the copper and lead. Dissolving the remainder in aqua regia again and adding sodium chloride, the solution was evaporated to yield rose-red Na3[RhCl6]·nH2O. After extraction with hot ethanol, additional zinc displaced the rhodium in the ionic compound, releasing the rhodium as free metal.
For decades, the rare element had only minor applications; for example, by the turn of the century, rhodium-containing thermocouples were used to measure temperatures up to 1800 °C. They have exceptionally good stability in the temperature range of 1300 to 1800 °C.
The first major application was electroplating for decorative uses and as corrosion-resistant coating. The introduction of the three-way catalytic converter by Volvo in 1976 increased the demand for rhodium. The previous catalytic converters used platinum or palladium, while the three-way catalytic converter used rhodium to reduce the amount of NOx in the exhaust.
Rhodium is a hard, silvery, durable metal that has a high reflectance. Rhodium metal does not normally form an oxide, even when heated. Oxygen is absorbed from the atmosphere only at the melting point of rhodium, but is released on solidification. Rhodium has both a higher melting point and lower density than platinum. It is not attacked by most acids: it is completely insoluble in nitric acid and dissolves slightly in aqua regia, a property that has been used to separate it from platinum ore.
Rhodium belongs to group 9 of the periodic table, but exhibits an atypical ground state valence electron configuration for that group, having only one electron in its outermost s orbital. This is also observed in the elements niobium (41) and ruthenium (44).
The common oxidation states of rhodium are +3 and +1. Complexes with rhodium in oxidation states 0, +2, and +4 are also well characterized. The few compounds at still higher oxidation states include rhodium pentafluoride, a tetrameric complex with the true formula Rh4F20), and rhodium hexafluoride.
Three rhodium oxides are Rh2O3 (a paramagnetic black powder), RhO2 (black when anhydrous but green as a hydrate), and RhO3 (only stable in the gas phase). A rhodium sulfide, Rh17S15, occurs naturally as a rare mineral miassite. Synthetic RhxSy are used as catalysts in for example H2-Br2 fuel cells.
All the Rh(III) halides are known. …
Rhodium is one of the rarest elements in the Earth's crust, with less than one part per billion. Its rarity affects its price and its use in commercial applications. The concentration of rhodium in nickel meteorites is typically 1 part per billion. Rhodium has been measured in some potatoes with concentrations between 0.8 and 30 ppt.
Rhodium ores are a mixture with other metals such as palladium, silver, platinum, and gold. Few rhodium minerals are known. The separation of rhodium from the other metals poses significant challenges. Principal production is located in South Africa, at 75%, with much less production in Russia and Zimbabwe. The annual world production flucuates around 30 tonnes. The price of rhodium (per troy ounce) is highly variable, ranging from less than US$700.00 in 2016 to nearly US$30,000.00 in 2021.
Rhodium is a fission product of uranium-235: each kilogram of fission product contains a significant amount of the lighter platinum group metals. Used nuclear fuel is therefore a potential source of rhodium, but the extraction is complex and expensive, and the presence of rhodium radioisotopes requires a period of cooling storage for multiple half-lives of the longest-lived isotope (101Rh with a half-life of 3.3 years, and 102mRh with a half-life of 2.9 years), or about 10 years. These factors make the source unattractive and no large-scale extraction has been attempted.
Rhodium is a fission product of uranium-235: each kilogram of fission product contains a significant amount of the lighter platinum group metals. Used nuclear fuel is therefore a potential source of rhodium, but the extraction is complex and expensive, and the presence of rhodium radioisotopes requires a period of cooling storage for multiple half-lives of the longest-lived isotope (101Rh with a half-life of 3.3 years, and 102mRh with a half-life of 2.9 years), or about 10 years. These factors make the source unattractive and no large-scale extraction has been attempted.
Naturally occurring rhodium is composed of only one isotope, 103Rh. With a nuclear spin of -1/2, 103Rh is well-suited for nuclear magnetic resonance spectroscopic studies. With a particularly low nuclear dipole moment, 103Rh exhibits very low receptivity.
The most stable radioisotopes are 101Rh with a half-life of 4.07 years, 102Rh with a half-life of 207 days, and 99Rh with a half-life of 16.1 days. Thirty-eight other radioisotopes have been characterized ranging from 90Rh to 128Rh; these have half-lives that are less than an hour except 100Rh (20.8 hours) and 105Rh (35.34 hours). Numerous meta states are also known, of which the most stable are 102mRh (3.742 years) and 101mRh (4.343 days).
In isotopes lighter than 103Rh (the stable isotope), the primary decay mode is electron capture and the primary decay product is ruthenium. In isotopes heavier than 103Rh, the primary decay mode is beta emission and the primary product is palladium.
Being a noble metal, pure rhodium is inert and harmless in elemental form. However, chemical complexes of rhodium can be reactive. For rhodium chloride, the median lethal dose (LD50) for rats is 198 mg (RhCl3) per kilogram of body weight.
People can be exposed to rhodium in the workplace by inhalation. The Occupational Safety and Health Administration (OSHA) has specified the legal limit (Permissible exposure limit) for rhodium exposure in the workplace at 0.1 mg/m3 over an 8-hour workday, and the National Institute for Occupational Safety and Health (NIOSH) has set the recommended exposure limit (REL), at the same level. At levels of 100 mg/m3, rhodium is immediately dangerous to life or health. For soluble compounds, the PEL and REL are both 0.001 mg/m3.