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— CH. 1 · DISCOVERY AND NAMING HISTORY —

Terbium

~5 min read · Ch. 1 of 7
7 sections
  • Swedish chemist Carl Gustaf Mosander detected terbium as an impurity in yttrium oxide during 1843. He separated yttria into three fractions named yttria, erbia, and terbia. The fraction called terbia originally held the pink color now attributed to erbium. The fraction labeled erbia contained what is today known as terbium and appeared yellow or dark orange in solution. Spectral analysis by Marc Delafontaine allowed separate elements to be identified but switched their names in his publications. A brief period followed where terbium was renamed mosandrum after its discoverer. The names have remained switched ever since despite the historical confusion. Yttrium, erbium, and terbium all derive their names from the village of Ytterby in Sweden. Terbium did not appear in pure form until ion exchange techniques became available decades later.

  • Terbium presents as a silvery-white rare earth metal soft enough to cut with a knife. It exists in two crystal allotropes with a transformation temperature of 1289 degrees Celsius between them. The element possesses sixty-five electrons arranged in the electron configuration [Xe]4f96s2. Only three electrons can be removed before nuclear charge prevents further ionization. Stability of the half-filled [Xe]4f7 configuration allows removal of a fourth electron under strong oxidizing agents like fluorine gas. Single terbium atoms have been isolated by implanting them into fullerene molecules for research purposes. The terbium(III) cation fluoresces in a bright lemon-yellow color resulting from a strong green emission line. This fluorescence combines with other lines in the orange and red spectrum. Terbium exhibits simple ferromagnetic ordering at temperatures below 219 Kelvin. Above 219 Kelvin it turns into a helical antiferromagnetic state where atomic moments align parallel within basal planes. This antiferromagnetism transforms into a disordered paramagnetic state at 230 Kelvin.

  • Terbium metal oxidizes readily in air to form a mixed terbium(III,IV) oxide. Most common oxidation states include +3 trivalent forms found in various compounds. Tetravalent terbium exists in solid state compounds such as terbium oxide and terbium tetrafluoride. In solution terbium typically forms trivalent species but can reach tetravalent states with ozone in highly basic aqueous conditions. Divalent Tb2+ complexes are known usually featuring bulky cyclopentadienyl-type ligands. A few coordination compounds contain terbium in its tetravalent state. Terbium combines with nitrogen carbon sulfur phosphorus boron selenium silicon and arsenic at elevated temperatures. These binary compounds mainly exhibit the +3 oxidation state while +2 appears rarely. Terbium(II) halides obtain by annealing terbium(III) halides in presence of metallic terbium inside tantalum containers. Terbium also forms sesquichloride which reduces further to terbium(I) chloride by annealing at 800 degrees Celsius. Terbium(IV) fluoride stands as the only halide tetravalent terbium can form. It emits relatively pure atomic fluorine when heated rather than mixture of fluoride vapors from other elements.

  • Naturally occurring terbium consists solely of its stable isotope terbium-159 making it mononuclidic and monoisotopic. Thirty-nine radioisotopes range from 135Tb to 174Tb characterize the element. Most stable synthetic radioisotopes include 158Tb with an eighteen-year half-life and 157Tb with a seventy-one year half-life. All remaining radioactive isotopes possess half-lives under three months with many lasting less than thirty minutes. Primary decay mode before the abundant stable isotope involves electron capture producing gadolinium isotopes. Beta minus decay follows after resulting in dysprosium isotopes. The element contains thirty-one nuclear isomers with masses ranging from 141 to 168. Most stable isomers are terbium-156m2 with twenty-four point four hour half-life and terbium-154m2 with twenty-two point seven hours. Terbium-149 offers promising potential for targeted alpha therapy due to its four-point one hour half-life. This specific isotope also serves as a candidate for positron emission tomography applications in medical diagnostics.

