Generated by DeepSeek V3.2| terbium | |
|---|---|
| Name | terbium |
| Number | 65 |
| Category | lanthanide |
| Group | n/a |
| Appearance | silvery white |
| Standard atomic weight | 158.92535 |
| Electron configuration | [Xe] 4f9 6s2 |
| Phase | solid |
| Melting point degC | 1356 |
| Boiling point degC | 3230 |
| Density g cm3 | 8.23 |
| Oxidation states | +3, +4, +2 |
| Crystal structure | hexagonal close-packed |
terbium. It is a silvery-white, malleable rare-earth element that is soft enough to be cut with a knife. This member of the lanthanide series is relatively stable in air compared to some of its reactive neighbors. Discovered in the 19th century, it finds critical modern uses in solid-state devices and as a dopant in crystalline materials.
Terbium exhibits typical trivalent chemistry, forming compounds like terbium(III) oxide and terbium(III) chloride. In its +4 oxidation state, it forms stable compounds such as terbium(IV) oxide, a property it shares with cerium and praseodymium. The element is ferromagnetic at temperatures below 219 Kelvin, and its ions are strongly paramagnetic. A key characteristic is its bright green photoluminescence, particularly from the 5D4→7F5 transition in the trivalent ion, which is exploited in various phosphors. Its metallic radius and behavior in alloys follow trends predicted by the lanthanide contraction.
The element was first identified in 1843 by Swedish chemist Carl Gustaf Mosander at the Karolinska Institute. He detected it as an impurity in yttrium oxide, which was originally mined from a quarry in the village of Ytterby in Sweden. Mosander named the oxide "terbia", after the village, leading to the element's eventual name. For many decades, terbium and its compounds were laboratory curiosities, with pure metallic terbium not isolated until the advent of modern ion-exchange techniques in the 20th century, developed by scientists like Frank Spedding at Iowa State University.
Terbium is never found in nature as a free element. It occurs in minerals such as xenotime, euxenite, and most significantly, monazite and bastnäsite, which are the principal commercial sources for all rare-earth elements. These ores are primarily mined in locations like the Mountain Pass mine in California and the Bayan Obo Mining District in Inner Mongolia. Industrial production involves complex solvent extraction and ion-exchange processes to separate terbium from other lanthanides, a method refined by operations like those at the Rhône-Poulenc plant in La Rochelle.
Terbium's primary application is in green phosphors for trichromatic lighting, used in fluorescent lamps and cathode ray tubes for televisions. It is a crucial component of zinc sulfide and yttrium aluminum garnet based phosphors. The alloy terfenol-D, which contains terbium, dysprosium, and iron, exhibits giant magnetostriction and is used in advanced sonar systems and precision actuators. Terbium is also doped into calcium fluoride, calcium tungstate, and strontium molybdate crystals for use in solid-state devices. Its salts are employed as dopants in fuel cell materials and in X-ray intensifying screens for medical imaging.
Terbium has no known biological role in any organism, including humans. Its compounds are generally considered to have low to moderate toxicity, similar to other heavy metals, but they should be handled with care. Industrial exposure to terbium dust or salts can pose a risk, potentially causing irritation to the respiratory system and skin. As with all rare-earth elements, environmental release from mining and refining processes, such as those associated with monazite processing, requires careful management to prevent ecosystem damage.