|Standard atomic weight (Ar, standard)|||
|Erbium in the periodic table|
|Electron configuration||[Xe] 4f12 6s2|
Electrons per shell
|2, 8, 18, 30, 8, 2|
|Phase at STP||solid|
|Melting point||1802 K (1529 °C, 2784 °F)|
|Boiling point||3141 K (2868 °C, 5194 °F)|
|Density (near r.t.)||9.066 g/cm3|
|when liquid (at m.p.)||8.86 g/cm3|
|Heat of fusion||19.90 kJ/mol|
|Heat of vaporization||280 kJ/mol|
|Molar heat capacity||28.12 J/(mol·K)|
3, 2, 1 |
|Electronegativity||Pauling scale: 1.24|
|Atomic radius||empirical: 176 pm|
|Covalent radius||189±6 pm|
|Crystal structure||hexagonal close-packed (hcp)|
|Speed of sound thin rod||2830 m/s (at 20 °C)|
|Thermal expansion||poly: 12.2 µm/(m·K) (r.t.)|
|Thermal conductivity||14.5 W/(m·K)|
|Electrical resistivity||poly: 0.860 µ?·m (r.t.)|
|Magnetic ordering||paramagnetic at 300 K|
|Magnetic susceptibility||+44,300.00·10-6 cm3/mol|
|Young's modulus||69.9 GPa|
|Shear modulus||28.3 GPa|
|Bulk modulus||44.4 GPa|
|Vickers hardness||430-700 MPa|
|Brinell hardness||600-1070 MPa|
|Naming||after Ytterby (Sweden), where it was mined|
|Discovery||Carl Gustaf Mosander|
|Main isotopes of erbium|
Erbium is a chemical element with symbol Er and atomic number 68. A silvery-white solid metal when artificially isolated, natural erbium is always found in chemical combination with other elements. It is a lanthanide, a rare earth element, originally found in the gadolinite mine in Ytterby in Sweden, from which it got its name.
Erbium's principal uses involve its pink-colored Er3+ ions, which have optical fluorescent properties particularly useful in certain laser applications. Erbium-doped glasses or crystals can be used as optical amplification media, where Er3+ ions are optically pumped at around 980 or and then radiate light at in stimulated emission. This process results in an unusually mechanically simple laser optical amplifier for signals transmitted by fiber optics. The wavelength is especially important for optical communications because standard single mode optical fibers have minimal loss at this particular wavelength.
In addition to optical fiber amplifier-lasers, a large variety of medical applications (i.e. dermatology, dentistry) rely on the erbium ion's emission (see Er:YAG laser) when lit at another wavelength, which is highly absorbed in water in tissues, making its effect very superficial. Such shallow tissue deposition of laser energy is helpful in laser surgery, and for the efficient production of steam which produces enamel ablation by common types of dental laser.
A trivalent element, pure erbium metal is malleable (or easily shaped), soft yet stable in air, and does not oxidize as quickly as some other rare-earth metals. Its salts are rose-colored, and the element has characteristic sharp absorption spectra bands in visible light, ultraviolet, and near infrared. Otherwise it looks much like the other rare earths. Its sesquioxide is called erbia. Erbium's properties are to a degree dictated by the kind and amount of impurities present. Erbium does not play any known biological role, but is thought to be able to stimulate metabolism.
Erbium can form propeller-shaped atomic clusters Er3N, where the distance between the erbium atoms is 0.35 nm. Those clusters can be isolated by encapsulating them into fullerene molecules, as confirmed by transmission electron microscopy.
Erbium metal tarnishes slowly in air and burns readily to form erbium(III) oxide:
Erbium is quite electropositive and reacts slowly with cold water and quite quickly with hot water to form erbium hydroxide:
Erbium metal reacts with all the halogens:
Naturally occurring erbium is composed of 6 stable isotopes, 162
, and 170
being the most abundant (33.503% natural abundance). 29 radioisotopes have been characterized, with the most stable being 169
with a half-life of , 172
with a half-life of , 160
with a half-life of , 165
with a half-life of , and 171
with a half-life of . All of the remaining radioactive isotopes have half-lives that are less than , and the majority of these have half-lives that are less than 4 minutes. This element also has 13 meta states, with the most stable being 167m
with a half-life of .