  • Terbium occurs within minerals including monazite containing up to 0.03 percent terbium and xenotime holding over 1 percent. Euxenite also contains significant amounts exceeding 1 percent terbium concentration. Crust abundance estimates place terbium at 1.2 milligrams per kilogram of Earth's crust. No terbium-dominant mineral has yet been discovered by geologists. Rich commercial sources currently include ion-absorption clays found in southern China. Concentrates from these clays contain about two-thirds yttrium oxide by weight and roughly 1 percent terbia. Small amounts occur in bastnäsite and monazite processed to recover heavy lanthanides like samarium europium and gadolinium. A rich terbium supply was discovered off Japan's Minamitori Island coast in 2018. That deposit holds enough material to meet global demand for four hundred twenty years. Large volumes of bastnäsite processed relative to ion-absorption clays contribute significantly to world supply.

  • Crushed terbium-containing minerals undergo treatment with hot concentrated sulfuric acid producing water-soluble sulfates. Acidic filtrates partially neutralize with caustic soda reaching pH levels between three and four. Thorium precipitates out as hydroxide and gets removed from the solution mixture. Ammonium oxalate converts rare earths into insoluble oxalates which decompose into oxides upon heating. Oxides dissolve in nitric acid excluding cerium whose oxide remains insoluble in that medium. Terbium separates as a double salt with ammonium nitrate through crystallization methods. Ion exchange serves as the most efficient separation routine for terbium salts from rare-earth solutions. Rare-earth ions sorb onto resin exchanging with hydrogen ammonium or cupric ions present within it. Selective washing removes rare earth ions using suitable complexing agents. Terbium metal produces by reducing anhydrous chloride or fluoride with calcium metal. Calcium and tantalum impurities remove via vacuum remelting distillation amalgam formation or zone melting techniques.

  • Terbium dopes calcium fluoride calcium tungstate and strontium molybdate used in solid-state devices. It stabilizes fuel cells operating at elevated temperatures alongside zirconium dioxide. Terfenol-D alloy expands or contracts when exposed to magnetic fields more than any other known alloy. This material finds use in actuators naval sonar systems sensors and magnetomechanical devices. Terbium increases verdet constant in long-distance fiber optic communication lines. Terbium-doped garnets function as optical isolators preventing reflected light from traveling back along fibers. Green phosphors utilize terbium oxides in fluorescent lamps color TV tubes and flat screen monitors. Brilliant fluorescence allows terbium to serve as probes in biochemistry resembling calcium behavior. Terbium green phosphors combine with divalent europium blue phosphors and trivalent europium red phosphors for trichromatic lighting. Trichromatic lighting provides much higher output per electrical energy unit compared to incandescent lighting. In 2023 researchers created a lattice with single iron atoms examined by synchrotron x-ray beams. This marked the first successful attempt characterizing single atoms at sub-atomic levels using terbium compounds.

Common questions

Who discovered terbium and when was it detected?

Swedish chemist Carl Gustaf Mosander detected terbium as an impurity in yttrium oxide during 1843. He separated yttria into three fractions named yttria, erbia, and terbia.

Where does the name terbium come from and what is its origin village?

Yttrium, erbium, and terbium all derive their names from the village of Ytterby in Sweden. The fraction labeled erbia contained what is today known as terbium and appeared yellow or dark orange in solution.

What are the physical properties and crystal structures of terbium metal?

Terbium presents as a silvery-white rare earth metal soft enough to cut with a knife. It exists in two crystal allotropes with a transformation temperature of 1289 degrees Celsius between them.

How many stable isotopes exist for natural terbium and which one is dominant?

Naturally occurring terbium consists solely of its stable isotope terbium-159 making it mononuclidic and monoisotopic. Thirty-nine radioisotopes range from 135Tb to 174Tb characterize the element.

Which minerals contain terbium and where are rich commercial sources located?

Terbium occurs within minerals including monazite containing up to 0.03 percent terbium and xenotime holding over 1 percent. Rich commercial sources currently include ion-absorption clays found in southern China.

What are the primary applications of terbium in modern technology and medicine?

Green phosphors utilize terbium oxides in fluorescent lamps color TV tubes and flat screen monitors. Terbium-149 offers promising potential for targeted alpha therapy due to its four-point one hour half-life.