The isotopes of erbium range in atomic weight from (143
) to (177
). The primary decay mode before the most abundant stable isotope, 166
, is electron capture, and the primary mode after is beta decay. The primary decay products before 166
are element 67 (holmium) isotopes, and the primary products after are element 69 (thulium) isotopes.
Erbium (for Ytterby, a village in Sweden) was discovered by Carl Gustaf Mosander in 1843. Mosander was working with a sample of what was thought to be the single metal oxide yttria, derived from the mineral gadolinite. He discovered that the sample contained at least two metal oxides in addition to pure yttria, which he named "erbia" and "terbia" after the village of Ytterby where the gadolinite had been found. Mosander was not certain of the purity of the oxides and later tests confirmed his uncertainty. Not only did the "yttria" contain yttrium, erbium, and terbium; in the ensuing years, chemists, geologists and spectroscopists discovered five additional elements: ytterbium, scandium, thulium, holmium, and gadolinium. Erbia and terbia, however, were confused at this time. A spectroscopist mistakenly switched the names of the two elements during spectroscopy. After 1860, terbia was renamed erbia and after 1877 what had been known as erbia was renamed terbia. Fairly pure Er2O3 was independently isolated in 1905 by Georges Urbain and Charles James. Reasonably pure erbium metal was not produced until 1934 when Klemm and Bommer reduced the anhydrous chloride with potassium vapor. It was only in the 1990s that the price for Chinese-derived erbium oxide became low enough for erbium to be considered for use as a colorant in art glass.
The concentration of erbium in the Earth crust is about 2.8 mg/kg and in the sea water 0.9 ng/L. This concentration is enough to make erbium about 45th in elemental abundance in the Earth's crust.
Like other rare earths, this element is never found as a free element in nature but is found bound in monazite sand ores. It has historically been very difficult and expensive to separate rare earths from each other in their ores but ion-exchange chromatography methods developed in the late 20th century have greatly brought down the cost of production of all rare-earth metals and their chemical compounds.
The principal commercial sources of erbium are from the minerals xenotime and euxenite, and most recently, the ion adsorption clays of southern China; in consequence, China has now become the principal global supplier of this element. In the high-yttrium versions of these ore concentrates, yttrium is about two-thirds of the total by weight, and erbia is about 4-5%. When the concentrate is dissolved in acid, the erbia liberates enough erbium ion to impart a distinct and characteristic pink color to the solution. This color behavior is similar to what Mosander and the other early workers in the lanthanides would have seen in their extracts from the gadolinite minerals of Ytterby.
Crushed minerals are attacked by hydrochloric or sulfuric acid that transforms insoluble rare-earth oxides into soluble chlorides or sulfates. The acidic filtrates are partially neutralized with caustic soda (sodium hydroxide) to pH 3-4. Thorium precipitates out of solution as hydroxide and is removed. After that the solution is treated with ammonium oxalate to convert rare earths into their insoluble oxalates. The oxalates are converted to oxides by annealing. The oxides are dissolved in nitric acid that excludes one of the main components, cerium, whose oxide is insoluble in HNO3. The solution is treated with magnesium nitrate to produce a crystallized mixture of double salts of rare-earth metals. The salts are separated by ion exchange. In this process, rare-earth ions are sorbed onto suitable ion-exchange resin by exchange with hydrogen, ammonium or cupric ions present in the resin. The rare earth ions are then selectively washed out by suitable complexing agent. Erbium metal is obtained from its oxide or salts by heating with calcium at under argon atmosphere.
Erbium's everyday uses are varied. It is commonly used as a photographic filter, and because of its resilience it is useful as a metallurgical additive. Other uses:
Erbium does not have a biological role, but erbium salts can stimulate metabolism. Humans consume 1 milligram of erbium a year on average. The highest concentration of erbium in humans is in the bones, but there is also erbium in the human kidneys and liver.